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质体系统发育基因组学为兰科植物的系统学、多样化及生物地理学提供了新的见解。

Plastid phylogenomics provides new insights into the systematics, diversification, and biogeography of (Orchidaceae).

作者信息

Chen Hai-Yao, Zhang Zhi-Rong, Yao Xin, Ya Ji-Dong, Jin Xiao-Hua, Wang Lin, Lu Lu, Li De-Zhu, Yang Jun-Bo, Yu Wen-Bin

机构信息

Center for Integrative Conservation & Yunnan Key Laboratory for the Conservation of Tropical Rainforests and Asian Elephants, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, Yunnan 666303, China.

University of Chinese Academy of Sciences, Huairou District, Beijing 101408, China.

出版信息

Plant Divers. 2024 Mar 12;46(4):448-461. doi: 10.1016/j.pld.2024.03.001. eCollection 2024 Jul.

DOI:10.1016/j.pld.2024.03.001
PMID:39280966
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11390606/
Abstract

(Orchidaceae: Epidendroideae), with around 60 species, is widely-distributed across Southeast Asia, providing a nice system for studying the processes that underlie patterns of biodiversity in the region. However, phylogenetic relationships of have not been well resolved, hampering investigations of species diversification and the biogeographical history of this genus. In this study, we construct a plastome phylogeny of 56 species, with four well-resolved major clades, which provides a framework for biogeographical and diversification rate analyses. Molecular dating and biogeographical analyses show that likely originated in the region spanning northern Indo-Burma to the eastern Himalayas during the early Miocene (∼21.10 Ma). It then rapidly diversified into four major clades in East Asia within approximately a million years during the middle Miocene. spp. migration to the adjacent regions (Borneo, Philippines, and Sulawesi) primarily occurred during the Pliocene-Pleistocene period. Our analyses indicate that the net diversification rate of has decreased since its origin, and is positively associated with changes in temperature and monsoon intensity. Favorable hydrothermal conditions brought by monsoon intensification in the early Miocene possibly contributed to the initial rapid diversification, after which the net diversification rate was reduced with the cooling climate after the middle Miocene. The transition from epiphytic to terrestrial habits may have enabled adaptation to cooler environments and colonization of northern niches, yet without a significant effect on diversification rates. This study provides new insights into how monsoon activity and temperature changes affected the diversification dynamics of plants in Southeast Asia.

摘要

(兰科:树兰亚科),约有60个物种,广泛分布于东南亚,为研究该地区生物多样性模式背后的过程提供了一个良好的系统。然而,该属的系统发育关系尚未得到很好的解决,这阻碍了对物种多样化和该属生物地理历史的研究。在本研究中,我们构建了56个物种的质体基因组系统发育树,有四个得到很好解决的主要分支,这为生物地理和多样化速率分析提供了一个框架。分子定年和生物地理分析表明,该属可能在中新世早期(约2110万年前)起源于印度 - 缅甸北部至东喜马拉雅地区。然后在中新世中期的大约一百万年时间里迅速在东亚分化为四个主要分支。该属物种向邻近地区(婆罗洲、菲律宾和苏拉威西岛)的迁移主要发生在上新世 - 更新世时期。我们的分析表明,该属自起源以来净多样化速率已经下降,并且与温度和季风强度的变化呈正相关。中新世早期季风增强带来的有利水热条件可能促成了最初的快速多样化,在此之后,随着中新世中期之后气候变冷,净多样化速率降低。从附生习性向地生习性的转变可能使该属能够适应更凉爽的环境并在北部生态位定殖,但对多样化速率没有显著影响。本研究为季风活动和温度变化如何影响东南亚植物的多样化动态提供了新的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/70d6a640a97f/figs8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/e86409ca6bca/gr1.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/059d99747ca8/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/7fa7a6903924/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/fd32bdb5e894/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/830dc331b4f6/figs1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/f73faa994ccd/figs2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/f542f435f5dc/figs3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/19a348642e2d/figs4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/756b70b2ca0f/figs5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/3a14edafe7a3/figs6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/e9d15005b1bc/figs7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/70d6a640a97f/figs8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/e86409ca6bca/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/299c4de86cbd/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/059d99747ca8/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/7fa7a6903924/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/fd32bdb5e894/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/830dc331b4f6/figs1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/f73faa994ccd/figs2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/f542f435f5dc/figs3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/19a348642e2d/figs4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/756b70b2ca0f/figs5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/3a14edafe7a3/figs6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/e9d15005b1bc/figs7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2567/11390606/70d6a640a97f/figs8.jpg

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