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中国常绿阔叶林成分对晚第四纪气候变化的特殊响应。

Idiosyncratic responses of evergreen broad-leaved forest constituents in China to the late Quaternary climate changes.

作者信息

Fan Dengmei, Hu Wan, Li Bo, Morris Ashley B, Zheng Min, Soltis Douglas E, Soltis Pamela S, Zhang Zhiyong

机构信息

Laboratory of Subtropical Biodiversity, Jiangxi Agricultural University, Nanchang, Jiangxi, 330045, China.

Department of Biology, Middle Tennessee State University, Murfreesboro, TN 37132, Tennessee, USA.

出版信息

Sci Rep. 2016 Aug 18;6:31044. doi: 10.1038/srep31044.

Abstract

Subtropical evergreen broad-leaved forest (EBLF) is one of the most important vegetation types in China. Inferences from palaeo-biome reconstruction (PBR) and phylogeography regarding range shift history of EBLF during the late Quaternary are controversial and should be reconciled. We compared phylogeographic patterns of three EBLF constituents in China, Castanopsis tibetana, Machilus thunbergii and Schima superba. Contrary to a chorus of previous phylogeographic studies and the results of species distribution modelling (SDM) of this study (in situ survival during the LGM), the three species displayed three different phylogeographic patterns that conform to either an in situ survival model or an expansion-contraction model. These results are partially congruent with the inference of PBR that EBLF was absent to the north of 24° N at the LGM. This study suggests that the constituents of EBLF could have responded idiosyncratically to climate changes during the Late Quaternary. The community assemblages of EBLF could have been changing over time, resulting in no palaeo-analogs to modern-day EBLF, which may be the main reason responsible for the failure of PBR to detect the occurrence of EBLF north of 24° N at the LGM.

摘要

亚热带常绿阔叶林是中国最重要的植被类型之一。关于第四纪晚期亚热带常绿阔叶林分布范围变化历史的古生物群落重建和系统地理学推断存在争议,需要进行调和。我们比较了中国亚热带常绿阔叶林的三个组成部分——西藏锥、黑壳楠和木荷的系统地理格局。与之前众多系统地理学研究的结果以及本研究的物种分布模型(末次盛冰期原地生存)结果相反,这三个物种呈现出三种不同的系统地理格局,符合原地生存模型或扩张 - 收缩模型。这些结果与古生物群落重建的推断部分一致,即末次盛冰期时北纬24°以北没有亚热带常绿阔叶林。本研究表明,亚热带常绿阔叶林的组成部分在第四纪晚期可能对气候变化有不同的响应。亚热带常绿阔叶林的群落组合可能随时间发生了变化,导致没有与现代亚热带常绿阔叶林相似的古群落,这可能是古生物群落重建未能检测到末次盛冰期时北纬24°以北存在亚热带常绿阔叶林的主要原因。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa7d/4989166/e27cd59606d2/srep31044-f1.jpg

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