Plesiosauria indet
publication ID |
https://doi.org/ 10.5852/cr-palevol2023v22a6 |
publication LSID |
urn:lsid:zoobank.org:pub:AB8DCA69-9BE5-44F1-877D-0E65F73B7186 |
DOI |
https://doi.org/10.5281/zenodo.14224676 |
persistent identifier |
https://treatment.plazi.org/id/0A1587CB-FFBC-7546-8D7C-F82EFB392F02 |
treatment provided by |
Felipe |
scientific name |
Plesiosauria indet |
status |
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( Fig. 5 I-L)
MATERIAL. — NPC CD 462 , 463 , 464 , 465 , four isolated teeth .
LOCALITY AND HORIZON. — Mangahouanga Stream , a northern tributary of Te Hoe River , inland Hawke’s Bay, North Island ( Fig. 1), New Zealand. Maungataniwha Sandstone Member of the Tahora Formation. Upper Campanian-lower Maastrichtian ( Vajda & Raine 2010).
REMARKS
These teeth have their enamel with few well-marked striations, and the crown comparatively shorter and blunter than those typically observed in elasmosaurids such as Tuarangisaurus keyesi Wiffen & Moisley, 1986 holotype ( Wiffen & Moisley 1986: figs 1-3, 15, 16). The lack of distinctive dental traits the specimens are reffered to Plesiosauria indet.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
Kingdom |
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Phylum |
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Class |
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SubClass |
Sauropterygia |
Order |
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SuperFamily |
Plesiosauroidea |
Family |