Rice Ritva, Kallonen Aki, Cebra-Thomas Judith, Gilbert Scott F
Developmental Biology, Institute of Biotechnology, University of Helsinki, Helsinki 00014, Finland;
Department of Physics, University of Helsinki, Helsinki 00014, Finland;
Proc Natl Acad Sci U S A. 2016 May 10;113(19):5317-22. doi: 10.1073/pnas.1600958113. Epub 2016 Apr 25.
The dorsal and ventral aspects of the turtle shell, the carapace and the plastron, are developmentally different entities. The carapace contains axial endochondral skeletal elements and exoskeletal dermal bones. The exoskeletal plastron is found in all extant and extinct species of crown turtles found to date and is synaptomorphic of the order Testudines. However, paleontological reconstructed transition forms lack a fully developed carapace and show a progression of bony elements ancestral to the plastron. To understand the evolutionary development of the plastron, it is essential to know how it has formed. Here we studied the molecular development and patterning of plastron bones in a cryptodire turtle Trachemys scripta We show that plastron development begins at developmental stage 15 when osteochondrogenic mesenchyme forms condensates for each plastron bone at the lateral edges of the ventral mesenchyme. These condensations commit to an osteogenic identity and suppress chondrogenesis. Their development overlaps with that of sternal cartilage development in chicks and mice. Thus, we suggest that in turtles, the sternal morphogenesis is prevented in the ventral mesenchyme by the concomitant induction of osteogenesis and the suppression of chondrogenesis. The osteogenic subroutines later direct the growth and patterning of plastron bones in an autonomous manner. The initiation of plastron bone development coincides with that of carapacial ridge formation, suggesting that the development of dorsal and ventral shells are coordinated from the start and that adopting an osteogenesis-inducing and chondrogenesis-suppressing cell fate in the ventral mesenchyme has permitted turtles to develop their order-specific ventral morphology.
龟壳的背侧和腹侧,即背甲和腹甲,在发育上是不同的实体。背甲包含轴向软骨内骨骼元素和外骨骼真皮骨。外骨骼腹甲在迄今发现的所有现存和已灭绝的龟类物种中都存在,是龟鳖目的共有衍征。然而,古生物学重建的过渡形态缺乏发育完全的背甲,且显示出腹甲祖先的一系列骨元素的演变。为了了解腹甲的进化发展,了解其形成方式至关重要。在此,我们研究了一种潜颈龟——滑龟腹甲骨骼的分子发育和模式形成。我们发现,腹甲发育始于发育阶段15,此时骨软骨生成间充质在腹侧间充质的侧缘为每个腹甲骨骼形成凝聚物。这些凝聚物确定了成骨特性并抑制软骨生成。它们的发育与鸡和小鼠胸骨软骨的发育重叠。因此,我们认为在龟类中,腹侧间充质中同时发生的成骨诱导和软骨生成抑制阻止了胸骨形态发生。成骨子程序随后以自主方式指导腹甲骨骼的生长和模式形成。腹甲骨骼发育的起始与背甲嵴的形成同时发生,这表明背侧和腹侧龟壳的发育从一开始就是协调的,并且在腹侧间充质中采用诱导成骨和抑制软骨生成的细胞命运使龟类能够发育出其特定目的腹侧形态。