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Is the East Asian flora ancient or not?

Authors :
Chen, Yong-Sheng
Deng, Tao
Zhou, Zhuo
Sun, Hang
Source :
National Science Review; Nov2018, Vol. 5 Issue 6, p920-932, 13p
Publication Year :
2018

Abstract

The East Asian flora (EAF) is a key biodiversity hotspot for understanding the origin and evolution of Northern Hemisphere floras, but there is an ongoing debate on whether it is a museum or a cradle for seed plants. Within the EAF, two main floras, the Sino-Himalayan Flora (mainly the Rhododendron Flora) and the Sino-Japanese Flora (mainly the Metasequoia Flora), have been recognized. Previous studies suggested that the EAF is ancient and the Metasequoia Flora is older than the Rhododendron Flora. To test this hypothesis, we synthesized molecular as well as fossil data on seed plants, focusing on the biogeographical origins and historical evolution of the EAF. We compared the ages of its two constituent floras, and examined the impact of the Asian monsoon and other environmental changes on the development of EAF through meta-analysis. Our results suggest that the EAF might be relatively young, with most of its clades originating since the Miocene. The Rhododendron Flora and the Metasequoia Flora are probably of a similar age. The formation and development of the Asian monsoon might have been the main factors that have driven the evolution of EAF. In the Rhododendron Flora, the north-south mountain chains increased the concentration of species and reduced extinction, and the barriers between the east and west have resulted in species differentiation, which triggered it to become a diversity center. The EAF appears to have multiple biogeographical origins, having closely affiliated not only with other floras in the Northern Hemisphere, but also with Gondwanan floras. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
20955138
Volume :
5
Issue :
6
Database :
Complementary Index
Journal :
National Science Review
Publication Type :
Academic Journal
Accession number :
133953713
Full Text :
https://doi.org/10.1093/nsr/nwx156