Linking South American dry regions by the Gran Chaco: Insights from the evolutionary history and ecological diversification of Gomphrena s.str. (Gomphrenoideae, Amaranthaceae)

María J. Bena, Matias C. Baranzelli, Santiago M. Costas, Andrea Cosacov, María C. Acosta, Andrés Moreira‐Muñoz, Alicia N. Sérsic
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Abstract

Abstract Geoclimatic events driving South American aridization have generated biota differentiation due to barriers and new environment formation. New environments allow species climatic niche evolution, or the geographical expansion of an existing one. Understanding the role these processes play may clarify the evolution of South American biota. Gomphrena L. ranges across almost all the continent's arid environments. We tested whether South American drylands are biogeographically connected through the Gran Chaco but, due to different aridity levels, lineage diversification could have also been associated with the evolution of climatic niches and morphological or physiological traits. With available data, we generated a dated phylogeny, estimated ancestral ranges, performed diversification analyses, reconstructed ancestral states of two characters, and examined if niches have changed between lineages. Results showed that Gomphrena diversified throughout the easternmost South American drylands ~15.4 Ma, and subsequently three independent clades colonized the western arid regions during the last Andean pulse, and after the marine transgressions (~4.8–0.4 Ma) via the Gran Chaco. The colonization implied an increase in the diversification rate of annuals over perennials and the progressive east–west differentiation of the occupied climatic niche. This diversification was influenced by C 4 photosynthesis, which could have acted as a niche opener to conquer new environments after the Paranaean Sea withdrew. Spatiotemporal patterns found in Gomphrena suggest that geographical expansion and evolution of climatic niches played a common but decoupled role in promoting diversification. These results show that the Gran Chaco may have acted as a historical connection linking South American drylands.

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通过大查科连接南美干旱地区:来自Gomphrena s.str的进化史和生态多样化的见解。(Gomphrenoideae苋科)
驱动南美干旱化的地缘气候事件由于屏障和新环境的形成而产生了生物群分化。新的环境允许物种的气候生态位进化,或者现有生态位的地理扩展。了解这些过程所起的作用可能会澄清南美生物群的进化。Gomphrena L.的分布范围几乎遍及非洲大陆所有的干旱环境。我们测试了南美旱地是否通过大查科在生物地理上相连,但由于不同的干旱程度,谱系多样化也可能与气候生态位和形态或生理特征的进化有关。利用现有数据,我们生成了一个确定年代的系统发育,估计了祖先范围,进行了多样化分析,重建了两个性状的祖先状态,并检查了生态位在谱系之间是否发生了变化。结果表明,Gomphrena在南美洲最东部的干旱地区(~ 15.4 Ma)呈现多样化,随后在最后一次安第斯脉冲期间以及经过大查科海侵(~4.8 ~ 0.4 Ma)后,三个独立的分支殖民了西部干旱地区。殖民化表明一年生植物的多样化率高于多年生植物,被占领的气候生态位呈东西分化的趋势。这种多样化受到c4光合作用的影响,这可能是在巴拉那海退出后征服新环境的生态位打开器。Gomphrena的时空格局表明,气候生态位的地理扩展和演化在促进多样性方面发挥了共同但不耦合的作用。这些结果表明,大查科可能是连接南美旱地的历史纽带。
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