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.

All labels observed (1)

Label Occurrences
Kolbeinsey Ridge hydrothermal vent field canonical 1

How this entity was disambiguated

Statements (38)

Predicate Object
instanceOf hydrothermal vent field
seafloor geothermal area
associatedWith Ignicoccus hospitalis
Nanoarchaeum equitans
biogeographicProvince North Atlantic hydrothermal vent province
countryOffshoreFrom Iceland
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
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
knownFor discovery of Nanoarchaeum equitans
high-temperature hydrothermal activity
hyperthermophilic archaeal communities
locatedIn Mid-Atlantic region
North Atlantic Ocean
linked to: North Atlantic
locatedOn Kolbeinsey Ridge
partOf Mid-ocean ridge system
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
North American Plate

How these facts were elicited

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