新地图上详细描述了巽他陆架的古排水

Shawn Cheng , Mohd Azahari Faidi
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引用次数: 0

摘要

巽他大陆架是一个主要的生物多样性热点,在这里可以找到一些地球上最特有的物种。这一重要生物区域的大部分多样性都是由更新世期间发生的海平面波动所塑造的。为了阐明该地区的历史,我们利用2023年海洋网格一般水深图(General Bathymetric Chart of the Oceans Grid 2023)获得的深度等高线,对巽他陆架50、75、100和120 m等深线以及120 m等深线上的古流域进行了高分辨率重建。这里展示的地图旨在重建巽他陆架古河流与当代河流之间的联系,并确定与这里发现的河流系统相关的动植物/生物可能的扩散路线和屏障。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Palaeodrainages of the Sunda Shelf detailed in new maps
The Sunda Shelf is a prime biodiversity hotspot where some of the planet's most endemic species can be found. Much of the diversity in this important bioregion has been shaped by sea-level fluctuations that took place during the Pleistocene. Using depth contours obtained from the General Bathymetric Chart of the Oceans Grid 2023, we provide high-resolution reconstruction of land areas and palaeo-drainages on the Sunda Shelf at the 50, 75, 100, and 120 m isobaths, as well as palaeo-catchments at the 120 m isobath, in order to elucidate the history of this region. The maps presented here aim to reconstruct the connection between palaeo-rivers in the Sunda Shelf and contemporary rivers and identify possible dispersal routes and barriers for the floras and faunas/biotas associated with riverine systems found here.
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