山岳形成と気候変動が高山生物多様性に与える影響を解明(Researchers Show Impact of Mountain Building and Climate Change on Alpine Biodiversity)

2025-12-22 中国科学院(CAS)

中国科学院西双版納熱帯植物園(XTBG)などの研究チームは、北半球の主要5山系を対象に、過去3000万年にわたる山脈形成と気候寒冷化が高山植物多様性を生み出した主要因であることを示した。34群・8456種の被子植物の系統解析と地質・古気候復元を統合し、山の隆起が新たな生息地を創出して種分化を促進し、寒冷化が高地間の連結性を高めて分散を可能にしたことを解明。チベット‐ヒマラヤ‐横断山脈は種の「ゆりかご」として現地分化が卓越し、欧州やイラノ・トゥラニアでは低地系統の高山適応が主、天山山脈は外来種導入が多いなど地域差も明らかにした。さらに近500万年の寒冷化で北極‐高山域が生物地理的交差点となった。

<関連情報>

北半球の高山植物の非同期的な出現は、造山運動と気候変動に対する生物集団の一般的な反応を明らかにする The asynchronous rise of Northern Hemisphere alpine floras reveals general responses of biotic assembly to orogeny and climate change

Wenna Ding, Richard H. Ree, Michael R. May, Philipp Brun, […] , and Niklaus E. Zimmermann
Science Advances  Published:19 Dec 2025
DOI:https://doi.org/10.1126/sciadv.adz1888

山岳形成と気候変動が高山生物多様性に与える影響を解明(Researchers Show Impact of Mountain Building and Climate Change on Alpine Biodiversity)

Abstract

Understanding how biotic assembly processes responded to past geoclimatic changes is key to explaining the origins of mountain biodiversity and the causes of regional disparities in species richness. Here, we jointly reconstructed geographic ranges and biome-niche evolution for 34 diverse plant clades across five major Northern Hemisphere mountain systems and quantified how late Neogene cooling increased arctic-alpine habitat connections across regions. We reveal that, while alpine floras originated asynchronously and were assembled through distinct evolutionary processes over the past 30 million years, general biological responses to orogeny and environmental change are apparent. Across regions, in situ diversification was consistently elevated during heightened phases of tectonic activity. Over the past 5 million years, enhanced arctic-alpine connectivity facilitated biotic interchange and positioned the boreal-arctic region as a major biogeographic crossroads linking Eurasia and North America.

1702地球物理及び地球化学
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