巽他古陆(英语:Sundaland)是生物地理学概念,指的是末次冰期由于海平面下降而在东南亚地区露出水面并连成一体的陆地。巽他古陆的相当一部分地区,今日都已位于海面以下,成为巽他陆架。仍然是陆地的部分,包括马来半岛婆罗洲爪哇岛苏门答腊岛等。巽他古地的东界为华莱士线(Wallace Line),即东洋界澳新界动物群的分界线。

巽他古陆示意图

参见

Wikiwand in your browser!

Seamless Wikipedia browsing. On steroids.

Every time you click a link to Wikipedia, Wiktionary or Wikiquote in your browser's search results, it will show the modern Wikiwand interface.

Wikiwand extension is a five stars, simple, with minimum permission required to keep your browsing private, safe and transparent.