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14.5 万至 3 万年前的旧石器时代晚期欧洲西部尼安德特人的生态位空间。

The Neanderthal niche space of Western Eurasia 145 ka to 30 ka ago.

机构信息

Department of Archeology and Heritage Studies, School of Culture and Society, Aarhus University, Moesgård Allé 20, Building 4216, 8270, Højbjerg, Denmark.

Center for Ecological Dynamics in a Novel Biosphere, Department of Biology, Aarhus University, Ny Munkegade 114-116, 8000, Aarhus C, Denmark.

出版信息

Sci Rep. 2024 Apr 2;14(1):7788. doi: 10.1038/s41598-024-57490-4.

Abstract

Neanderthals occupied Western Eurasia between 350 ka and 40 ka ago, during the climatically volatile Pleistocene. A key issue is to what extent Neanderthal populations expanded into areas of Western Eurasia and what conditions facilitated such range expansions. The range extent of Neanderthals is generally based on the distribution of Neanderthal material, but the land-altering nature of glacial periods has erased much of the already sparse material evidence of Neanderthals, particularly in the northern latitudes. To overcome this obstacle species distribution models can estimate past distributions of Neanderthals, however, most implementations are generally constrained spatially and temporally and may be artificially truncating the Neanderthal niche space. Using dated contexts from Neanderthal sites from across Western Eurasia, millennial-scale paleoclimate reconstructions, and a spatiotemporal species distribution model, we infer the fundamental climatic niche space of Neanderthals and estimate the extent of Neanderthal occupation. We find that (a.) despite the long timeframe, Neanderthals occupy a relatively narrow fundamental climatic niche space, (b.) the estimated projected potential Neanderthal niche space suggests a larger geographic range than the material record suggests, and (c.) that there was a general decline in the size of the projected potential Neanderthal niche from 145 ka ago onward, possibly contributing to their extinction.

摘要

尼安德特人在 35 万至 4 万年前的更新世气候动荡期间占据了西欧。一个关键问题是尼安德特人的种群在多大程度上扩展到了西欧地区,以及哪些条件促进了这种范围的扩展。尼安德特人的分布范围通常基于尼安德特人物质的分布,但冰川期改变地貌的性质抹去了尼安德特人本就稀少的物质证据的大部分,特别是在北纬地区。为了克服这一障碍,可以使用物种分布模型来估计尼安德特人过去的分布情况,但是,大多数实现方式在空间和时间上通常受到限制,并且可能会人为地截断尼安德特人的生态位空间。利用来自西欧各地尼安德特人遗址的有日期上下文、千年尺度的古气候重建和时空物种分布模型,我们推断了尼安德特人的基本气候生态位空间,并估计了尼安德特人居住的范围。我们发现:(a.)尽管时间跨度很长,但尼安德特人占据了相对狭窄的基本气候生态位空间;(b.)估计的潜在尼安德特人生态位空间表明其地理范围比物质记录所表明的要大;(c.)自 14.5 万年前以来,潜在尼安德特人生态位的预测规模普遍下降,这可能导致了他们的灭绝。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0943/10987600/db52ea8ef7c9/41598_2024_57490_Fig1_HTML.jpg

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