The Cenozoic palaeoenvironment of the Arctic Ocean › Научные исследования в СПбГУ

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The Cenozoic palaeoenvironment of the Arctic Ocean. / Moran, Kathryn; Backman, Jan; Brinkhuis, Henk; Clemens, Steven C.; Cronin, Thomas; Dickens, Gerald R.; Eynaud, Frédérique; Gattacceca, Jérôme; Jakobsson, Martin; Jordan, Richard W.; Kaminski, Michael; King, John; Koc, Nalan; Krylov, Alexey; Martinez, Nahysa; Matthiessen, Jens; McInroy, David; Moore, Theodore C.; Onodera, Jonaotaro; O'Regan, Matthew; Pälike, Heiko; Rea, Brice; Rio, Domenico; Sakamoto, Tatsuhiko; Smith, David C.; Stein, Ruediger; St John, Kristen; Suto, Itsuki; Suzuki, Noritoshi; Takahashi, Kozo; Watanabe, Mahito; Yamamoto, Masanobu; Farrell, John; Frank, Martin; Kubik, Peter; Jokat, Wilfried; Kristoffersen, Yngve.

в: Nature, Том 441, № 7093, 01.06.2006, стр. 601-605.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Moran, K, Backman, J, Brinkhuis, H, Clemens, SC, Cronin, T, Dickens, GR, Eynaud, F, Gattacceca, J, Jakobsson, M, Jordan, RW, Kaminski, M, King, J, Koc, N, Krylov, A, Martinez, N, Matthiessen, J, McInroy, D, Moore, TC, Onodera, J, O'Regan, M, Pälike, H, Rea, B, Rio, D, Sakamoto, T, Smith, DC, Stein, R, St John, K, Suto, I, Suzuki, N, Takahashi, K, Watanabe, M, Yamamoto, M, Farrell, J, Frank, M, Kubik, P, Jokat, W & Kristoffersen, Y 2006, 'The Cenozoic palaeoenvironment of the Arctic Ocean', Nature, Том. 441, № 7093, стр. 601-605. https://doi.org/10.1038/nature04800

APA

Moran, K., Backman, J., Brinkhuis, H., Clemens, S. C., Cronin, T., Dickens, G. R., Eynaud, F., Gattacceca, J., Jakobsson, M., Jordan, R. W., Kaminski, M., King, J., Koc, N., Krylov, A., Martinez, N., Matthiessen, J., McInroy, D., Moore, T. C., Onodera, J., ... Kristoffersen, Y. (2006). The Cenozoic palaeoenvironment of the Arctic Ocean. Nature, 441(7093), 601-605. https://doi.org/10.1038/nature04800

Vancouver

Moran K, Backman J, Brinkhuis H, Clemens SC, Cronin T, Dickens GR и пр. The Cenozoic palaeoenvironment of the Arctic Ocean. Nature. 2006 Июнь 1;441(7093):601-605. https://doi.org/10.1038/nature04800

Author

Moran, Kathryn ; Backman, Jan ; Brinkhuis, Henk ; Clemens, Steven C. ; Cronin, Thomas ; Dickens, Gerald R. ; Eynaud, Frédérique ; Gattacceca, Jérôme ; Jakobsson, Martin ; Jordan, Richard W. ; Kaminski, Michael ; King, John ; Koc, Nalan ; Krylov, Alexey ; Martinez, Nahysa ; Matthiessen, Jens ; McInroy, David ; Moore, Theodore C. ; Onodera, Jonaotaro ; O'Regan, Matthew ; Pälike, Heiko ; Rea, Brice ; Rio, Domenico ; Sakamoto, Tatsuhiko ; Smith, David C. ; Stein, Ruediger ; St John, Kristen ; Suto, Itsuki ; Suzuki, Noritoshi ; Takahashi, Kozo ; Watanabe, Mahito ; Yamamoto, Masanobu ; Farrell, John ; Frank, Martin ; Kubik, Peter ; Jokat, Wilfried ; Kristoffersen, Yngve. / The Cenozoic palaeoenvironment of the Arctic Ocean. в: Nature. 2006 ; Том 441, № 7093. стр. 601-605.

BibTeX

@article{7fc7a87c4f224b3e9dc514187489f8de,

title = "The Cenozoic palaeoenvironment of the Arctic Ocean",

abstract = "The history of the Arctic Ocean during the Cenozoic era (0-65 million years ago) is largely unknown from direct evidence. Here we present a Cenozoic palaeoceanographic record constructed from >400 m of sediment core from a recent drilling expedition to the Lomonosov ridge in the Arctic Ocean. Our record shows a palaeoenvironmental transition from a warm 'greenhouse' world, during the late Palaeocene and early Eocene epochs, to a colder 'icehouse' world influenced by sea ice and icebergs from the middle Eocene epoch to the present. For the most recent ∼14 Myr, we find sedimentation rates of 1-2 cm per thousand years, in stark contrast to the substantially lower rates proposed in earlier studies; this record of the Neogene reveals cooling of the Arctic that was synchronous with the expansion of Greenland ice (∼3.2 Myr ago) and East Antarctic ice (∼14 Myr ago). We find evidence for the first occurrence of ice-rafted debris in the middle Eocene epoch (∼45 Myr ago), some 35 Myr earlier than previously thought; fresh surface waters were present at ∼49 Myr ago, before the onset of ice-rafted debris. Also, the temperatures of surface waters during the Palaeocene/Eocene thermal maximum (∼55 Myr ago) appear to have been substantially warmer than previously estimated. The revised timing of the earliest Arctic cooling events coincides with those from Antarctica, supporting arguments for bipolar symmetry in climate change.",

author = "Kathryn Moran and Jan Backman and Henk Brinkhuis and Clemens, {Steven C.} and Thomas Cronin and Dickens, {Gerald R.} and Fr{\'e}d{\'e}rique Eynaud and J{\'e}r{\^o}me Gattacceca and Martin Jakobsson and Jordan, {Richard W.} and Michael Kaminski and John King and Nalan Koc and Alexey Krylov and Nahysa Martinez and Jens Matthiessen and David McInroy and Moore, {Theodore C.} and Jonaotaro Onodera and Matthew O'Regan and Heiko P{\"a}like and Brice Rea and Domenico Rio and Tatsuhiko Sakamoto and Smith, {David C.} and Ruediger Stein and {St John}, Kristen and Itsuki Suto and Noritoshi Suzuki and Kozo Takahashi and Mahito Watanabe and Masanobu Yamamoto and John Farrell and Martin Frank and Peter Kubik and Wilfried Jokat and Yngve Kristoffersen",

year = "2006",

month = jun,

day = "1",

doi = "10.1038/nature04800",

language = "English",

volume = "441",

pages = "601--605",

journal = "Nature",

issn = "0028-0836",

publisher = "Nature Publishing Group",

number = "7093",

}

RIS

TY - JOUR

T1 - The Cenozoic palaeoenvironment of the Arctic Ocean

AU - Moran, Kathryn

AU - Backman, Jan

AU - Brinkhuis, Henk

AU - Clemens, Steven C.

AU - Cronin, Thomas

AU - Dickens, Gerald R.

AU - Eynaud, Frédérique

AU - Gattacceca, Jérôme

AU - Jakobsson, Martin

AU - Jordan, Richard W.

AU - Kaminski, Michael

AU - King, John

AU - Koc, Nalan

AU - Krylov, Alexey

AU - Martinez, Nahysa

AU - Matthiessen, Jens

AU - McInroy, David

AU - Moore, Theodore C.

AU - Onodera, Jonaotaro

AU - O'Regan, Matthew

AU - Pälike, Heiko

AU - Rea, Brice

AU - Rio, Domenico

AU - Sakamoto, Tatsuhiko

AU - Smith, David C.

AU - Stein, Ruediger

AU - St John, Kristen

AU - Suto, Itsuki

AU - Suzuki, Noritoshi

AU - Takahashi, Kozo

AU - Watanabe, Mahito

AU - Yamamoto, Masanobu

AU - Farrell, John

AU - Frank, Martin

AU - Kubik, Peter

AU - Jokat, Wilfried

AU - Kristoffersen, Yngve

PY - 2006/6/1

Y1 - 2006/6/1

N2 - The history of the Arctic Ocean during the Cenozoic era (0-65 million years ago) is largely unknown from direct evidence. Here we present a Cenozoic palaeoceanographic record constructed from >400 m of sediment core from a recent drilling expedition to the Lomonosov ridge in the Arctic Ocean. Our record shows a palaeoenvironmental transition from a warm 'greenhouse' world, during the late Palaeocene and early Eocene epochs, to a colder 'icehouse' world influenced by sea ice and icebergs from the middle Eocene epoch to the present. For the most recent ∼14 Myr, we find sedimentation rates of 1-2 cm per thousand years, in stark contrast to the substantially lower rates proposed in earlier studies; this record of the Neogene reveals cooling of the Arctic that was synchronous with the expansion of Greenland ice (∼3.2 Myr ago) and East Antarctic ice (∼14 Myr ago). We find evidence for the first occurrence of ice-rafted debris in the middle Eocene epoch (∼45 Myr ago), some 35 Myr earlier than previously thought; fresh surface waters were present at ∼49 Myr ago, before the onset of ice-rafted debris. Also, the temperatures of surface waters during the Palaeocene/Eocene thermal maximum (∼55 Myr ago) appear to have been substantially warmer than previously estimated. The revised timing of the earliest Arctic cooling events coincides with those from Antarctica, supporting arguments for bipolar symmetry in climate change.

AB - The history of the Arctic Ocean during the Cenozoic era (0-65 million years ago) is largely unknown from direct evidence. Here we present a Cenozoic palaeoceanographic record constructed from >400 m of sediment core from a recent drilling expedition to the Lomonosov ridge in the Arctic Ocean. Our record shows a palaeoenvironmental transition from a warm 'greenhouse' world, during the late Palaeocene and early Eocene epochs, to a colder 'icehouse' world influenced by sea ice and icebergs from the middle Eocene epoch to the present. For the most recent ∼14 Myr, we find sedimentation rates of 1-2 cm per thousand years, in stark contrast to the substantially lower rates proposed in earlier studies; this record of the Neogene reveals cooling of the Arctic that was synchronous with the expansion of Greenland ice (∼3.2 Myr ago) and East Antarctic ice (∼14 Myr ago). We find evidence for the first occurrence of ice-rafted debris in the middle Eocene epoch (∼45 Myr ago), some 35 Myr earlier than previously thought; fresh surface waters were present at ∼49 Myr ago, before the onset of ice-rafted debris. Also, the temperatures of surface waters during the Palaeocene/Eocene thermal maximum (∼55 Myr ago) appear to have been substantially warmer than previously estimated. The revised timing of the earliest Arctic cooling events coincides with those from Antarctica, supporting arguments for bipolar symmetry in climate change.

UR - http://www.scopus.com/inward/record.url?scp=33745256185&partnerID=8YFLogxK

U2 - 10.1038/nature04800

DO - 10.1038/nature04800

M3 - Article

C2 - 16738653

VL - 441

SP - 601

EP - 605

JO - Nature

JF - Nature

SN - 0028-0836

IS - 7093

ER -

ID: 5505574