Becerra Judith X
Department of Entomology, University of Arizona, Tucson, AZ 85721, USA.
Proc Natl Acad Sci U S A. 2005 Aug 2;102(31):10919-23. doi: 10.1073/pnas.0409127102. Epub 2005 Jul 20.
Macroevolution examines the temporal patterns of biological diversity in deep time. When combined with biogeography, it can provide unique information about the historical changes in the distribution of communities and biomes. Here I document temporal and spatial changes of diversity in the genus Bursera and relate them to the origin and expansion of the tropical dry forests of Mexico. Bursera is very old, highly adapted to warm dry conditions, and a dominant member of the Mexican tropical dry forest. These characteristics make it a useful indicator of the history of this vegetation. I used a time-calibrated phylogeny to estimate Bursera's diversification rate at different times over the last 60 million years. I also reconstructed the geographic center and time of origin of all species and nodes from information on current distributions. Results show that between 30 and 20 million years ago, Bursera began a relatively rapid diversification. This suggests that conditions were favorable for its radiation and thus, very probably for the establishment of the dry forest as well. The oldest lineages diverged mostly in Western Mexico, whereas the more recent lineages diverged in the south-central part of the country. This suggests that the tropical dry forest probably first established in the west and then expanded south and east. The timing of the radiations in these areas corresponds to that suggested for formations of the mountainous systems in Western and Central Mexico, which have been previously recognized as critical for the persistence of the Mexican dry forest.
宏观进化研究的是漫长时间里生物多样性的时间模式。当与生物地理学相结合时,它可以提供有关群落和生物群落分布历史变化的独特信息。在这里,我记录了裂榄属植物多样性的时空变化,并将它们与墨西哥热带干旱森林的起源和扩张联系起来。裂榄属植物历史悠久,高度适应温暖干燥的环境,是墨西哥热带干旱森林的主要成员。这些特征使其成为这种植被历史的有用指标。我使用了一个经过时间校准的系统发育树来估计裂榄属植物在过去6000万年中不同时期的多样化速率。我还根据当前分布信息重建了所有物种和节点的地理中心及起源时间。结果表明,在3000万至2000万年前,裂榄属植物开始了相对快速的多样化。这表明当时的条件有利于其辐射,因此很可能也有利于干旱森林的形成。最古老的谱系大多在墨西哥西部分化,而较新的谱系在该国中南部分化。这表明热带干旱森林可能首先在西部形成,然后向南和向东扩张。这些地区辐射的时间与墨西哥西部和中部山区系统形成的时间一致,这些山区系统此前被认为对墨西哥干旱森林的存续至关重要。