Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period

J. Jouzel; N. I. Barkov; J. M. Barnola; M. Bender; J. Chappellaz; C. Genthon; V. M. Kotlyakov; V. Lipenkov; C. Lorius; J. R. Petit; D. Raynaud; G. Raisbeck; C. Ritz; T. Sowers; M. Stievenard; F. Yiou; P. Yiou

doi:10.1038/364407a0

Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period

J. Jouzel
, N. I. Barkov
, J. M. Barnola
, M. Bender
, J. Chappellaz
, C. Genthon
, V. M. Kotlyakov
, V. Lipenkov
, C. Lorius
, J. R. Petit
, D. Raynaud
, G. Raisbeck
, C. Ritz
, T. Sowers
, M. Stievenard
, F. Yiou
, P. Yiou

Institut Pierre Simon Laplace, CNRS and CEA
Laboratoire de Glaciologie et Géophysique de i'Environnement
Arctic and Antarctic Research Institute
CNRS
University of Rhode Island
Institute of Geography, Russian Academy of Sciences
Bât. 104-108

Résultats de recherche: Contribution à un journal › Article › Revue par des pairs

486 Citations (Scopus)

Résumé

The ice-core record of local temperature, dust accumulation and air composition at Vostok station, Antarctica, now extends back to the penultimate glacial period (∼140-200 kyr ago) and the end of the preceding interglacial. This yields a new glaciological timescale for the whole record, which is consistent with ocean records. Temperatures at Vostok appear to have been more uniformly cold in the penultimate glacial period than in the most recent one. Concentrations of CO₂ and CH₄ correlate well with temperature throughout the record.

langue originale	Anglais
Pages (de - à)	407-412
Nombre de pages	6
journal	Nature
Volume	364
Numéro de publication	6436
Les DOIs	https://doi.org/10.1038/364407a0
état	Publié - 1 janv. 1993

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10.1038/364407a0

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Jouzel, J., Barkov, N. I., Barnola, J. M., Bender, M., Chappellaz, J., Genthon, C., Kotlyakov, V. M., Lipenkov, V., Lorius, C., Petit, J. R., Raynaud, D., Raisbeck, G., Ritz, C., Sowers, T., Stievenard, M., Yiou, F., & Yiou, P. (1993). Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period. Nature, 364(6436), 407-412. https://doi.org/10.1038/364407a0

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title = "Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period",

abstract = "The ice-core record of local temperature, dust accumulation and air composition at Vostok station, Antarctica, now extends back to the penultimate glacial period (∼140-200 kyr ago) and the end of the preceding interglacial. This yields a new glaciological timescale for the whole record, which is consistent with ocean records. Temperatures at Vostok appear to have been more uniformly cold in the penultimate glacial period than in the most recent one. Concentrations of CO2 and CH4 correlate well with temperature throughout the record.",

author = "J. Jouzel and Barkov, \{N. I.\} and Barnola, \{J. M.\} and M. Bender and J. Chappellaz and C. Genthon and Kotlyakov, \{V. M.\} and V. Lipenkov and C. Lorius and Petit, \{J. R.\} and D. Raynaud and G. Raisbeck and C. Ritz and T. Sowers and M. Stievenard and F. Yiou and P. Yiou",

year = "1993",

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doi = "10.1038/364407a0",

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Jouzel, J, Barkov, NI, Barnola, JM, Bender, M, Chappellaz, J, Genthon, C, Kotlyakov, VM, Lipenkov, V, Lorius, C, Petit, JR, Raynaud, D, Raisbeck, G, Ritz, C, Sowers, T, Stievenard, M, Yiou, F & Yiou, P 1993, 'Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period', Nature, VOL. 364, Numéro 6436, p. 407-412. https://doi.org/10.1038/364407a0

TY - JOUR

T1 - Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period

AU - Jouzel, J.

AU - Barkov, N. I.

AU - Barnola, J. M.

AU - Bender, M.

AU - Chappellaz, J.

AU - Genthon, C.

AU - Kotlyakov, V. M.

AU - Lipenkov, V.

AU - Lorius, C.

AU - Petit, J. R.

AU - Raynaud, D.

AU - Raisbeck, G.

AU - Ritz, C.

AU - Sowers, T.

AU - Stievenard, M.

AU - Yiou, F.

AU - Yiou, P.

PY - 1993/1/1

Y1 - 1993/1/1

N2 - The ice-core record of local temperature, dust accumulation and air composition at Vostok station, Antarctica, now extends back to the penultimate glacial period (∼140-200 kyr ago) and the end of the preceding interglacial. This yields a new glaciological timescale for the whole record, which is consistent with ocean records. Temperatures at Vostok appear to have been more uniformly cold in the penultimate glacial period than in the most recent one. Concentrations of CO2 and CH4 correlate well with temperature throughout the record.

AB - The ice-core record of local temperature, dust accumulation and air composition at Vostok station, Antarctica, now extends back to the penultimate glacial period (∼140-200 kyr ago) and the end of the preceding interglacial. This yields a new glaciological timescale for the whole record, which is consistent with ocean records. Temperatures at Vostok appear to have been more uniformly cold in the penultimate glacial period than in the most recent one. Concentrations of CO2 and CH4 correlate well with temperature throughout the record.

U2 - 10.1038/364407a0

DO - 10.1038/364407a0

M3 - Article

AN - SCOPUS:0027879561

SN - 0028-0836

VL - 364

SP - 407

EP - 412

JO - Nature

JF - Nature

IS - 6436

ER -

Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period

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