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research article

Atmospheric science: Atmospheric methane and nitrous oxide of the late pleistocene from Antarctic Ice Cores

Spahni, R.
•
Chappellaz, J.
•
Stocker, T. F.
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November 25, 2005
Science

The European Project for Ice Coring in Antarctica Dome C ice core enables us to extend existing records of atmospheric methane (CH4) and nitrous oxide (N2O) back to 650,000 years before the present. A combined record of CH4 measured along the Dome C and the Vostok ice cores demonstrates, within the resolution of our measurements, that preindustrial concentrations over Antarctica have not exceeded 773 ± 15 ppbv (parts per billion by volume) during the past 650,000 years. Before 420,000 years ago, when interglacials were cooler, maximum CH4 concentrations were only about 600 ppbv, similar to lower Holocene values. In contrast, the N2O record shows maximum concentrations of 278 ± 7 ppbv, slightly higher than early Holocene values.

  • Details
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Type
research article
DOI
10.1126/science.1120132
Web of Science ID

WOS:000233600200038

Author(s)
Spahni, R.
Chappellaz, J.
Stocker, T. F.
Loulergue, L.
Hausammann, G.
Kawamura, K.
Fluckiger, J.
Schwander, J.
Raynaud, D.
Masson-Delmotte, V.
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Date Issued

2005-11-25

Publisher

American Association for the Advancement of Science (AAAS)

Published in
Science
Volume

310

Issue

5752

Start page

1317

End page

1321

Subjects

Concentration (process)

•

Glaciers

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Methane

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Atmospheric methanes

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Holocene values

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Interglacials

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Nitrous oxides

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Atmospheric chemistry

•

methane

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nitrous oxide

•

atmospheric chemistry

•

paleoatmosphere

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Pleistocene

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Antarctica

•

article

•

artifact

•

atmosphere

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climate change

•

greenhouse gas

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Holocene

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ice core record

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methanogenesis

•

priority journal

Editorial or Peer reviewed

REVIEWED

Written at

OTHER

EPFL units
SENSE  
Available on Infoscience
November 23, 2022
Use this identifier to reference this record
https://infoscience.epfl.ch/handle/20.500.14299/192590
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