Stratified prokaryote network in the oxic-anoxic transition of a deep sea halocline (Articolo in rivista)

Type
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  • Stratified prokaryote network in the oxic-anoxic transition of a deep sea halocline (Articolo in rivista) (literal)
Anno
  • 2006-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1038/nature04418 (literal)
Alternative label
  • Daffonchio, D.; Borin S.; Brusa T.; Brusetti L.; Van Der Wielen P.W.J.J.; Bolhuis H.; Yakimov M.M.; D'Auria G.; Giuliano L.; Marty D.; Tamburini C.; McGenity, T.J.; Hallsworth J.E.; Sass A.M.; Timmis, K.N.; Tselepides, A.; De Lange G.J.; Hübner A.; Thomson J.; Varnavas S.P.; Gasparoni F.; Gerber H.W.; Malinverno E.; Corselli C.; Garcin J.; McKew B.; Golyshin P.N.; Lampadariou N.; Polymenakou P.; Calore, D.; Cenedese S.; Zanon F.; Hoog S.; (2006)
    Stratified prokaryote network in the oxic-anoxic transition of a deep sea halocline
    in Nature (Lond.)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Daffonchio, D.; Borin S.; Brusa T.; Brusetti L.; Van Der Wielen P.W.J.J.; Bolhuis H.; Yakimov M.M.; D'Auria G.; Giuliano L.; Marty D.; Tamburini C.; McGenity, T.J.; Hallsworth J.E.; Sass A.M.; Timmis, K.N.; Tselepides, A.; De Lange G.J.; Hübner A.; Thomson J.; Varnavas S.P.; Gasparoni F.; Gerber H.W.; Malinverno E.; Corselli C.; Garcin J.; McKew B.; Golyshin P.N.; Lampadariou N.; Polymenakou P.; Calore, D.; Cenedese S.; Zanon F.; Hoog S.; (literal)
Pagina inizio
  • 203 (literal)
Pagina fine
  • 207 (literal)
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  • 440 (literal)
Rivista
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  • 5 (literal)
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  • 7081 (literal)
Note
  • PubMe (literal)
  • Scopu (literal)
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • CoNISMa, Ulr Università degli Studi di Milano, DiSTAM, 20133 Milan, Italy Department of Microbial Ecology, CEES, University of Groningen, 9751 NN Haren, Netherlands Istituto Per l'Ambiente Marino Costiero, CNR, 98122 Messina, Italy LMGEM, UMR 6117 CNRS Université de la Mediterranée, 13288 Marseille, France Department of Biological Sciences, University of Essex, Colchester, Essex CO4 3SQ, United Kingdom Division of Microbiology, GBF, 38122 Braunschweig, Germany Institute of Marine Biology of Crete, 71003 Heraklion, Greece Faculty of Geosciences, Geochemistry, Utrecht University, 3584 CD Utrecht, Netherlands Southampton Oceanography Centre, Southampton SO14 3EE, United Kingdom Department of Geology, University of Patras, 26100 Patras, GreeceTecnomare S.p.A., ENI Group, 30124 Venice, Italy Technische Fachhochschule Berlin, University of Applied Science, 13353 Berlin, Germany CoNISMa, Ulr Università degli Studi di Milano Bicocca, DGSG, 20126 Milan, Italy (literal)
Titolo
  • Stratified prokaryote network in the oxic-anoxic transition of a deep sea halocline (literal)
Abstract
  • The chemical composition of the Bannock basin has been studied in some detail1,2. We recently showed that unusual microbial populations, including a new division of Archaea (MSBL1)3, inhabit the NaCl-rich hypersaline brine. High salinities tend to reduce biodiversity4, but when brines come into contact with fresher water the natural haloclines formed frequently contain gradients of other chemicals, including permutations of electron donors and acceptors, that may enhance microbial diversity, activity and biogeochemical cycling5,6. Here we report a 2.5-m-thick chemocline with a steep NaCl gradient at 3.3 km within the water column betweeen Bannock anoxic hypersaline brine7 and overlying sea water. The chemocline supports some of the most biomass-rich and active microbial communities in the deep sea, dominated by Bacteria rather than Archaea, and including four major new divisions of Bacteria. Significantly higher metabolic activities were measured in the chemocline than in the overlying sea water and underlying brine; functional analyses indicate that a range of biological processes is likely to occur in the chemocline. Many prokaryotic taxa, including the phylogenetically new groups, were confined to defined salinities, and collectively formed a diverse, sharply stratified, deep-sea ecosystem with sufficient biomass to potentially contribute to organic geological deposits. (literal)
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