南美洲第四纪晚期历史上潜在的热带间稳定地区

IF 1.9 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
Mário André Trindade Dantas, Thais Rabito Pansani, Lidiane Asevedo, Thaísa Araújo, Lucas de Melo França, Wilcilene Santos de Aragão, Franciely da Silva Santos, Elisa Cravo, Felipe Rodrigues Waldherr, Celso Lira Ximenes
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引用次数: 0

摘要

南美洲是第四纪晚期巨型动物研究的重要古生物学背景。然而,人们对其古生物地理学和古生态学,以及晚更新世/全新世早期巨型动物近期灭绝的原因尚未完全了解。本研究旨在调查南美洲巨型动物的潜在地理分布和历史上的热带间稳定区(HISA)。我们利用古物种分布模型为 12 个巨型动物分类群(11 种食草动物和 1 种食肉动物)绘制了第四纪晚期间冰期和冰川期的地图:120 ka 和 21 ka。我们的模型以及同位素数据显示,HSIAs 主要发生在低海拔平原(<1000 米),并与季节性干旱森林生物群落相叠加。我们提出了两个 HSIA:西热带地区和巴西热带地区,后者是重新定义的。我们认为巴西热带地区比以前提出的要小得多,但仍然是晚更新世南美洲巨型动物的一个重要动物地理区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Potential historically intertropical stable areas during the Late Quaternary of South America
South America is a pivotal paleontological setting for Late Quaternary megafaunal research. Nonetheless, its paleobiogeography and paleoecology, and the causes for the recent extinction of megafauna in the Late Pleistocene/Early Holocene are not yet fully understood. This study aimed to investigate the potential geographical distribution and historically intertropical stable areas (HISAs) of South American megafauna. We generated maps using Paleo‐Species Distribution Models for 12 megafaunal taxa (11 herbivores and one carnivore) during interglacial and glacial periods in the Late Quaternary: 120 and 21 ka. Our models, together with isotopic data, show that the HSIAs occurred mainly in low‐altitude plains (<1000 m) and were superimposed on seasonal dry forest biomes. We propose the occurrence of two HSIAs: the West Intertropical Region and the Brazilian Intertropical Region, the latter being redefined. We suggest that the Brazilian Intertropical Region is much smaller than previously proposed, but was still a key zoogeographical region for megafauna in South America during the Late Pleistocene.
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来源期刊
Journal of Quaternary Science
Journal of Quaternary Science 地学-地球科学综合
CiteScore
4.70
自引率
8.70%
发文量
82
审稿时长
6-12 weeks
期刊介绍: The Journal of Quaternary Science publishes original papers on any field of Quaternary research, and aims to promote a wider appreciation and deeper understanding of the earth''s history during the last 2.58 million years. Papers from a wide range of disciplines appear in JQS including, for example, Archaeology, Botany, Climatology, Geochemistry, Geochronology, Geology, Geomorphology, Geophysics, Glaciology, Limnology, Oceanography, Palaeoceanography, Palaeoclimatology, Palaeoecology, Palaeontology, Soil Science and Zoology. The journal particularly welcomes papers reporting the results of interdisciplinary or multidisciplinary research which are of wide international interest to Quaternary scientists. Short communications and correspondence relating to views and information contained in JQS may also be considered for publication.
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