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在墨西哥发现水獭化石(食肉目,哺乳纲)解开了古生物地理学上的一个谜团。

Discovery of the fossil otter (Carnivora, Mammalia) in Mexico reconciles a palaeozoogeographic mystery.

作者信息

Tseng Z Jack, Pacheco-Castro Adolfo, Carranza-Castañeda Oscar, Aranda-Gómez José Jorge, Wang Xiaoming, Troncoso Hilda

机构信息

Department of Pathology and Anatomical Sciences, Jacobs School of Medicine and Biomedical Sciences, University at Buffalo, Buffalo, NY 14214, USA

Department of Vertebrate Paleontology, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, USA.

出版信息

Biol Lett. 2017 Jun;13(6). doi: 10.1098/rsbl.2017.0259.

Abstract

The North American fossil otter is thought to be partially convergent in ecological niche with the living sea otter , both having low-crowned crushing teeth and a close association with marine environments. Fossil records of are found in mostly marginal marine deposits in California and Florida; despite presence of very rich records of fossil terrestrial mammals in contemporaneous localities inland, no fossils are hitherto known in interior North America. Here we report the first occurrence of outside of Florida and California, in a land-locked terrestrial mammal fauna of the upper Miocene deposits of Juchipila Basin, Zacatecas State, Mexico. This new occurrence of is at least 200 km from the modern Pacific coastline, and nearly 600 km from the Gulf of Mexico. Besides providing further evidence that was not dependent on coastal marine environments as originally interpreted, this discovery leads us to propose a new east-to-west dispersal route between the Florida and California populations through central Mexico. The proximity of the fossil locality to nearby populations of modern neotropical otters suggests that trans-Mexican freshwater corridors for vertebrate species in riparian habitats may have persisted for a prolonged period of time, pre-dating the Great American Biotic Interchange.

摘要

北美化石水獭在生态位上被认为与现存的海獭部分趋同,二者都有低冠的臼齿且与海洋环境密切相关。其化石记录大多发现于加利福尼亚州和佛罗里达州的边缘海相沉积物中;尽管在内陆同期地点有非常丰富的陆生哺乳动物化石记录,但迄今为止在北美内陆尚未发现其化石。在此,我们报告在墨西哥萨卡特卡斯州胡奇皮拉盆地中新世晚期沉积的内陆陆生哺乳动物群中首次发现了佛罗里达州和加利福尼亚州以外的该物种。这种新发现的物种距离现代太平洋海岸线至少200公里,距离墨西哥湾近600公里。除了进一步证明该物种并不像最初所解释的那样依赖沿海海洋环境外,这一发现还促使我们提出一条新的从东到西的扩散路线,即佛罗里达州和加利福尼亚州的该物种种群通过墨西哥中部扩散。化石地点与附近现代新热带水獭种群的接近表明,河岸栖息地中脊椎动物物种的跨墨西哥淡水走廊可能已经持续了很长一段时间,早于大美洲生物交流。

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