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dc.contributor.authorConnelly, Douglas P.
dc.contributor.authorCopley, Jonathan T.
dc.contributor.authorMurton, Bramley J.
dc.contributor.authorStansfield, Kate
dc.contributor.authorTyler, Paul A.
dc.contributor.authorGerman, Christopher R.
dc.contributor.authorVan Dover, Cindy L.
dc.contributor.authorAmon, Diva
dc.contributor.authorFurlong, Maaten
dc.contributor.authorGrindlay, Nancy
dc.contributor.authorHayman, Nicholas
dc.contributor.authorHühnerbach, Veit
dc.contributor.authorJudge, Maria
dc.contributor.authorLe Bas, Tim
dc.contributor.authorMcPhail, Stephen
dc.contributor.authorMeier, Alexandra
dc.contributor.authorNakamura, Ko-ichi
dc.contributor.authorNye, Verity
dc.contributor.authorPebody, Miles
dc.contributor.authorPedersen, Rolf B.
dc.contributor.authorPlouviez, Sophie
dc.contributor.authorSands, Carla
dc.contributor.authorSearle, Roger C.
dc.contributor.authorStevenson, Peter
dc.contributor.authorTaws, Sarah
dc.contributor.authorWilcox, Sally
dc.date.accessioned2018-09-20T16:03:52Z
dc.date.available2018-09-20T16:03:52Z
dc.date.issued2012-01-10
dc.identifier.citationConnelly, Douglas P. Copley, Jonathan T.; Murton, Bramley J.; Stansfield, Kate; Tyler, Paul A.; German, Christopher R.; Van Dover, Cindy L.; Amon, Diva; Furlong, Maaten; Grindlay, Nancy; Hayman, Nicholas; Hühnerbach, Veit; Judge, Maria; Le Bas, Tim; McPhail, Stephen; Meier, Alexandra; Nakamura, Ko-ichi; Nye, Verity; Pebody, Miles; Pedersen, Rolf B.; Plouviez, Sophie; Sands, Carla; Searle, Roger C.; Stevenson, Peter; Taws, Sarah; Wilcox, Sally (2012). Hydrothermal vent fields and chemosynthetic biota on the world's deepest seafloor spreading centre. Nature Communications 3 ,
dc.identifier.issn2041-1723
dc.identifier.urihttp://hdl.handle.net/10379/10872
dc.description.abstractThe Mid-Cayman spreading centre is an ultraslow-spreading ridge in the Caribbean Sea. Its extreme depth and geographic isolation from other mid-ocean ridges offer insights into the effects of pressure on hydrothermal venting, and the biogeography of vent fauna. Here we report the discovery of two hydrothermal vent fields on the Mid-Cayman spreading centre. The Von Damm Vent Field is located on the upper slopes of an oceanic core complex at a depth of 2,300 m. High-temperature venting in this off-axis setting suggests that the global incidence of vent fields may be underestimated. At a depth of 4,960 m on the Mid-Cayman spreading centre axis, the Beebe Vent Field emits copper-enriched fluids and a buoyant plume that rises 1,100 m, consistent with >400 degrees C venting from the world's deepest known hydrothermal system. At both sites, a new morphospecies of alvinocaridid shrimp dominates faunal assemblages, which exhibit similarities to those of Mid-Atlantic vents.
dc.publisherSpringer Nature
dc.relation.ispartofNature Communications
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Ireland
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/ie/
dc.subjectmid-atlantic ridge
dc.subjectmassive sulfides
dc.subjectcritical-point
dc.subjectcayman trough
dc.subjectindian ridge
dc.subjectbiogeography
dc.subjectseawater
dc.subjectocean
dc.subjectevolution
dc.subjectsystems
dc.titleHydrothermal vent fields and chemosynthetic biota on the world's deepest seafloor spreading centre
dc.typeArticle
dc.identifier.doi10.1038/ncomms1636
dc.local.publishedsourcehttps://www.nature.com/articles/ncomms1636.pdf
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Attribution-NonCommercial-NoDerivs 3.0 Ireland
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 Ireland