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A phylogeny of Cenozoic macroperforate planktonic foraminifera from fossil data

机译:来自化石数据的新生代大孔浮游有孔虫的系统发育

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We present a complete phylogeny of macroperforate planktonic foraminifer species of the Cenozoic Era (~65 million years ago to present). The phylogeny is developed from a large body of palaeontological work that details the evolutionary relationships and stratigraphic (time) distributions of species-level taxa identified from morphology (‘morphospecies’). Morphospecies are assigned to morphogroups and ecogroups depending on test morphology and inferred habitat, respectively. Because gradual evolution is well documented in this clade, we have identified many instances of morphospecies intergrading over time, allowing us to eliminate ‘pseudospeciation’ and ‘pseudoextinction’ from the record and thereby permit the construction of a more natural phylogeny based on inferred biological lineages. Each cladogenetic event is determined as either budding or bifurcating depending on the pattern of morphological change at the time of branching. This lineage phylogeny provides palaeontologically calibrated ages for each divergence that are entirely independent of molecular data. The tree provides a model system for macroevolutionary studies in the fossil record addressing questions of speciation, extinction, and rates and patterns of evolution.
机译:我们提供了一个新生代(约6500万年前至今)的大孔浮游有孔虫物种的完整系统发育史。系统发育是从大量古生物学工作发展而来的,该工作详细描述了从形态学(“形态物种”)中识别出的物种级分类群的进化关系和地层(时间)分布。形态物种分别根据测试形态和推断的栖息地分配给形态群和生态群。由于进化枝在这一进化枝上有很好的记录,因此我们已经鉴定出许多形态物种随时间推移而发生的转变,从而使我们能够从记录中消除“拟物种”和“拟灭绝”,从而允许根据推断的生物学谱系构建更自然的系统发育。每个分支发生事件都取决于分支时形态变化的模式而确定为萌芽还是分支。该谱系系统发育为每个差异提供了古生物学校正的年龄,而这些年龄完全独立于分子数据。该树为化石记录中的宏观进化研究提供了一个模型系统,解决了物种形成,灭绝以及进化速率和模式的问题。

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