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  • AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI  (2)
  • Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard deviation; AWI_Paleo; DEPTH, sediment/rock; KL; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Sample, optional label/labor no; SO213/2; SO213/2_79-2; Sonne; SOPATRA; South Pacific Ocean; Δ14C  (2)
  • 053-2; 057-1; 087-1; 162-983; 165-1002; 172-1060; 175-1078C; 175-1084; 293; 311; 3664N/S; 63F/NL; 90b; 94-609; Agadir Canyon; ALIENOR; ALTITUDE; AMADEUS; Amazon Fan; AMOCINT, IMAGES XVII; Angola Basin; ARK-X/2; Atlantic; Atlantic Ocean; Atlantic sediment cores; Azores; BC; Benguela Current, South Atlantic Ocean; Blake-Bahama Outer Ridge, North Atlantic Ocean; Box corer; CALYPSO; Calypso Corer; Calypso square corer; Calypso Square Core System; CASQ; CASQS; Cayman Rise, Caribbean Sea; CD159; CD159-10; CD159-17; CEPAG; CH22KW31; CH69-K09; Charles Darwin; CHO288-54; Comment; COMPCORE; Composite Core; consistent dating; Continental Slope Northeast Brazil; Core; CORE; Corner Rise; DAPC2; Denmark Strait; De Soto Canyon; DRILL; Drilling/drill rig; East Atlantic; ENAM9321; ENAM93-21; Event label; EW9209-1JPC; Faeroes Bank; Falkland Plateau, Southern Falkland Plateau (same site as GC526); Faroe Islands margin; Florida Strait; French Guiana; GC; GC528 CORE_NO 528; GeoB1023-5; GeoB1515-1; GeoB16202-2; GeoB16206-1; GeoB16224-1; GeoB1711; GeoB1711-4; GeoB1720-2; GeoB3202-1; GeoB3910-2; GeoB4240-2; GeoB5546-2; GeoB6201-5; GeoB7920-2; GeoB9508-5; GeoB9526-5; GEOFAR; GEOSCIENCES, MARMARCORE; GGC; GGC5; Giant gravity corer; GIK12392-1; GIK15669-1; GIK23415-9; GL1090; GL-1090; Glomar Challenger; Gravity corer; Gravity corer (Kiel type); GS07-150-17/1GC-A; Iceland; IMAGES I; IMAGES IX - PAGE; IMAGES V; IMAGES XV - Pachiderme; James Clark Ross; Joides Resolution; JOPSII-8; JR20110128; JR244; JR244-GC528; KAL; Kasten corer; KF13; KF16; KL; KM31; KN_USA; KN159-5; KN166-2; Knorr; KNR140; KNR140-2-51GGC; KNR140-51GGC; KNR159-5; KNR159-5-36GGC; KNR159-5-42JPC; KNR166-2; KNR166-2-26; KNR166-2-26JPC; KNR166-2-29; KNR166-2-29JPC; KNR166-2-31; KNR166-2-31JPC; KNR166-2-73; KNR166-2-73GGC; KNR197-10; KNR197-10-GGC17; KNR31GPC5; last 40 ky; LATITUDE; Leg162; Leg165; Leg172; Leg175; Leg94; Le Noroit; Le Suroît; LONGITUDE; M12392-1; M16/2; M17/2; M20/2; M25; M34/4; M35/1; M35003-4; M37/1; M39/1; M39/1_08-3; M39008-3; M42/4b; M46/2; M53; M53_169; M53/1; M6/6; M65/1; Marge Ibérique; Maria S. Merian; Marion Dufresne (1995); MD01-2461; MD022575; MD02-2575; MD02-2588; MD02-2588Q; MD02-2592; MD02-2594; MD03-2697; MD03-2698; MD03-2705; MD03-2707; MD04-2805CQ; MD04-2805Q; MD04-2845; MD07-3076; MD07-3076Q; MD08-3167; MD08-3180; MD08-3227G; MD09-3246; MD09-3256; MD09-3256Q; MD101; MD114; MD123; MD127; MD128; MD134; MD140; MD141; MD159; MD16-3511; MD16-3511Q; MD168; MD173; MD952002; MD95-2002; MD952006; MD95-2006; MD952010; MD95-2010; MD952014; MD95-2014; MD952037; MD95-2037; MD952039; MD95-2039; MD952040; MD95-2040; MD952041; MD95-2041; MD952042; MD95-2042; MD99-2281; MD99-2284; MD99-2331; MD99-2334; Meriadzec; Meteor (1964); Meteor (1986); Method comment; MSM20/3; N. Shetland channel; NA87-22; Namibia continental slope; Newfoundland margin; North Atlantic; North Atlantic/FLANK; North East Atlantic; Northeast Brasilian Margin; Norwegian Sea; OCE205-103GGC; OCE205-2-100GGC; OCE205-2-100GGGC; OCE205-2-103GGC; OCE326-GGC5; off Rio Paraiba do Sul; off West Africa; PALEOCINAT; PALEOCINAT II; PC; Persistent Identifier; PICABIA; Piston corer; Piston corer (BGR type); Polarstern; Porto Seamount; PRIVILEGE; PS2644-5; PS31; PS31/160-5; RAPiD-10-1P; RAPiD-17-5P; Reference/source; RETRO-2; REYKJANES-RÜCKEN; S94-2-KS04; SL; SO82; SO82_5-2; Sonne; South Atlantic; South Atlantic Ocean; Southern Ocean; South of Iceland; SU81-18; SU90-08; SU90-24; SU92; SU92-03; SWAF; Tagus-Sado canyon system; TNO57-21; Uniform resource locator/link to graphic; V29; V29-202; Vema; Victor Hensen; Vigo; Voring Plateau; western South Atlantic  (1)
Document type
Keywords
Publisher
Years
  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Klages, Johann Philipp; Kuhn, Gerhard; Hillenbrand, Claus-Dieter; Smith, James A; Graham, Alastair G C; Nitsche, Frank-Oliver; Frederichs, Thomas; Jernas, Patrycja E; Gohl, Karsten; Wacker, Lukas (2017): Limited grounding-line advance onto the West Antarctic continental shelf in the easternmost Amundsen Sea Embayment during the last glacial period. PLoS ONE, 12(7), e0181593, https://doi.org/10.1371/journal.pone.0181593
    Publication Date: 2023-05-12
    Description: Precise knowledge about the extent of the West Antarctic Ice Sheet (WAIS) at the Last Glacial Maximum (LGM; c. 26.5-19 cal. ka BP) is important in order to 1) improve paleo-ice sheet reconstructions, 2) provide a robust empirical framework for calibrating paleo-ice sheet models, and 3) locate potential shelf refugia for Antarctic benthos during the last glacial period. However, reliable reconstructions are still lacking for many WAIS sectors, particularly for key areas on the outer continental shelf, where the LGM-ice sheet is assumed to have terminated. In many areas of the outer continental shelf around Antarctica, direct geological data for the presence or absence of grounded ice during the LGM is lacking because of post-LGM iceberg scouring. This also applies to most of the outer continental shelf in the Amundsen Sea. Here we present detailed marine geophysical and new geological data documenting a sequence of glaciomarine sediments up to ~12 m thick within the deep outer portion of Abbot Trough, a palaeo-ice stream trough on the outer shelf of the Amundsen Sea Embayment. The upper 2-3 meters of this sediment drape contain calcareous foraminifera of Holocene and (pre-)LGM age and, in combination with palaeomagnetic age constraints, indicate that continuous glaciomarine deposition persisted here since well before the LGM, possibly even since the last interglacial period. Our data therefore indicate that the LGM grounding line, whose exact location was previously uncertain, did not reach the shelf edge everywhere in the Amundsen Sea. The LGM grounding line position coincides with the crest of a distinct grounding-zone wedge ~100 km inland from the continental shelf edge. Thus, an area of 〉6000 km² remained free of grounded ice through the last glacial cycle, requiring the LGM grounding line position to be re-located in this sector, and suggesting a new site at which Antarctic shelf benthos may have survived the last glacial period.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 17 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-06-27
    Keywords: Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard deviation; AWI_Paleo; DEPTH, sediment/rock; KL; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Sample, optional label/labor no; SO213/2; SO213/2_79-2; Sonne; SOPATRA; South Pacific Ocean; Δ14C
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-06-27
    Keywords: Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard deviation; AWI_Paleo; DEPTH, sediment/rock; KL; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Sample, optional label/labor no; SO213/2; SO213/2_79-2; Sonne; SOPATRA; South Pacific Ocean; Δ14C
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
    Location Call Number Limitation Availability
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Ronge, Thomas A; Tiedemann, Ralf; Lamy, Frank; Köhler, Peter; Alloway, Brent V; De Pol-Holz, Ricardo; Pahnke, Katharina; Southon, John; Wacker, Lukas (2016): Radiocarbon constraints on the extent and evolution of the South Pacific carbon pool. Nature Communications, 7, 12 pp, https://doi.org/10.1038/ncomms11487
    Publication Date: 2024-04-20
    Description: During the last deglaciation, the opposing patterns of atmospheric CO2 and radiocarbon activities (D14C) suggest the release of 14C-depleted CO2 from old carbon reservoirs. Although evidences point to the deep Pacific as a major reservoir of this 14C-depleted carbon, its extent and evolution still need to be constrained. Here we use sediment cores retrieved along a South Pacific transect to reconstruct the spatio-temporal evolution of D14C over the last 30,000 years. In ~2,500-3,600 m water depth, we find 14C-depleted deep waters with a maximum glacial offset to atmospheric 14C (DD14C = -1,000 per mil). Using a box model, we test the hypothesis that these low values might have been caused by an interaction of aging and hydrothermal CO2 influx. We observe a rejuvenation of circumpolar deep waters synchronous and potentially contributing to the initial deglacial rise in atmospheric CO2. These findings constrain parts of the glacial carbon pool to the deep South Pacific.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 25 datasets
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-06-18
    Description: Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear character of the climate system and underlining the possibility of rapid climate shifts in response to anthropogenic greenhouse gas forcing. To date, these rapid changes in climate and ocean circulation are still not fully explained. One obstacle hindering progress in our understanding of the interactions between past ocean circulation and climate changes is the difficulty of accurately dating marine cores. Here, we present a set of 92 marine sediment cores from the Atlantic Ocean for which we have established age-depth models that are consistent with the Greenland GICC05 ice core chronology, and computed the associated dating uncertainties, using a new deposition modeling technique. This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean. Moreover, this data set is of direct use in paleoclimate modeling studies.
    Keywords: 053-2; 057-1; 087-1; 162-983; 165-1002; 172-1060; 175-1078C; 175-1084; 293; 311; 3664N/S; 63F/NL; 90b; 94-609; Agadir Canyon; ALIENOR; ALTITUDE; AMADEUS; Amazon Fan; AMOCINT, IMAGES XVII; Angola Basin; ARK-X/2; Atlantic; Atlantic Ocean; Atlantic sediment cores; Azores; BC; Benguela Current, South Atlantic Ocean; Blake-Bahama Outer Ridge, North Atlantic Ocean; Box corer; CALYPSO; Calypso Corer; Calypso square corer; Calypso Square Core System; CASQ; CASQS; Cayman Rise, Caribbean Sea; CD159; CD159-10; CD159-17; CEPAG; CH22KW31; CH69-K09; Charles Darwin; CHO288-54; Comment; COMPCORE; Composite Core; consistent dating; Continental Slope Northeast Brazil; Core; CORE; Corner Rise; DAPC2; Denmark Strait; De Soto Canyon; DRILL; Drilling/drill rig; East Atlantic; ENAM9321; ENAM93-21; Event label; EW9209-1JPC; Faeroes Bank; Falkland Plateau, Southern Falkland Plateau (same site as GC526); Faroe Islands margin; Florida Strait; French Guiana; GC; GC528 CORE_NO 528; GeoB1023-5; GeoB1515-1; GeoB16202-2; GeoB16206-1; GeoB16224-1; GeoB1711; GeoB1711-4; GeoB1720-2; GeoB3202-1; GeoB3910-2; GeoB4240-2; GeoB5546-2; GeoB6201-5; GeoB7920-2; GeoB9508-5; GeoB9526-5; GEOFAR; GEOSCIENCES, MARMARCORE; GGC; GGC5; Giant gravity corer; GIK12392-1; GIK15669-1; GIK23415-9; GL1090; GL-1090; Glomar Challenger; Gravity corer; Gravity corer (Kiel type); GS07-150-17/1GC-A; Iceland; IMAGES I; IMAGES IX - PAGE; IMAGES V; IMAGES XV - Pachiderme; James Clark Ross; Joides Resolution; JOPSII-8; JR20110128; JR244; JR244-GC528; KAL; Kasten corer; KF13; KF16; KL; KM31; KN_USA; KN159-5; KN166-2; Knorr; KNR140; KNR140-2-51GGC; KNR140-51GGC; KNR159-5; KNR159-5-36GGC; KNR159-5-42JPC; KNR166-2; KNR166-2-26; KNR166-2-26JPC; KNR166-2-29; KNR166-2-29JPC; KNR166-2-31; KNR166-2-31JPC; KNR166-2-73; KNR166-2-73GGC; KNR197-10; KNR197-10-GGC17; KNR31GPC5; last 40 ky; LATITUDE; Leg162; Leg165; Leg172; Leg175; Leg94; Le Noroit; Le Suroît; LONGITUDE; M12392-1; M16/2; M17/2; M20/2; M25; M34/4; M35/1; M35003-4; M37/1; M39/1; M39/1_08-3; M39008-3; M42/4b; M46/2; M53; M53_169; M53/1; M6/6; M65/1; Marge Ibérique; Maria S. Merian; Marion Dufresne (1995); MD01-2461; MD022575; MD02-2575; MD02-2588; MD02-2588Q; MD02-2592; MD02-2594; MD03-2697; MD03-2698; MD03-2705; MD03-2707; MD04-2805CQ; MD04-2805Q; MD04-2845; MD07-3076; MD07-3076Q; MD08-3167; MD08-3180; MD08-3227G; MD09-3246; MD09-3256; MD09-3256Q; MD101; MD114; MD123; MD127; MD128; MD134; MD140; MD141; MD159; MD16-3511; MD16-3511Q; MD168; MD173; MD952002; MD95-2002; MD952006; MD95-2006; MD952010; MD95-2010; MD952014; MD95-2014; MD952037; MD95-2037; MD952039; MD95-2039; MD952040; MD95-2040; MD952041; MD95-2041; MD952042; MD95-2042; MD99-2281; MD99-2284; MD99-2331; MD99-2334; Meriadzec; Meteor (1964); Meteor (1986); Method comment; MSM20/3; N. Shetland channel; NA87-22; Namibia continental slope; Newfoundland margin; North Atlantic; North Atlantic/FLANK; North East Atlantic; Northeast Brasilian Margin; Norwegian Sea; OCE205-103GGC; OCE205-2-100GGC; OCE205-2-100GGGC; OCE205-2-103GGC; OCE326-GGC5; off Rio Paraiba do Sul; off West Africa; PALEOCINAT; PALEOCINAT II; PC; Persistent Identifier; PICABIA; Piston corer; Piston corer (BGR type); Polarstern; Porto Seamount; PRIVILEGE; PS2644-5; PS31; PS31/160-5; RAPiD-10-1P; RAPiD-17-5P; Reference/source; RETRO-2; REYKJANES-RÜCKEN; S94-2-KS04; SL; SO82; SO82_5-2; Sonne; South Atlantic; South Atlantic Ocean; Southern Ocean; South of Iceland; SU81-18; SU90-08; SU90-24; SU92; SU92-03; SWAF; Tagus-Sado canyon system; TNO57-21; Uniform resource locator/link to graphic; V29; V29-202; Vema; Victor Hensen; Vigo; Voring Plateau; western South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 563 data points
    Location Call Number Limitation Availability
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