The theory that Earth's history includes mass extinctions is supported by several lines of scientific evidence:
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Fossil Record: The fossil record provides clear evidence of mass extinction events, marked by abrupt changes in biodiversity. For example, the fossil layers indicate a sharp decline in the number of species during events like the Permian-Triassic extinction, which saw around 90-96% of marine species disappear.
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Geological Stratigraphy: Geologists have identified distinct boundaries in the Earth's strata, known as boundary layers, that coincide with mass extinction events. The K-T boundary, for example, marks the transition between the Cretaceous and Paleogene periods and is associated with the extinction of the dinosaurs, coinciding with a layer enriched in iridium, which is rare on Earth but more common in asteroids.
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Isotope Analysis: Studies of stable and radioactive isotopes in sedimentary rocks help scientists understand changes in climate and ecology during mass extinctions. For instance, fluctuations in carbon isotopes indicate significant shifts in the carbon cycle during extinction events.
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Global Climate Change Evidence: During many mass extinctions, there is evidence of significant climate change, including increased volcanic activity, drastic shifts in temperature, and ocean anoxia (lack of oxygen in ocean waters), which are linked to both the Permian-Triassic and Cretaceous-Paleogene extinctions.
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Paleobiogeography: The distribution of fossil organisms across different continents supports the idea of mass extinctions. The presence of similar species in widely separated geographic areas before an extinction event suggests a once common distribution that was drastically reduced.
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Impact Evidence: For the K-Pg extinction (formerly known as the K-T boundary), the discovery of the Chicxulub crater in Mexico provided compelling evidence of a massive asteroid impact, which is widely believed to have contributed to the extinction of the dinosaurs and many other species.
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Mathematical Models: Some researchers have applied mathematical models to extinction data, showing that extinction rates correlate with environmental changes over geological time scales, suggesting that certain thresholds lead to mass extinction events.
Collectively, these pieces of evidence confirm the occurrence of mass extinction events in Earth's history and help scientists understand the causes and consequences of these dramatic biological turnover events.