ONTOGENIC EVOLUTION OF BONE-STRUCTURE IN LATE CRETACEOUS PLESIOSAURIAFROM NEW-ZEALAND

Citation
J. Wiffen et al., ONTOGENIC EVOLUTION OF BONE-STRUCTURE IN LATE CRETACEOUS PLESIOSAURIAFROM NEW-ZEALAND, Geobios, 28(5), 1995, pp. 625-640
Citations number
57
Categorie Soggetti
Paleontology
Journal title
ISSN journal
00166995
Volume
28
Issue
5
Year of publication
1995
Pages
625 - 640
Database
ISI
SICI code
0016-6995(1995)28:5<625:OEOBIL>2.0.ZU;2-S
Abstract
Histological observations of homologous bones (vertebrae, ribs, humeru s, phalanges) among conspecific juvenile and adult Upper Cretaceous pl esiosaurs from New Zealand (elasmosaurs and pliosaurs) demonstrates a unique ''ontogenetic trajectory'' of skeletal histogenesis in these an imals. While juveniles demonstrate a ''pachyosteosclerotic'' condition of the skeleton, adults have a very light ''osteoporotic-like'' bone structure. Until now, one or the other of these histological specializ ations was known among aquatic tetrapods, adapted along contrasting pa thways to this environment, either by ballasting (pachyosteosclerosis : e.g. sirenians) or by lightening (osteoporotic-like adaptation : e.g . modern cetaceans) of the skeleton. The successive occurrence of thes e constrasting conditions during ontogenesis of a single organism had never been reported, as far as we know, but could well be an ontogenet ic characteristic of Plesiosaurs sensu lato. The significance of these findings are discussed in various phylogenetical, functional and pale oecological contexts. The ontogenetic trajectory of the plesiosaur ske leton is interpreted within the general framework of developmental het erochrony. Specifically, it suggests that juvenile plesiosaurs kept a conservative (plesiomorphic) ecology for sauropterygians, as poorly mo bile, lagoon or shore dwellers while, in contrast, the adults would sh ift towards much more active locomotory behaviours in the open sea.