A Turonian polycotylid plesiosaur (Reptilia: Sauropterygia) from Obira Town, Hokkaido, and its biostratigraphic and paleoecological significance

被引:4
|
作者
Sato, Tamaki [1 ]
Hanai, Tomoya [2 ]
Hayashi, Shoji [3 ,4 ]
Nishimura, Tomohiro [5 ]
机构
[1] Tokyo Gakugei Univ, Dept Astron & Earth Sci, Koganei, Tokyo 1848501, Japan
[2] Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, Bunkyo Ku, 7-3-1 Hongo, Tokyo 1130033, Japan
[3] Okayama Univ Sci, Fac Biosphere Geosphere Sci, Kita Ku, Ridaicho 1-1, Okayama 7000005, Japan
[4] Osaka Univ, Grad Sch Engn, Div Mat & Mfg Sci, 2-1 Yamada Oka, Suita, Osaka 5650871, Japan
[5] Hobetsu Museum, 80-6 Hobetsu, Mukawa Town, Hokkaido 0540211, Japan
关键词
Cenomanian-Turonian boundary; histology; ontogeny; Plesiosauria; Polycotylidae; FORE-ARC BASIN; CENOMANIAN/TURONIAN BOUNDARY; ONTOGENIC STAGES; BONE-HISTOLOGY; SOUTHERN UTAH; TROPIC SHALE; JAPAN; PACHYOSTOSIS; PLIOSAUR; DINOSAUR;
D O I
10.2517/2017PR024
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The Polycotylidae are short-necked plesiosaurs known from the Cretaceous in various parts of the world, but only a few occurrences have been documented in Japan, where elasmosaurid remains are much more common. An indeterminate polycotylid specimen from the Upper Cretaceous in Obira Town, Hokkaido, is described. Characteristics of the vertebrae and clavicular arch support its taxonomic affinity. The Turonian occurrence of the specimen indicates the continuous presence of the Polycotylidae across the Cenomanian-Turonian boundary in the northwestern Pacific. Macroscopic osteological features of the vertebrae and clavicular arch indicate an advanced stage of ossification, and there are histological characteristics suggesting slowed growth. The osteoporotic-like condition implies a high degree of aquatic adaption.
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页码:265 / 278
页数:14
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