首页> 外文期刊>Palaios: An International Journal of the Society of Economic Paleontologists & Mineralogists >An assessment of morphological fidelity in the sub-fossil record of a terebratulide brachiopod
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An assessment of morphological fidelity in the sub-fossil record of a terebratulide brachiopod

机译:对terebratulide腕足动物的亚化石记录中形态保真度的评估

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摘要

The process of time-averaging can have deleterious effects on the recognition of morphological variability in the fossil record. To explore this issue, a geometric morphometric study was conducted on a life and death assemblage of the terebratulide brachiopod Terebratalia transversa. The results from several geometric morphometric techniques (including Procrustes analysis and thin-plate spline) confirm a high degree of morphological variability with little change in mean shape between the living and sub-fossil assemblages. Additionally, there is no evidence of distinct morphogroups in either assemblage, as postulated for the species in previous studies. These trends persist at all depths and size classes. The similar range of morphological variability at each site suggests a common causal factor such as a similar array of microenvironments available at all depths. One implication of this consistency in morphological variability between the living and sub-fossil assemblages is that the variability of a fossil assemblage of this species could be used to estimate single-generation variability during the time-averaged interval. Furthermore, the potential for recognizing the full range of shape variability in the sub-fossil record of a highly variable species is encouraging for the pursuit of species recognition in the fossil record. Very good fidelity of the sub-fossil assemblage with respect to morphological variability is documented here for the first time in brachiopods, and agrees well with the findings of similar studies of other taxa.
机译:时间平均过程可能对化石记录中形态变异的识别产生有害影响。为了探讨这个问题,对terebratulide brachiopod terebratalia transversa的生死组合进行了几何形态计量学研究。几种几何形态计量学技术(包括Procrustes分析和薄板样条曲线)的结果证实了高度的形态变异性,在活体和次化石组合之间的平均形状几乎没有变化。此外,没有证据表明这两种组合中都有不同的吗基,正如先前研究中假定的那样。这些趋势在所有深度和尺寸级别上均持续存在。每个位点的形态变异范围相似,表明存在共同的因果关系,例如在所有深度都可获得相似的微环境阵列。这种生物和次化石组合之间形态变异的一致性的一个暗示是,该物种的化石组合的变异可用于估计时间平均间隔内的单代变异。此外,在高度可变物种的亚化石记录中识别各种形状变化的潜力,对于追求在化石记录中进行物种识别令人鼓舞。首次在腕足类动物中记录了亚化石组合在形态变异性方面的极高保真度,与其他类群的类似研究结果十分吻合。

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