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过去 600 万年人类进化过程中,东非大裂谷系统长期的生物同质化。

Long-term biotic homogenization in the East African Rift System over the last 6 million years of hominin evolution.

机构信息

Department of Archaeology, University of Cambridge, Cambridge, UK.

Department of Anthropology and Geography, Colorado State University, Fort Collins, CO, USA.

出版信息

Nat Ecol Evol. 2024 Sep;8(9):1751-1759. doi: 10.1038/s41559-024-02462-0. Epub 2024 Jul 15.

Abstract

Eastern Africa preserves the most complete record of human evolution anywhere in the world but we have little knowledge of how long-term biogeographic dynamics in the region influenced hominin diversity and distributions. Here, we use spatial beta diversity analyses of mammal fossil records from the East African Rift System to reveal long-term biotic homogenization (increasing compositional similarity of faunas) over the last 6 Myr. Late Miocene and Pliocene faunas (~6-3 million years ago (Ma)) were largely composed of endemic species, with the shift towards biotic homogenization after ~3 Ma being driven by the loss of endemic species across functional groups and a growing number of shared grazing species. This major biogeographic transition closely tracks the regional expansion of grass-dominated ecosystems. Although grazers exhibit low beta diversity in open environments of the Early Pleistocene, the high beta diversity of Mio-Pliocene browsers and frugivores occurred in the context of extensive woody vegetation. We identify other key aspects of the Late Cenozoic biogeographic development of eastern Africa, their likely drivers and place the hominin fossil record in this context. Because hominins were undoubtedly influenced by many of the same factors as other eastern African mammals, this provides a new perspective on the links between environmental and human evolutionary histories.

摘要

东非保留了世界上最完整的人类进化记录,但我们对该地区长期的生物地理动态如何影响人类多样性和分布知之甚少。在这里,我们使用东非裂谷系统哺乳动物化石记录的空间β多样性分析来揭示过去 600 万年以来长期的生物同质性(动物群组成相似性增加)。中新世晚期和上新世(约 600 万至 300 万年前)的动物群主要由特有物种组成,而大约 300 万年前以来的生物同质性的转变是由功能群中特有物种的丧失以及越来越多的共同食草物种驱动的。这一主要的生物地理转变与以草为主导的生态系统在该地区的扩张密切相关。尽管食草动物在更新世早期开阔环境中的β多样性较低,但中新世浏览者和食果者的高β多样性是在广泛的木质植被背景下发生的。我们确定了东非晚新生代生物地理发展的其他关键方面、它们的可能驱动因素,并将人类化石记录置于这一背景下。因为人类无疑受到了与其他东非哺乳动物相同的许多因素的影响,所以这为环境和人类进化史之间的联系提供了一个新的视角。

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