Hebdon Nicholas, Polly P David, Peterman David Joseph, Ritterbush Kathleen A
Dept. of Biological Sciences, Chapman University, Keck Center, 450 North Center Street, Orange, CA, 92866.
Departments of Earth & Atmospheric Science, Biology, and Anthropology, Indiana University, Bloomington, IN, 47405, USA.
Integr Comp Biol. 2022 Jun 6. doi: 10.1093/icb/icac034.
A boom in technological advancements over the last two decades has driven a surge in both the diversity and power of analytical tools available to biomechanical and functional morphology research. However, in order to adequately investigate each of these dense datasets, one must often consider only one functional narrative at a time. There is more to each organism than any one of these form-function relationships. Joint performance landscapes determined by maximum likelihood are a valuable tool that can be used to synthesize our understanding of these multiple functional hypotheses to further explore an organism's ecology. We present an example framework for applying these tools to such a problem using the morphological transition of ammonoids from the Middle Triassic to the Early Jurassic. Across this time interval, morphospace occupation shifts from a broad occupation across Westermann Morphospace to a dense occupation of a region emphasizing an exposed umbilicus and modest frontal profile. The hydrodynamic capacities and limitations of the shell have seen intense scrutiny as a likely explanation of this transition. However, conflicting interpretations of hydrodynamic performance remain despite this scrutiny, with scant offerings of alternative explanations. Our analysis finds that hydrodynamic measures of performance do little to explain the shift in morphological occupation, highlighting a need for a more robust investigation of alternative functional hypotheses that are often intellectually set aside. With this we show a framework for consolidating the current understanding of the form-function relationships in an organism, and assess when they are insufficiently characterizing the dynamics those data are being used to explain. We aim to encourage the broader adoption of this framework and these ideas as a foundation to bring the field close to comprehensive synthesis and reconstruction of organisms.
在过去二十年里,技术进步的蓬勃发展推动了生物力学和功能形态学研究可用分析工具在多样性和功能上的激增。然而,为了充分研究这些密集数据集的每一个,人们通常必须一次只考虑一种功能描述。每个生物体都比这些形式-功能关系中的任何一种包含更多内容。由最大似然法确定的关节性能景观是一种有价值的工具,可用于综合我们对这些多种功能假设的理解,以进一步探索生物体的生态学。我们提供了一个示例框架,用于将这些工具应用于这样一个问题,即利用中三叠世到早侏罗世菊石的形态转变。在这个时间间隔内,形态空间占据从广泛占据韦斯特曼形态空间转变为密集占据一个强调暴露脐部和适度正面轮廓的区域。壳体的流体动力学能力和局限性作为这种转变的一种可能解释受到了深入研究。然而,尽管有这种研究,流体动力学性能的相互矛盾的解释仍然存在,而替代解释却很少。我们的分析发现,流体动力学性能测量对形态占据的转变几乎没有解释作用,这凸显了需要对那些通常在智力上被搁置的替代功能假设进行更有力的研究。借此,我们展示了一个框架,用于巩固目前对生物体中形式-功能关系的理解,并评估它们在何时不足以表征那些数据所用于解释的动态。我们旨在鼓励更广泛地采用这个框架和这些理念,作为使该领域接近对生物体进行全面综合和重建的基础。