Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean
We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle model. The carbon cycle model employs circulation fields which were derived from previous climate simulations. All sediment dat...
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| Format: | Dataset |
| Language: | English |
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PANGAEA
2011
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| Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.758334 https://doi.org/10.1594/PANGAEA.758334 |
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Open Polar |
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PANGAEA - Data Publisher for Earth & Environmental Science |
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0010PG 0016PG 0021PG 0026PG 0029PG 0032PG 0033GGC 0036PG 0038PG 0044PG 0050PG 0055PG 0058PG 0066PG 0071PG 0075PG 0082PG 0091PG 0100GGC 06MT15_2 06MT41_3 108-658 108-659 162-980 162-982 175-1084 175-1085A 175-1087A 177-1088 293 313 68-502_Site 81-552 90b Agadir Canyon Age comment Agulhas Basin AII60-13APC ALB-226 also published as VM28-122 Amazon Fan Angola Basin ANT-IV/1c ANT-IX/4 ANT-VIII/3 Arctic Ocean Argentine Basin ARK-II/5 ARK-VIII/3 Hesse, Tilman Butzin, Martin Bickert, Torsten Lohmann, Gerrit Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean |
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0010PG 0016PG 0021PG 0026PG 0029PG 0032PG 0033GGC 0036PG 0038PG 0044PG 0050PG 0055PG 0058PG 0066PG 0071PG 0075PG 0082PG 0091PG 0100GGC 06MT15_2 06MT41_3 108-658 108-659 162-980 162-982 175-1084 175-1085A 175-1087A 177-1088 293 313 68-502_Site 81-552 90b Agadir Canyon Age comment Agulhas Basin AII60-13APC ALB-226 also published as VM28-122 Amazon Fan Angola Basin ANT-IV/1c ANT-IX/4 ANT-VIII/3 Arctic Ocean Argentine Basin ARK-II/5 ARK-VIII/3 |
| description |
We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle model. The carbon cycle model employs circulation fields which were derived from previous climate simulations. All sediment data have been thoroughly quality controlled, focusing on epibenthic foraminiferal species (such as Cibicidoides wuellerstorfi or Planulina ariminensis) to improve the comparability of model and sediment core carbon isotopes. The model captures the general d13C pattern indicated by present-day water column data and Late Holocene sediment cores but underestimates intermediate and deep water values in the South Atlantic. The best agreement with glacial reconstructions is obtained for a model scenario with an altered freshwater balance in the Southern Ocean that mimics enhanced northward sea ice export and melting away from the zone of sea ice production. This results in a shoaled and weakened North Atlantic Deep Water flow and intensified Antarctic Bottom Water export, hence confirming previous reconstructions from paleoproxy records. Moreover, the modeled abyssal ocean is very cold and very saline, which is in line with other proxy data evidence. |
| format |
Dataset |
| author |
Hesse, Tilman Butzin, Martin Bickert, Torsten Lohmann, Gerrit |
| author_facet |
Hesse, Tilman Butzin, Martin Bickert, Torsten Lohmann, Gerrit |
| author_sort |
Hesse, Tilman |
| title |
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean |
| title_short |
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean |
| title_full |
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean |
| title_fullStr |
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean |
| title_full_unstemmed |
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean |
| title_sort |
compilation of 220 sediment core δ¹³c data from the glacial atlantic ocean |
| publisher |
PANGAEA |
| publishDate |
2011 |
| url |
https://doi.pangaea.de/10.1594/PANGAEA.758334 https://doi.org/10.1594/PANGAEA.758334 |
| op_coverage |
MEDIAN LATITUDE: 10.773327 * MEDIAN LONGITUDE: -21.986460 * SOUTH-BOUND LATITUDE: -46.764000 * WEST-BOUND LONGITUDE: -80.130000 * NORTH-BOUND LATITUDE: 82.023700 * EAST-BOUND LONGITUDE: 17.633000 * DATE/TIME START: 1957-05-19T00:00:00 * DATE/TIME END: 2005-06-24T01:23:00 * MINIMUM ELEVATION: -5105.0 m * MAXIMUM ELEVATION: 0.0 m |
| long_lat |
ENVELOPE(-80.130000,17.633000,82.023700,-46.764000) |
| genre |
Antarc* Antarctic Arctic Arctic Ocean Foraminifera* North Atlantic Deep Water North Atlantic Sea ice Southern Ocean |
| genre_facet |
Antarc* Antarctic Arctic Arctic Ocean Foraminifera* North Atlantic Deep Water North Atlantic Sea ice Southern Ocean |
| op_source |
Supplement to: Hesse, Tilman; Butzin, Martin; Bickert, Torsten; Lohmann, Gerrit (2011): A model-data comparison of d13C in the glacial Atlantic Ocean. Paleoceanography, 26, PA3220, https://doi.org/10.1029/2010PA002085 |
| op_relation |
Arz, Helge Wolfgang; Pätzold, Jürgen; Wefer, Gerold (1998): Correlated millennial-scale changes in surface hydrography and terrigenous sediment yield inferred from last-glacial marine deposits off northeastern Brazil. Quaternary Research, 50(2), 157-166, https://doi.org/10.1006/qres.1998.1992 Bauch, Henning A; Erlenkeuser, Helmut; Spielhagen, Robert F; Struck, Ulrich; Matthiessen, Jens; Thiede, Jörn; Heinemeier, Jan (2001): A multiproxy reconstruction of the evolution of deep and surface waters in the subarctic Nordic seas over the last 30,000 years. Quaternary Science Reviews, 20(4), 659-678, https://doi.org/10.1016/S0277-3791(00)00098-6 Bertram, Caroline J; Elderfield, Henry; Shackleton, Nicholas J; McDonald, J A (1995): Cadmium/calcium and carbon isotope reconstructions of the glacial northeast Atlantic Ocean. Paleoceanography, 10(3), 563-578, https://doi.org/10.1029/94PA03058 Beveridge, N; Elderfield, Henry; Shackleton, Nicholas J (1995): Deep thermohaline circulation in the low-latitude Atlantic during the last glacial. Paleoceanography, 10(3), 643-660, https://doi.org/10.1029/94PA03353 Bickert, Torsten; Mackensen, Andreas (2004): Last glacial to holocene changes in South Atlantic Deep Water Circulation. In: Wefer, G; Mulitza, S & Ratmeyer, V (eds.), The South Atlantic in the Late Quaternary: Reconstruction of Material Budgets and Current Systems, Springer, Berlin, Heidelberg, New York, 671-693 Bickert, Torsten; Wefer, Gerold (1996): Late Quaternary deep water circulation in the South Atlantic: Reconstruction from carbonate dissolution and benthic stable isotopes. In: Wefer, G; Berger, W H; Siedler, G & Webb, D (eds.), The South Atlantic: Present and Past Circulation. Springer-Verlag, Berlin, 103, 599-620 Bickert, Torsten; Wefer, Gerold (1999): South Atlantic and benthic foraminifer 13C deviations: Implications for reconstructing the Late Quaternary deep-water circulation. Deep Sea Research Part II: Topical Studies in Oceanography, 46(1-2), 437-452, https://doi.org/10.1016/S0967-0645(98)00098-8 Boyle, Edward A; Keigwin, Lloyd D (1985): Comparison of Atlantic and Pacific paleochemical records for the last 215.000 years: changes in deep ocean circulation and chemical inventories. Earth and Planetary Science Letters, 76(1-2), 135-150, https://doi.org/10.1016/0012-821X(85)90154-2 Boyle, Edward A; Keigwin, Lloyd D (1987): North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature. Nature, 330(6143), 35-40, https://doi.org/10.1038/330035a0 Castañeda, Isla S; Mulitza, Stefan; Schefuß, Enno; Lopes dos Santos, Raquel A; Sinninghe Damsté, Jaap S; Schouten, Stefan (2009): Wet phases in the Sahara/Sahel region and human migration patterns in North Africa. Proceedings of the National Academy of Sciences of the United States of America, 106(48), 20159-20163, https://doi.org/10.1073/pnas.0905771106 Curry, William B; Duplessy, Jean-Claude; Labeyrie, Laurent D; Shackleton, Nicholas J (1988): Changes in the distribution of d13C of deep water Sigma-CO2 between the last glaciation and the Holocene. Paleoceanography, 3(3), 317-341, https://doi.org/10.1029/PA003i003p00317 Curry, William B; Lohmann, G P (1982): Carbon isotopic changes in benthic foraminifera from the Western South Atlantic: Reconstruction of glacial abyssal circulation patterns. Quaternary Research, 18(2), 218-235, https://doi.org/10.1016/0033-5894(82)90071-0 deMenocal, Peter B; Oppo, Delia W; Fairbanks, Richard G; Prell, Warren L (1992): Pleistocene d13C variability of North Atlantic intermediate water. Paleoceanography, 7(2), 229-250, https://doi.org/10.1029/92PA00420 Duplessy, Jean-Claude (1982): North Atlantic deep water circulation during the last climate cycle. Bulletin de l'Institut de Geologie du Bassin d'Aquitaine, 31, 379-391 Freudenthal, Tim; Meggers, Helge; Henderiks, Jorijntje; Kuhlmann, Holger; Moreno, Ana; Wefer, Gerold (2002): Upwelling intensity and filament activity off Morocco during the last 250,000 years. Deep Sea Research Part II: Topical Studies in Oceanography, 49(17), 3655-3674, https://doi.org/10.1016/S0967-0645(02)00101-7 Hodell, David A; Venz, Kathryn A; Charles, Christopher D; Ninnemann, Ulysses S (2003): Pleistocene vertical carbon isotope and carbonate gradients in the South Atlantic sector of the Southern Ocean. Geochemistry, Geophysics, Geosystems, 4(1), 1004, https://doi.org/10.1029/2002GC000367 Jung, Simon J A (1996): Wassermassenaustausch zwischen NE-Atlantik und Nordmeer während der letzten 300 000/80 000 Jahre im Abbild stabiler O- und C- Isotope. Berichte aus dem Sonderforschungsbereich 313, Christian-Albrechts-Universität, Kiel, 61, 104 pp, https://doi.org/10.2312/reports-sfb313.1996.61 Keigwin, Lloyd D (2004): Radiocarbon and stable isotope constraints on Last Glacial Maximum and Younger Dryas ventilation in the western North Atlantic. Paleoceanography, 19(4), PA4012, https://doi.org/10.1029/2004PA001029 Keigwin, Lloyd D; Schlegel, M A (2002): Ocean ventilation and sedimentation since the glacial maximum at 3 km in the western North Atlantic. Geochemistry, Geophysics, Geosystems, 3(6), 1034, https://doi.org/10.1029/2001GC000283 Lynch-Stieglitz, Jean; Curry, William B; Oppo, Delia W; Ninnemann, Ulysses S; Charles, Christopher D; Munson, J (2006): Meridional overturning circulation in the South Atlantic at the Last Glacial Maximum. Geochemistry, Geophysics, Geosystems, 7(10), Q10N03, https://doi.org/10.1029/2005GC001226 Mackensen, Andreas; Grobe, Hannes; Hubberten, Hans-Wolfgang; Kuhn, Gerhard (1994): Benthic foraminiferal assemblages and the d13C-signal in the atlantic sector of the Southern Ocean: glacial-to-interglacial contrasts. In: Zahn, R; Pederson, T F; Kaminiski, M A & Labeyrie, L (eds.), Carbon cycling in the glacial ocean: constraints on the ocean's role in global change, Springer-Verlag, Berlin, Heidelberg, NATO ASI Series I17, 105-144 McManus, Jerry F; Oppo, Delia W; Cullen, James L (1999): A 0.5-million-year record of millennial-scale climate variability in the North Atlantic. 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CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
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https://doi.org/10.1594/PANGAEA.75833410.1029/2010PA00208510.1006/qres.1998.199210.1016/S0277-3791(00)00098-610.1029/94PA0305810.1029/94PA0335310.1016/S0967-0645(98)00098-810.1016/0012-821X(85)90154-210.1038/330035a010.1073/pnas.090577110610.1029/PA003i00 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.758334 2024-09-15T17:47:33+00:00 Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean Hesse, Tilman Butzin, Martin Bickert, Torsten Lohmann, Gerrit MEDIAN LATITUDE: 10.773327 * MEDIAN LONGITUDE: -21.986460 * SOUTH-BOUND LATITUDE: -46.764000 * WEST-BOUND LONGITUDE: -80.130000 * NORTH-BOUND LATITUDE: 82.023700 * EAST-BOUND LONGITUDE: 17.633000 * DATE/TIME START: 1957-05-19T00:00:00 * DATE/TIME END: 2005-06-24T01:23:00 * MINIMUM ELEVATION: -5105.0 m * MAXIMUM ELEVATION: 0.0 m 2011 text/tab-separated-values, 1646 data points https://doi.pangaea.de/10.1594/PANGAEA.758334 https://doi.org/10.1594/PANGAEA.758334 en eng PANGAEA Arz, Helge Wolfgang; Pätzold, Jürgen; Wefer, Gerold (1998): Correlated millennial-scale changes in surface hydrography and terrigenous sediment yield inferred from last-glacial marine deposits off northeastern Brazil. Quaternary Research, 50(2), 157-166, https://doi.org/10.1006/qres.1998.1992 Bauch, Henning A; Erlenkeuser, Helmut; Spielhagen, Robert F; Struck, Ulrich; Matthiessen, Jens; Thiede, Jörn; Heinemeier, Jan (2001): A multiproxy reconstruction of the evolution of deep and surface waters in the subarctic Nordic seas over the last 30,000 years. Quaternary Science Reviews, 20(4), 659-678, https://doi.org/10.1016/S0277-3791(00)00098-6 Bertram, Caroline J; Elderfield, Henry; Shackleton, Nicholas J; McDonald, J A (1995): Cadmium/calcium and carbon isotope reconstructions of the glacial northeast Atlantic Ocean. Paleoceanography, 10(3), 563-578, https://doi.org/10.1029/94PA03058 Beveridge, N; Elderfield, Henry; Shackleton, Nicholas J (1995): Deep thermohaline circulation in the low-latitude Atlantic during the last glacial. Paleoceanography, 10(3), 643-660, https://doi.org/10.1029/94PA03353 Bickert, Torsten; Mackensen, Andreas (2004): Last glacial to holocene changes in South Atlantic Deep Water Circulation. In: Wefer, G; Mulitza, S & Ratmeyer, V (eds.), The South Atlantic in the Late Quaternary: Reconstruction of Material Budgets and Current Systems, Springer, Berlin, Heidelberg, New York, 671-693 Bickert, Torsten; Wefer, Gerold (1996): Late Quaternary deep water circulation in the South Atlantic: Reconstruction from carbonate dissolution and benthic stable isotopes. In: Wefer, G; Berger, W H; Siedler, G & Webb, D (eds.), The South Atlantic: Present and Past Circulation. Springer-Verlag, Berlin, 103, 599-620 Bickert, Torsten; Wefer, Gerold (1999): South Atlantic and benthic foraminifer 13C deviations: Implications for reconstructing the Late Quaternary deep-water circulation. Deep Sea Research Part II: Topical Studies in Oceanography, 46(1-2), 437-452, https://doi.org/10.1016/S0967-0645(98)00098-8 Boyle, Edward A; Keigwin, Lloyd D (1985): Comparison of Atlantic and Pacific paleochemical records for the last 215.000 years: changes in deep ocean circulation and chemical inventories. Earth and Planetary Science Letters, 76(1-2), 135-150, https://doi.org/10.1016/0012-821X(85)90154-2 Boyle, Edward A; Keigwin, Lloyd D (1987): North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature. Nature, 330(6143), 35-40, https://doi.org/10.1038/330035a0 Castañeda, Isla S; Mulitza, Stefan; Schefuß, Enno; Lopes dos Santos, Raquel A; Sinninghe Damsté, Jaap S; Schouten, Stefan (2009): Wet phases in the Sahara/Sahel region and human migration patterns in North Africa. Proceedings of the National Academy of Sciences of the United States of America, 106(48), 20159-20163, https://doi.org/10.1073/pnas.0905771106 Curry, William B; Duplessy, Jean-Claude; Labeyrie, Laurent D; Shackleton, Nicholas J (1988): Changes in the distribution of d13C of deep water Sigma-CO2 between the last glaciation and the Holocene. Paleoceanography, 3(3), 317-341, https://doi.org/10.1029/PA003i003p00317 Curry, William B; Lohmann, G P (1982): Carbon isotopic changes in benthic foraminifera from the Western South Atlantic: Reconstruction of glacial abyssal circulation patterns. Quaternary Research, 18(2), 218-235, https://doi.org/10.1016/0033-5894(82)90071-0 deMenocal, Peter B; Oppo, Delia W; Fairbanks, Richard G; Prell, Warren L (1992): Pleistocene d13C variability of North Atlantic intermediate water. Paleoceanography, 7(2), 229-250, https://doi.org/10.1029/92PA00420 Duplessy, Jean-Claude (1982): North Atlantic deep water circulation during the last climate cycle. Bulletin de l'Institut de Geologie du Bassin d'Aquitaine, 31, 379-391 Freudenthal, Tim; Meggers, Helge; Henderiks, Jorijntje; Kuhlmann, Holger; Moreno, Ana; Wefer, Gerold (2002): Upwelling intensity and filament activity off Morocco during the last 250,000 years. Deep Sea Research Part II: Topical Studies in Oceanography, 49(17), 3655-3674, https://doi.org/10.1016/S0967-0645(02)00101-7 Hodell, David A; Venz, Kathryn A; Charles, Christopher D; Ninnemann, Ulysses S (2003): Pleistocene vertical carbon isotope and carbonate gradients in the South Atlantic sector of the Southern Ocean. Geochemistry, Geophysics, Geosystems, 4(1), 1004, https://doi.org/10.1029/2002GC000367 Jung, Simon J A (1996): Wassermassenaustausch zwischen NE-Atlantik und Nordmeer während der letzten 300 000/80 000 Jahre im Abbild stabiler O- und C- Isotope. 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Paleoceanography, 26, PA3220, https://doi.org/10.1029/2010PA002085 0010PG 0016PG 0021PG 0026PG 0029PG 0032PG 0033GGC 0036PG 0038PG 0044PG 0050PG 0055PG 0058PG 0066PG 0071PG 0075PG 0082PG 0091PG 0100GGC 06MT15_2 06MT41_3 108-658 108-659 162-980 162-982 175-1084 175-1085A 175-1087A 177-1088 293 313 68-502_Site 81-552 90b Agadir Canyon Age comment Agulhas Basin AII60-13APC ALB-226 also published as VM28-122 Amazon Fan Angola Basin ANT-IV/1c ANT-IX/4 ANT-VIII/3 Arctic Ocean Argentine Basin ARK-II/5 ARK-VIII/3 dataset 2011 ftpangaea https://doi.org/10.1594/PANGAEA.75833410.1029/2010PA00208510.1006/qres.1998.199210.1016/S0277-3791(00)00098-610.1029/94PA0305810.1029/94PA0335310.1016/S0967-0645(98)00098-810.1016/0012-821X(85)90154-210.1038/330035a010.1073/pnas.090577110610.1029/PA003i00 2024-08-21T00:02:27Z We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle model. The carbon cycle model employs circulation fields which were derived from previous climate simulations. All sediment data have been thoroughly quality controlled, focusing on epibenthic foraminiferal species (such as Cibicidoides wuellerstorfi or Planulina ariminensis) to improve the comparability of model and sediment core carbon isotopes. The model captures the general d13C pattern indicated by present-day water column data and Late Holocene sediment cores but underestimates intermediate and deep water values in the South Atlantic. The best agreement with glacial reconstructions is obtained for a model scenario with an altered freshwater balance in the Southern Ocean that mimics enhanced northward sea ice export and melting away from the zone of sea ice production. This results in a shoaled and weakened North Atlantic Deep Water flow and intensified Antarctic Bottom Water export, hence confirming previous reconstructions from paleoproxy records. Moreover, the modeled abyssal ocean is very cold and very saline, which is in line with other proxy data evidence. Dataset Antarc* Antarctic Arctic Arctic Ocean Foraminifera* North Atlantic Deep Water North Atlantic Sea ice Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-80.130000,17.633000,82.023700,-46.764000) |