The Equus Datum and the Early Radiation of Equus in China

To approach a comprehensive understanding of the Equus Datum, we summarize the history of the study of Chinese fossil equids, from the “dragon bones” stage to scientific investigation, by Chinese, European and American people, and then review the stenonid species in China and discuss the phylogeneti...

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Main Authors: Boyang Sun, Tao Deng
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-11-01
Series:Frontiers in Ecology and Evolution
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fevo.2019.00429/full
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author Boyang Sun
Boyang Sun
Tao Deng
Tao Deng
Tao Deng
author_facet Boyang Sun
Boyang Sun
Tao Deng
Tao Deng
Tao Deng
author_sort Boyang Sun
collection DOAJ
description To approach a comprehensive understanding of the Equus Datum, we summarize the history of the study of Chinese fossil equids, from the “dragon bones” stage to scientific investigation, by Chinese, European and American people, and then review the stenonid species in China and discuss the phylogenetic relationships of early Equus. We conclude that there were at least two dispersal waves of Equus into the Old World from North America, and the second wave led to a radiation of the genus Equus in China. In China, the ages of the lower boundaries of the fossiliferous layers in classical Early Pleistocene faunal localities are all around 2.5 Ma (close to the age of the lower boundary of the Quaternary) according to magnetostratigraphic and biostratigraphic analyses. All of the geochronological results reveal China as an evolutionary center of Equus in Eurasia. In the late Neogene, the dominant equid lineage in China was Hipparionini. Even in the Pliocene, when hipparionines were not as widespread as before, there were still 5 genera and 7 species. In the Early Pleistocene, the hipparionines included only 2 genera and 2 species. In the meantime, global cooling caused Arctic ice sheets to form, lowering the sea level so that the Bering land bridge fell dry and allowed Equus to disperse into China. The rise of Equus was accompanied by the recession of hipparionines. The dispersal and radiation of Equus in China were not a coincidence, but a complicated process of adaptation and competition, and a comprehensive outcome of significant climatic, tectonic and biotic events.
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spelling doaj.art-643c8c9addc144b4a4d40b3f6a92c1ff2022-12-22T02:07:21ZengFrontiers Media S.A.Frontiers in Ecology and Evolution2296-701X2019-11-01710.3389/fevo.2019.00429451220The Equus Datum and the Early Radiation of Equus in ChinaBoyang Sun0Boyang Sun1Tao Deng2Tao Deng3Tao Deng4Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, ChinaCAS Center for Excellence in Life and Paleoenvironment, Beijing, ChinaKey Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, ChinaCAS Center for Excellence in Life and Paleoenvironment, Beijing, ChinaUniversity of Chinese Academy of Sciences, Beijing, ChinaTo approach a comprehensive understanding of the Equus Datum, we summarize the history of the study of Chinese fossil equids, from the “dragon bones” stage to scientific investigation, by Chinese, European and American people, and then review the stenonid species in China and discuss the phylogenetic relationships of early Equus. We conclude that there were at least two dispersal waves of Equus into the Old World from North America, and the second wave led to a radiation of the genus Equus in China. In China, the ages of the lower boundaries of the fossiliferous layers in classical Early Pleistocene faunal localities are all around 2.5 Ma (close to the age of the lower boundary of the Quaternary) according to magnetostratigraphic and biostratigraphic analyses. All of the geochronological results reveal China as an evolutionary center of Equus in Eurasia. In the late Neogene, the dominant equid lineage in China was Hipparionini. Even in the Pliocene, when hipparionines were not as widespread as before, there were still 5 genera and 7 species. In the Early Pleistocene, the hipparionines included only 2 genera and 2 species. In the meantime, global cooling caused Arctic ice sheets to form, lowering the sea level so that the Bering land bridge fell dry and allowed Equus to disperse into China. The rise of Equus was accompanied by the recession of hipparionines. The dispersal and radiation of Equus in China were not a coincidence, but a complicated process of adaptation and competition, and a comprehensive outcome of significant climatic, tectonic and biotic events.https://www.frontiersin.org/article/10.3389/fevo.2019.00429/fullEquus Datumstenonidevolutionenvironment changepaleozoogeography
spellingShingle Boyang Sun
Boyang Sun
Tao Deng
Tao Deng
Tao Deng
The Equus Datum and the Early Radiation of Equus in China
Frontiers in Ecology and Evolution
Equus Datum
stenonid
evolution
environment change
paleozoogeography
title The Equus Datum and the Early Radiation of Equus in China
title_full The Equus Datum and the Early Radiation of Equus in China
title_fullStr The Equus Datum and the Early Radiation of Equus in China
title_full_unstemmed The Equus Datum and the Early Radiation of Equus in China
title_short The Equus Datum and the Early Radiation of Equus in China
title_sort equus datum and the early radiation of equus in china
topic Equus Datum
stenonid
evolution
environment change
paleozoogeography
url https://www.frontiersin.org/article/10.3389/fevo.2019.00429/full
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