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Robustness despite uncertainty: regional climate data reveal the dominant role of humans in explaining global extinctions of Late Quaternary megafauna

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TLDR
This paper presented a global analysis of the causes of megafaunal extinction using high-resolution climate reconstructions and explicitly investigated the sensitivity of their results to uncertainty in the palaeological record.
Abstract
Debate over the Late Quaternary megafaunal extinctions has focussed on whether human colonisation or climatic changes were more important drivers of extinction, with few extinctions being unambiguously attributable to either. Most analyses have been geographically or taxonomically restricted and the few quantitative global analyses have been limited by coarse temporal resolution or overly simplified climate reconstructions or proxies. We present a global analysis of the causes of these extinctions which uses high-resolution climate reconstructions and explicitly investigates the sensitivity of our results to uncertainty in the palaeological record. Our results show that human colonisation was the dominant driver of megafaunal extinction across the world but that climatic factors were also important. We identify the geographic regions where future research is likely to have the most impact, with our models reliably predicting extinctions across most of the world, with the notable exception of mainland Asia where we fail to explain the apparently low rate of extinction found in in the fossil record. Our results are highly robust to uncertainties in the palaeological record, and our main conclusions are unlikely to change qualitatively following minor improvements or changes in the dates of extinctions and human colonisation.

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Biodiversity losses and conservation responses in the Anthropocene.

TL;DR: Many examples of conservation success show that losses can be halted and even reversed, and building on these lessons to turn the tide of biodiversity loss will require bold and innovative action to transform historical relationships between human populations and nature.
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Ecological consequences of human niche construction: Examining long-term anthropogenic shaping of global species distributions

TL;DR: This work focuses on four major phases that witnessed broad anthropogenic alterations to biodiversity—the Late Pleistocene global human expansion, the Neolithic spread of agriculture, the era of island colonization, and the emergence of early urbanized societies and commercial networks.
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Megafauna and ecosystem function from the Pleistocene to the Anthropocene

TL;DR: Progress is reviewed in understanding of how megafauna affect ecosystem physical and trophic structure, species composition, biogeochemistry, and climate, drawing on special features of PNAS and Ecography that have been published as a result of an international workshop held in Oxford in 2014.
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The Sixth Mass Extinction: fact, fiction or speculation?

TL;DR: Differences in extinction rates are reviewed according to realms: marine species face significant threats but, although previous mass extinctions were largely defined by marine invertebrates, there is no evidence that the marine biota has reached the same crisis as the non-marine biota, and island species have suffered far greater rates than continental ones.
References
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Journal ArticleDOI

Mammal invaders on islands: impact, control and control impact

TL;DR: It is difficult to predict the outcome of the removal of key species, such as a top predator, given the numerous and complex population interactions among island species, and justifies careful pre‐control study and preparation prior to initiating the eradication of an alien species, in order to avoid an ecological catastrophe.
Journal ArticleDOI

Assessing the Causes of Late Pleistocene Extinctions on the Continents

TL;DR: Evidence now supports the idea that humans contributed to extinction on some continents, but human hunting was not solely responsible for the pattern of extinction everywhere, and suggests that the intersection of human impacts with pronounced climatic change drove the precise timing and geography of extinction in the Northern Hemisphere.
Book

Quaternary extinctions : a prehistoric revolution

TL;DR: Quaternary Extinctions as discussed by the authors presents the latest and most comprehensive examination of these questions and is regarded as a kind of standard encyclopedia for Pleistocene vertebrate paleontology for years to come.
Journal ArticleDOI

The Late Pleistocene Dispersal of Modern Humans in the Americas

TL;DR: Current genetic evidence implies dispersal from a single Siberian population toward the Bering Land Bridge no earlier than about 30,000 years ago, then migration from Beringia to the Americas sometime after 16,500 years ago.
Journal ArticleDOI

Late Quaternary Extinctions: State of the Debate

TL;DR: Results from recent studies suggest that humans precipitated extinction in many parts of the globe through combined direct (hunting) and perhaps indirect (competition, habitat alteration) impacts, but that the timing and geography of extinction might have been different and the worldwide magnitude less, had not climatic change coincided with human impacts in many places.
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