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Episodic fresh surface waters in the Eocene Arctic Ocean
Brinkhuis, H.; Schouten, S.; Collinson, M.E.; Sluijs, A.; Sinninghe Damsté, J.S.; Dickens, G.R.; Huber, M.; Cronin, T.M.; Onodera, J.; Takahashi, K.; Bujak, J.P.; Stein, R.; van der Burgh, J.; Eldrett, J.S.; Harding, I.C.; Lotter, A.F.; Sangiorgi, F.; van Konijnenburg-van Cittert, H.; de Leeuw, J.W.; Matthiessen, J.; Backman, J.; Moran, K.; Expedition 302 Scientists (2006). Episodic fresh surface waters in the Eocene Arctic Ocean. Nature (Lond.) 441(7093): 606-609
In: Nature: International Weekly Journal of Science. Nature Publishing Group: London. ISSN 0028-0836; e-ISSN 1476-4687, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

    Environments > Palaeoenvironments
    Geological time > Phanerozoic > Geological time > Cenozoic > Paleogene > Palaeogene > Eocene
    Water > Fresh water
    PN, Arctisch [Marine Regions]
    Marien; Zoet water

Auteurs  Top 
  • Brinkhuis, H., meer
  • Schouten, S.
  • Collinson, M.E.
  • Sluijs, A.
  • Sinninghe Damsté, J.S.
  • Dickens, G.R.
  • Huber, M.
  • Cronin, T.M., meer
  • Onodera, J.
  • Takahashi, K.
  • Bujak, J.P.
  • Stein, R.
  • van der Burgh, J.
  • Eldrett, J.S.
  • Harding, I.C.
  • Lotter, A.F.
  • Sangiorgi, F.
  • van Konijnenburg-van Cittert, H.
  • de Leeuw, J.W., meer
  • Matthiessen, J.
  • Backman, J.
  • Moran, K.
  • Expedition 302 Scientists

    It has been suggested, on the basis of modern hydrology and fully coupled palaeoclimate simulations, that the warm greenhouse conditions1 that characterized the early Palaeogene period (55--45Myr ago) probably induced an intensified hydrological cycle2 with precipitation exceeding evaporation at high latitudes3. Little field evidence, however, has been available to constrain oceanic conditions in the Arctic during this period. Here we analyse Palaeogene sediments obtained during the Arctic Coring Expedition, showing that large quantities of the free-floating fern Azolla grew and reproduced in the Arctic Ocean by the onset of the middle Eocene epoch (~50Myr ago). The Azolla and accompanying abundant freshwater organic and siliceous microfossils indicate an episodic freshening of Arctic surface waters during an ~800,000-year interval. The abundant remains of Azolla that characterize basal middle Eocene marine deposits of all Nordic seas4-7 probably represent transported assemblages resulting from freshwater spills from the Arctic Ocean that reached as far south as the North Sea8. The termination of the Azolla phase in the Arctic coincides with a local sea surface temperature rise from ~10 °C to 13 °C, pointing to simultaneous increases in salt and heat supply owing to the influx of waters from adjacent oceans. We suggest that onset and termination of the Azolla phase depended on the degree of oceanic exchange between Arctic Ocean and adjacent seas.

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