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dc.contributor.authorGeorgieva, M
dc.contributor.authorPaull, CK
dc.contributor.authorLittle, CTS
dc.contributor.authorMcGann, M
dc.contributor.authorSahy, D
dc.contributor.authorCondon, D
dc.contributor.authorLundsten, L
dc.contributor.authorPewsey, J
dc.contributor.authorCaress, DW
dc.contributor.authorVrijenhoek, RC
dc.date.accessioned2019-03-20T10:38:22Z
dc.date.available2019-03-20T10:38:22Z
dc.date.issued2019-03-19
dc.date.submitted2019-03-19
dc.identifier.citationGeorgieva MN, Paull CK, Little CTS, McGann M, Sahy D, Condon D, Lundsten L, Pewsey J, Caress DW and Vrijenhoek RC (2019) Discovery of an Extensive Deep-Sea Fossil Serpulid Reef Associated With a Cold Seep, Santa Monica Basin, California. Front. Mar. Sci. 6:115. doi: 10.3389/fmars.2019.00115en_US
dc.identifier.issn2296-7745
dc.identifier.doi10.3389/fmars.2019.00115
dc.identifier.urihttp://hdl.handle.net/10141/622448
dc.description.abstractMultibeam bathymetric mapping of the Santa Monica Basin in the eastern Pacific has revealed the existence of a number of elevated bathymetric features, or mounds, harboring cold seep communities. During 2013–2014, mounds at 600 m water depth were observed for the first time and sampled by Monterey Bay Aquarium Research Institute’s ROV Doc Ricketts. Active cold seeps were found, but surprisingly one of these mounds was characterized by massive deposits composed of fossil serpulid worm tubes (Annelida: Serpulidae) exhibiting various states of mineralization by authigenic carbonate. No living serpulids with equivalent tube morphologies were found at the site; hence the mound was termed “Fossil Hill.” In the present study, the identity of the fossil serpulids and associated fossil community, the ages of fossils and authigenic carbonates, the formation of the fossil serpulid aggregation, and the geological structure of the mound are explored. Results indicate that the tubes were most likely made by a deep-sea serpulid lineage, with radiocarbon dating suggesting that they have a very recent origin during the Late Pleistocene, specifically to the Last Glacial Maximum 20,000 years ago. Additional U-Th analyses of authigenic carbonates mostly corroborate the radiocarbon dates, and also indicate that seepage was occurring while the tubes were being formed. We also document similar, older deposits along the approximate trajectory of the San Pedro Basin Fault. We suggest that the serpulid tube facies formed in situ, and that the vast aggregation of these tubes at Fossil Hill is likely due to a combination of optimal physical environmental conditions and chemosynthetic production, which may have been particularly intense as a result of sea-level lowstand during the Last Glacial Maximum.en_US
dc.publisherFrontiers Mediaen_US
dc.relation.isreplacedby10141/622649
dc.relation.isreplacedbyhttp://hdl.handle.net/10141/622649
dc.rightsopenAccessen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleDiscovery of an extensive deep-sea fossil serpulid reef associated with a cold seep, Santa Monica Basin, Californiaen_US
dc.typeJournal Articleen_US
dc.identifier.journalFrontiers in Marine Scienceen_US
dc.identifier.volume6en_US
pubs.organisational-group/Natural History Museum
pubs.organisational-group/Natural History Museum/Science Group
pubs.organisational-group/Natural History Museum/Science Group/Functional groups
pubs.organisational-group/Natural History Museum/Science Group/Functional groups/Research
pubs.organisational-group/Natural History Museum/Science Group/Functional groups/Research/LS Research
pubs.organisational-group/Natural History Museum/Science Group/Life Sciences
dc.embargoNot knownen_US
elements.import.authorGeorgieva, Men_US
elements.import.authorPaull, CKen_US
elements.import.authorLittle, CTSen_US
elements.import.authorMcGann, Men_US
elements.import.authorSahy, Den_US
elements.import.authorCondon, Den_US
elements.import.authorLundsten, Len_US
elements.import.authorPewsey, Jen_US
elements.import.authorCaress, DWen_US
elements.import.authorVrijenhoek, RCen_US
dc.description.nhmCopyright © 2019 Georgieva, Paull, Little, McGann, Sahy, Condon, Lundsten, Pewsey, Caress and Vrijenhoek. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. The attached file is the published version of the article.en_US
dc.subject.nhmtubewormen_US
dc.subject.nhmlast glacial maximumen_US
dc.subject.nhmgas hydrateen_US
dc.subject.nhmvesicomyidaeen_US
dc.subject.nhmAnnelidaen_US
dc.subject.nhmpaleobiologyen_US
dc.subject.nhmeastern Pacificen_US
dc.subject.nhmmethane seepen_US
refterms.dateFOA2019-03-20T10:38:23Z


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