A late Paleoproterozoic (1.74 Ga) deep‐sea, low‐temperature, iron‐oxidizing microbial hydrothermal vent community from Arizona, USA

Modern marine hydrothermal vents occur in a wide variety of tectonic settings and are characterized by seafloor emission of fluids rich in dissolved chemicals and rapid mineral precipitation. Some hydrothermal systems vent only low‐temperature Fe‐rich fluids, which precipitate deposits dominated by...

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Bibliographic Details
Published in:Geobiology 2021-05, Vol.19 (3), p.228-249
Main Authors: Little, Crispin T. S., Johannessen, Karen C., Bengtson, Stefan, Chan, Clara S., Ivarsson, Magnus, Slack, John F., Broman, Curt, Thorseth, Ingunn H., Grenne, Tor, Rouxel, Olivier J., Bekker, Andrey
Format: Article
Language:English
Subjects:
Arizona
Benthos
Den föränderliga jorden
Dissolved chemicals
Diversity of life
Encrustation
Fe-oxidizing bacteria
Filaments
Fluids
Hydrothermal springs
Hydrothermal Vents
Iron
Iron - analysis
jasper
late Paleoproterozoic
Livets mångfald
Manganese
Mineralization
Mineralogy
Ocean floor
Oceans
Oceans and Seas
Oxidation
Oxidation-Reduction
Oxidoreductions
Precambrian
Sciences of the Universe
Seawater
Secretion
Sheaths
Silica
Temperature
The changing Earth
Verde mining district
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