Papers

Peer-reviewed
Jul 3, 2014

A probable shark dorsal fin spine fragment from the Early Triassic of the Arrow Rocks sequence, Whangaroa, northern New Zealand

New Zealand Journal of Geology and Geophysics
  • J. A. Grant-Mackie
  • ,
  • S. Yamakita
  • ,
  • T. Matsumoto
  • ,
  • R. S. Hori
  • ,
  • A. Takemura
  • ,
  • Y. Aita
  • ,
  • S. Takahashi
  • ,
  • H. J. Campbell

Volume
57
Number
3
First page
295
Last page
299
Language
English
Publishing type
Research paper (scientific journal)
DOI
10.1080/00288306.2014.889722
Publisher
Taylor and Francis Asia Pacific

The ornament on a small external cast in pink chert shows considerable similarity with that of various Middle Palaeozoic and Triassic fish genera. It comes from the Permian-Triassic Oruatemanu Formation of Arrow Rocks, Whangaroa area, eastern Northland. Conodont faunas from a few metres above and below the sample allow correlation with the Neospathodus pakistanensis zone of the Early Triassic, which is assigned to the late Dienerian (late Induan), with adjacent conodont zone faunas in their correct stratigraphic association. The cast is assumed to be that of a small fragment of fin spine, most likely from the junction area of the crown and root on the right-hand side of a dorsal fin spine, possibly anterior, of a marine ctenacanthoid shark, a basal shark order not previously recorded from New Zealand.

Link information
DOI
https://doi.org/10.1080/00288306.2014.889722
ID information
  • DOI : 10.1080/00288306.2014.889722
  • ISSN : 1175-8791
  • ISSN : 0028-8306
  • SCOPUS ID : 84926408549

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