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  • PANGAEA  (12)
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  • 1
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    Age determination of sediment core MD07-3088 (2013)
    PANGAEA
    In:  Supplement to: Siani, Giuseppe; Michel, Elisabeth; De Pol-Holz, Ricardo; DeVries, Tim; Lamy, Frank; Carel, Mélanie; Isguder, Gulay; Dewilde, Fabien; Lourantou, Anna (2013): Carbon isotope records reveal precise timing of enhanced Southern Ocean upwelling during the last deglaciation. Nature Communications, 4, 1-9, https://doi.org/10.1038/ncomms3758
    Details
    Publication Date: 2023-01-13
    Description: The Southern Ocean plays a prominent role in the Earth's climate and carbon cycle. Changes in the Southern Ocean circulation may have regulated the release of CO2 to the atmosphere from a deep-ocean reservoir during the last deglaciation. However, the path and exact timing of this deglacial CO2 release are still under debate. Here we present measurements of deglacial surface reservoir 14C age changes in the eastern Pacific sector of the Southern Ocean, obtained by 14C dating of tephra deposited over the marine and terrestrial regions. These results, along with records of foraminifera benthic-planktic 14C age and d13C difference, provide evidence for three periods of enhanced upwelling in the Southern Ocean during the last deglaciation, supporting the hypothesis that Southern Ocean upwelling contributed to the deglacial rise in atmospheric CO2. These independently dated marine records suggest synchronous changes in the Southern Ocean circulation and Antarctic climate during the last deglaciation.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
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    (Supplementary Table S2) Compiled radiocarbon data. Planktic and benthic radiocarbon dates, B-P offset and Delta14C estimates from core MD07-3088 (2013)
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Keywords: Age, 14C conventional; Age, dated; Age, dated, error to older; Age, dated, error to younger; Age, dated material; Age, dated standard deviation; Age, difference; Age, difference error; Calendar age; CALYPSO2; Calypso Corer II; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; IMAGES XV - Pachiderme; Marion Dufresne (1995); MD07-3088; MD159; Sample, optional label/labor no; δ14C; δ14C, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 456 data points
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  • 3
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    Stable carbon isotope ratios of carbon dioxide from EDC and Berkner Island ice cores for 40-50 ka BP
    PANGAEA
    In:  Supplement to: Schaefer, Hinrich; Lourantou, Anna; Chappellaz, Jérôme A; Lüthi, Dieter; Bereiter, Bernhard; Barnola, Jean-Marc (2011): On the suitability of partially clathrated ice for analysis of concentration and d13C of palaeo-atmospheric CO2. Earth and Planetary Science Letters, 307(3-4), 334-340, https://doi.org/10.1016/j.epsl.2011.05.007
    Details
    Publication Date: 2023-06-27
    Description: The stable carbon isotopic signature of carbon dioxide (d13CO2) measured in the air occlusions of polar ice provides important constraints on the carbon cycle in past climates. In order to exploit this information for previous glacial periods, one must use deep, clathrated ice, where the occluded air is preserved not in bubbles but in the form of air hydrates. Therefore, it must be established whether the original atmospheric d13CO2 signature can be reconstructed from clathrated ice. We present a comparative study using coeval bubbly ice from Berkner Island and ice from the bubble-clathrate transformation zone (BCTZ) of EPICA Dome C (EDC). In the EDC samples the gas is partitioned into clathrates and remaining bubbles as shown by erroneously low and scattered CO2 concentration values, presenting a worst-case test for d13CO2 reconstructions. Even so, the reconstructed atmospheric d13CO2 values show only slightly larger scatter. The difference to data from coeval bubbly ice is statistically significant. However, the 0.16 per mil magnitude of the offset is small for practical purposes, especially in light of uncertainty from non-uniform corrections for diffusion related fractionation that could contribute to the discrepancy. Our results are promising for palaeo-atmospheric studies of d13CO2 using a ball mill dry extraction technique below the BCTZ of ice cores, where gas is not subject to fractionation into microfractures and between clathrate and bubble reservoirs.
    Keywords: Berkner Island; BIC; Carbon dioxide; Carbon dioxide, standard deviation; DEPTH, ice/snow; Dome C; Dome C, Antarctica; EDC; EPICA; EPICA Dome C; European Project for Ice Coring in Antarctica; Event label; Gas age; ICEDRILL; Ice drill; Mass spectrometer Finnigan MAT 252; Sample code/label; see reference(s); δ13C, carbon dioxide, atmospheric; δ13C, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 162 data points
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  • 4
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    Measurements of stable carbon isotope ratios of CO2 over the last 24000 years and CO2 concentration measurements on Antarctic ice cores using three different methods (2012)
    PANGAEA
    In:  Supplement to: Schmitt, Jochen; Schneider, Robert; Elsig, Joachim; Leuenberger, Daiana; Lourantou, Anna; Chappellaz, Jérôme A; Köhler, Peter; Joos, Fortunat; Stocker, Thomas F; Leuenberger, Markus Christian; Fischer, Hubertus (2012): Carbon isotope constraints on the deglacial CO2 rise from ice cores. Science, 336(6082), 711-714, https://doi.org/10.1126/science.1217161
    Details
    Publication Date: 2023-07-12
    Description: The stable carbon isotope ratio of atmospheric CO2 (d13Catm) is a key parameter in deciphering past carbon cycle changes. Here we present d13Catm data for the past 24,000 years derived from three independent records from two Antarctic ice cores. We conclude that a pronounced 0.3 per mil decrease in d13Catm during the early deglaciation can be best explained by upwelling of old, carbon-enriched waters in the Southern Ocean. Later in the deglaciation, regrowth of the terrestrial biosphere, changes in sea surface temperature, and ocean circulation governed the d13Catm evolution. During the Last Glacial Maximum, d13Catm and atmospheric CO2 concentration were essentially constant, which suggests that the carbon cycle was in dynamic equilibrium and that the net transfer of carbon to the deep ocean had occurred before then.
    Keywords: Antarctica; Dome C; DRILL; Drilling/drill rig; EDC96; EDC99; EPICA; European Project for Ice Coring in Antarctica; ICEDRILL; Ice drill; TALDICE; Talos_Dome
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 5
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    Monte Carlo average of stable carbon isotope ratio of atmospheric CO2 from three Antarctic ice cores (2012)
    PANGAEA
    Details
    Publication Date: 2023-07-12
    Keywords: Calculated; EPICA; European Project for Ice Coring in Antarctica; Gas age; δ13C, carbon dioxide, atmospheric; δ13C, carbon dioxide, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 71814 data points
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  • 6
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    Stable carbon isotope ratio of atmospheric CO2 of ice core Talos Dome, Bern sublimation (2012)
    PANGAEA
    Details
    Publication Date: 2023-10-13
    Keywords: Carbon dioxide; Carbon dioxide, standard deviation; Correction; DEPTH, ice/snow; Gas age; ICEDRILL; Ice drill; Replicates; TALDICE; Talos_Dome; Talos Dome Ice Core; δ13C, carbon dioxide, atmospheric; δ13C, carbon dioxide, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
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  • 7
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    (Supplementary Table S1) Tephra ages and sea surface reservoir 14C ages estimates in core MD07-3088 (2013)
    PANGAEA
    Details
    Publication Date: 2023-11-04
    Keywords: Age, 14C conventional; Age, dated; Age, dated material; Age, dated standard deviation; Calendar age; CALYPSO2; Calypso Corer II; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eruption; IMAGES XV - Pachiderme; Marion Dufresne (1995); MD07-3088; MD159; Origin; Reference/source; Reservoir effect/correction; Reservoir effect/correction, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 139 data points
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  • 8
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    Surface Ocean CO2 Atlas (SOCAT) V1.4 (2013)
    PANGAEA
    In:  Supplement to: Pfeil, Benjamin; Olsen, Are; Bakker, Dorothee C E; Hankin, Steven; Koyuk, Heather; Kozyr, Alexander; Malczyk, Jeremy; Manke, Ansley; Metzl, Nicolas; Sabine, Christopher L; Akl, John; Alin, Simone R; Bellerby, Richard G J; Borges, Alberto Vieira; Boutin, Jacqueline; Brown, Peter J; Cai, Wei-Jun; Chavez, Francisco P; Chen, Arthur; Cosca, Catherine E; Fassbender, Andrea J; Feely, Richard A; González-Dávila, Melchor; Goyet, Catherine; Hardman-Mountford, Nicolas J; Heinze, Christoph; Hood, E Maria; Hoppema, Mario; Hunt, Christopher W; Hydes, David; Ishii, Masao; Johannessen, Truls; Jones, Steve D; Key, Robert M; Körtzinger, Arne; Landschützer, Peter; Lauvset, Siv K; Lefèvre, Nathalie; Lenton, Andrew; Lourantou, Anna; Merlivat, Liliane; Midorikawa, Takashi; Mintrop, Ludger J; Miyazaki, Chihiro; Murata, Akihiko; Nakadate, Akira; Nakano, Yoshiyuki; Nakaoka, Shin-Ichiro; Nojiri, Yukihiro; Omar, Abdirahman M; Padín, Xose Antonio; Park, Geun-Ha; Paterson, Kristina; Pérez, Fiz F; Pierrot, Denis; Poisson, Alain; Ríos, Aida F; Santana-Casiano, Juana Magdalena; Salisbury, Joe; Sarma, Vedula V S S; Schlitzer, Reiner; Schneider, Bernd; Schuster, Ute; Sieger, Rainer; Skjelvan, Ingunn; Steinhoff, Tobias; Suzuki, Toru; Takahashi, Taro; Tedesco, Kathy; Telszewski, Maciej; Thomas, Helmuth; Tilbrook, Bronte; Tjiputra, Jerry; Vandemark, Doug; Veness, Tony; Wanninkhof, Rik; Watson, Andrew J; Weiss, Ray F; Wong, Chi Shing; Yoshikawa-Inoue, Hisayuki (2013): A uniform, quality controlled Surface Ocean CO2 Atlas (SOCAT). Earth System Science Data, 5(1), 125-143, https://doi.org/10.5194/essd-5-125-2013
    Details
    Publication Date: 2024-02-02
    Description: A well-documented, publicly available, global data set of surface ocean carbon dioxide (CO2) parameters has been called for by international groups for nearly two decades. The Surface Ocean CO2 Atlas (SOCAT) project was initiated by the international marine carbon science community in 2007 with the aim of providing a comprehensive, publicly available, regularly updated, global data set of marine surface CO2, which had been subject to quality control (QC). Many additional CO2 data, not yet made public via the Carbon Dioxide Information Analysis Center (CDIAC), were retrieved from data originators, public websites and other data centres. All data were put in a uniform format following a strict protocol. Quality control was carried out according to clearly defined criteria. Regional specialists performed the quality control, using state-of-the-art web-based tools, specially developed for accomplishing this global team effort. SOCAT version 1.5 was made public in September 2011 and holds 6.3 million quality controlled surface CO2 data points from the global oceans and coastal seas, spanning four decades (1968-2007). Three types of data products are available: individual cruise files, a merged complete data set and gridded products. With the rapid expansion of marine CO2 data collection and the importance of quantifying net global oceanic CO2 uptake and its changes, sustained data synthesis and data access are priorities.
    Keywords: 0306SFC_PRT; 061ASFC_PRT; 06AQ19860627-track; 06AQ19860928-track; 06AQ19911114-track; 06AQ19911210-track; 06AQ19921005-track; 06AQ19930128-track; 06AQ19930228-track; 06AQ19931019-track; 06AQ19940524-track; 06AQ19951206-track; 06AQ19960320-track; 06AQ19980411-track; 06AQ19990327-track; 06AQ20001004-track; 06AQ20001026-track; 06BE19961010-track; 06CK20060523-track; 06CK20060715-track; 06CK20060821-track; 06GA19960613-track; 06GA276_3; 06LB19831130-track; 06LB19840107-track; 06LB19840629-track; 06LB19850110-track; 06LB19850313-track; 06LB19850812-track; 06LB19860116-track; 06LB19860323-track; 06LB19860801-track; 06LB19861011-track; 06LB19861214-track; 06LB19870221-track; 06LB19870501-track; 06LB19870721-track; 06LB19870920-track; 06LB19871126-track; 06LB19871231-track; 06LB19880204-track; 06MT18_1; 06MT19910903-track; 06MT19920510-track; 06MT19921229-track; 06MT19941012-track; 06MT19941119-track; 06MT19950714-track; 06MT19960607-track; 06MT19960622-track; 06MT19970106-track; 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20070613_TC2; 20070620_TC2; 20070627_TC2; 20070703_TC2; 20070709_TC2; 20070716_TC2; 20070723_TC2; 20070730_TC2; 2007-07-BS; 20070806_TC2; 20070815_TC2; 20070820_TC2; 20070827_TC2; 2007-08-BS; 20070903_TC2; 20070910_TC2; 20070917_TC2; 20071001_TC2; 20071008_TC2; 20071010_TC2; 20071015_TC2; 20071023_TC2; 20071105_TC2; 20071115_TC2; 20071120_TC2; 20071128_TC2; 20071204_TC2; 20071211_TC2; 20071218_TC2; 20071225_TC2; 24N98L1; 24N98L2; 26GC20010421-track; 26GC20010831-track; 26NA20050107; 26NA20050107-track; 26NA20050115; 26NA20050115-track; 26NA20050130; 26NA20050130-track; 26NA20050207; 26NA20050207-track; 26NA20050317; 26NA20050317-track; 26NA20050321; 26NA20050321-track; 26NA20050402; 26NA20050402-track; 26NA20050420; 26NA20050420-track; 26NA20050502; 26NA20050502-track; 26NA20050511; 26NA20050511-track; 26NA20050523; 26NA20050523-track; 26NA20050531; 26NA20050531-track; 26NA20050614; 26NA20050614-track; 26NA20050624; 26NA20050624-track; 26NA20050714; 26NA20050714-track; 26NA20050720; 26NA20050720-track; 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    Type: Dataset
    Format: application/zip, 1851 datasets
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  • 9
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    Stable carbon isotope ratio of atmospheric CO2 of ice core EDC96, Bern sublimation (2012)
    PANGAEA
    Details
    Publication Date: 2024-03-18
    Keywords: Antarctica; Carbon dioxide; Carbon dioxide, standard deviation; Correction; DEPTH, ice/snow; Dome C; EDC96; EPICA; European Project for Ice Coring in Antarctica; Gas age; ICEDRILL; Ice drill; Replicates; δ13C, carbon dioxide, atmospheric; δ13C, carbon dioxide, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 10
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    Stable carbon isotope ratio of atmospheric CO2 of ice core EDC96, Grenoble ball mill (2012)
    PANGAEA
    Details
    Publication Date: 2024-03-18
    Keywords: Antarctica; Carbon dioxide; Carbon dioxide, standard deviation; Correction; DEPTH, ice/snow; Dome C; EDC96; EPICA; European Project for Ice Coring in Antarctica; Gas age; ICEDRILL; Ice drill; δ13C, carbon dioxide, atmospheric; δ13C, carbon dioxide, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 372 data points
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    DATA PANGAEA
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