来自印度阿萨姆邦晚渐新世的Barringtonia Forster和Forster(卵黄科)叶子

G. Srivastava, R. Mehrotra
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引用次数: 1

摘要

印度东北部被认为是印度板块与欧亚板块碰撞后植物从印度向东南亚迁移的走廊,反之亦然。卵磷脂科的化石记录在全球范围内非常稀少。我们报道了印度阿萨姆邦晚渐新世沉积物中Barringtonia (Lecythidaceae)的化石叶片。该属的现代分布和化石记录表明其起源于冈瓦纳衍生大陆。在印度板块和欧亚板块碰撞和完全融合之后,该属最有可能从印度迁移到东南亚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Barringtonia Forster & Forster (Lecythidaceae) leaf from the late Oligocene of Assam, India
Northeast India is considered as corridor for the plant migration from India to Southeast Asia and vice–versa after the collision of Indian Plate with the Eurasian Plate. The fossil record of the family Lecythidaceae is very sparse globally. We report a fossil leaf of Barringtonia (Lecythidaceae) from the late Oligocene sediments of Assam, India. The modern distribution and fossil records of the genus indicate its origin in Gondwana derived continents. After collision and complete suturing of the Indian and Eurasian plates the genus most likely migrated from India to Southeast Asia.
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