PROPEAMUSSIIDAE ABBOTT, 1954

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 : 9

publication ID

https://doi.org/ 10.5070/P9361044567

publication LSID

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

DOI

https://doi.org/10.5281/zenodo.13750302

persistent identifier

https://treatment.plazi.org/id/7A6D87C5-FFD2-1E1A-7B66-4E65FA9FFEA9

treatment provided by

Felipe

scientific name

PROPEAMUSSIIDAE ABBOTT, 1954
status

 

PROPEAMUSSIIDAE ABBOTT, 1954 View in CoL

FIG. 13 View Figure 13

Two partial, mostly decorticated, possibly right, valves of an indeterminate Propeamussiidae are represented in the Tsm Caldecott Tunnel fauna. On first glance they appear to have interior radial ribs as in the genus Propeamussium ; however, they do not originate at the umbo and therefore are interpreted as cracks formed in the shell during or after deposition. The family is distributed worldwide and according to Waller (1971) occurs in water depths from 275 to 2,740 m. It ranges in age from the Jurassic to Holocene (Moore 1984).

Kingdom

Animalia

Phylum

Mollusca

Class

Bivalvia

Order

Pectinida

Family

Propeamussiidae

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