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Global late Quaternary megafauna extinctions linked to humans, not climate change

机译:全球第四纪晚期大型动物灭绝与人类有关,与气候变化无关

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摘要

The late Quaternary megafauna extinction was a severe global-scale event. Two factors, climate change and modern humans, have received broad support as the primary drivers, but their absolute and relative importance remains controversial. To date, focus has been on the extinction chronology of individual or small groups of species, specific geographical regions or macroscale studies at very coarse geographical and taxonomic resolution, limiting the possibility of adequately testing the proposed hypotheses. We present, to our knowledge, the first global analysis of this extinction based on comprehensive country-level data on the geographical distribution of all large mammal species (more than or equal to 10 kg) that have gone globally or continentally extinct between the beginning of the Last Interglacíal at ? 132 000 years BP and the late Holocene 1000 years BP, testing the relative roles played by glacial-inte?glacial climate change and humans. We show that the seventy of extinction is strongly tied to hominin palaeobiogeogra-phy, with at most a weak, Eurasia-specific link to climate change. This first pecies-leve macroscale analysis at relatively high geographical resol-ution provides strong support for modern humans as the primary driver of the worldwide megafauna losses during the late Quaternary.
机译:第四纪晚期大型动物灭绝是一个严重的全球性事件。气候变化和现代人类这两个因素已得到广泛支持,成为主要驱动力,但它们的绝对和相对重要性仍存在争议。迄今为止,关注点已集中在非常粗糙的地理和分类学分辨率上的单个或小组物种,特定地理区域或宏观研究的灭绝时间,限制了充分检验所提出的假设的可能性。据我们所知,本次灭绝是首次全球性分析,它是根据国家级综合数据得出的,而该数据是自全球人类灭绝之初至全球灭绝的所有大型哺乳动物(大于或等于10千克)的地理分布的。最后的冰川在? 132 000年BP和全新世1000年BP,测试了冰河间气候变化和人类之间的相对作用。我们表明,灭绝的七十年代与人参古生物地理学密切相关,至多与气候变化至多与欧亚大陆无关。这是在相对较高的地理分辨率下进行的第一个小规模水平的宏观分析,为现代人类提供了有力的支持,因为现代人类是第四纪后期世界范围内大型动物丧失的主要推动力。

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