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dc.contributor.authorTaylor, James
dc.contributor.authorDevey, Colin
dc.contributor.authorLe Saout, Morgane
dc.contributor.authorPetersen, Sven
dc.contributor.authorKwasnitschka, Tom
dc.contributor.authorFrutos, Inmaculada
dc.contributor.authorLinse, Katrin
dc.contributor.authorLörz, Anne-Nina
dc.contributor.authorPałgan, Dominik
dc.contributor.authorTandberg, Anne Helene Solberg
dc.contributor.authorSvavarsson, Jörundur
dc.contributor.authorThorhallsson, Daniel
dc.contributor.authorTomkowicz, Adrianna
dc.contributor.authorEgilsdottir, Hrönn
dc.contributor.authorRagnarsson, Stefán Á.
dc.contributor.authorRenz, Jasmin
dc.contributor.authorMarkaseva, Elena A.
dc.contributor.authorGollner, Sabine
dc.contributor.authorPaulus, Eva
dc.contributor.authorKongsrud, Jon Anders
dc.contributor.authorBeermann, Jan
dc.contributor.authorKocot, Kevin M.
dc.contributor.authorMeißner, Karin
dc.contributor.authorBartholomä, Alexander
dc.contributor.authorHoffman, Leon
dc.contributor.authorVannier, Pauline
dc.contributor.authorMarsteinsson, Viggó
dc.contributor.authorRapp, Hans Tore
dc.contributor.authorDiaz-Agras, Guillermo
dc.contributor.authorTato, Ramiro
dc.contributor.authorBrix, Saskia
dc.date.accessioned2022-02-14T08:49:42Z
dc.date.available2022-02-14T08:49:42Z
dc.date.created2021-11-11T10:18:49Z
dc.date.issued2021
dc.identifier.issn2296-7745
dc.identifier.urihttps://hdl.handle.net/11250/2978622
dc.description.abstractDuring RV MS Merian expedition MSM75, an international, multidisciplinary team explored the Reykjanes Ridge from June to August 2018. The first area of study, Steinahóll (150–350 m depth), was chosen based on previous seismic data indicating hydrothermal activity. The sampling strategy included ship- and AUV-mounted multibeam surveys, Remotely Operated Vehicle (ROV), Epibenthic Sledge (EBS), and van Veen grab (vV) deployments. Upon returning to Steinahóll during the final days of MSM75, hydrothermal vent sites were discovered using the ROV Phoca (Kiel, GEOMAR). Here we describe and name three new, distinct hydrothermal vent site vulnerable marine ecosystems (VMEs); Hafgufa, Stökkull, Lyngbakr. The hydrothermal vent sites consisted of multiple anhydrite chimneys with large quantities of bacterial mats visible. The largest of the three sites (Hafgufa) was mapped, and reconstructed in 3D. In total 23,310 individual biological specimens were sampled comprising 41 higher taxa. Unique fauna located in the hydrothermally venting areas included two putative new species of harpacticoid copepod (Tisbe sp. nov. and Amphiascus sp. nov.), as well as the sponge Lycopodina cupressiformis (Carter, 1874). Capitellidae Grube, 1862 and Dorvilleidae Chamberlin, 1919 families dominated hydrothermally influenced samples for polychaetes. Around the hydrothermally influenced sites we observed a notable lack of megafauna, with only a few species being present. While we observed hydrothermal associations, the overall species composition is very similar to that seen at other shallow water vent sites in the north of Iceland, such as the Mohns Ridge vent fields, particularly with peracarid crustaceans. We therefore conclude the community overall reflects the usual “background” fauna of Iceland rather than consisting of “vent endemic” communities as is observed in deeper vent systems, with a few opportunistic species capable of utilizing this specialist environment.en_US
dc.language.isoengen_US
dc.publisherFrontiers Mediaen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleThe Discovery and Preliminary Geological and Faunal Descriptions of Three New Steinahóll Vent Sitesen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2021 Taylor, Devey, Le Saout, Petersen, Frutos, Linse, Lörz, Pałgan, Tandberg, Svavarsson, Thorhallsson, Tomkowicz, Egilsdóttir, Ragnarsson, Renz, Markhaseva, Gollner, Paulus, Kongsrud, Beermann, Kocot, Meißner, Bartholomä, Hoffman, Vannier, Marteinsson, Rapp, Díaz-Agras, Tato and Brix.en_US
dc.source.articlenumber520713en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.3389/fmars.2021.520713
dc.identifier.cristin1953554
dc.source.journalFrontiers in Marine Scienceen_US
dc.subject.nsiVDP::Marinbiologi: 497en_US
dc.subject.nsiVDP::Marine biology: 497en_US
dc.subject.nsiVDP::Marinbiologi: 497en_US
dc.subject.nsiVDP::Marine biology: 497en_US
dc.identifier.citationFrontiers in Marine Science. 2021, 8, 520713.en_US
dc.source.volume8en_US


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal