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印度西高止山脉南部晚古新世-早始新世赤道雨林避难所的证据。

Evidence of late Palaeocene-early Eocene equatorial rain forest refugia in southern Western Ghats, India.

机构信息

Birbal Sahni Institute of Palaeobotany, Lucknow 226 007 India.

出版信息

J Biosci. 2009 Nov;34(5):777-97. doi: 10.1007/s12038-009-0062-y.

Abstract

Equatorial rain forests that maintain a balance between speciation and extinction are hot-spots for studies of biodiversity. Western Ghats in southern India have gained attention due to high tropical biodiversity and endemism in their southern most area. We attempted to track the affinities of the pollen fl ora of the endemic plants of Western Ghat area within the fossil palynoflora of late Palaeocene-early Eocene (approximately 55-50 Ma) sedimentary deposits of western and northeastern Indian region. The study shows striking similarity of extant pollen with twenty eight most common fossil pollen taxa of the early Palaeogene. Widespread occurrences of coal and lignite deposits during early Palaeogene provide evidence of existence of well diversified rain forest community and swampy vegetation in the coastal low lying areas all along the western and northeastern margins of the Indian subcontinent. Prevalence of excessive humid climate during this period has been seen as a result of equatorial positioning of Indian subcontinent, superimposed by a long term global warming phase (PETM and EECO) during the early Palaeogene. The study presents clear evidence that highly diversifi ed equatorial rain forest vegetation once widespread in the Indian subcontinent during early Palaeogene times, are now restricted in a small area as a refugia in the southernmost part of the Western Ghat area. High precipitation and shorter periods of dry months seem to have provided suitable environment to sustain lineages of ancient tropical vegetation in this area of Western Ghats in spite of dramatic climatic changes subsequent to the post India-Asia collision and during the Quaternary and Recent times.

摘要

赤道雨林在物种形成和灭绝之间保持平衡,是生物多样性研究的热点。印度南部的西高止山脉因其南部地区的热带生物多样性和特有性而受到关注。我们试图追踪西高止山脉特有植物的花粉区系与印度西部和东北部晚古新世-早始新世(约 55-50 Ma)沉积地层中化石花粉区系的亲缘关系。研究表明,现存花粉与早古新世最常见的 28 个化石花粉类群具有惊人的相似性。早古新世广泛出现的煤和褐煤矿床为沿海低地存在多样化的雨林群落和沼泽植被提供了证据,这些地区沿着印度次大陆的西部和东北部边缘延伸。在这段时间里,赤道地区的位置和长期的全球变暖阶段(PETM 和 EECO)导致了过度潮湿的气候,这一现象已经被观察到。研究清楚地表明,高度多样化的赤道雨林植被在早古新世曾经广泛分布在印度次大陆,现在仅限于西高止山脉最南端的一个小区域作为避难所。高降雨量和较短的干旱月份似乎为维持西高止山脉地区古老热带植被的谱系提供了适宜的环境,尽管在印度-亚洲碰撞之后以及第四纪和现代时期发生了剧烈的气候变化。

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