Biodiversity and Climate Research Centre (BiK-F) & Senckenberg Gesellschaft für Naturforschung, Department of Botany and Molecular Evolution, Grunelius-Moellgaard Laboratory, Senckenberganlage 25, D-60325 Frankfurt am Main, Germany.
Am J Bot. 2013 Sep;100(9):1800-10. doi: 10.3732/ajb.1300059. Epub 2013 Sep 9.
Climatic and geological changes have been considered as major drivers of biological diversification. However, it has been generally assumed that lineages retain common environmental affinities, suggesting a limited capacity to switch their climatic niche. We tested this assumption with a study of the evolution of climatic niches in the Neotropical tree genus Cedrela (Meliaceae). •
We combined distribution models of extant Cedrela with a dated molecular phylogeny based on one nuclear (ITS) and three plastid markers (psbA-trnH, trnS-G and psbB-T-N) to reconstruct the evolutionary dynamics of climatic niches. We calculated relative disparity of climatic tolerances over time to test for niche evolution within subclades or divergence between subclades and conservatism among closely related groups. Published fossil records and studies on paleosols were evaluated for the distribution and climatic conditions of extinct Cedrela. •
The fossil record of Cedrela suggested a major biome shift from paratropical conditions into warm-temperate seasonal climates in the Early Oligocene of western North America. In the Miocene, Cedrela extended from North America (John Day Formation, Oregon, USA) to southern Central America (Gatún, Panama). Diversification in the early evolutionary history was mainly driven by changes in precipitation. Temperature had an increasing impact on ecological diversification of the genus from the Miocene onwards. Sister-species comparisons revealed that recent speciation events may be related to divergence of climatic tolerances. •
Our study highlights the complexity of climatic niche dynamics, and shows how conservatism and evolution have acted on different temporal scales and climatic parameters in Cedrela.
气候和地质变化被认为是生物多样化的主要驱动因素。然而,人们普遍认为谱系保留了共同的环境亲和力,这表明它们切换气候生态位的能力有限。我们通过对新热带雪松属(楝科)的气候生态位进化的研究来检验这一假设。
我们将现存雪松属的分布模型与基于一个核(ITS)和三个质体标记(psbA-trnH、trnS-G 和 psbB-T-N)的已测序分子系统发育相结合,以重建气候生态位的进化动态。我们计算了随着时间的推移气候容忍度的相对差异,以检验亚群内的生态位进化或亚群之间的分歧以及密切相关群体之间的保守性。已发表的化石记录和古土壤研究评估了已灭绝雪松属的分布和气候条件。
雪松属的化石记录表明,在北美西部早渐新世,从副热带条件向暖温带季节性气候发生了重大生物群转变。在中新世,雪松属从北美(美国俄勒冈州约翰·戴恩地层)延伸到中美洲南部(巴拿马加通)。早期进化历史上的多样化主要是由降水变化驱动的。从中新世开始,温度对该属的生态多样化产生了越来越大的影响。姐妹种比较表明,最近的物种形成事件可能与气候容忍度的分歧有关。
我们的研究强调了气候生态位动态的复杂性,并展示了雪松属在不同时间尺度和气候参数上的保守性和进化是如何作用的。