Museum für Naturkunde, Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, 10115 Berlin, Germany;
Department of Maritime Civilizations, Leon H. Charney School of Marine Science and The Leon Recanati Institute for Maritime Studies, University of Haifa, 3498838 Haifa, Israel.
Proc Natl Acad Sci U S A. 2021 Aug 3;118(31). doi: 10.1073/pnas.2105719118.
Biotic interactions between Africa and Eurasia across the Levant have invoked particular attention among scientists aiming to unravel early human dispersals. However, it remains unclear whether behavioral capacities enabled early modern humans to surpass the Saharo-Arabian deserts or if climatic changes triggered punctuated dispersals out of Africa. Here, we report an unusual subfossil assemblage discovered in a Judean Desert's cliff cave near the Dead Sea and dated to between ∼42,000 and at least 103,000 y ago. Paleogenomic and morphological comparisons indicate that the specimens belong to an extinct subspecies of the eastern African crested rat, subspecies nova, which diverged from the modern eastern African populations in the late Middle Pleistocene ∼226,000 to 165,000 y ago. The reported paleomitogenome is the oldest so far in the Levant, opening the door for future paleoDNA analyses in the region. Species distribution modeling points to the presence of continuous habitat corridors connecting eastern Africa with the Levant during the Last Interglacial ∼129,000 to 116,000 y ago, providing further evidence of the northern ingression of African biomes into Eurasia and reinforcing previous suggestions of the critical role of climate change in Late Pleistocene intercontinental biogeography. Furthermore, our study complements other paleoenvironmental proxies with local-instead of interregional-paleoenvironmental data, opening an unprecedented window into the Dead Sea rift paleolandscape.
非洲和欧亚大陆之间通过黎凡特的生物相互作用引起了科学家们的特别关注,他们旨在解开早期人类扩散的谜团。然而,目前尚不清楚是否是行为能力使早期现代人能够超越撒哈拉-阿拉伯沙漠,还是气候变化引发了非洲以外的间歇性扩散。在这里,我们报告了在死海附近的朱迪亚沙漠悬崖洞穴中发现的一个不寻常的化石组合,其年代可追溯到约 42000 年前至至少 103000 年前。古基因组学和形态比较表明,这些标本属于东非冠毛鼠的一个已灭绝亚种 nova,它在中更新世晚期(约 226000 至 165000 年前)与现代东非种群分化。报告的古线粒体基因组是迄今为止在黎凡特地区发现的最古老的线粒体基因组,为该地区未来的古 DNA 分析开辟了大门。物种分布模型表明,在上一个间冰期(约 129000 至 116000 年前),连接东非和黎凡特的连续栖息地走廊存在,这进一步证明了非洲生物群系向北侵入欧亚大陆,并加强了先前关于气候变化在晚更新世洲际生物地理学中起关键作用的建议。此外,我们的研究用局部而不是区域间的古环境数据补充了其他古环境示踪剂,为死海裂谷古景观打开了一个前所未有的窗口。