of
Sample: Sample No. L9-82-BS-32-3 -- USGS No. Cenozoic loc. M8065
Locality: Field No. L9-82-BS-32-3
Description: Mudstone or fine-grained sandstone dredged from continental margin at water depths of 1,300 to 1,500 meters in the Bering Sea; latitude 59o, 17.4 min., N., longitude 178o, 30.6 min. W. project number 9830-00506.
Location: Alaska Quadrangle: Unknown
Lat.: 59o17.4 ' Long.: 178o30.6 '
Reference
Title: Report on Referred Fossils ,  1982 (12/09)
Report by: Louie Marincovich , Jr.
Referred by: Mile Marlow
Age: Pliocene-Holocene (Pliocene? - Holocene)
Comment:This rare species was known previously only from the western Beaufort Sea in depths of 585 to 2,195 meters. The species has no record as a fossil and the genus is cited in the literature as “Recent and possibly Pliocene,” though without any reliable basis for the “Pliocene” age call. Many “Pliocene” age calls for Arctic invertebrates done in past years have turned out to be Pleistocene using more modern criteria.

The small chunk of matrix that contained this mollusk appears to be diatomaceous, and fragments of what look like ostracods are common too. It would be very worthwhile to submit this matrix, or more like it, to John Barron (P$S, Menlo Park) for diatom analysis and/or to Elisabeth Brouwers (P&S, Denver) for ostracode analysis; preferably, you have enough matrix to give them both a chance at age-dating your sample.

Because the one specimen of AXINULUS CAREYI is articulated and closed, and shows no signs of abrasion, it presumably was deposited in situ and not transported after death, and it is also very unlikely that it has been reworked from an older deposit.

Occurrence(s)
No. Group Name Qty Notes
1 Bivalves Axinulus careyi Bernard, 1979 - 1 articulated, closed specimen 1