Klein Nicole, Scheyer Torsten M
State Museum of Natural History Stuttgart, Rosenstein 1, 70191, Stuttgart, Germany.
Palaeontological Institute and Museum, University of Zurich, Karl Schmid-Strasse 4, CH-8006, Zurich, Switzerland.
Naturwissenschaften. 2017 Feb;104(1-2):4. doi: 10.1007/s00114-016-1427-3. Epub 2016 Dec 22.
The tuatara (Sphenodon punctatus) from New Zealand is often-erroneously-identified as a 'living fossil', although it is the lone survivor of a large, successful radiation of Rhynchocephalia, sister taxon to squamates (lizards and snakes), that thrived through the Mesozoic and Cenozoic and experienced an intricate evolution of life histories and feeding habits. Within Rhynchocephalia, only Pleurosauridae are thought to be marine and piscivorous. Here, we present bone histological data of the Jurassic pleurosaurid Palaeopleurosaurus, showing osteosclerosis (i.e. bone mass increase) in its gastralia, and some osteosclerosis in its rib but no increase in bone mass in the femur, supporting a gradual skeletal specialization for an aquatic way of life. Similar to Sphenodon, the bone tissue deposited in Palaeopleurosaurus is lamellar zonal bone. The femoral growth pattern in Palaeopleurosaurus differs from that of terrestrial Sphenodon in a more irregular spacing of growth marks and deposition of non-annual (i.e. non-continuous) rest lines, indicating strong dependency on exogenous factors. The annual growth mark count in adult but not yet fully grown Palaeopleurosaurus is much lower when compared to adult individuals of Sphenodon, which could indicate a lower lifespan for Palaeopleurosaurus. Whereas the gastral ribs of Palaeopleurosaurus and Sphenodon are similar in composition, the ribs of Sphenodon differ profoundly in being separated into a proximal tubular rib part with a thick cortex, and an elliptical, flared ventral part characterised by extremely thin cortical bone. The latter argues against a previously inferred protective function of the ventral rib parts for the vulnerable viscera in Sphenodon.
来自新西兰的喙头蜥(Sphenodon punctatus)常被错误地认定为“活化石”,尽管它是喙头目大量成功演化物种中的唯一幸存者,喙头目是有鳞目(蜥蜴和蛇)的姐妹分类单元,在中生代和新生代繁盛一时,经历了复杂的生活史和摄食习性演化。在喙头目内部,只有侧颈龙科被认为是海洋生物且以鱼类为食。在此,我们展示了侏罗纪侧颈龙科古侧颈龙的骨组织学数据,显示其腹肋有骨硬化现象(即骨量增加),肋骨也有一些骨硬化,但股骨骨量未增加,这支持了其骨骼为适应水生生活方式而逐渐特化的观点。与喙头蜥类似,古侧颈龙沉积的骨组织是层状带状骨。古侧颈龙的股骨生长模式与陆生喙头蜥不同,其生长标记间距更不规则,且有非年度(即不连续)休止线的沉积,表明对外部因素有很强的依赖性。与成年喙头蜥个体相比,尚未完全成年的古侧颈龙成年个体的年度生长标记计数要低得多,这可能表明古侧颈龙的寿命较短。尽管古侧颈龙和喙头蜥的腹肋组成相似,但喙头蜥的肋骨有很大差异,分为近端管状肋骨部分,其皮质较厚,以及椭圆形、向外扩张的腹侧部分,其皮质骨极薄。后者反驳了之前推断的喙头蜥腹侧肋骨部分对脆弱内脏的保护功能。