CHONDRICHTHYES HUXLEY, 1880

Charles L. Powell, Ii, Clites, Erica C. & Poust, Ashley W., 2019, Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA, PaleoBios 36, pp. 1-34 : 18

publication ID

https://doi.org/ 10.5070/P9361044567

publication LSID

lsid:zoobank.org:pub:EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9

persistent identifier

https://treatment.plazi.org/id/7A6D87C5-FFCB-1E03-7B6A-4E84FA92FDB4

treatment provided by

Felipe

scientific name

CHONDRICHTHYES HUXLEY, 1880
status

 

CHONDRICHTHYES HUXLEY, 1880

CARCHARINIFORMES COMPAGNO, 1973 CARCHARHINIFORMES INDET.

Two small (1–2 mm) fragments of a shark tooth (UCMP 270010) nonetheless preserve portions of a serrated crown. The serrations are very fine, symmetrical, and numerous with 6–7 per millimeter.

It is difficult to identify these fragments, but several shark groups have serrations of similar size and density, including members of the carcharhinids and the Lamniformes . The fine and dense nature of the serrations are more similar to the genus Carcharhinus than the larger serrations of Carcharocles , but the incomplete fossil does not permit identification beyond Order.

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