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The Early Miocene Onset of a Ventilated Circulation Regime in the Arctic Ocean

Jakobsson, Martin (author)
Stockholms universitet,Institutionen för geologi och geokemi,Marin geovetenskap
Backman, Jan (author)
Stockholms universitet,Institutionen för geologi och geokemi,Marin geovetenskap
Rudels, Bert (author)
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Nycander, Jonas (author)
Stockholms universitet,Meteorologiska institutionen (MISU),Oceanografi
Frank, Martin (author)
Mayer, Larry (author)
Jokat, Wilfried (author)
Sangiorgi, Fransesca (author)
O'Regan, Matt (author)
Brinkhuis, Henk (author)
King, John (author)
Moran, Kathryn (author)
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 (creator_code:org_t)
Springer Science and Business Media LLC, 2007
2007
English.
In: Nature. - : Springer Science and Business Media LLC. - 0028-0836 .- 1476-4687. ; 447:7147, s. 986-990
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Deep-water formation in the northern North Atlantic Ocean and the Arctic Ocean is a key driver of the global thermohaline circulation and hence also of global climate. Deciphering the history of the circulation regime in the Arctic Ocean has long been prevented by the lack of data from cores of Cenozoic sediments from the Arctic’s deep-sea floor. Similarly, the timing of the opening of a connection between the northern North Atlantic and the Arctic Ocean, permitting deep-water exchange, has been poorly constrained. This situation changed when the first drill cores were recovered from the central Arctic Ocean. Here we use these cores to show that the transition from poorly oxygenated to fully oxygenated (‘ventilated’) conditions in the Arctic Ocean occurred during the later part of early Miocene times. We attribute this pronounced change in ventilation regime to the opening of the Fram Strait. A palaeo-geographic and palaeo-bathymetric reconstruction of the Arctic Ocean, together with a physical oceanographic analysis of the evolving strait and sill conditions in the Fram Strait, suggests that the Arctic Ocean went from an oxygenpoor ‘lake stage’, to a transitional ‘estuarine sea’ phase with variable ventilation, and finally to the fully ventilated ‘ocean’ phase 17.5 Myr ago. The timing of this palaeo-oceanographic change coincides with the onset of the middle Miocene climatic optimum, although it remains unclear if there is a causal relationship between these two events.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Multidisciplinär geovetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geosciences, Multidisciplinary (hsv//eng)

Keyword

Arctic Ocean
Paleoclimate
Fram Strait
Ocean circulation
Other earth sciences
Övrig geovetenskap
Exogenous earth sciences
Exogen geovetenskap

Publication and Content Type

ref (subject category)
art (subject category)

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