Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum
The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming ~55 million years ago, superimposed on an already warm world1, 2, 3. This warming is associated with a severe shoaling of the ocean calcite compensation depth4 and a >2.5 per mil negative carbon isotope exc...
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Online Access: | https://orca.cardiff.ac.uk/id/eprint/10753/ https://doi.org/10.1038/nature05043 |
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ftunivcardiff:oai:https://orca.cardiff.ac.uk:10753 2023-05-15T14:27:57+02:00 Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum Pagani, Mark Pedentchouk, Nikolai Huber, Matthew Sluijs, Appy Schouten, Stefan Brinkhuis, Henk Sinninghe Damsté, Jaap S. Dickens, Gerald R. Expedition 302 Scientists, ES Backman, Jan Clemens, Steve Cronin, Thomas Eynaud, Frédérique Gattacceca, Jérôme Jakobsson, Martin Jordan, Ric Kaminski, Michael King, John Koc, Nalân Martinez, Nahysa C. McInroy, David Moore Jr, Theodore C. O'Regan, Matthew Onodera, Jonaotaro Pälike, Heiko Rea, Brice Rio, Domenico Sakamoto, Tatsuhiko Smith, David C. St John, Kristen E. K. Suto, Itsuki Suzuki, Noritoshi Takahashi, Kozo Watanabe, Mahito Yamamoto, Masanobu 2006 https://orca.cardiff.ac.uk/id/eprint/10753/ https://doi.org/10.1038/nature05043 unknown NPG Pagani, Mark, Pedentchouk, Nikolai, Huber, Matthew, Sluijs, Appy, Schouten, Stefan, Brinkhuis, Henk, Sinninghe Damsté, Jaap S., Dickens, Gerald R., Expedition 302 Scientists, ES, Backman, Jan, Clemens, Steve, Cronin, Thomas, Eynaud, Frédérique, Gattacceca, Jérôme, Jakobsson, Martin, Jordan, Ric, Kaminski, Michael, King, John, Koc, Nalân, Martinez, Nahysa C., McInroy, David, Moore Jr, Theodore C., O'Regan, Matthew, Onodera, Jonaotaro, Pälike, Heiko, Rea, Brice, Rio, Domenico, Sakamoto, Tatsuhiko, Smith, David C., St John, Kristen E. K., Suto, Itsuki, Suzuki, Noritoshi, Takahashi, Kozo, Watanabe, Mahito and Yamamoto, Masanobu 2006. Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum. Nature 442 (7103) , pp. 671-675. 10.1038/nature05043 https://doi.org/10.1038/nature05043 doi:10.1038/nature05043 GC Oceanography Q Science (General) Article PeerReviewed 2006 ftunivcardiff https://doi.org/10.1038/nature05043 2022-09-25T20:17:42Z The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming ~55 million years ago, superimposed on an already warm world1, 2, 3. This warming is associated with a severe shoaling of the ocean calcite compensation depth4 and a >2.5 per mil negative carbon isotope excursion in marine and soil carbonates1, 2, 3, 4. Together these observations indicate a massive release of 13C-depleted carbon4 and greenhouse-gas-induced warming. Recently, sediments were recovered from the central Arctic Ocean5, providing the first opportunity to evaluate the environmental response at the North Pole at this time. Here we present stable hydrogen and carbon isotope measurements of terrestrial-plant- and aquatic-derived n-alkanes that record changes in hydrology, including surface water salinity and precipitation, and the global carbon cycle. Hydrogen isotope records are interpreted as documenting decreased rainout during moisture transport from lower latitudes and increased moisture delivery to the Arctic at the onset of the Palaeocene/Eocene thermal maximum, consistent with predictions of poleward storm track migrations during global warming6. The terrestrial-plant carbon isotope excursion (about -4.5 to -6 per mil) is substantially larger than those of marine carbonates. Previously, this offset was explained by the physiological response of plants to increases in surface humidity2. But this mechanism is not an effective explanation in this wet Arctic setting, leading us to hypothesize that the true magnitude of the excursion—and associated carbon input—was greater than originally surmised. Greater carbon release and strong hydrological cycle feedbacks may help explain the maintenance of this unprecedented warmth. Article in Journal/Newspaper Arctic Arctic Global warming North Pole Cardiff University: ORCA (Online Research @ Cardiff) Arctic North Pole Nature 442 7103 671 675 |
institution |
Open Polar |
collection |
Cardiff University: ORCA (Online Research @ Cardiff) |
op_collection_id |
ftunivcardiff |
language |
unknown |
topic |
GC Oceanography Q Science (General) |
spellingShingle |
GC Oceanography Q Science (General) Pagani, Mark Pedentchouk, Nikolai Huber, Matthew Sluijs, Appy Schouten, Stefan Brinkhuis, Henk Sinninghe Damsté, Jaap S. Dickens, Gerald R. Expedition 302 Scientists, ES Backman, Jan Clemens, Steve Cronin, Thomas Eynaud, Frédérique Gattacceca, Jérôme Jakobsson, Martin Jordan, Ric Kaminski, Michael King, John Koc, Nalân Martinez, Nahysa C. McInroy, David Moore Jr, Theodore C. O'Regan, Matthew Onodera, Jonaotaro Pälike, Heiko Rea, Brice Rio, Domenico Sakamoto, Tatsuhiko Smith, David C. St John, Kristen E. K. Suto, Itsuki Suzuki, Noritoshi Takahashi, Kozo Watanabe, Mahito Yamamoto, Masanobu Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum |
topic_facet |
GC Oceanography Q Science (General) |
description |
The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming ~55 million years ago, superimposed on an already warm world1, 2, 3. This warming is associated with a severe shoaling of the ocean calcite compensation depth4 and a >2.5 per mil negative carbon isotope excursion in marine and soil carbonates1, 2, 3, 4. Together these observations indicate a massive release of 13C-depleted carbon4 and greenhouse-gas-induced warming. Recently, sediments were recovered from the central Arctic Ocean5, providing the first opportunity to evaluate the environmental response at the North Pole at this time. Here we present stable hydrogen and carbon isotope measurements of terrestrial-plant- and aquatic-derived n-alkanes that record changes in hydrology, including surface water salinity and precipitation, and the global carbon cycle. Hydrogen isotope records are interpreted as documenting decreased rainout during moisture transport from lower latitudes and increased moisture delivery to the Arctic at the onset of the Palaeocene/Eocene thermal maximum, consistent with predictions of poleward storm track migrations during global warming6. The terrestrial-plant carbon isotope excursion (about -4.5 to -6 per mil) is substantially larger than those of marine carbonates. Previously, this offset was explained by the physiological response of plants to increases in surface humidity2. But this mechanism is not an effective explanation in this wet Arctic setting, leading us to hypothesize that the true magnitude of the excursion—and associated carbon input—was greater than originally surmised. Greater carbon release and strong hydrological cycle feedbacks may help explain the maintenance of this unprecedented warmth. |
format |
Article in Journal/Newspaper |
author |
Pagani, Mark Pedentchouk, Nikolai Huber, Matthew Sluijs, Appy Schouten, Stefan Brinkhuis, Henk Sinninghe Damsté, Jaap S. Dickens, Gerald R. Expedition 302 Scientists, ES Backman, Jan Clemens, Steve Cronin, Thomas Eynaud, Frédérique Gattacceca, Jérôme Jakobsson, Martin Jordan, Ric Kaminski, Michael King, John Koc, Nalân Martinez, Nahysa C. McInroy, David Moore Jr, Theodore C. O'Regan, Matthew Onodera, Jonaotaro Pälike, Heiko Rea, Brice Rio, Domenico Sakamoto, Tatsuhiko Smith, David C. St John, Kristen E. K. Suto, Itsuki Suzuki, Noritoshi Takahashi, Kozo Watanabe, Mahito Yamamoto, Masanobu |
author_facet |
Pagani, Mark Pedentchouk, Nikolai Huber, Matthew Sluijs, Appy Schouten, Stefan Brinkhuis, Henk Sinninghe Damsté, Jaap S. Dickens, Gerald R. Expedition 302 Scientists, ES Backman, Jan Clemens, Steve Cronin, Thomas Eynaud, Frédérique Gattacceca, Jérôme Jakobsson, Martin Jordan, Ric Kaminski, Michael King, John Koc, Nalân Martinez, Nahysa C. McInroy, David Moore Jr, Theodore C. O'Regan, Matthew Onodera, Jonaotaro Pälike, Heiko Rea, Brice Rio, Domenico Sakamoto, Tatsuhiko Smith, David C. St John, Kristen E. K. Suto, Itsuki Suzuki, Noritoshi Takahashi, Kozo Watanabe, Mahito Yamamoto, Masanobu |
author_sort |
Pagani, Mark |
title |
Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum |
title_short |
Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum |
title_full |
Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum |
title_fullStr |
Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum |
title_full_unstemmed |
Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum |
title_sort |
arctic hydrology during global warming at the palaeocene/eocene thermal maximum |
publisher |
NPG |
publishDate |
2006 |
url |
https://orca.cardiff.ac.uk/id/eprint/10753/ https://doi.org/10.1038/nature05043 |
geographic |
Arctic North Pole |
geographic_facet |
Arctic North Pole |
genre |
Arctic Arctic Global warming North Pole |
genre_facet |
Arctic Arctic Global warming North Pole |
op_relation |
Pagani, Mark, Pedentchouk, Nikolai, Huber, Matthew, Sluijs, Appy, Schouten, Stefan, Brinkhuis, Henk, Sinninghe Damsté, Jaap S., Dickens, Gerald R., Expedition 302 Scientists, ES, Backman, Jan, Clemens, Steve, Cronin, Thomas, Eynaud, Frédérique, Gattacceca, Jérôme, Jakobsson, Martin, Jordan, Ric, Kaminski, Michael, King, John, Koc, Nalân, Martinez, Nahysa C., McInroy, David, Moore Jr, Theodore C., O'Regan, Matthew, Onodera, Jonaotaro, Pälike, Heiko, Rea, Brice, Rio, Domenico, Sakamoto, Tatsuhiko, Smith, David C., St John, Kristen E. K., Suto, Itsuki, Suzuki, Noritoshi, Takahashi, Kozo, Watanabe, Mahito and Yamamoto, Masanobu 2006. Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum. Nature 442 (7103) , pp. 671-675. 10.1038/nature05043 https://doi.org/10.1038/nature05043 doi:10.1038/nature05043 |
op_doi |
https://doi.org/10.1038/nature05043 |
container_title |
Nature |
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442 |
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7103 |
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