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Geomorphology Drives Amphibian Beta Diversity in Atlantic Forest Lowlands of Southeastern Brazil

机译:地貌学驱动巴西东南部大西洋森林低地的两栖动物β多样性

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摘要

Beta diversity patterns are the outcome of multiple processes operating at different scales. Amphibian assemblages seem to be affected by contemporary climate and dispersal-based processes. However, historical processes involved in present patterns of beta diversity remain poorly understood. We assess and disentangle geomorphological, climatic and spatial drivers of amphibian beta diversity in coastal lowlands of the Atlantic Forest, southeastern Brazil. We tested the hypothesis that geomorphological factors are more important in structuring anuran beta diversity than climatic and spatial factors. We obtained species composition via field survey (N = 766 individuals), museum specimens (N = 9,730) and literature records (N = 4,763). Sampling area was divided in four spatially explicit geomorphological units, representing historical predictors. Climatic descriptors were represented by the first two axis of a Principal Component Analysis. Spatial predictors in different spatial scales were described by Moran Eigenvector Maps. Redundancy Analysis was implemented to partition the explained variation of species composition by geomorphological, climatic and spatial predictors. Moreover, spatial autocorrelation analyses were used to test neutral theory predictions. Beta diversity was spatially structured in broader scales. Shared fraction between climatic and geomorphological variables was an important predictor of species composition (13%), as well as broad scale spatial predictors (13%). However, geomorphological variables alone were the most important predictor of beta diversity (42%). Historical factors related to geomorphology must have played a crucial role in structuring amphibian beta diversity. The complex relationships between geomorphological history and climatic gradients generated by the Serra do Mar Precambrian basements were also important. We highlight the importance of combining spatially explicit historical and contemporary predictors for understanding and disentangling major drivers of beta diversity patterns.
机译:Beta多样性模式是在不同规模下运行的多个过程的结果。两栖动物的组合似乎受到当代气候和基于传播的过程的影响。但是,目前有关β多样性模式的历史过程仍然知之甚少。我们评估和解开了巴西东南部大西洋森林沿海低地两栖动物β多样性的地貌,气候和空间驱动力。我们检验了以下假设:与气候和空间因素相比,地貌因素在构造无环β多样性方面更为重要。我们通过现场调查(N = 766个个体),博物馆标本(N = 9,730)和文献记录(N = 4,763)获得了物种组成。抽样区域分为四个空间明确的地貌单位,代表历史预测因素。气候描述符由主成分分析的前两个轴表示。 Moran Eigenvector Maps描述了不同空间尺度的空间预测因子。进行了冗余分析,以通过地貌,气候和空间预测因子对解释的物种组成变化进行划分。此外,空间自相关分析用于测试中性理论的预测。 Beta多样性在更广泛的范围内具有空间结构。气候和地貌变量之间的共享分数是物种组成的重要预测因子(占13%),也是广泛的空间预测因子(占13%)。但是,仅地貌变量是β多样性最重要的预测因子(42%)。与地貌相关的历史因素在构造两栖动物的β多样性中必须发挥了至关重要的作用。 Serra do Mar前寒武纪基底产生的地貌史和气候梯度之间的复杂关系也很重要。我们强调了将空间上明确的历史和当代预测因子结合在一起对于理解和解开β多样性模式的主要驱动因素的重要性。

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