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Experimental evidence that the Ornstein‐Uhlenbeck model best describes the evolution of leaf litter decomposability

机译:实验证明Ornstein-Uhlenbeck模型最能描述叶片凋落物可分解性的演变

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AbstractLeaf litter decomposability is an important effect trait for ecosystem functioning. However, it is unknown how this effect trait evolved through plant history as a leaf ‘afterlife’ integrator of the evolution of multiple underlying traits upon which adaptive selection must have acted. Did decomposability evolve in a Brownian fashion without any constraints? Was evolution rapid at first and then slowed? Or was there an underlying mean-reverting process that makes the evolution of extreme trait values unlikely? Here, we test the hypothesis that the evolution of decomposability has undergone certain mean-reverting forces due to strong constraints and trade-offs in the leaf traits that have afterlife effects on litter quality to decomposers. In order to test this, we examined the leaf litter decomposability and seven key leaf traits of 48 tree species in the temperate area of China and fitted them to three evolutionary models: Brownian motion model (BM), Early burst model (EB), and Ornstein-Uhlenbeck model (OU). The OU model, which does not allow unlimited trait divergence through time, was the best fit model for leaf litter decomposability and all seven leaf traits. These results support the hypothesis that neither decomposability nor the underlying traits has been able to diverge toward progressively extreme values through evolutionary time. These results have reinforced our understanding of the relationships between leaf litter decomposability and leaf traits in an evolutionary perspective and may be a helpful step toward reconstructing deep-time carbon cycling based on taxonomic composition with more confidence.
机译:摘要凋落物可分解性是生态系统功能的重要影响特征。但是,尚不清楚这种效应性状是如何通过植物历史演变成叶子的“来世”整合者,而这些性状是多种潜在性状进化的基础,必须进行适应性选择。可分解性是否在没有任何约束的情况下以布朗方式发展?起初发展迅速,然后放缓了吗?还是存在潜在的均值回复过程,使得极端特质值的演化不太可能?在这里,我们检验以下假设:可分解性的演变经历了一定的均值回复力,这归因于叶片性状的强大约束和折衷,这些折衷对分解者的产后质量有影响。为了验证这一点,我们研究了中国温带地区48种树种的凋落物分解性和7个关键叶片性状,并将它们拟合为三种进化模型:布朗运动模型(BM),早期爆发模型(EB)和奥恩斯坦-乌伦贝克模型(OU)。 OU模型不允许随时间的无限性状发散,它是叶片凋落物可分解性和所有七个叶片性状的最佳拟合模型。这些结果支持以下假设:可分解性和基本特征都无法通过进化的时间逐渐趋向极端值。这些结果从进化的角度加强了我们对凋落物可分解性与叶片性状之间关系的理解,并且可能是一个有助于更自信地基于分类学成分重建深层碳循环的有益步骤。

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