<documentid="30AC37210EB6C8493D47A137793206DF"ID-CLB-Dataset="42509"ID-DOI="10.11646/zootaxa.3861.5.1"ID-GBIF-Dataset="0b368704-d9cc-4a82-8248-bc4c06dcf781"ID-ISSN="1175-5326"ID-Zenodo-Dep="252462"ID-ZooBank="E62DB6C3-0C5F-4898-99C4-1BEC70DD1734"IM.materialsCitations_approvedBy="felipe"IM.metadata_approvedBy="felipe"IM.taxonomicNames_approvedBy="felipe"checkinTime="1460912037909"checkinUser="plazi"docAuthor="Kaim, Andrzej, Jenkins, Robert G., Tanabe, Kazushige & Kiel, Steffen"docDate="2014"docId="03F4372EFFF2685AFF3404B8FC22F83B"docLanguage="en"docName="zt03861p440.pdf"docOrigin="Zootaxa 3861 (5)"docStyle="DocumentStyle:647186512141C8FC8976D5BCC54AEB7D.9:Zootaxa.2013-.journal_article"docStyleId="647186512141C8FC8976D5BCC54AEB7D"docStyleName="Zootaxa.2013-.journal_article"docStyleVersion="9"docTitle="Pseudanchura biangulata Anderson 1938, n. sp."docType="treatment"docVersion="12"lastPageNumber="421"masterDocId="FFCD4F56FFE6684EFFA30151FFDCFFC8"masterDocTitle="Mollusks from late Mesozoic seep deposits, chiefly in California"masterLastPageNumber="440"masterPageNumber="401"pageNumber="421"updateTime="1732587323739"updateUser="ExternalLinkService">
<bibRefCitationid="EFCCFBC9FFF2685AFE7C04B8FD7AF9CB"author="Anderson"box="[479,678,1513,1539]"pageId="20"pageNumber="421"refString="Anderson, F. M. (1938) Lower Cretaceous deposits in California and Oregon. Geological Society of America Special Papers, 16, 1 - 339. http: // dx. doi. org / 10.1130 / spe 16 - p 1"type="journal article"year="1938">Anderson, 1938</bibRefCitation>
<figureCitationid="13669ABDFFF2685AFF3C075DFEC5F9EC"box="[159,281,1548,1573]"captionStart="FIGURE 9. A – D"captionStartId="21.[151,250,606,628]"captionTargetBox="[169,1417,195,584]"captionTargetId="figure@21.[169,1417,195,584]"captionTargetPageId="21"captionText="FIGURE 9. A – D. Pseudanchura biangulata (Anderson, 1938) from Late Barremian (Early Cretaceous) seep site at Eagle Creek, Shasta County, California, USA. A. CAS 73132. B – D. Juvenile CAS 73133. E – F. Diaphana sp. from? Valanginian (Early Cretaceous) seep carbonates at West Berryessa, Napa County, California, USA; GZG. INV. 84994."httpUri="https://zenodo.org/record/252471/files/figure.png"pageId="20"pageNumber="421">Fig. 9A–D</figureCitation>
<bibRefCitationid="EFCCFBC9FFF2685AFDF70705FD2DF9A2"author="Anderson"box="[596,753,1620,1642]"pageId="20"pageNumber="421"refString="Anderson, F. M. (1938) Lower Cretaceous deposits in California and Oregon. Geological Society of America Special Papers, 16, 1 - 339. http: // dx. doi. org / 10.1130 / spe 16 - p 1"type="journal article"year="1938">Anderson 1938</bibRefCitation>
The best preserved specimen (CAS 73132) is composed of six high-spired whorls. Two earliest are rounded with poorly visible ornamentation spiral riblets while the third whorl bears no ornamentation apart from strong median keel. The aperture and apertural extensions not preserved in the investigated specimens.
<emphasisid="B9295A2AFFF2685AFF640653FE29F8D3"bold="true"box="[199,501,1794,1819]"pageId="20"pageNumber="421">Material and occurrence.</emphasis>
Two poorly preserved juvenile specimens (
<collectionCodeid="ED4C1EFDFFF2685AFC7E0652FBC9F8D3"LSID="urn:lsid:biocol.org:col:34700"box="[989,1045,1795,1819]"httpUri="http://biocol.org/urn:lsid:biocol.org:col:15690"name="California Academy of Sciences"pageId="20"pageNumber="421">CAS</collectionCode>
73132, 73133). Eagle Creek (Late Barremian, Early Cretaceous).
has been reported from a couple of localities in the Ono area by
<bibRefCitationid="EFCCFBC9FFF2685AFB0D061BFAB0F8AB"author="Anderson"box="[1198,1388,1866,1891]"pageId="20"pageNumber="421"refString="Anderson, F. M. (1938) Lower Cretaceous deposits in California and Oregon. Geological Society of America Special Papers, 16, 1 - 339. http: // dx. doi. org / 10.1130 / spe 16 - p 1"type="journal article"year="1938">Anderson (1938)</bibRefCitation>
and it remains uncertain whether they were seep locations or "normal" deep water sediments. Most likely the association of
with seep carbonates is fortuitous as aporrhaids are gastropods typical for soft bottom marine environments during Mesozoic times and they have been found at various Jurassic to Paleocene seep deposits (
<bibRefCitationid="EFCCFBC9FFF2685AFEA2068BFE0CF83B"author="Kaim"box="[257,464,2010,2035]"pageId="20"pageNumber="421"refString="Kaim, A., Kobayashi, Y., Echizenya, H. Jenkins, R. G. & Tanabe, K. (2008 b) Chemosynthesis-based associations on Cretaceous plesiosaurid carcasses. Acta Palaeontologica Polonica, 53, 97 - 104. http: // dx. doi. org / 10.4202 / app. 2008.0106"type="journal article"year="2008"yearSuffix="b">
<bibRefCitationid="EFCCFBC9FFF2685AFD7D068BFC2EF83B"author="Agirrezabala"box="[734,1010,2010,2035]"pageId="20"pageNumber="421"refString="Agirrezabala, L. M., Kiel, S., Blumenberg, M., Schafer, N. & Reitner, J. (2013) Outcrop analogues of pockmarks and associated methane-seep carbonates: A case study from the Lower Cretaceous (Albian) of the Basque-Cantabrian Basin, western Pyrenees. Palaeogeography, Palaeoclimatology, Palaeoecology, 390, 94 - 115. http: // dx. doi. org / 10.1016 / j. palaeo. 2012.11.020"type="journal article"year="2013">