2020
DOI: 10.1111/jse.12640
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A unique record of Cercis from the late early Miocene of interior Asia and its significance for paleoenvironments and paleophytogeography

Abstract: The climatic impacts of the Tibetan Plateau since the Neogene and the phytogeographic pattern changes of formerly widely‐distributed forest communities on the plateau remain poorly constrained. Today, Cercis L. (Fabaceae) is a well‐known arborescent genus typically distributed in subtropical to warm temperate zones of the Northern Hemisphere, and Paleogene fossil occurrences from Eurasia and North America show a long history of the genus in mid‐low latitudes of the Northern Hemisphere. Here, we describe a foss… Show more

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Cited by 10 publications
(4 citation statements)
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“…The landscape plant Cercis chinensis Bunge is a member of the Leguminosae family and is native to China and is known for its pink or milky white flowers in April, fruit in October, and almost circular leaf shape [1] . Apart from its ornamental role, it can also be seen as a botanical plant for nectar.…”
Section: Introductionmentioning
confidence: 99%
“…The landscape plant Cercis chinensis Bunge is a member of the Leguminosae family and is native to China and is known for its pink or milky white flowers in April, fruit in October, and almost circular leaf shape [1] . Apart from its ornamental role, it can also be seen as a botanical plant for nectar.…”
Section: Introductionmentioning
confidence: 99%
“…According to X.-C. Li et al (2021), the centre of origin and further distribution of the genus Cercis L. are sub-tropical climate zones and southern warm temperate climates in Asia, southern Europe, and the southwestern United States. And the Paleogene fossils from Eurasia and North America indicate a long history of the genus.…”
Section: Discussionmentioning
confidence: 99%
“…Additionally, the elevation of the Zeku Basin (see Fig. 1 for location, present day elevation 3440 to 4300 m asl) during the Middle Miocene is speculated to have been 1200 to 1400 m asl ( 51 ) or <2400 m asl ( 52 ). Combining this evidence, we conclude that the basins in the NTP were at lower elevations before the Late Miocene and were then intensely uplifted until 8 to 6 Ma.…”
Section: Rise Of the Ntpmentioning
confidence: 99%