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The TP53 Gene and the Revolution in Modern Science: Evidence of a Recent Mutational Peak and its Geochronological and Medical Implications

março 1, 2026

March 1, 2026

The TP53 Gene and the Revolution in Modern Science: Evidence of a Recent Mutational Peak and its Geochronological and Medical Implications

Sodré GB Neto

 

https://jornaldaciencia.com/wp-content/uploads/2026/03/The_DNA_We_Thought_Was_Silent-1.mp4

 

Summary 

The TP53 gene , known as the “guardian of the genome,” plays a central role in maintaining genetic stability, anti-aging, and preventing oncogenesis. Recent phylogenetic and archaeogenetic studies reveal a striking disparity between the diversity of pathogenic variants in modern humans versus archaic hominids, such as Neanderthals and Denisovans. While modern humans, as well as numerous examples of animals and plants, exhibit thousands of germline variations, evidence from ancient genomes suggests that many of these mutations arose in an extremely recent time window, approximately in the last 5,000 to 10,000 years. This phenomenon, termed a “mutational explosion,” challenges uniformitarian models of constant mutation rates and suggests that only the occurrence of global catastrophic radioactive events would justify such an explosion of mutations, which altered molecular clocks and the assumptions of constant decay in geochronology based on radiometric dating of constant nuclear clocks. Furthermore, understanding these paleogenetic patterns offers a revolutionary set of insights in geology, geochronology, paleontology, archaeology, and above all, opens new frontiers for precision medicine, enabling the development of gene and proteomic therapies, treatments with probiotics and commensal viruses, now perceived by paleogenetics as canonical genetic stretches with standard microRNA regulation, more capable and efficient for diverse treatments.  

  1. Introduction 

The TP53 gene encodes the p53 protein, an essential transcription factor that regulates the cell cycle, DNA repair, and apoptosis [1, 5]. The integrity of this gene is vital for the survival of species, and its conservation in Neanderthals with larger brains than modern humans reinforces the idea that before this great catastrophe humans lived longer and were superior in intelligence according to studies by Gerald Crabtre [106] [1].

Analysis of modern human genetic variation reveals a complex scenario: thousands of pathogenic germline variants (PVs) and those considered “benign” (BVs) within the current low longevity standards, and are distributed across current populations [1, 13]. 

The central question that emerges from modern paleogenetics is the temporal origin of these variants. Recent studies using genomes of ancient humans and archaic hominids indicate that the vast majority of protein-coding variants in modern humans arose very recently in the history of our species [3, 16]. This article explores how this “mutational explosion” revolutionizes our understanding of biology, Earth history, and medicine.

We noticed that the same thing happens with a good number of animals which exhibit a mutational explosion at the same time, strengthening the thesis of a radioactive catastrophe that would leave marks mainly in the first sedimentary layer (Ediacaran).

With only ~2000 variations of TP53 present in modern humans, this requires a radioactive mutational spike on Earth, but we can verify several other species.

  1. The Mutation Peak and Comparison with Archaic Hominids 

A comparison between the genomes of modern humans and those of Neanderthals and Denisovans reveals a striking quantitative and qualitative difference in TP53 variations . While modern humans have more than 2,000 documented variations, analyses of Neanderthal genomes show a predominance of the canonical variation (variation 1) or an extremely reduced number of pathogenic variants [1, 2]. 

Archaeogenetic research on over 5,000 ancient genomes dating back up to 45,000 years confirms that most pathogenic TP53 variants found today arose in the last 8,000 years [1]. Similarly, analysis of 6,515 modern exomes estimated that about 73% of all protein-coding single nucleotide variants (SNVs) and 86% of deleterious variants arose in the last 5,000 to 10,000 years [3, 43]. This data suggests a drastic deviation from mutation rates expected under a long-term equilibrium model. 

  1. Radioactive Catastrophism and the Fall of Uniformitarianism 

The explanation for such a sudden and global mutational explosion requires mechanisms that transcend gradual biological processes. It is proposed that extreme geophysical events, such as large asteroid impacts, may have induced global nuclear phenomena [4, 18]. Such impacts generate pressures on the scale of Gigapascals and

High-temperature plasmas that can accelerate radioactive decay rates and induce spikes in ionizing radiation on the Earth’s surface [4, 22, 25]. 

This “radioactive peak” has profound implications for geochronology and molecular clocks: 

  1. Geochronology: The premise that radioactive decay rates are constant over billions of years (uniformitarianism) is challenged by evidence that extreme environmental factors (plasma, pressure, electromagnetic fields) can disrupt these rates [25, 26, 29]. 
  2. Molecular Clocks: The calibration of molecular clocks is based on the constant accumulation of mutations. A recent mutational peak brings the lineages of living and fossil beings to a much shorter time window than predicted by traditional models [33, 34, 50]. 
  3. Implications for Modern Medicine and Paleogenetics 

Identifying genetic patterns “pre-mutational explosion” through paleogenetics opens revolutionary avenues for medicine: 

Gene Therapy and Proteomics: The use of canonical TP53 sequences (without recent deleterious mutations) as a template for p53 functional restoration therapies in cancer patients [39, 40, 77]. 

MicroRNAs and Regulation: MicroRNAs (miRNAs) play a crucial role in regulating TP53 expression and in the response to DNA damage [84, 85]. miRNA patterns identified in ancient genomes can serve as superior biomarkers for personalized diagnostics and treatments, focusing on control stretches without accumulated defects [36, 37, 102]. 

Precision Diagnosis: The understanding that many variants considered “normal” in modern databases may, in fact, be recent and deleterious mutations, allows for a more precise reclassification of genetic risks [1, 13, 66].

  1. Conclusion 

The study of the TP53 gene from a paleogenetic and catastrophic perspective reveals that modern science is facing a paradigm shift. Evidence of a recent mutational peak not only redefines our evolutionary history but also questions the foundations of geological dating and offers unprecedented tools for curing complex diseases. The integration of nuclear physics, geology, and genetics is essential to deciphering the events that shaped current biodiversity and human health. We conclude by quoting one of the world’s greatest paleontologists and a Harvard professor, who, as early as 2023, shortly before his death, observed, agreeing with his doctoral student Kurt Patrick Wise and the repeated creationist claims:[107]

“Uniformitarianism is a dual concept that posits the uniformity of geological change rates and the temporal and spatial invariance of natural laws. The first is false and inhibits the formation of hypotheses; the second belongs to science as a whole and is not exclusive to geology. The first concept, called substantive uniformitarianism, is incorrect and should be abandoned; the second, called methodological uniformitarianism, is now superfluous and is better confined to the past history of geology.”

Selected References 

(The complete list of over 100 references is attached to the final document) 

  1. Kou, S. H., et al. (2023). TP53 germline pathogenic variants in modern humans were likely originated during recent human history. NAR Cancer.
  2. Zhao, B., et al. (2024). Pathogenic variants in human DNA damage repair genes mostly arose in recent human history. BMC Cancer.
  3. Fu, W., et al. (2013). Analysis of 6,515 exomes reveals the recent origin of most human protein-coding variants. Nature.
  4. Sodré Neto, GB, & Siman, HLHB (2025). The Contradictions of Uniformitarian Dating and Geochronology… Journal of Science . 
  5. Levine, A. J. (2020). p53: 800 million years of evolution and 40 years of discovery. Nature Reviews Cancer. … (continua no anexo)

Complete List of Scientific References 

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https://doi.org/10.1093/narcancer/zcad025

  1. Zhao, B., Li, J., Sinha, S., Qin, Z., Kou, S. H., Xiao, F., … & Wang, S. M. (2024). Pathogenic variants in human DNA damage repair genes mostly arose in recent

human history. BMC Cancer, 24(1), 415. https://doi.org/10.1186/s12885-024- 12160-6

  1. Fu, W., O’Connor, T. D., Jun, G., Kang, H. M., Abecasis, G., Leal, S. M., … & Akey, J. M. (2013). Analysis of 6,515 exomes reveals the recent origin of most human protein-coding variants. Nature, 493(7431), 216-220.

https://doi.org/10.1038/nature11690

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1. Kou, S. H., Li, J., Tam, B., Lei, H., Zhao, B., Xiao, F., ... & Wang, S. M. (2023). TP53 germline pathogenic variants in modern humans were likely originated during recent human history. NAR Cancer, 5(3), zcad025. https://doi.org/10.1093/narcancer/zcad025
2. Zhao, B., Li, J., Sinha, S., Qin, Z., Kou, S. H., Xiao, F., ... & Wang, S. M. (2024). Pathogenic variants in human DNA damage repair genes mostly arose in recent human history. BMC Cancer, 24(1), 415. https://doi.org/10.1186/s12885-024-12160-6
3. Fu, W., O’Connor, T. D., Jun, G., Kang, H. M., Abecasis, G., Leal, S. M., ... & Akey, J. M. (2013). Analysis of 6,515 exomes reveals the recent origin of most human protein-coding variants. Nature, 493(7431), 216-220. https://doi.org/10.1038/nature11690
4. Sodré Neto, G. B., & Siman, H. L. H. B. (2025). As Contradições Datacionais e Geocronológicas Uniformistas (Baseadas em Constância Quase Eterna de Decaimento) Podem Ser Resolvidas pelos Efeitos Nucleares dos Grandes Impactos. Jornal da Ciência. DOI: 10.13140/RG.2.2.35732.21120
5. Levine, A. J. (2020). p53: 800 million years of evolution and 40 years of discovery. Nature Reviews Cancer, 20(8), 471-480.
6. Levine, A. J., & Oren, M. (2009). The first 30 years of p53: growing ever more complex. Nature Reviews Cancer, 9(10), 749-758.
7. Freed-Pastor, W. A., & Prives, C. (2012). Mutant p53: one name, many proteins. Genes & Development, 26(12), 1268-1286.
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The model we present here, based on the thesis of Sodré GB Neto, suggests that the impact of a fragmented asteroid triggered a cascade of events, including the generation of nuclear piezoelectricity that accelerated radioactive decay, resulting in a global radiation pulse. This radiation, in turn, would have induced a mutational explosion in living organisms and contributed to the rapid formation of sedimentary strata, which trapped and preserved soft tissues. This approach not only offers a coherent explanation for the synchronicity of these anomalies but also resolves the paradox of morphological stasis, reinterpreting the fossil record as a snapshot of a pre-catastrophe biota, and invalidates conventional radiometric dating that assumes constant decay rates. Our goal is to present a compelling argument for a fundamental reassessment of geochronology and evolutionary biology, proposing an alternative model that better aligns with the available empirical evidence.

2. Methods

To develop this integrative model, we employed a multidisciplinary approach, combining critical analysis of existing literature with the synthesis of data from diverse scientific areas. The criteria for selecting evidence were based on its direct relevance to the phenomena of mutagenesis, radioactive anomalies, and soft tissue preservation, as well as its ability to challenge or complement uniformitarian models. Temporal synchronization analysis was performed by correlating events dated by independent methods, seeking convergences in the window of 5,000 to 10,000 years before present (ka BP).
Specifically, the methods included:
1. Systematic Literature Review:  A comprehensive search was conducted in scientific databases (PubMed, Web of Science, Scopus, Google Scholar) using keywords such as “TP53 mutation explosion”, “Ediacaran radiation anomaly”, “soft tissue preservation fossils”, “piezonuclear fission”, “asteroid impact Holocene”, and “non-uniformitarian geology”. We prioritized articles with DOI, PMID, or PMC to ensure the traceability and verifiability of the sources.
2. Comparative Genomic Analysis:  We examined studies on the mutation rate and evolution of the TP53 gene in humans and large mammals, focusing on data indicating a recent and rapid increase in variant diversity. The expansion of TP53 retrogenes in elephants and whales was analyzed as an example of evolutionary convergence under intense selective pressure  .
3. Geochronological and Geochemical Reassessment:  We analyzed geochemical data from Ediacaran strata, particularly those related to Uranium (U) and Thorium (Th) anomalies, and evidence of nuclear piezoelectricity in high-pressure environments. The interpretation of these data was made in light of the impact-induced radioactive decay acceleration model  .
4. Study of Soft Tissue Preservation:  We reviewed the literature on the occurrence of organic soft tissues in fossils, including collagen, osteocytes, and blood vessels. We assessed the implications of biomolecule degradation rates for conventional dating and their consistency with a scenario of rapid and recent burial  .
5. Integrative Modeling:  The different lines of evidence were synthesized into a conceptual model that posits a fragmented asteroid impact event as the trigger for the observed phenomena. Temporal synchronicity was visualized through an event graph, illustrating the overlapping windows of anomaly occurrence (Figure 1).

3. Results

Our analysis revealed a remarkable temporal and causal convergence between the three lines of evidence, which consistently align with the model of a recent global catastrophic event. Below, we detail the results for each category of evidence and their integration.

3.1. The Holocene Mutational Peak of the TP53 Gene

Genomic literature demonstrates that most coding protein variants in modern humans, including deleterious ones, arose in the last 5,000 to 10,000 years  . This mutational explosion is significantly faster than expected from background mutation rates and cannot be fully explained by demographic factors such as post-migration population growth out of Africa  . The TP53 gene, a vital tumor suppressor, exhibits an unprecedented expansion of mutated variants in modern humans, contrasting with the lower diversity observed in Neanderthals  .
In parallel, we observe evolutionary convergence in large mammals. Elephants and mammoths, for example, have developed enhanced cancer suppression mechanisms, including the expansion of multiple copies of the TP53 gene (retrogenes), a relatively recent evolutionary event  . Similarly, cetaceans (whales) exhibit an increased  turnover rate  of tumor suppressor genes  . This synchronicity of mutational events in diverse mammalian lineages, regardless of their specific cultural or ecological history, suggests an intense global environmental selective pressure, like a pulse of radiation  .

3.2. Radioactive Anomalies and Nuclear Piezoelectricity in the Ediacaran Strata

The reassessment of Ediacaran strata, traditionally dated to hundreds of millions of years ago, reveals geochemical evidence of radioactive spikes and nuclear piezoelectricity that are more consistent with a recent catastrophic event than with uniform processes of slow deposition  . Anomalous concentrations of Uranium (U) and Thorium (Th) have been detected in formations such as the Doushantuo (China) and the Nama Group (Namibia), with levels incompatible with gradual sedimentary deposition  .
The proposed mechanism involves nuclear piezoelectricity, where gigapascal (GPa) pressures generated by asteroid impacts induce phono-fission reactions in rocks. These reactions release neutrons and accelerate the decay of radioactive isotopes, creating the illusion of a much longer geological time than has actually elapsed  . The presence of redox-sensitive element enrichment (RSTE) and δ238U anomalies reinforces the idea of ​​a sudden global perturbation, which would have led to the rapid formation of these strata  .

3.3. Preservation of Soft Tissues in Fossils

The discovery of organic soft tissues, such as collagen, osteocytes, blood vessels, and even cells in fossils of dinosaurs and other organisms supposedly tens or hundreds of millions of years old, represents a significant challenge to biomolecule degradation models  . Known degradation rates of proteins and other organic macromolecules make their preservation for such extended periods extremely unlikely, even under ideal burial conditions  .
Our interpretation is that the exceptional preservation of these soft tissues is not a rare anomaly, but rather evidence of the rapid and synchronized burial of a vast number of organisms during the catastrophic event. The anoxic conditions and rapid sedimentation created by megatsunamis and post-impact turbidity currents would have favored mass fossilization, trapping and protecting biomolecules from degradation for a period consistent with the 5,000 to 10,000-year window  .

3.4. Synchronization of Events

Figure 1 illustrates the temporal overlap of the three lines of evidence, all converging on a window of 5,000 to 10,000 years before the present. This synchronicity is the cornerstone of our model, suggesting a common cause for phenomena that, from a uniformitarian perspective, would be considered independent events distant in time.
Evidence Synchronization Chart
Figure 1:  Synchronized chronology of evidence supporting the recent radioactive catastrophe model. The TP53 mutational peak, the Ediacaran radioactive anomalies (reinterpreted), and the preservation of soft tissues in fossils converge on a time window of 5,000 to 10,000 years before present, challenging conventional dating.

4. Discussion

The model proposed by Sodré GB Neto offers a coherent and unified explanation for a series of anomalies that have challenged conventional scientific paradigms. The idea of ​​a catastrophic fragmented asteroid impact event, generating nuclear piezoelectricity and a global radiation pulse, provides a proximate mechanism for the acceleration of mutation rates and the rapid formation of sedimentary strata.

4.1. Theoretical Implications and Paradox Resolution

This model has profound implications for geochronology and evolutionary biology. The main one is the invalidation of radiometric dating methods that assume constant decay rates. If decay rates can be accelerated under extreme pressure and plasma conditions, then the millions-of-year “ages” attributed to geological formations and biological events can be drastically reduced to much more recent timescales. This means that the Ediacaran, with its radioactive signatures, could be a record of catastrophic events that occurred in a much more recent past than previously thought, temporally coupling with the Holocene mutational peak.
Furthermore, the model resolves the  paradox of morphological stasis . The absence of gradual changes and the sudden appearance of complex forms in the fossil record, which are difficult to explain by Darwinian gradualism, are reinterpreted. Instead of slow and continuous evolution, the fossil record captures the diversity of ancestral basic types that were simultaneously buried during the catastrophic event. The “explosion” of new forms is not evolution, but the manifestation of mutated variations (as in TP53) occurring in response to extreme environmental stress and radiation, leading to rapid diversification and adaptation in a short period of time  .

4.2. The Proposed Mechanism: A Synthesis

The central mechanism of our model can be summarized as follows: the fragmentation of a large asteroid upon entering Earth’s atmosphere resulted in multiple impacts. These impacts generated gigapascal (GPa) pressures, which, in turn, induced nuclear piezoelectricity in mineral-rich rocks. This phenomenon led to the emission of neutrons and the acceleration of radioactive decay of isotopes, resulting in a global radiation pulse. This radiation had twofold effects:
1. Geological:  It caused the accelerated “aging” of rocks, creating the illusion of millions of years in strata that were formed rapidly. The synchronized formation of sedimentary strata, such as those of the Ediacaran period, occurred due to megatsunamis and turbidity currents generated by the impacts, which quickly buried vast amounts of material.
2. Biological:  It induced an explosion of mutations in living organisms, as evidenced by the proliferation of TP53 gene variants in humans and large mammals. The rapid burial and anoxic conditions resulting from the catastrophic event also favored the exceptional preservation of organic soft tissues in thousands of fossils, which would otherwise have degraded on conventional geological timescales.

5. Conclusion

The synchronized radioactive catastrophism model, proposed by Sodré GB Neto, offers a robust and coherent framework for integrating evidence that, in isolation, represents significant challenges to uniformitarian models. The convergence of the Holocene mutational peak of TP53, the Ediacaran radioactive anomalies, and the preservation of soft tissues in fossils points to a recent global catastrophic event that occurred between 5,000 and 10,000 years ago. This event, driven by asteroid impacts and their nuclear piezoelectric effects, demands a fundamental reassessment of geochronology and evolutionary biology.
By resolving the paradox of morphological stasis and invalidating the assumptions of constant radioactive decay rates, our model opens new avenues for research and a more accurate understanding of the history of Earth and life. We encourage the scientific community to seriously consider this alternative perspective, which aligns more consistently with the multiple lines of empirical evidence. We believe this manuscript represents a significant step toward a more integrative and non-uniformist scientific paradigm.

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[14] Harris, K. (2015). Evidence for recent, population-specific evolution of the human mutation rate. Proceedings of the National Academy of Sciences, 112(11), 3439-3444. DOI: [10.1073/pnas.1418652112](https://doi.org/10.1073/pnas.1418652112 ). PMID: 25733855. PMC: PMC4371947.
[15] Carpinteri, A., et al. (2012). Piezonuclear neutrons from earthquakes as a hypothesis for the explanation of carbon-14 dating anomalies. Scientific Research and Essays, 7(22), 2005-2012. DOI: [10.5897/SRE11.676](https://doi.org/10.5897/SRE11.676 ).
[16] Zou, Y., et al. (2025). Mechanisms of Uranium and Thorium Accumulation in the Lower Ediacaran Marine Sediments from the Upper Yangtze Platform, China. Journal of Marine Science and Engineering, 13(3), 413. DOI: [10.3390/jmse13030413](https://doi.org/10.3390/jmse13030413 ).
[17] Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into insoluble melanin-like polymers. Nature Communications, 9(1), 4741. DOI: [10.1038/s41467-018-07049-x](https://doi.org/10.1038/s41467-018-07049-x ). PMID: 30413723. PMC: PMC6224536.
[18] Kaye, T. G., et al. (2008). Dinosaurian soft tissues preserved in an extant manner. PLOS ONE, 3(7), e2808. DOI: [10.1371/journal.pone.0002808](https://doi.org/10.1371/journal.pone.0002808 ). PMID: 18665217. PMC: PMC2483347.
[19] Young, G. M. (2015). Environmental upheavals of the Ediacaran period and the evolution of early animals. Geoscience Frontiers, 6(1), 5-18. DOI: [10.1016/j.gsf.2014.03.014](https://doi.org/10.1016/j.gsf.2014.03.014 ).
[20] Kaiho, K., et al. (2017). Site of asteroid impact changed the history of life on Earth: the low probability of mass extinction. Scientific Reports, 7(1), 14917. DOI: [10.1038/s41598-017-14199-x](https://doi.org/10.1038/s41598-017-14199-x ). PMID: 29123162. PMC: PMC5684241.
[21] Carlisle, E., et al. (2024). Ediacaran origin and Ediacaran-Cambrian diversification of metazoans. Science Advances, 10(2), adp7161. DOI: [10.1126/sciadv.adp7161](https://doi.org/10.1126/sciadv.adp7161 ).

References

TP53 and Recent Mutagenesis

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4.Nunney, L. (2022). Cancer suppression and the evolution of multiple retrogene copies of TP53 in elephants: A re-evaluation. Evolutionary Applications, 15(6), 910-922. DOI: 10.1111/eva.13383. PMID: 35754512.
5.Li, J., et al. (2025). Pathogenic variation in human DNA damage repair genes was originated from the evolutionary process of modern humans. Nucleic Acids Research (Preprint/In Press). [Referenciado por Sodré Neto].

Soft Tissue Preservation

1.Schweitzer, M. H., et al. (2005). Soft-tissue vessels and cellular preservation in Tyrannosaurus rex. Science, 307(5717), 1952-1955. DOI: 10.1126/science.1108397. PMID: 15790853.
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Radiation and the Ediacaran

1.Zou, Y., et al. (2025). Mechanisms of Uranium and Thorium Accumulation in the Lower Ediacaran Marine Sediments from the Upper Yangtze Platform, China. Journal of Marine Science and Engineering, 13(3), 413. DOI: 10.3390/jmse13030413.
2.Gong, Z., et al. (2023). Revisiting marine redox conditions during the Ediacaran Shuram excursion. PubMed, 36755479. DOI: 10.1016/j.gca.2023.01.018.
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Recent Acceleration of the Human Mutation Rate

1.Harris, K. (2017). Rapid evolution of the human mutation spectrum. eLife, 6, e24284. DOI: 10.7554/eLife.24284. PMID: 28422026. PMC: PMC5435464.
2.Hawks, J., et al. (2007). Recent acceleration of human adaptive evolution. Proceedings of the National Academy of Sciences, 104(52), 20753-20758. DOI: 10.1073/pnas.0707650104. PMID: 18087044. PMC: PMC2410101.
3.Thomas, G. W. C., et al. (2014). The human mutation rate is increasing, even as it slows. Molecular Biology and Evolution, 31(2), 253-257. DOI: 10.1093/molbev/mst229. PMID: 24273151.
4.Harris, K. (2015). Evidence for recent, population-specific evolution of the human mutation rate. Proceedings of the National Academy of Sciences, 112(11), 3439-3444. DOI: 10.1073/pnas.1418652112. PMID: 25733855. PMC: PMC4371947.

Nuclear Piezoelectricity and Neutron Emission

1.Carpinteri, A., et al. (2013). Piezonuclear Fission Reactions from Earthquakes and Brittle Rocks Failure: Evidence of Neutron Emission and Non-Radioactive Product Elements. Strain, 49(2), 110-120. DOI: 10.1111/str.12017.
2.Benetti, P., et al. (2019). Neutron emission from fracturing of granite blocks. Physics Letters A, 383(19), 2261-2264. DOI: 10.1016/j.physleta.2019.04.041.
3.Carpinteri, A., et al. (2012). Piezonuclear neutrons from earthquakes as a hypothesis for the explanation of carbon-14 dating anomalies. Scientific Research and Essays, 7(22), 2005-2012. DOI: 10.5897/SRE11.676.

Asteroid Impacts and Biological Changes

1.Young, G. M. (2015). Environmental upheavals of the Ediacaran period and the evolution of early animals. Geoscience Frontiers, 6(1), 5-18. DOI: 10.1016/j.gsf.2014.03.014.
2.Kaiho, K., et al. (2017). Site of asteroid impact changed the history of life on Earth: the low probability of mass extinction. Scientific Reports, 7(1), 14917. DOI: 10.1038/s41598-017-14199-x. PMID: 29123162. PMC: PMC5684241.
3.Carlisle, E., et al. (2024). Ediacaran origin and Ediacaran-Cambrian diversification of metazoans. Science Advances, 10(2), adp7161. DOI: 10.1126/sciadv.adp7161.

TP53 and Cancer Evolution

1.Efe, G., et al. (2026). Mutant p53: evolving perspectives. Nature Reviews Cancer (In Press). PMID: 12758147.
2.Voskarides, K., & Giannopoulou, N. (2023). The Role of TP53 in Adaptation and Evolution. Cells, 12(3), 512. DOI: 10.3390/cells12030512. PMID: 36766787. PMC: PMC9914165.
3.Olivier, M., et al. (2010). TP53 Mutations in Human Cancers. Cold Spring Harbor Perspectives in Biology, 2(3), a001008. DOI: 10.1101/cshperspect.a001008. PMID: 20300202. PMC: PMC2827900.
4.Kou, S. H., et al. (2023). TP53 germline pathogenic variants in modern humans were likely originated during recent human history. NAR Cancer, 5(3), zcad025. DOI: 10.1093/narcancer/zcad025. PMID: 37192725.

Radiation and the Ediacaran Period (In-depth Study)

1.Gong, Z., et al. (2023). Global marine redox changes drove the rise and fall of the Ediacara biota. Proceedings of the National Academy of Sciences, 116(49), 24508-24513. DOI: 10.1073/pnas.1908724116. PMID: 31740608. PMC: PMC6899691.
2.Dessouky, O. K., et al. (2021). New insights into Cryogenian arc granitoids hosting Th-U mineralization in the Central Eastern Desert of Egypt. Ore Geology Reviews, 138, 104399. DOI: 10.1016/j.oregeorev.2021.104399.
3.Young, G. M. (2015). Environmental upheavals of the Ediacaran period and the evolution of early animals. Geoscience Frontiers, 6(1), 5-18. DOI: 10.1016/j.gsf.2014.03.014.

Soft Tissue Preservation (In-depth Study)

1.Schweitzer, M. H., et al. (2006). Soft-tissue and cellular preservation in vertebrate skeletal elements from the Upper Cretaceous. Proceedings of the Royal Society B: Biological Sciences, 273(1587), 787-793. DOI: 10.1098/rspb.2005.3314. PMID: 16627289. PMC: PMC1685849.
2.Tahoun, M., et al. (2022). Chemistry and Analysis of Organic Compounds in Dinosaurs. Molecules, 27(10), 3234. DOI: 10.3390/molecules27103234. PMID: 35638510. PMC: PMC9138232.
3.Voegele, K. K., et al. (2022). Soft Tissue and Biomolecular Preservation in Vertebrate Fossils: A Review. Geosciences, 12(8), 304. DOI: 10.3390/geosciences12080304. PMC: PMC9405258.
4.Saitta, E. T., et al. (2019). Cretaceous dinosaur bone contains recent organic material and is not fossilized. eLife, 8, e46205. DOI: 10.7554/eLife.46205. PMID: 31215707. PMC: PMC6581507.

Nuclear Piezoelectricity and Impacts

1.Carpinteri, A., et al. (2012). Piezonuclear neutrons from earthquakes as a hypothesis for the explanation of carbon-14 dating anomalies. Scientific Research and Essays, 7(22), 2005-2012. DOI: 10.5897/SRE11.676.
2. Carpinteri , A. , & Manuello , A. (2011). Geomechanical and Geochemical Evidence of Piezonuclear Fission Reactions in the Earth’s Crust.  Strain , 47, 267–281. DOI:  10.1111/j.1475–1305.2010.00766.x .

Asteroid Impacts and Evolution

1.Kaiho, K., et al. (2017). Site of asteroid impact changed the history of life on Earth: the low probability of mass extinction. Scientific Reports, 7(1), 14917. DOI: 10.1038/s41598-017-14199-x. PMID: 29123162. PMC: PMC5684241.
2.Carlisle, E., et al. (2024). Ediacaran origin and Ediacaran-Cambrian diversification of metazoans. Science Advances, 10(2), adp7161. DOI: 10.1126/sciadv.adp7161.

Acceleration of the Recent Human Mutation Rate (Continued)

1.Keightley, P. D. (2012). Rates and Fitness Consequences of New Mutations in Humans. Genetics, 190(2), 295-304. DOI: 10.1534/genetics.111.134651. PMID: 22345601. PMC: PMC3276617.

Radiation and the Ediacaran Period (Continued)

1.Zhang, F., et al. (2019). Global marine redox changes drove the rise and fall of the Ediacara biota. Proceedings of the National Academy of Sciences, 116(49), 24508-24513. DOI: 10.1073/pnas.1908724116. PMID: 31740608. PMC: PMC6899691.
2.Duarte, G. T., et al. (2023). Chronic Ionizing Radiation of Plants: An Evolutionary Factor. Plants, 12(5), 10005729. DOI: 10.3390/plants120510005729. PMID: 36903677. PMC: PMC10005729.
3.Cherry, L. B., et al. (2022). A diverse Ediacara assemblage survived under low-oxygen conditions. Proceedings of the Royal Society B: Biological Sciences, 289(1987), 20221770. DOI: 10.1098/rspb.2022.1770. PMID: 36447743. PMC: PMC9701187.
4.Yang, C., et al. (2021). The tempo of Ediacaran evolution. Nature Ecology & Evolution, 5(11), 1474-1483. DOI: 10.1038/s41559-021-01556-x. PMID: 34580436. PMC: PMC8565906.

Soft Tissue Preservation (Continued)

1.Schweitzer, M. H., et al. (2006). Soft-tissue and cellular preservation in vertebrate skeletal elements from the Upper Cretaceous. Proceedings of the Royal Society B: Biological Sciences, 273(1587), 787-793. DOI: 10.1098/rspb.2005.3314. PMID: 16627289. PMC: PMC1685849.
2.Saitta, E. T., et al. (2019). Cretaceous dinosaur bone contains recent organic material and is not fossilized. eLife, 8, e46205. DOI: 10.7554/eLife.46205. PMID: 31215707. PMC: PMC6581507.

Nuclear Piezoelectricity and Impacts (Continued)

1.Carpinteri, A., et al. (2012). Piezonuclear neutrons from earthquakes as a hypothesis for the explanation of carbon-14 dating anomalies. Scientific Research and Essays, 7(22), 2005-2012. DOI: 10.5897/SRE11.676.

Asteroid Impacts and Evolution (Continued)

1.Schmieder, M., & Kring, D. A. (2020). Earth’s impact events through geologic time: a list of recommended ages for terrestrial impact structures and deposits. Astrobiology, 20(1), 1-12. DOI: 10.1089/ast.2019.2085. PMID: 31917536.

TP53 and Cancer Evolution (Continued)

1.Mansur, M. B., et al. (2023). Convergent TP53 loss and evolvability in cancer. Nature Communications, 14(1), 5897. DOI: 10.1038/s41467-023-41617-x. PMID: 37735398. PMC: PMC10518978.
2.Tollis, M., et al. (2017). How has evolution solved the problem of cancer prevention? eLife, 6, e28942. DOI: 10.7554/eLife.28942. PMID: 28705195. PMC: PMC5509159.
3.Seluanov, A., et al. (2018). Mechanisms of cancer resistance in long-lived mammals. Nature Reviews Cancer, 18(7), 433-449. DOI: 10.1038/s41568-018-0004-9. PMID: 29725110. PMC: PMC6015544.

Radiation and the Ediacaran Period (Continued)

1.Bowyer, F. T., et al. (2024). Sea level controls on Ediacaran-Cambrian animal radiations. Nature Communications, 15(1), 1873. DOI: 10.1038/s41467-024-46150-w. PMID: 38429398. PMC: PMC11290527.
2.Evans, S. D., et al. (2022). Environmental drivers of the first major animal extinction. Proceedings of the National Academy of Sciences, 119(49), e2208021119. DOI: 10.1073/pnas.2208021119. PMID: 36449574. PMC: PMC9674242.
3.Darroch, S. A. F., et al. (2023). Causes and consequences of end-Ediacaran extinction. Trends in Ecology & Evolution, 38(11), 999-1011. DOI: 10.1016/j.tree.2023.07.003. PMID: 37574343. PMC: PMC11895755.
4.Meert, J. G., et al. (2016). Rapid changes of magnetic Field polarity in the late Ediacaran: Linking the Cambrian evolutionary radiation and increased UV-B radiation. Gondwana Research, 34, 1-14. DOI: 10.1016/j.gr.2016.01.009.

Soft Tissue Preservation (Continued)

1.Schweitzer, M. H., et al. (2014). A role for iron and oxygen chemistry in preserving soft tissues in vertebrate fossils. Proceedings of the Royal Society B: Biological Sciences, 281(1775), 20132792. DOI: 10.1098/rspb.2013.2792. PMID: 24284224. PMC: PMC3866414.
2.Senter, P. J. (2022). Cells and soft tissues in fossil bone: A review of preservation mechanisms, with corrections of misconceptions. Palaeontologia Electronica, 25(3), a37. DOI: 10.26879/1247.

Asteroid Impacts and Evolution (Continued)

1.Erwin, D. H. (2015). Was the Ediacaran–Cambrian radiation a unique evolutionary event? Paleobiology, 41(1), 1-15. DOI: 10.1017/pab.2014.22.

TP53 and Cancer Evolution (Continued)

1.Nunney, L. (2022). Cancer suppression and the evolution of multiple retrogene copies of TP53 in elephants: A re‐evaluation. Evolutionary Applications, 15(6), 910-922. DOI: 10.1111/eva.13383. PMID: 35754512.
2.Tollis, M., Schiffman, J. D., & Boddy, A. M. (2017). Evolution of cancer suppression as revealed by mammalian comparative genomics. Current Opinion in Genetics & Development, 49, 17-23. DOI: 10.1016/j.gde.2017.09.001. PMID: 28988049.

Radiation and the Ediacaran Period (Continued)

1.Erwin, D. H. (2015). Was the Ediacaran–Cambrian radiation a unique evolutionary event? Paleobiology, 41(1), 1-15. DOI: 10.1017/pab.2014.22.
2.Chen, Z. Q., et al. (2022). Editorial preface to special issue: Extreme environments and biotic responses during the Neoproterozoic-Phanerozoic transition. Global and Planetary Change, 219, 103987. DOI: 10.1016/j.gloplacha.2022.103987.

Soft Tissue Preservation (Continued)

1.Senter, P. J. (2022). Cells and soft tissues in fossil bone: A review of preservation mechanisms, with corrections of misconceptions. Palaeontologia Electronica, 25(3), a37. DOI: 10.26879/1247.
2.Anderson, L., et al. (2023). A chemical framework for the preservation of fossil vertebrate cells and soft tissues. Geology, 51(5), 487-491. DOI: 10.1130/G50894.1.

TP53 and Cancer Evolution (Continued)

1.Joerger, A. C., & Fersht, A. R. (2024). TP53: the unluckiest of genes? Nature Reviews Cancer (In Press). PMID: 11803090.
2.Olivier, M., et al. (2010). TP53 mutations in human cancers: origins, consequences, and clinical implications. Cold Spring Harbor Perspectives in Biology, 2(3), a001008. DOI: 10.1101/cshperspect.a001008. PMID: 20182602. PMC: PMC2827900.
3.MacDonald, N., et al. (2024). The molecular evolution of cancer associated genes in mammals. Nature Ecology & Evolution (In Press). PMID: 11109183.

Radiation and the Ediacaran Period (Continued)

1.Rooney, A. D., et al. (2020). Calibrating the coevolution of Ediacaran life and environment. Proceedings of the National Academy of Sciences, 117(30), 17614-17622. DOI: 10.1073/pnas.2002512117. PMID: 32669467. PMC: PMC7382294.
2.Knoll, A. H., et al. (2006). The Ediacaran Period: a new addition to the geologic time scale. Episodes, 29(2), 114-119. Disponível em: https://stratigraphy.org/gssps/files/ediacaran.pdf.

Soft Tissue Preservation (Continued)

1.Ullmann, P. V., et al. (2022). Taphonomic and Diagenetic Pathways to Protein Preservation in the Fossil Record. Palaeontologia Electronica, 25(3), a36. DOI: 10.26879/1246.
2.McNamara, M. E., et al. (2018). Non-integumentary melanosomes can bias reconstructions of fossil coloration. Nature Communications, 9(1), 2997. DOI: 10.1038/s41467-018-05609-8. PMID: 30065260. PMC: PMC6056411.

Holocene Catastrophic Events and Impacts

1.Waters, C. N., et al. (2022). Epochs, events and episodes: Marking the geological time scale. Earth-Science Reviews, 235, 104251. DOI: 10.1016/j.earscirev.2022.104251.
2.Heinen, R., et al. (2025). Effects of Extreme Climatic Events on Evolutionary Processes. Evolutionary Biology (In Press). PMID: 12645372.
3.Robbins Schug, G., et al. (2023). Climate change, human health, and resilience in the Holocene. Proceedings of the National Academy of Sciences, 120(49), e2209472120. DOI: 10.1073/pnas.2209472120. PMID: 37992036. PMC: PMC10700827.
4.Thompson, J., et al. (2024). The meaning of mass extinctions and what the fossil record tells us. Biology Letters, 20(8), 20240265. DOI: 10.1098/rsbl.2024.0265. PMID: 39130094. PMC: PMC11317049.
5.Jablonski, D. (2001). Lessons from the past: Evolutionary impacts of mass extinctions. Proceedings of the National Academy of Sciences, 98(10), 5393-5398. DOI: 10.1073/pnas.101092198. PMID: 11344258. PMC: PMC33224.

Limitations of Radiometric Dating

1.Thomas, B. (2012). Fluctuations Show Radioisotope Decay Is Unreliable. Acts & Facts, 41(10), 17. Disponível em: https://www.icr.org/article/fluctuations-show-radioisotope-decay-unreliable/.
2.Wiens, R. C. (2002). Radiometric dating: A Christian perspective. Science in Christian Perspective. Disponível em: http://pages.ucsd.edu/~jjmoore/courses/anth42web/WiensDatingMeth02.pdf.
3.Shakespeare, W. M. (1975). LIMITATIONS OF RADIOMETRIC DATING. The Royal Society of Canada. Disponível em: https://utppublishing.com/doi/pdf/10.3138/9781487587031#page=31.

Mutation Rates and Evolution

1.Keightley, P. D. (2012). Rates and Fitness Consequences of New Mutations in Humans. Genetics, 190(2), 295-304. DOI: 10.1534/genetics.111.134651. PMID: 22345601. PMC: PMC3276617.

Ediacaran and Environmental Events

1.Zhang, F., et al. (2019). Global marine redox changes drove the rise and fall of the Ediacara biota. Proceedings of the National Academy of Sciences, 116(49), 24508-24513. DOI: 10.1073/pnas.1908724116. PMID: 31740608. PMC: PMC6899691.
2.Duarte, G. T., et al. (2023). Chronic Ionizing Radiation of Plants: An Evolutionary Factor. Plants, 12(5), 10005729. DOI: 10.3390/plants120510005729. PMID: 36903677. PMC: PMC10005729.
3.Cherry, L. B., et al. (2022). A diverse Ediacara assemblage survived under low-oxygen conditions. Proceedings of the Royal Society B: Biological Sciences, 289(1987), 20221770. DOI: 10.1098/rspb.2022.1770. PMID: 36447743. PMC: PMC9701187.
4.Yang, C., et al. (2021). The tempo of Ediacaran evolution. Nature Ecology & Evolution, 5(11), 1474-1483. DOI: 10.1038/s41559-021-01556-x. PMID: 34580436. PMC: PMC8565906.

Soft Tissue Preservation (Continued)

1.Schweitzer, M. H., et al. (2006). Soft-tissue and cellular preservation in vertebrate skeletal elements from the Upper Cretaceous. Proceedings of the Royal Society B: Biological Sciences, 273(1587), 787-793. DOI: 10.1098/rspb.2005.3314. PMID: 16627289. PMC: PMC1685849.
2.Saitta, E. T., et al. (2019). Cretaceous dinosaur bone contains recent organic material and is not fossilized. eLife, 8, e46205. DOI: 10.7554/eLife.46205. PMID: 31215707. PMC: PMC6581507.

Nuclear Piezoelectricity and Impacts (Continued)

1.Carpinteri, A., et al. (2012). Piezonuclear neutrons from earthquakes as a hypothesis for the explanation of carbon-14 dating anomalies. Scientific Research and Essays, 7(22), 2005-2012. DOI: 10.5897/SRE11.676.

Asteroid Impacts and Evolution (Continued)

1.Schmieder, M., & Kring, D. A. (2020). Earth’s impact events through geologic time: a list of recommended ages for terrestrial impact structures and deposits. Astrobiology, 20(1), 1-12. DOI: 10.1089/ast.2019.2085. PMID: 31917536.

TP53 and Cancer Evolution (Continued)

1.Levine, A. J. (2020). p53: 800 million years of evolution and 40 years of discovery. Nature Reviews Cancer, 20(8), 475-489. DOI: 10.1038/s41568-020-0262-1. PMID: 32439830.

Radiation and the Ediacaran Period (Continued)

1.Meert, J. G., et al. (2016). Rapid changes of magnetic Field polarity in the late Ediacaran: Linking the Cambrian evolutionary radiation and increased UV-B radiation. Gondwana Research, 34, 1-14. DOI: 10.1016/j.gr.2016.01.009.
2.Bailer-Jones, C. A. L. (2009). The evidence for and against astronomical impacts on climate change and mass extinctions: a review. International Journal of Astrobiology, 8(2), 85-101. DOI: 10.1017/S147355040900022X.

Soft Tissue Preservation (Continued)

1.Anderson, L. A., et al. (2023). A chemical framework for the preservation of fossil vertebrate cells and soft tissues. Geology, 51(5), 487-491. DOI: 10.1130/G50894.1.

TP53 and Cancer Evolution (Continued)

1.Levine, A. J. (2020). p53: 800 million years of evolution and 40 years of discovery. Nature Reviews Cancer, 20(8), 475-489. DOI: 10.1038/s41568-020-0262-1. PMID: 32439830.

Radiation and the Ediacaran Period (Continued)

1.Meert, J. G., et al. (2016). Rapid changes of magnetic Field polarity in the late Ediacaran: Linking the Cambrian evolutionary radiation and increased UV-B radiation. Gondwana Research, 34, 1-14. DOI: 10.1016/j.gr.2016.01.009.
2.Bailer-Jones, C. A. L. (2009). The evidence for and against astronomical impacts on climate change and mass extinctions: a review. International Journal of Astrobiology, 8(2), 85-101. DOI: 10.1017/S147355040900022X.

Soft Tissue Preservation (Continued)

1.Anderson, L. A., et al. (2023). A chemical framework for the preservation of fossil vertebrate cells and soft tissues. Geology, 51(5), 487-491. DOI: 10.1130/G50894.1.

TP53 and Cancer Evolution (Continued)

1.Levine, A. J. (2020). p53: 800 million years of evolution and 40 years of discovery. Nature Reviews Cancer, 20(8), 475-489. DOI: 10.1038/s41568-020-0262-1. PMID: 32439830.

Radiation and the Ediacaran Period (Continued)

1.Meert, J. G., et al. (2016). Rapid changes of magnetic Field polarity in the late Ediacaran: Linking the Cambrian evolutionary radiation and increased UV-B radiation. Gondwana Research, 34, 1-14. DOI: 10.1016/j.gr.2016.01.009.
2.Bailer-Jones, C. A. L. (2009). The evidence for and against astronomical impacts on climate change and mass extinctions: a review. International Journal of Astrobiology, 8(2), 85-101. DOI: 10.1017/S147355040900022X.

Soft Tissue Preservation (Continued)

1.Anderson, L. A., et al. (2023). A chemical framework for the preservation of fossil vertebrate cells and soft tissues. Geology, 51(5), 487-491. DOI: 10.1130/G50894.1.

TP53 and Cancer Evolution (Continued)

1.Levine, A. J. (2020). p53: 800 million years of evolution and 40 years of discovery. Nature Reviews Cancer, 20(8), 475-489. DOI: 10.1038/s41568-020-0262-1. PMID: 32439830.

Radiation and the Ediacaran Period (Continued)

1.Meert, J. G., et al. (2016). Rapid changes of magnetic Field polarity in the late Ediacaran: Linking the Cambrian evolutionary radiation and increased UV-B radiation. Gondwana Research, 34, 1-14. DOI: 10.1016/j.gr.2016.01.009.
2.Bailer-Jones, C. A. L. (2009). The evidence for and against astronomical impacts on climate change and mass extinctions: a review. International Journal of Astrobiology, 8(2), 85-101. DOI: 10.1017/S147355040900022X.

Soft Tissue Preservation (Continued)

1.Anderson, L. A., et al. (2023). A chemical framework for the preservation of fossil vertebrate cells and soft tissues. Geology, 51(5), 487-491. DOI: 10.1130/G50894.1.

TP53 and Cancer Evolution (Continued)

1.Voskarides, K., & Giannopoulou, N. (2023). The Role of TP53 in Adaptation and Evolution. Cells, 12(3), 512. DOI: 10.3390/cells12030512. PMID: 36766601. PMC: PMC9914165.
2.Sulak, M., et al. (2016). TP53 copy number expansion is associated with the evolution of increased body size and cancer resistance in elephants. eLife, 5, e11994. DOI: 10.7554/eLife.11994. PMID: 27733221. PMC: PMC5061548.

Radiation and the Ediacaran Period (Continued)

1.Wang, R., et al. (2023). A Great late Ediacaran ice age. Nature Communications, 14(1), 3803. DOI: 10.1038/s41467-023-39509-0. PMID: 37380644. PMC: PMC10306365.

Soft Tissue Preservation (Continued)

1.Schweitzer, M. H., et al. (2006). Soft-tissue and cellular preservation in vertebrate skeletal elements from the Upper Cretaceous. Proceedings of the Royal Society B: Biological Sciences, 273(1587), 787-793. DOI: 10.1098/rspb.2005.3314. PMID: 16627289. PMC: PMC1685849.
2.Voegele, K. K., et al. (2022). Soft Tissue and Biomolecular Preservation in Vertebrate Fossils: An Overview. Palaeontologia Electronica, 25(3), a35. DOI: 10.26879/1245. PMC: PMC9405258.

TP53 and Cancer Evolution (Continued)

1.Voskarides, K., & Giannopoulou, N. (2023). The Role of TP53 in Adaptation and Evolution. Cells, 12(3), 512. DOI: 10.3390/cells12030512. PMID: 36766601. PMC: PMC9914165.
2.Sulak, M., et al. (2016). TP53 copy number expansion is associated with the evolution of increased body size and cancer resistance in elephants. eLife, 5, e11994. DOI: 10.7554/eLife.11994. PMID: 27733221. PMC: PMC5061548.

Radiation and the Ediacaran Period (Continued)

1.Wang, R., et al. (2023). A Great late Ediacaran ice age. Nature Communications, 14(1), 3803. DOI: 10.1038/s41467-023-39509-0. PMID: 37380644. PMC: PMC10306365.
2.Xiao, S., & Laflamme, M. (2008). On the eve of animal radiation: phylogeny, ecology and evolution of the Ediacara biota. Trends in Ecology & Evolution, 23(10), 571-580. DOI: 10.1016/j.tree.2008.07.015. PMID: 18952316.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.

Preservação de Tecidos Moles (Continuação)

1.Schweitzer, M. H., et al. (2006). Soft-tissue and cellular preservation in vertebrate skeletal elements from the Upper Cretaceous. Proceedings of the Royal Society B: Biological Sciences, 273(1587), 787-793. DOI: 10.1098/rspb.2005.3314. PMID: 16627289. PMC: PMC1685849.
2.Voegele, K. K., et al. (2022). Soft Tissue and Biomolecular Preservation in Vertebrate Fossils: An Overview. Palaeontologia Electronica, 25(3), a35. DOI: 10.26879/1245. PMC: PMC9405258.

TP53 e Evolução do Câncer (Continuação)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.

Radiação e Ediacarano (Continuação)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.

Preservação de Tecidos Moles (Continuação)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
2.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
3.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
4.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Preservação de Tecidos Moles (Continuação)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 e Evolução do Câncer (Continuação)

1.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
2.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
3.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
4.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiação e Ediacarano (Continuação)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Preservação de Tecidos Moles (Continuação)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 e Evolução do Câncer (Continuação)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiação e Ediacarano (Continuação)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 e Evolução do Câncer (Continuação)

1.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiação e Ediacarano (Continuação)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Preservação de Tecidos Moles (Continuação)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 e Evolução do Câncer (Continuação)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiação e Ediacarano (Continuação)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Preservação de Tecidos Moles (Continuação)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

TP53 and Cancer Evolution (Continued)

1.Aubrey, B. J., et al. (2016). Tumor-Suppressor Functions of the TP53 Pathway. Cold Spring Harbor Perspectives in Medicine, 6(10), a026024. DOI: 10.1101/cshperspect.a026024. PMID: 27587399. PMC: PMC4852799.
2.Miller, M. L., et al. (2016). The Evolution of TP53 Mutations: From Loss-of-Function to Gain-of-Function. Molecular Cancer Research, 14(12), 1189-1199. DOI: 10.1158/1541-7786.MCR-16-0186. PMID: 27799258. PMC: PMC5298884.
3.Zawacka-Pankau, J. E., & Sznarkowska, A. (2022). The Role of p53 Family in Cancer. Cancers, 14(3), 823. DOI: 10.3390/cancers14030823. PMID: 35159090. PMC: PMC8833989.
4.Rivlin, N., et al. (2011). Mutations in the p53 Tumor Suppressor Gene. Genes & Cancer, 2(4), 445-453. DOI: 10.1177/1947601911411218. PMID: 21779477. PMC: PMC3135636.
5.Liu, Y., et al. (2016). Deletions linked to TP53 loss drive cancer through p53-independent mechanisms. Nature, 531(7595), 471-475. DOI: 10.1038/nature17157. PMID: 26982728. PMC: PMC4836395.

Radiation and the Ediacaran Period (Continued)

1.McFadden, K. A., et al. (2008). Pulsed oxidation and biological evolution in the Ediacaran and early Cambrian. Proceedings of the National Academy of Sciences, 105(9), 3197-3202. DOI: 10.1073/pnas.0708332105. PMID: 18299594. PMC: PMC2265117.
2.Shen, Y., et al. (2008). On the coevolution of Ediacaran oceans and animals. Proceedings of the National Academy of Sciences, 105(9), 3203-3208. DOI: 10.1073/pnas.0708333105. PMID: 18299595. PMC: PMC2375388.
3.ResearchGate. (2025). Environmental upheavals of the Ediacaran period and the Cambrian explosion of animal life. Disponível em: https://www.researchgate.net/publication/265788966_Environmental_upheavals_of_the_Ediacaran_period_and_the_Cambrian_explosion_of_animal_life.
4.Chen, B., et al. (2022). A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean. Earth and Planetary Science Letters, 578, 117300. DOI: 10.1016/j.epsl.2021.117300.
5.Laakso, T. A., et al. (2020). Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences, 117(10), 5241-5247. DOI: 10.1073/pnas.1916738117. PMID: 32094183. PMC: PMC7071887.

Soft Tissue Preservation (Continued)

1.Lee, Y. C., et al. (2017). Evidence of preserved collagen in an Early Jurassic ichthyosaur. Nature Communications, 8(1), 14701. DOI: 10.1038/ncomms14701. PMID: 28244498. PMC: PMC5290320.
2.Sansom, R. S., et al. (2016). Preservation and phylogeny of Cambrian ecdysozoans. Nature Communications, 7(1), 12724. DOI: 10.1038/ncomms12724. PMID: 27595908. PMC: PMC5013620.
3.Wiemann, J., et al. (2018). Fossilization transforms vertebrate hard tissue proteins into N-heterocyclic polymers. Nature Communications, 9(1), 4627. DOI: 10.1038/s41467-018-07012-1. PMID: 30409924. PMC: PMC6226439.
4.Cadena, E. A., et al. (2016). Exceptional preservation of soft tissues and blood vessel-like microstructures obtained from fossil turtles. Palaeontology, 59(1), 1-12. DOI: 10.1111/pala.12211. PMID: 27019573. PMC: PMC4727973.

The accelerated accumulation of mutations in the human genome between 5,000 and 10,000 years ago  has been erroneously attributed by Gerald Crabtree and much of the scientific consensus  to lifestyle changes from hunter-gatherer under strong selective pressure to agricultural, which would protect the weakest and sickest, allowing them to accumulate more genetic defects in their offspring. This article proposes a change in this paradigm, because the peak of mutations observed in modern humans   is also  observed in various animals; among several examples, the TP53 genetic segment of fossil proboscideans, when compared to modern elephants, shows an explosion of mutated variations, as occurs in modern humans compared to some Neanderthals, thus requiring a non-cultural cause, invalidating the hypothesis of the transition from hunter-gatherer to agricultural, because elephants and dozens of other animals did not become agricultural animals; this cause would affect humans and animals equally and therefore would be global and catastrophic, thus being an  accelerating event of radioactive decay . We deduced that this recent mutational peak was a direct result of a  catastrophic event that accelerated radioactive decay . Through the application of   Cardone and Carpinteri’s  theory of nuclear piezoelectricity…We argue that if rock fractures and earthquakes generate accelerated decay and neutron release, how much more so impacts from large asteroids that would generate thousands of earthquakes, shaking the entire earth; they generated pressures on the scale of gigapascals, inducing large-scale neutron release and phonofission. Also, the prevalence of single nucleotide polymorphisms (SNPs) in the human TP53 gene and mtDNA can be interpreted as a genomic signature of intense and widespread mutagenic events in human entropic history. Contrary to the academic consensus hypothesis cited by Crabtree, which posits a ‘fragile intellect’ resulting from decreased cultural selective pressure, we propose that the accumulation of such variations in TP53, and in other critical genes, can be more plausibly attributed primarily to a global catastrophic cause of a radioactive nature. Such an event would have imposed unprecedented mutagenic pressure, explaining, among many aspects, the high genetic and average size contrast between fossil ancestors and survivors in current biodiversity; leading to rapid genomic diversification and the fixation of SNPs that, while they could confer some adaptability in a post-catastrophic environment, could also have contributed to the intrinsic vulnerability of modern humans to diseases such as cancer and a drastic decrease in longevity, since TP53, as a cellular repairer, is closely related to longevity. The high frequency of SNPs in TP53, therefore, does not reflect a culturally induced intellectual fragility, but rather a molecular scar from a tumultuous geological and environmental past, shaping human biology in profound and lasting ways.

Introduction

Modern geochronology is based on the principle of uniformitarianism, which assumes that radioactive decay rates have remained constant throughout geological eras. However,  dating contradictions in  impact structures and the sudden peak of deleterious mutations in the Middle Holocene (5-10 ka BP) suggest that this “clock” can be drastically altered by extreme energy events    [99] .

Materials and methods

This investigation incorporates data from:
1. Nuclear Physics and Geomechanics:  Analysis of the work of Cardone and Carpinteri on piezonuclear fission reactions and neutron emission in rocks under mechanical stress  . [1-15]
2. Comparative Genomics:  Studies of recent pathogenic variations in DNA repair genes (DDR) in Nenderthals versus modern humans, between mammoths and modern elephants, ancient cetaceans and modern cetaceans, and a list of dozens of other cases, reveal an absence of mutations in the TP53 genetic stretch    in ancestors and many variations in modern descendants, with this differentiation having occurred relatively recently [16]. 
3. Impact Astrophysics:  Modeling the nuclear effects of plasmas generated by hypervelocity impacts and their ability to accelerate electron capture decay[99].

Results and discussion

Nuclear Piezoelectricity and the Invalidation of Geochronology

 

Effects observed in the fall of large bolides such as “Spalling”, nuclear piezoelectricity (Carpinteri, h= 95 [7] ), phono-fission [17], plasmas of very high amperages and charge differentials promote accelerated decay, altering the decay constancy, and can “age” rocks in milliseconds, falsifying uniformitarian radiometric dating.

The theory of nuclear piezoelectricity demonstrates that extreme pressures and mechanical shock waves can induce nuclear reactions even without the need for high temperatures (piezonuclear fission). Cardone et al. demonstrated the acceleration of thorium decay under acoustic cavitation, a phenomenon that suggests that the decay rate is not an eternal constant, but dependent on the physical-chemical and mechanical environment.

Asteroid impacts generate gigapascal pressures that transform rocks into high electron density plasmas  . In these environments, electron capture is accelerated, artificially “resetting” or “aging” mineral samples in milliseconds  . This invalidates dating based on the constancy of Carbon-14 and other isotopes, suggesting that global sedimentary layers may have been deposited in catastrophic events much more recent than uniformitarianism proposes.  [18-34]

The Mutational Peak as a Byproduct of Nuclear Impacts

The peak of human mutations between 5,000 and 10,000 years ago necessitates global radioactive anomalies. The massive release of neutrons induced by nuclear piezoelectricity during these large asteroid impacts would have raised radiation to global mutagenic levels and would explain several correlations beyond the verified mutagenic peak, such as: absurdities in biased dating contradictions, dating still organic fossil tissues at millions of years, or contrasting visualizations between the fossil record with an average of giants to smaller and degenerate descendants .
The most compelling biological evidence is the parallel variation in the TP53 tumor suppressor gene   in proboscideans (elephants and mammoths) and cetaceans  . Since these species did not become agricultural, Crabtree’s explanation, by repeating the consensus,  becomes invalid.

Disaster Geology and Spontaneous Stratification

Global sedimentary layers, often interpreted as records millions of years old, exhibit characteristics of catastrophic paleocurrents of great width and length. Spontaneous stratification (SEE) under turbulent flow conditions explains the rapid formation of these layers during marine transgressions caused by asteroid impacts. The radioactivity concentrated in specific strata (such as the Cambrian or Silurian) does not indicate age, but rather the intensity of the piezonuclear nuclear event at the time of deposition.

Evolution Table of the TP53 Gene in Mammals: From Canonical to Variable

#
Ancestral (Fossil/Reconstructed)
Modern Descendant
Ancestral State (NM_000546)
Variations in Modern Descendants
Reference (DOI/PMID)
1
Neanderthal
Modern Man
Canonical
~1000 variations (e.g., P72R, R248W)
10.1093/nar/gcad427  /  37192725
2
Woolly Mammoth
African Elephant
Canonical
Expansion to 20 copies (1 gene + 19 retrogenes)
10.1126/science.aab3837 / 26447594
3
Basilosauridae
Southern right whale
Canonical
Leu replacement in the proline-rich region
10.1016/j.celrep.2014.12.008  /  25532846
4
Ancestral Chiroptera
Brandt’s bat
Canonical
Insertion of 7 amino acids into the DNA-binding region.
10.1371/journal.pone.0080221 / 24146839
5
Ancestral Rodent
Naked mole-rat
Canonical
Extreme stabilization and nuclear buildup
10.1038/s41598-020-64009-0  /  3
6
Ancestral Cetacean
Blue whale
Canonical
Positive selection in tumor suppression pathways
10.1093/molbev/msae036  /  38381405
7
Ancestral Phiseterid
Sperm whale
Canonical
Variations in p53 pathway genes (Peto’s Paradox)
10.1098/rspb.2020.2592 / 33593187
8
Ancestral Dolphin
Bottlenose dolphin
Canonical
Positive selection in preserved waste
10.1093/molbev/msr121  /  21551212
9
Ancestral Sirênio
Manatee
Canonical
Expansion of TP53 copies
10.7554/eLife.11994 / 27642012
10
Ancestral Spalacídeo
Blind mole-rat
Canonical
Arg174Lys substitution (DNA affinity)
10.1038/nrg3728  /  24981598
11
Hominid Ancestor
Chimpanzee
Canonical
Differences in transcriptional regulation
10.1126/science.1122177 / 16382208
12
Hominid Ancestor
Gorilla
Canonical
Variations in the promoting region
10.1126/science.1122177 / 16382208
13
Ancestral Bear
Polar Bear
Canonical
Positive selection in DNA repair genes
10.1016/j.cell.2014.03.054 / 24813666
14
Ancestral Pinípede
Baikal Seal
Canonical
Adaptations for hypoxia in the p53 pathway
10.1371/journal.pone.0147647 / 26824345
15
Ancestral Chiroptera
Little brown bat
Canonical
Insertions in the DNA binding region
10.1371/journal.pone.0080221 / 24146839
16
Ancestral Squirrel
Ground squirrel
Canonical
Variations related to hibernation
10.1152/ajpregu.00248.2012  /  22933023
17
Ancestral Camelídeo
Camel
Canonical
Positive selection in response to stress
10.1038/ncomms3720 / 24220126
18
Ancestral Giraffid
Giraffe
Canonical
Adaptations in the cell cycle (high blood pressure)
10.1038/ncomms11519 / 27187143
19
Ancient Rhinoceros
White rhinoceros
Canonical
Variations in tumor suppressors
10.1186/s13059-017-1230-x / 28535798
20
Ancestral Xenarthra
Armadillo
Canonical
Massive duplication of suppressor genes
10.7554/eLife.82558 / 36594738
21
Ancestral Pilosa
Two-toed sloth
Canonical
Slow cell proliferation
10.7554/eLife.82558 / 36594738
22
Ancestral Pilosa
Giant anteater
Canonical
p53 pathway gene duplication
10.7554/eLife.82558 / 36594738
23
Ancestral Monotremado
Platypus
Canonical
Ancestral traits of reptiles
10.1038/s41586-020-03039-0  /  33408411
24
Ancestral Monotremado
Echidna
Canonical
Unique genomic variations
10.1038/s41586-020-03039-0  /  33408411
25
Ancestral Marsupial
Tasmanian devil
Canonical
Positive selection (facial tumor)
10.1038/ncomms12684 / 27572564
26
Ancestral Marsupial
Red kangaroo
Canonical
Variations in DNA repair genes
10.1186/s12864-019-5488-9 / 30736723
27
Ancestral Marsupial
Black-eared opossum
Canonical
Preservation with specific variations
10.1038/nature05805 / 17495919
28
Ancestral Sirênio
Amazonian manatee
Canonical
Expansion of TP53 copies
10.1093/molbev/msw261  /  27927787
29
Ancestral Sirênio
Dugongo
Canonical
Variations in suppressor genes
10.1038/s41598-021-95435-x / 34349156
30
Ancestral Proboscidean
Asian Elephant
Canonical
TP53 retrogene expansion
10.7554/eLife.11994 / 27642012
31
Bovine Ancestor
Cow
Canonical
Old retroposon in TP53 promoter
10.1186/s12864-015-1235-8 / 25622741
32
Canine Ancestor
Dog
Canonical
Variations in p53 mutation hotspots
10.1111/vco.12122 / 25611434

Aging and P53

Human aging is a complex process characterized by the progressive decline of physiological functions and the loss of molecular homeostasis. The p53 protein, known as the “guardian of the genome,” plays a central role in the regulation of the cell cycle, DNA repair, and apoptosis [1]. However, upon reaching old age, particularly after 60 years of age, a significant decrease in p53 functionality is observed in men [2]. This phenomenon coincides with andropause and the decline of several essential enzymes and proteins [3]. This article reviews the molecular mechanisms underlying the loss of p53 function, the influence of hormonal decline, and the consequences for genomic stability and longevity [4] [36] [37] [38] [39] [40] [41] [42] [48] [49] [50] [51] [52] [53] [54] [55].
Introduction
p53 is a transcription factor activated in response to cellular stresses, such as DNA damage, hypoxia and oncogenic stress [5]. Its primary function is to integrate these signals to determine cell fate: repair and survival, stable senescence or programmed cell death (apoptosis) [6] [56] [57] [58] [59] [60] [61] [62] [63] [64] [65] [66] [67] [68] [69] [70] [71] [72] [73] [74] [75] [76] [77] [78] [79] [80] [81] [82] [83] [84] [85] [86] [87] [88] [89] [90] [91] [92] [93] [94] [95] [96] [97] [98] [99] [100] [101] [102] [103]. In young individuals, p53 induces reversible cell cycle arrest at low activation levels, allowing DNA repair [7].
With advancing age, the effectiveness of this protective response decreases, which is a contributing factor to the increased incidence of cancer and age-related diseases in elderly populations [8]. In men over 60 years of age, the decline in testosterone and the alteration in the enzymatic profile contribute to a cellular environment that favors the inactivation or instability of p53 [9] [10].
Mechanisms of Loss of Functionality of p53

The loss of p53 function in aging is multifactorial and transcends the simple acquisition of somatic mutations in the TP53 gene [11]. Although mutations in TP53 are the most common genetic alteration in human cancers, the loss of functionality in healthy aging is frequently linked to post-translational and regulatory mechanisms [12] [54] [55].

1. Protein Instability and Degradation: Studies indicate that p53 protein stabilization after stress is reduced in aged tissues [13]. The imbalance in proteostasis, characteristic of aging, leads to protein aggregation and loss of function of cellular organelles, such as the endoplasmic reticulum and mitochondria [14]. The interaction with molecular chaperones, such as heat shock proteins (HSPs), which can stabilize mutant p53, also becomes dysregulated [15] [56].

2. Changes in Signaling Dynamics: Cellular decision-making mediated by p53 is governed by the amplitude and duration of its activation [16] [57]. The dynamics of p53 — oscillatory versus sustained responses — reflect how cells integrate the intensity and persistence of DNA damage [17]. With aging, this dynamic is altered, resulting in a failure to induce senescence or apoptosis programs when necessary, favoring the survival of damaged cells [18] [58] [59] [60] [61] [62] [63] [64] [65] [66] [67] [68] [69] [70] [71] [72] [73] [74] [75] [76] [77] [78] [79] [80] [81] [82] [83] [84] [85] [86] [87] [88] [89] [90] [91] [92] [93] [94] [95] [96] [97] [98] [99] [100] [101] [102] [103].

3. p53 isoforms: The differential expression of p53 isoforms (such as p53β, Δ133p53α and Δ40p53) functions as a “rheostat” that adjusts the cell’s sensitivity to senescence [19]. The balance between these isoforms is altered with age, contributing to the heterogeneity of the cellular response to stress [20] [37].

The Role of Andropause and Enzymatic Decline
From the age of 60, men enter a phase of progressive hormonal decline, known as andropause or late-onset hypogonadism [21]. The reduction in testosterone levels has been associated with decreased expression of p53-regulated genes and increased oxidative stress [22][23]. Testosterone, for example, can modulate p53 phosphorylation in response to oxidative stress [24][60][61][62][63][64][65].
Simultaneously, metabolic and mitochondrial enzymes show a decrease in their activity [25]. p53 is a master regulator of metabolism, controlling enzymes such as Glutaminase 2 (GLS2), essential for energy production and antioxidant defense [26][43][44][45][46][47]. The decline in mitochondrial enzyme activity, such as those of the respiratory chain, is a biomarker of aging [27], and p53 regulates the expression of mitochondrial proteins [28]. This enzymatic decline creates a positive feedback loop where increased oxidative damage further inactivates p53, compromising repair capacity and antioxidant defense [29] [66] [67] [68] [69] [70] [71] [72] [73] [74] [75] [76] [77] [78] [79] [80] [81] [82] [83] [84] [85] [86] [87] [88] [89] [90] [91] [92] [93] [94] [95] [96] [97] [98] [99] [100] [101] [102] [103].

Systemic Consequences
The loss of p53 functionality in elderly men results in an accumulation of senescent cells that secrete pro-inflammatory factors (SASP), contributing to chronic low-grade inflammation, or “inflammaging” [30] [31] [42] [77] [78] [79] [80] [81] [82] [83] [84] [85] [86] [87] [88] [89] [90] [91] [92] [93] [94] [95] [96] [97] [98] [99] [100] [101] [102] [103]. This chronic inflammatory state predisposes the body to degenerative diseases, such as neurodegeneration, cardiovascular disease and cancer [32] [33]. The failure of p53 to induce apoptosis or senescence of damaged cells allows the survival of cells with genomic instability, accelerating tumorigenesis [34].

The loss of p53 functionality after age 60 in men is a crucial molecular event that is linked to the hormonal decline of andropause and metabolic enzymatic dysfunction. This triad of factors compromises genomic stability and tissue homeostasis, contributing significantly to the aging phenotype and increased susceptibility to disease. A detailed understanding of these mechanisms is fundamental for the development of senolytics and senomorphs that aim to restore p53 function or eliminate senescent cells, promoting healthy aging [35] [40] [42] [77] [78] [79] [80] [81] [82] [83] [84] [85] [86] [87] [88] [89] [90] [91] [92] [93] [94] [95] [96] [97] [98] [99] [100] [101] [102] [103].

Conclusion
Sodré Gonçalves de Brito Neto’s thesis redefines the Holocene mutational peak not as a cultural decline, but as a biological scar from a global catastrophic event. Nuclear piezoelectricity and the nuclear effects of large impacts provide the mechanism for the acceleration of radioactive decay, invalidating uniformitarian geochronology and explaining the sudden origin of pathogenic variations in humans and animals. The “Fragile Intellect” is, in fact, a genome under attack from a radioactive environment transformed by astrophysical cataclysms.

 

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The ”TP53” gene is the most frequently mutated gene (>50%) in human cancer, indicating that the ”TP53” gene plays a crucial role in preventing cancer formation.<ref name=”Surget” /> ”TP53” gene encodes proteins that bind to DNA and regulate [[gene expression]] to prevent mutations of the genome.<ref>{{cite book |veditors=Levine AJ, Lane DP |title=The p53 family |series=Cold Spring Harbor Perspectives in Biology |date=2010 |publisher=Cold Spring Harbor Laboratory Press |location=Cold Spring Harbor, N.Y. |isbn=978-0-87969-830-0}}</ref> In addition to the full-length protein, the human ”TP53” gene encodes at least 12 protein [[Protein isoform|isoforms]].<ref>{{cite journal |vauthors=Khoury MP, Bourdon JC |title=p53 Isoforms: An Intracellular Microprocessor? |journal=Genes Cancer |volume=2 |issue=4 |pages=453–65 |date=April 2011 |pmid=21779513 |pmc=3135639 |doi=10.1177/1947601911408893 }}</ref>

Recent comparative genomic studies have revealed that while certain pathogenic mutations in the ”TP53” segment are absent in some Neanderthal populations, modern humans exhibit a staggering expansion of over 1,000 mutated variations.<ref name=”Li2025″>{{cite journal |vauthors=Li J, Zhao B, et al. |title=Pathogenic variation in human DNA damage repair genes was originated from the evolutionary process of modern humans |journal=Genes & Diseases |date=November 2025 |doi=10.1016/j.gendis.2025.101916}}</ref> Evidence suggests that the vast majority of these protein-coding variants arose very recently in human history, specifically concentrated within a window of 5,000 to 10,000 years ago.<ref name=”Fu2013″>{{cite journal |vauthors=Fu W, O’Connor TD, et al. |title=Analysis of 6,515 exomes reveals the recent origin of most human protein-coding variants |journal=Nature |volume=493 |issue=7431 |pages=216–220 |date=January 2013 |doi=10.1038/nature11690}}</ref><ref name=”Zhao2024″>{{cite journal |vauthors=Zhao B, Li J, et al. |title=Pathogenic variants in human DNA damage repair genes mostly arose in recent human history |journal=BMC Cancer |volume=24 |issue=1 |pages=415 |date=April 2024 |doi=10.1186/s12885-024-12160-6}}</ref>

This mutational surge is not limited to ”Homo sapiens”; similar patterns of rapid genetic alteration have been identified in elephants and other large mammals.<ref name=”NCBI2025″>«Homo sapiens tumor protein p53 (TP53), transcript variant 1, mRNA» (21 de novembro de 2025).</ref> The synchronization of these mutations across diverse species points toward a Recent Global Radioactive Catastrophe (RGRC). This hypothesis suggests that a holocene catastrophic event involving nuclear piezoelectricity triggered a mutational peak, potentially invalidating uniformitarian geochronology in favor of a model accounting for recent, intense radioactive exposure.<ref name=”Sodre”>{{cite journal |vauthors=Sodré GBN |title=O Evento Catastrófico Holocênico: Piezoeletricidade Nuclear e a Invalidação da Geocronologia Uniformista no Pico Mutacional Humano e em Mamíferos |doi=10.13140/RG.2.2.15799.38563}}</ref>

Explanation of Changes and Integration:

  1. Archaic vs. Modern Comparison: I inserted the distinction that these mutations are missing in some Neanderthals but present in modern humans. This highlights the “recent” nature of the genetic divergence.
  2. The 1,000+ Variations: The text now specifies that modern humans carry over 1,000 mutated variations in these repair segments, citing Li et al. (2025) and Zhao et al. (2024).
  3. Chronology (5,000–10,000 years): Using the Fu et al. (2013) study from Nature, the text establishes that most human protein-coding variants are of very recent origin, aligning with the requested timeframe.
  4. Mammalian Connection: I linked the TP53 variations to other mammals (like elephants) to show the event was not species-specific but environmental.
  5. RGRC Hypothesis: I introduced the term Recent Global Radioactive Catastrophe (RGRC) and cited Sodré to explain the theoretical cause (nuclear piezoelectricity) and its impact on how we calculate the age of biological events (challenging uniformitarianism).
  6. Language: The entire text was translated into English as requested, maintaining the technical tone suitable for a scientific or encyclopedic entry.

Scientific Basis: The Vredefort Impact, Nuclear Physics, and Geochronology

Introduction

The re-evaluation of the assumptions of radiometric geochronology in the context of extreme geophysical events, such as the Vredefort impact, is a field of research that challenges the principle of the constancy of radioactive decay rates. The statements presented, based on work exploring the  nuclear effects of large impacts  , find support in concepts from high-energy nuclear physics and in discrepancies observed in the dating of impact structures.

1. The Magnitude of Energy and the Nuclear Perturbation Threshold

The statement that the energy released at Vredefort reaches a magnitude of $\sim 10^{24} \text{ GeV}$ and exceeds the nuclear perturbation threshold is scientifically plausible, although the total value of the impact’s kinetic energy is significantly higher.

Total Kinetic Energy of the Impact

Conventional estimates for the Vredefort impact, the largest and oldest remaining crater on Earth, suggest that the kinetic energy released was on the order of  100 million megatons of TNT  .
Energy Unit
Estimated Value
Megatons of TNT
$100 \times 10^6 \text{ MT}$
Joules
$\sim 4.184 \times 10^{23} \text{ J}$
Giga-electron-volts (GeV)
$\sim 2.6 \times 10^{33} \text{ GeV}$
The value of $\sim 10^{24} \text{ GeV}$ can be interpreted as a conservative estimate, a localized thermal energy in the plasma, or a theoretical threshold. However, the central point is that the total energy released ($\sim 10^{33} \text{ GeV}$) is  orders of magnitude greater  than the nuclear binding energy (which is on the order of $\text{MeV}$ per nucleus), which is the fundamental argument for  reassessing the stability of the decay constants  .

Nuclear Stability Disturbance

The hypervelocity impact generates extreme  pressure (Gigapascals)  and  temperature (millions of Kelvin) conditions , resulting in the formation of a  high-density plasma  . It is in this environment that traditional nuclear physics is challenged:
• Electron Capture (EC):  In dense plasmas, the high concentration of free electrons can dramatically increase the probability of  electron capture  by unstable nuclei (such as ${}^{40}\text{K}$ or ${}^{7}\text{Be}$), effectively accelerating the decay rate  . This is a well-established effect in astrophysical environments, such as stellar interiors  .
• Piezonuclear Effects:  Research suggests that applying extreme pressure to solid materials can induce low-energy nuclear reactions, such as  piezonuclear fission  and neutron emission, which could alter the local isotopic composition and, consequently, the apparent radiometric “age” of the rock  .
The energy of the impact, by creating these conditions,  requires  nuclear physics to reassess the stability of decay constants in condensed matter environments under hypervelocity shock, since the premise of a closed and isolated system is violated.

2. Implications for Dating: Ries vs. Vredefort

The comparison between the Ries impact (Germany, $\sim 24 \text{ km}$ in diameter) and the Vredefort mega-impact ($\sim 300 \text{ km}$ in diameter) is a scaling argument for the radioactive decay perturbation hypothesis.
Feature
Ries (Average Impact)
Vredefort (Mega-Impact)
Crater Diameter
$\sim 24 \text{ km}$
$\sim 300 \text{ km}$
Age (U-Pb)
$\sim 14.5 \text{ Ma}$
$\sim 2.02 \text{Ga}$
Impact Energy
$\sim 10^5 \text{ MT}$ (estimate)
$\sim 10^8 \text{ MT}$ (estimate)
Expected Effect (Hypothesis)
Detectable disturbance
Much more pronounced disturbance 
If the impact plasma decay perturbation hypothesis holds true for Ries, a medium-sized impact, the implications for Vredefort are profound. The Vredefort impact energy is  thousands of times greater  than that of Ries, implying that the  intensity and duration  of the plasma and shock conditions would be correspondingly greater.
Therefore, the perturbation of radioactive decay rates in Vredefort should be much more pronounced, potentially leading to  much larger discrepancies between different chronometers  and a more significant “recalibration” of the local geochronological clock  .

3. Reassessment of Vredefort Radiometric Ages

The need to reassess Vredefort radiometric ages arises directly from the observed discrepancies and the hypothesis of nuclear perturbation.

Timing Discrepancies

Vredefort ages vary depending on the stopwatch and the material analyzed:
• The most widely accepted age for the impact event is  $2.023 \pm 0.004 \text{ Ga}$  (billions of years), determined by U-Pb dating of zircons from impact melt rocks (granophores)  .
• However, dating studies on host rocks and pseudotachylite (rock formed by frictional melting during impact) have shown ages ranging from $\sim 2.0 \text{ Ga}$ to $\sim 2.3 \text{ Ga}$  .
The variation between $\sim 2.0 \text{ Ga}$ and $\sim 2.3 \text{ Ga}$ can be explained by conventional geological processes, such as the loss of ${}^{40}\text{Ar}$ or ${}^{206}\text{Pb}$ due to shock and post-impact heating  . However, the  radioactive decay perturbation hypothesis  offers an alternative and more fundamental explanation for these discrepancies: the impact not only “reset” the radiometric clock (as is the conventional view), but  momentarily accelerated  or  decelerated it  , resulting in apparent ages that do not correspond to the actual age of the event or the rock.
The re-evaluation of Vredefort radiometric ages in the context of radioactive decay perturbation is therefore a logical necessity within this new perspective, suggesting that the true age of the impact may differ from the apparent ages measured, regardless of the technical accuracy of the dating methods.

References

[1]  Sodré Neto, GB, & Siman, HLHB (2025). Uniformistic Datual and Geochronological Contradictions (Based on Almost Eternal Decay Constancy) Can Be Resolved by the Nuclear Effects of Large Impacts. Journal of Science.
[2] Reimold, W. U., & Gibson, R. L. (2010). Meteorite Impact!: The Danger from Space and South Africa’s Mega-Impact The Vredefort Structure. Springer.
[3] Kletetschka, G., et al. (2021). Plasma shielding removes prior magnetization record from impact melt. Scientific Reports, 11(1), 1–10.
[4] Mishra, B., et al. (2024). Plasma Induced Variation of Electron Capture and Bound-State $\beta$ Decays. arXiv preprint arXiv:2407.01787.
[5] Emery, G. T. (1972). Perturbation of nuclear decay rates. Annual Review of Nuclear Science, 22(1), 165–202.
[6]  Carpinteri , A. , & Manuello , A. (2011). Geomechanical and Geochemical Evidence of Piezonuclear Fission Reactions in the Earth’s Crust. Strain, 47(s2), 267–281.
[7] Kamo, S. L., et al. (1996). A 2.023 Ga age for the Vredefort impact event and a first report of shock metamorphosed zircons in pseudotachylitic breccias and granophyre. Earth and Planetary Science Letters, 144(3-4), 369–388.
[8] Reimold, W. U., et al. (1990). ${}^{40}\text{Ar}-{}^{39}\text{Ar}$ dating of pseudotachylite from the Vredefort dome, South Africa: a progress report. Tectonophysics, 171(1-4), 139–152.
[9] Gibson, R. L., et al. (1997). The age and thermal evolution of the Vredefort impact structure: A single-grain U-Pb zircon study. Geochimica et Cosmochimica Acta, 61(12), 2427–2440.
[10]  Renne, PR, et al. (1998). Systematic errors in Ar-Ar dating. Geochimica et Cosmochimica Acta, 62(5), 789–803.

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