Enhanced precipitation has driven the evolution of subtropical evergreen broad‐leaved forests in eastern China since the early Miocene: Evidence from ring‐cupped oaks

IF 3.7
Dong‐Mei Jin, Quan Yuan, Xi‐Ling Dai, Gregor Kozlowski, Yi‐Gang Song
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引用次数: 1

Abstract

Abstract Subtropical evergreen broad‐leaved forest (EBLF) is the predominant vegetation type in eastern China. However, the majority of the region it covers in eastern China was an arid area during the Paleogene. The temporal history and essential factors involved in the evolution of subtropical EBLFs in eastern China remain enigmatic. Here we report on the niche evolution of Quercus section Cyclobalanopsis , which appeared in south China and Japan during the Eocene and became a dominant component of subtropical EBLFs since the Miocene in eastern Asia, using integrative analysis of occurrences, climate data and a dated phylogeny of 35 species in Cyclobalanopsis . Species within clades Cyclobalanoides, Lamellosa, and Helferiana mainly exist in the Himalaya–Hengduan region, adapting to a plateau climate, while species within the other clades mainly live in eastern China under the control of the East Asian monsoon. Reconstructed history showed that significant divergence of climatic tolerance in Cyclobalanopsis began around 19 million years ago (Ma) in the early Miocene. Simultaneously, disparities in precipitation of wettest/warmest quarter and annual precipitation were markedly enhanced in Cyclobalanopsis , especially in the recent eastern clades. During the Miocene, the marked radiation of Cyclobalanopsis and many other dominant taxa of subtropical EBLFs strongly suggest the rapid formation and expansion of subtropical EBLFs in eastern China. Our research highlights that the intensification of the East Asian monsoon and subsequent occupation of new niches by the ancient clades already present in the south may have jointly promoted the formation of subtropical EBLFs in eastern China since the early Miocene.

Abstract Image

中新世早期以来,降水增强推动了中国东部亚热带常绿阔叶林的演变:来自环杯栎树的证据
摘要亚热带常绿阔叶林(EBLF)是中国东部地区的主要植被类型。但其覆盖的中国东部大部分地区在古近纪时期是干旱地区。中国东部亚热带常绿阔叶林演变的时间历史和要素仍然是一个谜。本文通过对35种青冈的发生、气候和系统发育资料的综合分析,对其生态位演化进行了研究。青冈在始新世出现于中国南方和日本,并在中新世以来成为东亚亚热带常绿森林的主要组成部分。Cyclobalanoides、Lamellosa和Helferiana主要分布在喜马拉雅山-横断地区,适应高原气候,其他支系主要分布在中国东部,受东亚季风控制。重建的历史表明,青冈在气候耐受性上的显著分化始于1900万年前的中新世早期。与此同时,青冈最湿/最暖季和年降水量的差异显著增强,特别是在最近的东部支系。中新世期间,青冈等亚热带eblf优势类群的显著辐射表明中国东部亚热带eblf的快速形成和扩展。研究结果表明,早中新世以来,东亚季风的增强和南方已存在的古枝对新生态位的占领可能共同促进了中国东部亚热带eblf的形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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