Atlantic meridional overturning circulation during the last glacial maximum

Jean Lynch-Stieglitz; Jess F. Adkins; William B. Curry; Trond Dokken; Ian R. Hall; Juan Carlos Herguera; Joël J.M. Hirschi; Elena V. Ivanova; Catherine Kissel; Olivier Marchal; Thomas M. Marchitto; I. Nicholas McCave; Jerry F. McManus; Stefan Mulitza; Ulysses Ninnemann; Frank Peeters; Ein Fen Yu; Rainer Zahn

doi:10.1126/science.1137127

Atlantic meridional overturning circulation during the last glacial maximum

Jean Lynch-Stieglitz, Jess F. Adkins, William B. Curry, Trond Dokken, Ian R. Hall, Juan Carlos Herguera, Joël J.M. Hirschi, Elena V. Ivanova, Catherine Kissel, Olivier Marchal, Thomas M. Marchitto, I. Nicholas McCave, Jerry F. McManus, Stefan Mulitza, Ulysses Ninnemann, Frank Peeters, Ein Fen Yu, Rainer Zahn

Producción científica: Contribución a una revista › Artículo de revisión › Investigación › revisión exhaustiva

336 Citas (Scopus)

Resumen

The circulation of the deep Atlantic Ocean during the height of the last ice age appears to have been quite different from today. We review observations implying that Atlantic meridional overturning circulation during the Last Glacial Maximum was neither extremely sluggish nor an enhanced version of present-day circulation. The distribution of the decay products of uranium in sediments is consistent with a residence time for deep waters in the Atlantic only slightly greater than today. However, evidence from multiple water-mass tracers supports a different distribution of deep-water properties, including density, which is dynamically linked to circulation.

Idioma original	Inglés
Páginas (desde-hasta)	66-69
Publicación	Science
Volumen	316
N.º	5821
DOI	https://doi.org/10.1126/science.1137127
Estado	Publicada - 6 abr 2007

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Lynch-Stieglitz, J., Adkins, J. F., Curry, W. B., Dokken, T., Hall, I. R., Herguera, J. C., Hirschi, J. J. M., Ivanova, E. V., Kissel, C., Marchal, O., Marchitto, T. M., McCave, I. N., McManus, J. F., Mulitza, S., Ninnemann, U., Peeters, F., Yu, E. F., & Zahn, R. (2007). Atlantic meridional overturning circulation during the last glacial maximum. Science, 316(5821), 66-69. https://doi.org/10.1126/science.1137127

@article{92f6261bbabf48e48a41826000fc020f,

title = "Atlantic meridional overturning circulation during the last glacial maximum",

abstract = "The circulation of the deep Atlantic Ocean during the height of the last ice age appears to have been quite different from today. We review observations implying that Atlantic meridional overturning circulation during the Last Glacial Maximum was neither extremely sluggish nor an enhanced version of present-day circulation. The distribution of the decay products of uranium in sediments is consistent with a residence time for deep waters in the Atlantic only slightly greater than today. However, evidence from multiple water-mass tracers supports a different distribution of deep-water properties, including density, which is dynamically linked to circulation.",

author = "Jean Lynch-Stieglitz and Adkins, \{Jess F.\} and Curry, \{William B.\} and Trond Dokken and Hall, \{Ian R.\} and Herguera, \{Juan Carlos\} and Hirschi, \{Jo{\"e}l J.M.\} and Ivanova, \{Elena V.\} and Catherine Kissel and Olivier Marchal and Marchitto, \{Thomas M.\} and McCave, \{I. Nicholas\} and McManus, \{Jerry F.\} and Stefan Mulitza and Ulysses Ninnemann and Frank Peeters and Yu, \{Ein Fen\} and Rainer Zahn",

year = "2007",

month = apr,

day = "6",

doi = "10.1126/science.1137127",

language = "English",

volume = "316",

pages = "66--69",

number = "5821",

}

Lynch-Stieglitz, J, Adkins, JF, Curry, WB, Dokken, T, Hall, IR, Herguera, JC, Hirschi, JJM, Ivanova, EV, Kissel, C, Marchal, O, Marchitto, TM, McCave, IN, McManus, JF, Mulitza, S, Ninnemann, U, Peeters, F, Yu, EF & Zahn, R 2007, 'Atlantic meridional overturning circulation during the last glacial maximum', Science, vol. 316, n.º 5821, pp. 66-69. https://doi.org/10.1126/science.1137127

TY - JOUR

T1 - Atlantic meridional overturning circulation during the last glacial maximum

AU - Lynch-Stieglitz, Jean

AU - Adkins, Jess F.

AU - Curry, William B.

AU - Dokken, Trond

AU - Hall, Ian R.

AU - Herguera, Juan Carlos

AU - Hirschi, Joël J.M.

AU - Ivanova, Elena V.

AU - Kissel, Catherine

AU - Marchal, Olivier

AU - Marchitto, Thomas M.

AU - McCave, I. Nicholas

AU - McManus, Jerry F.

AU - Mulitza, Stefan

AU - Ninnemann, Ulysses

AU - Peeters, Frank

AU - Yu, Ein Fen

AU - Zahn, Rainer

PY - 2007/4/6

Y1 - 2007/4/6

N2 - The circulation of the deep Atlantic Ocean during the height of the last ice age appears to have been quite different from today. We review observations implying that Atlantic meridional overturning circulation during the Last Glacial Maximum was neither extremely sluggish nor an enhanced version of present-day circulation. The distribution of the decay products of uranium in sediments is consistent with a residence time for deep waters in the Atlantic only slightly greater than today. However, evidence from multiple water-mass tracers supports a different distribution of deep-water properties, including density, which is dynamically linked to circulation.

AB - The circulation of the deep Atlantic Ocean during the height of the last ice age appears to have been quite different from today. We review observations implying that Atlantic meridional overturning circulation during the Last Glacial Maximum was neither extremely sluggish nor an enhanced version of present-day circulation. The distribution of the decay products of uranium in sediments is consistent with a residence time for deep waters in the Atlantic only slightly greater than today. However, evidence from multiple water-mass tracers supports a different distribution of deep-water properties, including density, which is dynamically linked to circulation.

UR - https://www.scopus.com/pages/publications/34147171532

U2 - 10.1126/science.1137127

DO - 10.1126/science.1137127

M3 - Review article

SN - 0036-8075

VL - 316

SP - 66

EP - 69

JO - Science

JF - Science

IS - 5821

ER -

Atlantic meridional overturning circulation during the last glacial maximum

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