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The Science of Nature

, 104:4 | Cite as

Microanatomy and life history in Palaeopleurosaurus (Rhynchocephalia: Pleurosauridae) from the Early Jurassic of Germany

  • Nicole Klein
  • Torsten M. Scheyer
Original Paper

Abstract

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.

Keywords

Sphenodon punctatus Aquatic adaptation Histology Microanatomy Femur Ribs Gastralia 

Notes

Acknowledgements

We are indebted to R. Schoch (SMNS) and C. Klug (PIMUZ) who kindly gave permission for sampling specimens. Ch. Wimmer-Pfeil (SMNS) and Ch. Kolb and K. Veitschegger (PIMUZ) are thanked for the production of thin sections. M. Kamenz (SMNS) helped to prepare the specimen for histological sampling. This work was partially funded by the SNSF (grant no. 31003A-149506 to TMS).

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Copyright information

© Springer-Verlag Berlin Heidelberg 2016

Authors and Affiliations

  1. 1.State Museum of Natural History StuttgartStuttgartGermany
  2. 2.Palaeontological Institute and MuseumUniversity of ZurichZurichSwitzerland

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