チベット高原固有植物の進化と時間軸を解明(Scientists Reveal Timeline and Uneven Evolution of Endemic Flora on Qinghai-Tibet Plateau)

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2025-06-24 中国科学院(CAS)

チベット高原固有植物の進化と時間軸を解明(Scientists Reveal Timeline and Uneven Evolution of Endemic Flora on Qinghai-Tibet Plateau)

Topographic map of the Qinghai-Tibet Plateau and representative plants (Image by IBCAS)

中国科学院植物研究所の王偉教授率いる研究チームは、青蔵高原(QTP)の固有植物相の進化過程を明らかにし、その起源が従来の想定よりもはるかに古い始新世初期に遡ることを発見した。QTPは3つのサブ地域(高原平台部、ヒマラヤ、横断山脈)から成り、世界有数の温帯生物多様性を誇る。本研究では、QTP固有の82属1740種にわたる37系統を分析し、標高差と生態的ニッチの分化が植物の固有化を駆動したことを示した。特に横断山脈は最古の固有系統を抱える「多様性の源」として重要であり、保全上の優先地域として注目される。研究成果は、地域ごとに異なる地質・気候変動が植物進化に与える影響を浮き彫りにした。

<関連情報>

新生代の地質気候変動が青海チベット高原の固有植物の進化動態を動かした Cenozoic geoclimatic changes drove the evolutionary dynamics of floristic endemism on the Qinghai–Tibet Plateau

Guan-Long Cao, Xiao-Qian Li, Jun Zhang, +7 , and Wei Wang
Proceedings of the National Academy of Sciences  Published:June 23, 2025
DOI:https://doi.org/10.1073/pnas.2426017122

Significance

The Qinghai–Tibet Plateau (QTP) is a hotspot of biodiversity and endemism. Our multitaxon analysis shows that the endemic flora of the QTP had emerged by the Early Eocene. Both long-term in situ speciation and immigration have been responsible for the formation of the floristic endemism in the QTP region, but their contributions to the three subregions of the QTP are markedly different. The processes producing the floristic endemism of the three subregions of the QTP appear asynchronous, probably associated with different geoclimatic events. We further show that the Hengduan Mountains hosts the oldest endemic components of the flora and has served as an important “pump” and “sink” of unique biodiversity, highlighting its great conservation value.

Abstract

The Qinghai–Tibet Plateau (QTP) harbors extraordinarily high levels of biodiversity and endemism. The region is warming at a rate twice the global average, yet the evolutionary dynamics of its unique biota are poorly understood. Here, we used the endemic land plant genera of the QTP to investigate how its floristic endemism was shaped over time by Cenozoic geoclimatic changes. We first clarified that the QTP hosts 82 endemic land plant genera; we found that the origins of these endemic genera were most likely driven by ecological niche and elevation differentiation, caused by the uplift of the QTP and associated climate change. By sampling 37 land plant clades that together encompass 1,740 species, covering all 82 endemic genera, we show that QTP floristic endemism had emerged by the Early Eocene. Furthermore, the unique biodiversity of the QTP comprises a mix of indigenous elements and immigrants. Among the three subregions of the QTP (Plateau Platform, Himalaya, and the Hengduan Mountains), the processes associated with floristic endemism are asynchronous, reflecting different geoclimatic events with the Miocene as a particularly critical period. The relative contributions of in situ speciation and immigration to the unique biodiversity of the three subregions are also markedly different; in situ speciation dominated in the Hengduan Mountains, which hosts the oldest endemic components of the flora and has served as an important “pump” and “sink” of unique biodiversity. These findings provide insights into how past geoclimatic events may have shaped floristic endemism on the QTP and also have important conservation implications.

生物環境工学
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