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古组织学数据揭示的古生代和中生代四足动物的脊椎发育

Vertebral Development in Paleozoic and Mesozoic Tetrapods Revealed by Paleohistological Data.

作者信息

Danto Marylène, Witzmann Florian, Fröbisch Nadia B

机构信息

Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany.

Department of Ecology and Evolutionary Biology, Brown University, Providence, Rhode Island, RI 02912, United States of America.

出版信息

PLoS One. 2016 Apr 13;11(4):e0152586. doi: 10.1371/journal.pone.0152586. eCollection 2016.

Abstract

Basal tetrapods display a wide spectrum of vertebral centrum morphologies that can be used to distinguish different tetrapod groups. The vertebral types range from multipartite centra in stem-tetrapods, temnospondyls, and seymouriamorphs up to monospondylous centra in lepospondyls and have been drawn upon for reconstructing major evolutionary trends in tetrapods that are now considered textbook knowledge. Two modes of vertebral formation have been postulated: the multipartite vertebrae formed first as cartilaginous elements with subsequent ossification. The monospondylous centrum, in contrast, was formed by direct ossification without a cartilaginous precursor. This study describes centrum morphogenesis in basal tetrapods for the first time, based on bone histology. Our results show that the intercentra of the investigated stem-tetrapods consist of a small band of periosteal bone and a dense network of endochondral bone. In stereospondyl temnospondyls, high amounts of calcified cartilage are preserved in the endochondral trabeculae. Notably, the periosteal region is thickened and highly vascularized in the plagiosaurid stereospondyls. Among "microsaur" lepospondyls, the thickened periosteal region is composed of compact bone and the notochordal canal is surrounded by large cell lacunae. In nectridean lepospondyls, the periosteal region has a spongy structure with large intertrabecular spaces, whereas the endochondral region has a highly cancellous structure. Our observations indicate that regardless of whether multipartite or monospondylous, the centra of basal tetrapods display first endochondral and subsequently periosteal ossification. A high interspecific variability is observed in growth rate, organization, and initiation of periosteal ossification. Moreover, vertebral development and structure reflect different lifestyles. The bottom-dwelling Plagiosauridae increase their skeletal mass by hyperplasy of the periosteal region. In nectrideans, the skeletal mass decreases, as the microstructure is spongy and lightly built. Additionally, we observed that vertebral structure is influenced by miniaturization in some groups. The phylogenetic information that can be drawn from vertebral development, however, is limited.

摘要

基干四足动物呈现出广泛的椎体形态,可用于区分不同的四足动物类群。椎体类型从茎型四足动物、离片锥类和蜥螈形类中的多部分椎体,到壳椎类中的单椎体,这些椎体类型已被用于重建四足动物的主要进化趋势,如今这已成为教科书知识。人们推测了两种椎体形成模式:多部分椎体首先形成软骨成分,随后骨化。相比之下,单椎体是通过直接骨化形成的,没有软骨前体。本研究首次基于骨组织学描述了基干四足动物椎体的形态发生。我们的结果表明,所研究的茎型四足动物的间椎体由一小条骨膜骨和致密的软骨内骨网络组成。在全椎类离片锥类中,软骨内小梁中保留了大量钙化软骨。值得注意的是,在阔齿龙科全椎类中,骨膜区域增厚且血管高度丰富。在“微体龙类”壳椎类中,增厚的骨膜区域由密质骨组成,脊索管被大的细胞腔包围。在游螈目壳椎类中,骨膜区域具有海绵状结构,小梁间隙大,而软骨内区域具有高度松质的结构。我们的观察表明,无论多部分椎体还是单椎体,基干四足动物的椎体首先进行软骨内骨化,随后进行骨膜骨化。在骨膜骨化的生长速率、组织和起始方面观察到高度的种间变异性。此外,椎体发育和结构反映了不同的生活方式。底栖的阔齿龙科通过骨膜区域的增生增加其骨骼质量。在游螈目中,由于微观结构是海绵状且结构轻盈,骨骼质量下降。此外,我们观察到在一些类群中椎体结构受小型化影响。然而,从椎体发育中可以得出的系统发育信息是有限的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4385/4830443/7c1495dd5905/pone.0152586.g001.jpg

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