State Museum of Natural History Stuttgart , Rosenstein 1, 70191 Stuttgart, Germany.
Palaeontological Institute and Museum , University of Zurich , Karl Schmid-Strasse 4, 8006 Zürich, Switzerland.
R Soc Open Sci. 2015 Jul 8;2(7):140440. doi: 10.1098/rsos.140440. eCollection 2015 Jul.
Placodontia is a clade of durophagous, near shore marine reptiles from Triassic sediments of modern-day Europe, Middle East and China. Although much is known about their primary anatomy and palaeoecology, relatively little has been published regarding their life history, i.e. ageing, maturation and growth. Here, growth records derived from long bone histological data of placodont individuals are described and modelled to assess placodont growth and life-history strategies. Growth modelling methods are used to confirm traits documented in the growth record (age at onset of sexual maturity, age when asymptotic length was achieved, age at death, maximum longevity) and also to estimate undocumented traits. Based on these growth models, generalized estimates of these traits are established for each taxon. Overall differences in bone tissue types and resulting growth curves indicate different growth patterns and life-history strategies between different taxa of Placodontia. Psephoderma and Paraplacodus grew with lamellar-zonal bone tissue type and show growth patterns as seen in modern reptiles. Placodontia indet. aff. Cyamodus and some Placodontia indet. show a unique combination of fibrolamellar bone tissue regularly stratified by growth marks, a pattern absent in modern sauropsids. The bone tissue type of Placodontia indet. aff. Cyamodus and Placodontia indet. indicates a significantly increased basal metabolic rate when compared with modern reptiles. Double lines of arrested growth, non-annual rest lines in annuli, and subcycles that stratify zones suggest high dependence of placodont growth on endogenous and exogenous factors. Histological and modelled differences within taxa point to high individual developmental plasticity but sexual dimorphism in growth patterns and the presence of different taxa in the sample cannot be ruled out.
齿龙目是一类具有较强咬合力的近岸海洋爬行动物,来自现代欧洲、中东和中国的三叠纪沉积物。尽管人们对它们的主要解剖结构和古生态学有了很多了解,但相对而言,关于它们的生活史,即衰老、成熟和生长的研究却很少。本文描述并建立了来自齿龙个体长骨组织学数据的生长记录,以评估齿龙的生长和生活史策略。生长模型方法用于确认生长记录中记录的特征(性成熟开始的年龄、达到渐近长度的年龄、死亡年龄、最大寿命),并估计未记录的特征。基于这些生长模型,为每个分类单元建立了这些特征的综合估计值。不同的骨组织类型和由此产生的生长曲线之间的总体差异表明,齿龙目不同分类单元之间的生长模式和生活史策略存在差异。Psephoderma 和 Paraplacodus 具有层状-带状骨组织类型,其生长模式与现代爬行动物相似。Placodontia indet. aff. Cyamodus 和一些 Placodontia indet. 显示出纤维-层状骨组织的独特组合,这种组织类型具有生长标记的规则分层,而现代晰脚类动物中不存在这种模式。Placodontia indet. aff. Cyamodus 和 Placodontia indet. 的骨组织类型与现代爬行动物相比,表明基础代谢率显著增加。生长线的双停顿线、年轮中的非年度休息线以及分层带的亚周期表明,齿龙的生长高度依赖于内源性和外源性因素。分类单元内的组织学和模型差异表明个体发育具有高度的可塑性,但生长模式存在性二型性,并且不能排除样本中存在不同的分类单元。