The Permian-Triassic Extinction Event: Causes, Consequences, and Contemporary Relevance

Sirui Shen

doi:10.62051/gs9fsn90

Authors

Sirui Shen

DOI:

https://doi.org/10.62051/gs9fsn90

Keywords:

Permian-Triassic extinction, Mass extinction, Siberian Traps volcanism, Ecosystem recovery, Paleoclimate.

Abstract

This study presents an overview of the Permian-Triassic extinction event — recognized as the most catastrophic biotic crisis that has occurred on Earth. We trace the path of scientific discovery with respect to the timing, scale, and causation of this dual-phased calamity. A comparison is made between its effects on marine and terrestrial ecosystems; note that 96% of all marine species and later 70% of all terrestrial vertebrate species were wiped out during these extinctions. Consider now the intricate weave of environmental maladies — spurred predominantly by Siberian Traps volcanism — which brought forth swift global warming begetting oceanic dead zones along with high acidity levels leading to anoxia on a worldwide scale. An examination of the reasons and repercussions of the PT extinction leads us to make comparisons with present-day anthropogenic climate change and loss of biodiversity, thus underscoring the importance that paleontological investigations have for contemporary environmental challenges. This integration offers hints about ecosystem resilience and vulnerability dynamics which underscore the necessity of differential weighing both the magnitude and rapidity of environmental changes against biological responses toward global perturbations.

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