T216 Mass Extinctions as Natural Experiments in Earth System Perturbations I

Wednesday, 18 October 2023
8:00 AM - 12:00 PM
301 / 302

THEORY AND CLASSIFICATION OF MASS EXTINCTIONS

Paper number: T216-3
Program: Technical Sessions
Time: 8:25 AM – 8:40 AM

Authors

  • Thomas Algeo Presenting Author
    University of Cincinnati, Cincinnati, OH
  • Jun Shen
    China University of Geosciences, Wuhan

Abstract

Theory regarding the causation of mass extinctions is in need of systematization. Every mass extinction has both an ultimate cause, i.e., the trigger that leads to various climato-environmental changes, and one or more proximate cause(s), i.e., the specific climato-environmental changes that result in elevated biotic mortality. With regard to ultimate causes, strong cases can be made that bolide impacts, large igneous province eruptions, and bioevolutionary events have each triggered one or more of the Phanerozoic Big Five mass extinctions, whereas other proposed mechanisms (e.g., tectonic forcing, solar flares, gamma bursts, and supernova explosions) remain entirely in the realm of speculation. With regard to proximate mechanisms, most extinctions can be clearly categorized as either carbon-release or carbon-burial events, the former associated with a nexus of climato-environmental changes that include warming, ocean acidification, reduced productivity, and lower carbonate δ13C values, whereas the latter are associated with cooling, increased productivity, and higher carbonate δ13C values. Mass extinction causation can be usefully classified using a matrix of ultimate and proximate factors, in which the end-Cretaceous bolide impact and end-Permian plus end-Triassic large igneous eruptions were carbon-release events, and the Late Ordovician and Late Devonian were carbon-burial events with bioevolutionary triggers (i.e., the spread of non-vascular and vascular land plants, respectively). The Paleoproterozoic and Neoproterozoic also experienced major carbon-burial episodes with bioevolutionary triggers (i.e., spread of oxygenic cyanobacteria and early metazoans, respectively), possibly accompanied by extinctions among existing biotic communities. The impending Sixth Mass Extinction of the Anthropocene will be a carbon-release event with a bioevolutionary trigger (i.e., human technology), thus representing a new type of biocrisis. Theory regarding mass extinction causation has suffered from insufficiently critical thinking: (1) claims of a common ultimate cause for all mass extinctions are suspect given fundamentally different patterns of proximate climato-environmental causation; and (2) the hypothesis of periodicity in extinctions depended on the now-discredited idea of a common extrinsic mechanism (i.e., bolide impacts).

Geological Society of America Abstracts with Programs. Vol. 55, No. 6

doi: 10.1130/abs/2023AM-388510

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