Research Article| May 01, 2017 Extinction selectivity among marine fishes during multistressor global change in the end-Permian and end-Triassic crises Priscilla Vázquez; Priscilla Vázquez 1Department of Earth and Planetary Sciences, University of California, Santa Cruz, California 95064, USA Search for other works by this author on: GSW Google Scholar Matthew E. Clapham Matthew E. Clapham * *E-mail: mclapham@ucsc.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Priscilla Vázquez 1Department of Earth and Planetary Sciences, University of California, Santa Cruz, California 95064, USA Matthew E. Clapham * *E-mail: mclapham@ucsc.edu Publisher: Geological Society of America Received: 26 Aug 2016 Revision Received: 30 Dec 2016 Accepted: 05 Jan 2017 First Online: 28 Jun 2017 Online Issn: 1943-2682 Print Issn: 0091-7613 © 2017 Geological Society of America Geology (2017) 45 (5): 395–398. https://doi.org/10.1130/G38531.1 Article history Received: 26 Aug 2016 Revision Received: 30 Dec 2016 Accepted: 05 Jan 2017 First Online: 28 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Priscilla Vázquez, Matthew E. Clapham; Extinction selectivity among marine fishes during multistressor global change in the end-Permian and end-Triassic crises. Geology 2017;; 45 (5): 395–398. doi: https://doi.org/10.1130/G38531.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Ancient mass extinction events such as the end-Permian and end-Triassic crises provide analogues for multistressor global change of ocean warming, pH reduction, and deoxygenation. Organism physiology is hypothesized to be a key trait influencing vulnerability to these stressors, but it is not certain how physiology predicts survival over evolutionary time scales and when organisms are faced with opposing or synergistic stressors. Fishes (bony fishes and chondrichthyan fishes) are active organisms with high aerobic scope for thermal tolerance and well-developed acid-base regulation, traits that should confer resilience to global change. To test this, we compiled a database of fossil marine fish occurrences to quantify extinction rates during background and mass extinctions from the Permian through Early Jurassic, using maximum likelihood estimation to compare extinction trajectories with marine invertebrates. Our results show that fewer chondrichthyan fishes underwent extinction than marine invertebrates during the end-Permian crisis. End-Triassic chondrichthyan extinction rates also were not elevated above background levels. In contrast, bony fishes underwent an end-Triassic extinction comparable to that of marine invertebrates. The differing responses of these two groups imply that a more active physiology can be advantageous during global change, although not uniformly. Permian–Triassic chondrichthyan fishes may have had broader environmental tolerances, facilitating survival. Alternatively, the larger offspring size of chondrichthyan fishes may provide greater energy reserves to offset the demands of warming and acidification. Although more active organisms have adult adaptations for thermal tolerance and pH regulation, some may nevertheless be susceptible to global change during early life stages. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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