Literature DB >> 33168739

Overkill, glacial history, and the extinction of North America's Ice Age megafauna.

David J Meltzer1.   

Abstract

The end of the Pleistocene in North America saw the extinction of 38 genera of mostly large mammals. As their disappearance seemingly coincided with the arrival of people in the Americas, their extinction is often attributed to human overkill, notwithstanding a dearth of archaeological evidence of human predation. Moreover, this period saw the extinction of other species, along with significant changes in many surviving taxa, suggesting a broader cause, notably, the ecological upheaval that occurred as Earth shifted from a glacial to an interglacial climate. But, overkill advocates ask, if extinctions were due to climate changes, why did these large mammals survive previous glacial-interglacial transitions, only to vanish at the one when human hunters were present? This question rests on two assumptions: that previous glacial-interglacial transitions were similar to the end of the Pleistocene, and that the large mammal genera survived unchanged over multiple such cycles. Neither is demonstrably correct. Resolving the cause of large mammal extinctions requires greater knowledge of individual species' histories and their adaptive tolerances, a fuller understanding of how past climatic and ecological changes impacted those animals and their biotic communities, and what changes occurred at the Pleistocene-Holocene boundary that might have led to those genera going extinct at that time. Then we will be able to ascertain whether the sole ecologically significant difference between previous glacial-interglacial transitions and the very last one was a human presence.

Entities:  

Keywords:  North America; Pleistocene extinctions; glacial−interglacial climate change; human overkill; megafauna

Mesh:

Year:  2020        PMID: 33168739      PMCID: PMC7682371          DOI: 10.1073/pnas.2015032117

Source DB:  PubMed          Journal:  Proc Natl Acad Sci U S A        ISSN: 0027-8424            Impact factor:   11.205


  35 in total

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Journal:  Nature       Date:  2010-05-23       Impact factor: 49.962

6.  Fossil and genomic evidence constrains the timing of bison arrival in North America.

Authors:  Duane Froese; Mathias Stiller; Peter D Heintzman; Alberto V Reyes; Grant D Zazula; André E R Soares; Matthias Meyer; Elizabeth Hall; Britta J L Jensen; Lee J Arnold; Ross D E MacPhee; Beth Shapiro
Journal:  Proc Natl Acad Sci U S A       Date:  2017-03-13       Impact factor: 11.205

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Journal:  Nature       Date:  2014-02-06       Impact factor: 49.962

8.  A new genus of horse from Pleistocene North America.

Authors:  Peter D Heintzman; Grant D Zazula; Ross DE MacPhee; Eric Scott; James A Cahill; Brianna K McHorse; Joshua D Kapp; Mathias Stiller; Matthew J Wooller; Ludovic Orlando; John Southon; Duane G Froese; Beth Shapiro
Journal:  Elife       Date:  2017-11-28       Impact factor: 8.140

9.  Ancient environmental DNA reveals shifts in dominant mutualisms during the late Quaternary.

Authors:  Martin Zobel; John Davison; Mary E Edwards; Christian Brochmann; Eric Coissac; Pierre Taberlet; Eske Willerslev; Mari Moora
Journal:  Nat Commun       Date:  2018-01-10       Impact factor: 14.919

10.  Climate-driven ecological stability as a globally shared cause of Late Quaternary megafaunal extinctions: the Plaids and Stripes Hypothesis.

Authors:  Daniel H Mann; Pamela Groves; Benjamin V Gaglioti; Beth A Shapiro
Journal:  Biol Rev Camb Philos Soc       Date:  2018-08-22
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2.  Late Pleistocene shrub expansion preceded megafauna turnover and extinctions in eastern Beringia.

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5.  Small brains predisposed Late Quaternary mammals to extinction.

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  5 in total

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