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探讨多倍体植物生物地理学纬度梯度的历史驱动因素:多分支视角。

Investigating historical drivers of latitudinal gradients in polyploid plant biogeography: A multiclade perspective.

机构信息

Department of Biological Sciences, University of Arkansas, Fayetteville, 72701, AR, USA.

Department of Ecology & Evolutionary Biology, University of Toronto, Toronto, M5S 3B2, ON, Canada.

出版信息

Am J Bot. 2024 Aug;111(8):e16356. doi: 10.1002/ajb2.16356. Epub 2024 Jun 12.

Abstract

PREMISE

The proportion of polyploid plants in a community increases with latitude, and different hypotheses have been proposed about which factors drive this pattern. Here, we aimed to understand the historical causes of the latitudinal polyploidy gradient using a combination of ancestral state reconstruction methods. Specifically, we assessed whether (1) polyploidization enables movement to higher latitudes (i.e., polyploidization precedes occurrences in higher latitudes) or (2) higher latitudes facilitate polyploidization (i.e., occurrence in higher latitudes precedes polyploidization).

METHODS

We reconstructed the ploidy states and ancestral niches of 1032 angiosperm species at four paleoclimatic time slices ranging from 3.3 million years ago to the present, comprising taxa from four well-represented clades: Onagraceae, Primulaceae, Solanum (Solanaceae), and Pooideae (Poaceae). We used ancestral niche reconstruction models alongside a customized discrete character evolution model to allow reconstruction of states at specific time slices. Patterns of latitudinal movement were reconstructed and compared in relation to inferred ploidy shifts.

RESULTS

No single hypothesis applied equally well across all analyzed clades. While significant differences in median latitudinal occurrence were detected in the largest clade, Poaceae, no significant differences were detected in latitudinal movement in any clade.

CONCLUSIONS

Our preliminary study is the first to attempt to connect ploidy changes to continuous latitudinal movement, but we cannot favor one hypothesis over another. Given that patterns seem to be clade-specific, more clades must be analyzed in future studies for generalities to be drawn.

摘要

前提

随着纬度的增加,群落中的多倍体植物的比例增加,并且已经提出了不同的假设来解释哪些因素导致了这种模式。在这里,我们旨在使用祖先状态重建方法的组合来了解纬度多倍体梯度的历史原因。具体来说,我们评估了(1)多倍化是否使植物能够向更高的纬度移动(即多倍化先于高纬度发生),或者(2)更高的纬度是否有利于多倍化(即高纬度的发生先于多倍化)。

方法

我们重建了 1032 种被子植物在四个古气候时间切片中的倍性状态和祖先生态位,这些时间切片的范围从 330 万年前到现在,包括来自四个代表性较好的类群的分类群:柳叶菜科、报春花科、茄科和禾本科。我们使用祖先生态位重建模型和定制的离散字符进化模型来允许在特定时间切片上重建状态。在与推断的倍性变化相关的情况下,重建了纬度移动的模式并进行了比较。

结果

没有一个假设适用于所有分析的类群。虽然在最大的类群禾本科中检测到中位数纬度发生的显著差异,但在任何类群中都没有检测到纬度移动的显著差异。

结论

我们的初步研究是第一个尝试将倍性变化与连续的纬度移动联系起来的研究,但我们不能偏袒任何一个假设。鉴于模式似乎是类群特有的,未来的研究必须分析更多的类群,才能得出一般性的结论。

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