School of Earth and Ocean Sciences, Cardiff University, UK.
Biol Rev Camb Philos Soc. 2011 Nov;86(4):900-27. doi: 10.1111/j.1469-185X.2011.00178.x. Epub 2011 Apr 15.
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.
我们呈现了新生代(约 6500 万年前至今)大型有孔浮游有孔虫属种的完整系统发育关系。该系统发育关系是从大量古生物学工作中发展而来的,这些工作详细描述了从形态学上鉴定出的种级分类单元的进化关系和地层(时间)分布(“形态种”)。形态种根据测试形态学和推断的栖息地分别归入形态群和生态群。由于该分支中有充分的渐变进化记录,我们已经确定了许多形态种随时间逐渐变化的实例,从而可以从记录中消除“假种化”和“假灭绝”,并允许根据推断的生物谱系构建更自然的系统发育关系。每个分支事件都根据分支时形态变化的模式确定为出芽或分叉。该谱系系统发育关系为每个分歧提供了古生物学校准的年龄,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,可用于解决物种形成、灭绝以及进化速度和模式的问题。