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The Quaternary megafaunal extinction and the fate of Neanderthals: An integrative working hypothesis

机译:第四纪大型动物灭绝与尼安德特人的命运:一个综合的工作假设

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摘要

The last great extinction that has happened throughout the Earth's life history (the Quaternary Megafaunal Extinction) exterminated more than 178 species of the world's largest mammals. Different hypotheses to explain this extinction have been proposed, from environmental catastrophes to predator avoidance, or even volcanic activity and meteorite impact. Currently, many researchers see the Sixth Extinction as a total or partial result of past climatic changes. The mechanism of Neanderthal extinction is a controversial issue of broad interest among human palaeontologists and evolutionary biologists. This paper presents an integrative working hypothesis to elucidate this extinction, based on their killing/ predation as habitual part of the competition strategy of anatomically modern humans, and in the context of the wider Quaternary Megafaunal Extinction. Following this working hypothesis, Neanderthal extinction should be seen as being a mere branch of the Quaternary Megafaunal Extinction. The ecologically K early Homo sapiens would exterminate other K species, most of them megafauna, including the medium-sized non-sapiens human species. Neanderthals were part of the large mammal prey potentially hunted by our species, in the same way that historically orang-utans, gorillas and chimpanzees still are. Most probably, the same happened whenever a technologically more evolved Homo species overlapped with other less technologically evolved one.
机译:整个地球生命历史上发生的最后一次大灭绝(第四纪巨型动物灭绝)消灭了世界上最大的178种以上的哺乳动物。从环境灾难到避免捕食者,甚至火山活动和陨石撞击,已经提出了不同的假设来解释这种灭绝。目前,许多研究人员将第六次灭绝视为过去气候变化的全部或部分结果。尼安德特人灭绝的机制是人类古生物学家和进化生物学家广泛关注的一个有争议的问题。本文提出了一个综合的工作假说来阐明这种灭绝,这是基于它们作为解剖学现代人类竞争策略的惯性部分的杀灭/捕食,以及在更广泛的第四纪大型动物灭绝的背景下提出的。根据这一可行的假设,尼安德特人的灭绝应被视为第四纪巨型动物灭绝的一个分支。具有生态学意义的K早期智人将消灭其他K物种,其中大多数是大型动物,包括中等大小的非人类物种。尼安德特人是我们物种可能猎取的大型哺乳动物猎物的一部分,与历史上的猩猩,大猩猩和黑猩猩一样。每当技术进化程度更高的人类物种与其他技术进化程度更低的人类重叠时,同样可能发生。

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  • 来源
    《Quaternary International》 |2013年第8期|69-72|共4页
  • 作者单位

    Area de Prehistoria, Universitat Rovira i Virgili (URV), Tarragona, Catalonia, Spain,Instirut Catala de Paleoecologia Humana i Evolucio Social (IPHES), Placa de la Imperial Tarraco 1, ES-43005 Tarragona, Catalonia, Spain;

    Institudo Catalana de Recerca i Estudis Avancats (ICREA), Barcelona. Catalonia, Spain,Area de Prehistoria, Universitat Rovira i Virgili (URV), Tarragona, Catalonia, Spain,Instirut Catala de Paleoecologia Humana i Evolucio Social (IPHES), Placa de la Imperial Tarraco 1, ES-43005 Tarragona, Catalonia, Spain;

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