Kolbeinsey Ridge hydrothermal vent field

E890315

The Kolbeinsey Ridge hydrothermal vent field is a seafloor area of geothermal activity along the Kolbeinsey Ridge in the North Atlantic, notable as the site where the hyperthermophilic archaeon Nanoarchaeum equitans was first discovered.

Jump to: Statements Referenced by

Statements (38)

Predicate Object
instanceOf hydrothermal vent field
seafloor geothermal area
associatedWith Ignicoccus hospitalis NERFINISHED
Nanoarchaeum equitans NERFINISHED
biogeographicProvince North Atlantic hydrothermal vent province NERFINISHED
countryOffshoreFrom Iceland NERFINISHED
discovered before 2002
ecosystemType deep-sea chemosynthetic community
environmentType deep-sea hydrothermal vent environment
fluidSource geothermal circulation through oceanic crust
geologicalSetting divergent plate boundary
mid-ocean ridge
hasDiscovery Nanoarchaeum equitans NERFINISHED
hasHydrothermalActivity black smoker-type venting
high-temperature fluid discharge
hasResearchInterest early evolution of Archaea
extreme temperature adaptation in microbes
microbial symbiosis
heatSource magma beneath mid-ocean ridge
isPartOf Kolbeinsey Ridge volcanic system NERFINISHED
knownFor discovery of Nanoarchaeum equitans
high-temperature hydrothermal activity
hyperthermophilic archaeal communities
locatedIn Mid-Atlantic region NERFINISHED
North Atlantic Ocean NERFINISHED
locatedOn Kolbeinsey Ridge NERFINISHED
partOf Mid-ocean ridge system NERFINISHED
process seafloor spreading
researchField extremophile biology
geochemistry
marine microbiology
oceanography
significance evidence for diverse archaeal lineages in hydrothermal vents
type locality of Nanoarchaeum equitans
supports chemosynthetic ecosystems
hyperthermophilic microorganisms
tectonicPlate Eurasian Plate NERFINISHED
North American Plate NERFINISHED

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Nanoarchaeum equitans discoveryLocation Kolbeinsey Ridge hydrothermal vent field