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.