Carcharhinus obscurus, LESUEUR, 1818

Charles L. Powell, Ii, Clites, Erica C. & Poust, Ashley W., 2022, Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA, PaleoBios 36, pp. 1-34 : 23

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-FFC0-1E08-79C6-4CA6FEEFFB02

treatment provided by

Felipe

scientific name

Carcharhinus obscurus
status

 

CARCHARHINUS OBSCURUS LESUEUR, 1818 View in CoL

FIG. 41 View Figure 41

early Miocene L. columbiana ( Clark and Arnold, 1923) is distinguished by its smaller size and being more inflated. Lucinoma aequizonatum (Stearns, 1890) occurs in the eastern Pacific, however, it is not known from deposits older than middle Pleistocene (Powell and Ponti 2007), and is easily distinguished by its different shape and broader sculpture.

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