Centre for Ecological Sciences, Indian Institute of Science, Bangalore 560 012, India.
J Biosci. 2009 Nov;34(5):687-97. doi: 10.1007/s12038-009-0057-8.
The remarkable geological and evolutionary history of peninsular India has generated much interest in the patterns and processes that might have shaped the current distributions of its endemic biota. In this regard the "Out-of-India" hypothesis, which proposes that rafting peninsular India carried Gondwanan forms to Asia after the break-up of Gondwana super continent, has gained prominence. Here we have reviewed molecular studies undertaken on a range of taxa of supposedly Gondwanan origin to better understand the Out-of-India scenario. This re-evaluation of published molecular studies indicates that there is mounting evidence supporting Out-of-India scenario for various Asian taxa. Nevertheless, in many studies the evidence is inconclusive due to lack of information on the age of relevant nodes. Studies also indicate that not all Gondwanan forms of peninsular India dispersed out of India. Many of these ancient lineages are confi ned to peninsular India and therefore are relict Gondwanan lineages. Additionally, for some taxa an "Into India" rather than "Out-of-India" scenario better explains their current distribution. To identify the "Out-of-India" component of Asian biota it is imperative that we understand the complex biogeographical history of India. To this end, we propose three oversimplified yet explicit phylogenetic predictions. These predictions can be tested through the use of molecular phylogenetic tools in conjunction with palaeontological and geological data.
印度半岛非凡的地质和演化历史引发了人们对可能塑造其特有生物区系当前分布模式和过程的极大兴趣。在这方面,“印度之外”假说引起了人们的关注,该假说认为,冈瓦纳超级大陆解体后,印度半岛的漂流将冈瓦纳形式带到了亚洲。在这里,我们回顾了对一系列假定源自冈瓦纳的分类群进行的分子研究,以更好地了解印度之外的情景。对已发表的分子研究的重新评估表明,有越来越多的证据支持亚洲各种分类群的印度之外情景。然而,在许多研究中,由于缺乏有关相关节点年龄的信息,证据尚无定论。研究还表明,并非印度半岛上的所有冈瓦纳形式都散布到了印度之外。这些古老的谱系中的许多都局限于印度半岛,因此是冈瓦纳遗留的谱系。此外,对于某些分类群,“进入印度”而不是“离开印度”的情景更好地解释了它们当前的分布。为了确定亚洲生物区系的“印度之外”成分,我们必须了解印度复杂的生物地理历史。为此,我们提出了三个简单但明确的系统发育预测。这些预测可以通过使用分子系统发育工具结合古生物学和地质学数据来进行检验。