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  • 2015-2019  (787,988)
  • 1965-1969  (8)
  • 1960-1964  (7)
  • 1955-1959  (5)
  • 2016  (787,988)
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Year
  • 1
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    PANGAEA
    In:  Supplement to: Ho, Sze Ling; Laepple, Thomas (2016): Flat meridional temperature gradient in the early Eocene in the subsurface rather than surface ocean. Nature Geoscience, https://doi.org/10.1038/ngeo2763
    Publication Date: 2024-07-01
    Description: This dataset contains the collection of available published paired Uk'37 and Tex86 records spanning multi-millennial to multi-million year time scales, as well as a collection of Mg/Ca-derived temperatures measured in parallel on surface and subsurface dwelling foraminifera, both used in the analyses of Ho and Laepple, Nature Geoscience 2016. As the signal-to-noise ratios of proxy-derived Holocene temperatures are relatively low, we selected records that contain at least the last deglaciation (oldest sample 〉18kyr BP).
    Keywords: 130-806; 138-850; 145-882; 161-977A; 165-999A; 175-1085; 184-1143; 184-1146; 184-1147; 202-1239; 202-1240; 202-1241; 202-1241C; 293G; 313; 64PE-174P13; 77; Alboran Sea; Arabian Sea; AUSCAN; AWI_PerDyn; Benguela Current, South Atlantic Ocean; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; Caribbean Sea; CD129; Charles Darwin; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Eastern Mediterranean, Continental slope off Israel; Elevation of event; Equatorial East Pacific; Event label; GC; GeoB10038-4; GeoB12610-2; GeoB7702-3; GeoB7926-2; GeoB9528-3; GEOSCIENCES, MARMARCORE; Giant piston corer; GPC; Gravity corer; Gravity corer (Kiel type); Guaymas Basin; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES VIII - MONA; IMAGES VII - WEPAMA; IMAGES XII - MARCO POLO; IMAGES XIV - MARCO POLO 2; Joides Resolution; KAL; Kasten corer; KL-74, AS-12; Latitude of event; Leg130; Leg138; Leg145; Leg161; Leg165; Leg175; Leg184; Leg202; Longitude of event; M52/2; M53/1; M65/1; M75/2; M75/2_97-2; Marion Dufresne (1995); MD012378; MD01-2378; MD012390; MD01-2390; MD01-2461; MD022515; MD02-2515; MD032607; MD03-2607; MD052904; MD05-2904; MD06-3067; MD104; MD106; MD111; MD122; MD123; MD126; MD131; MD147; MD155; MD96-2048; MD972146; MD97-2146; MD972151; MD97-2151; MD982195; MD98-2195; Meteor (1986); Method comment; Mindanao; NIOP-C2; NIOP-C2_905_PC; North Pacific Ocean; North-West African margin; PABESIA; PC; PEGASE; Pemba Channel; Permafrost Research (Periglacial Dynamics) @ AWI; Persistent Identifier; Piston corer; Professor Logachev; Reference/source; SL; SO184/1; SO18460; SO185; SO213/2; SO213/2_59-2; SO42; SO42-74KL; Sonne; SOPATRA; South China Sea; Southern Ocean; South Pacific Ocean; Species; SW Indian Ocean; Timor Sea; TTR-12_293G; TTR-12/3; Tyro; V12; V12-107; Vema; VITAL; Walvis Ridge; WIND; WIND-28K
    Type: Dataset
    Format: text/tab-separated-values, 159 data points
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  • 2
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    PANGAEA
    In:  Department of Physical Geography, University of Stockholm | Supplement to: Siewert, Matthias Benjamin; Hugelius, Gustaf; Heim, Birgit; Faucherre, Samuel (2016): Landscape controls and vertical variability of soil organic carbon storage in permafrost-affected soils of the Lena River Delta. CATENA, 147, 725-741, https://doi.org/10.1016/j.catena.2016.07.048
    Publication Date: 2024-07-01
    Description: To project the future development of the soil organic carbon (SOC) storage in permafrost environments, the spatial and vertical distribution of key soil properties and their landscape controls needs to be understood. This article reports findings from the Arctic Lena River Delta where we sampled 50 soil pedons. These were classified according to the U.S.D.A. Soil Taxonomy and fall mostly into the Gelisol soil order used for permafrost-affected soils. Soil profiles have been sampled for the active layer (mean depth 58 ± 10 cm) and the upper permafrost to one meter depth. We analyze SOC stocks and key soil properties, i.e. C%, N%, C/N, bulk density, visible ice and water content. These are compared for different landscape groupings of pedons according to geomorphology, soil and land cover and for different vertical depth increments. High vertical resolution plots are used to understand soil development. These show that SOC storage can be highly variable with depth. We recommend the treatment of permafrost-affected soils according to subdivisions into: the surface organic layer, mineral subsoil in the active layer, organic enriched cryoturbated or buried horizons and the mineral subsoil in the permafrost. The major geomorphological units of a subregion of the Lena River Delta were mapped with a land form classification using a data-fusion approach of optical satellite imagery and digital elevation data to upscale SOC storage. Landscape mean SOC storage is estimated to 19.2 ± 2.0 kg C/m**2. Our results show that the geomorphological setting explains more soil variability than soil taxonomy classes or vegetation cover. The soils from the oldest, Pleistocene aged, unit of the delta store the highest amount of SOC per m2 followed by the Holocene river terrace. The Pleistocene terrace affected by thermal-degradation, the recent floodplain and bare alluvial sediments store considerably less SOC in descending order.
    Keywords: Changing Permafrost in the Arctic and its Global Effects in the 21st Century; PAGE21
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2024-07-01
    Description: This data collection presents the compilation of scientific results of the EU project BENGAL.
    Keywords: 12812-002; 12913-002; 12914-003; 12923-002; 12923-005; 12923-013; 12925-004; 12925-008; 12926-001; 12926-002; 12930-004; 12930-005; 12930-006; 12930-007; 12930-010; 12930-014; 12930-015; 12930-017; 12930-018; 12930-022; 12930-023; 12930-025; 12930-026; 12930-027; 12930-028; 12930-029; 12930-032; 12930-034; 12930-035; 12930-036; 12930-037; 12930-038; 12930-039; 12930-040; 12930-044; 12930-045; 12930-046; 12930-048; 12930-049; 12930-052; 12930-055; 12930-059; 12930-061; 12930-063; 12930-064; 12930-065; 12930-066; 12930-068; 12930-071; 12930-073; 12930-075; 12930-078; 12930-081; 12930-082; 12930-084; 12930-087; 12930-093; 12930-095; 13077-001; 13077-004; 13077-006; 13077-012; 13077-014; 13077-015; 13077-018; 13077-019; 13077-021; 13077-023; 13077-024; 13077-025; 13077-026; 13077-035; 13077-036; 13077-047; 13077-057; 13077-058; 13077-059; 13077-060; 13077-062; 13077-063; 13077-065; 13077-069; 13077-070; 13077-071; 13077-072; 13077-078; 13077-087; 13077-089; 13077-090; 13077-093; 13077-096; 13077-097; 13077-098; 13077-099; 13078-006; 13078-008; 13078-010; 13078-011; 13078-012; 13078-013; 13078-015; 13078-016; 13078-017; 13078-018; 13078-019; 13078-027; 13078-029; 13078-031; 13078-037; 13078-038; 13200-001; 13200-004; 13200-005; 13200-007; 13200-008; 13200-009; 13200-010; 13200-011; 13200-012; 13200-016; 13200-017; 13200-018; 13200-020; 13200-021; 13200-022; 13200-024; 13200-025; 13200-026; 13200-027; 13200-028; 13200-029; 13200-030; 13200-032; 13200-033; 13200-035; 13200-036; 13200-039; 13200-041; 13200-045; 13200-046; 13200-047; 13200-048; 13200-049; 13200-051; 13200-052; 13200-053; 13200-058; 13200-059; 13200-060; 13200-061; 13200-062; 13200-063; 13200-065; 13200-068; 13200-069; 13200-070; 13200-071; 13200-073; 13200-074; 13200-075; 13200-077; 13200-078; 13200-080; 13200-081; 13200-082; 13200-083; 13200-084; 13200-087; 13200-089; 13200-090; 13200-091; 13200-093; 13200-094; 13200-096; 13200-099; 13201-001; 13201-002; 13201-005; 13368-003; 13368-004; 13368-007; 13368-008; 13368-012; 13368-014; 13368-015; 13368-019; 13368-022; 13368-023; 13368-024; 13368-025; 13368-026; 13368-028; 13368-030; 13368-036; 13368-039; 13368-040; 13368-042; 13368-044; 13368-045; 13368-047; 13368-048; 13368-049; 13368-051; 13368-052; 13368-053; 13368-055; 13368-056; 13368-057; 13370-004; 13370-005; 13370-006; 13627-005; 13627-008; 13627-010; 13627-011; 13627-012; 13627-014; 13627-015; 13627-017; 13627-022; 13627-023; 13627-024; 269; 356; 362; 372; 373; 54301-002; 54301-003; 54301-005; 54301-008; 54301-009; 54301-010; 54301-012; 54301-014; 54301-016; 54301-019; 54301-021; 54301-023; 64PE123; ALBEX lander; Autonome colonisation module; Baited free-fall benthic amphipod trap; BC; Bengal; BENGAL; Benthic Biology and Geochemistry of a North-eastern Atlantic Abyssal Locality; BIO; Biology; BN; Bottom net; Bottom water sampler; Box corer; BWS; CH135; Challenger; Chalut à perche (6 m beam trawl); CMA; CP; CTD/Rosette; CTD-RO; Current meter, Aanderaa; D217; D222/1; D222/2; D226; D229; D231; D236; D237; DEMAR; DI236_08-1; DI236_11-1; DI236_16-1; DI236_18-1; DI236_21-1; DI236_23-1; DI236_25-1; DI236_28-1; DI236_29-1; DI236_31-1; DI236_34-1; DI236_42-1; DI236_45-1; DI236_49-1; Discovery (1962); D-MOC-01; D-MOC-02; D-MOC-03; D-MOC-04; D-MOC-07; Dy222_FFR-05; FFR; FFR-01; FFR-02; FFR-04; Free vehicle respirometer; FT-04; FTS; GBGL; GBGL-01; GBGL-02; Göteborg lander; IMBC; IMBC lander; KASTEN; Kasten corer (1 m**2); M36/4; M36/4_MC1; M36/4_MC4; M36/4_MC5; M36/5; M36/5_MC26; M36/5_MC27; M36/5_MC28; M36/6; M36/6_368FFR; M36/6_371BWS; M36/6_372MUC; M36/6_373MUC; M36/6_375MSN; M36/6_380MSN; M36/6_381BWS; M36/6_BWS-19; M36/6_BWS-20; M36/6_MC33; M36/6_MC38; M36/6_MC41; M42/2; M42/2_363-1; M42/2_365; M42/2_366; M42/2_367; M42/2_368-2; M42/2_368-3; M42/2_370; M42/2_373; M42/2_374-2; M42/2_374-3; M42/2_377-1; M42/2_377-5; M42/2_377-6; M42/2_380-2; M42/2_380-3; M42/2_380-4; M42/2_381; M42/2_384-1; M42/2_385; M42/2_386; M42/2_388-1; M42/2_388-2; M42/2_391-2; M42/2_397-1; M42/2_397-3; M42/2_417; M42/2_418; M42/2_419; M42/2_420; M42/2_421-2; M42/2_421-3; M42/2_421-5; M42/2_422; M42/2_424-1; M42/2_424-2; M42/2_424-4; M42/2_425; M42/2_426-2; M42/2_429-1; M42/2_429-2; M42/2_430; M42/2_432-1; M42/2_433; M42/2_434-1; M42/2_434-2; M42/2_436; M42/2_438; M42/2_BWS-01; M42/2_BWS-02; M42/2_BWS-04; M42/2_BWS-05; M42/2_BWS-09; M42/2_BWS-10; M42/2_BWS-12; M42/2_CTD-03; M42/2_CTD-05; M42/2_CTD-06; M42/2_CTD-07; M42/2_CTD-08; M42/2_CTD-09; M42/2_CTD-13; M42/2_CTD-22; M42/2_CTD-24; M42/2_CTD-25; M42/2_CTD-28; M42/2_CTD-29; M42/2_CTD-31; M42/2_MC-04; M42/2_MC-09; M42/2_MC1; M42/2_MC2; M42/2_MC27; M42/2_MC28; M42/2_MC29; M42/2_MC-30; M42/2_MC31; M42/2_MC-32; M42/2_MC34; M42/2_MC-34; M42/2_MC4; M42/2_MC5; M42/2_MC6; M42/2_MC7; M42/2_MC8; MACOL; MCB57; MCB57-74; MCB92; MCS; MEGAC; MegaCorer; Meteor (1986); MOC; MOC1; MOCNESS opening/closing plankton net; MOCNESS opening/closing plankton net 1 sqm; MSN; MUC; MULT; MultiCorer; MultiCorer, small; MultiCorer Barnett pattern (12-57); MultiCorer Barnett pattern (4-57.8-74); MultiCorer Barnett pattern (8-92); Multiple investigations; Multiple opening/closing net; NIOZL; OTSB14; PAP; PAP-XIX; PAP-XV; PAP-XVIII; PAP-XX; PAP-XXIIIa; Pelagia; Photo sledge; PLG123; PLG123/12-1; PLG123/13-2; PLG123/13-3; PLG123/13-5; PLG123/13-6; PLG123/13-7; PLG123/14-1; Porcupine Abyssal Plain; RESP; Respirometer; RK127; RK128; RK130; SAPS; Sediment profile imagery; Semi-balloon trawl; SEP; South Atlantic Ocean; Spade box corer; Stand-alone pumps; Trap, sediment; TRAPS; VEGBOXC; Vertical amphipod trap; VET
    Type: Dataset
    Format: application/zip, 515 datasets
    Location Call Number Expected Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Schröder, Jan F; Holbourn, Ann E; Kuhnt, Wolfgang; Küssner, Kevin (2016): Variations in sea surface hydrology in the southern Makassar Strait over the past 26 kyr. Quaternary Science Reviews, 154, 143-156, https://doi.org/10.1016/j.quascirev.2016.10.018
    Publication Date: 2024-07-01
    Description: We present centennial-scale records of sea surface temperature and oxygen isotopes in a sediment core from Mandar Bay, offshore Sulawesi in the southern Makassar Strait, which provide new insights into the variability of Indonesian climate over the past 26 kyr. The age model for the core is constrained by 17 AMS radiocarbon ages, with a surface ocean reservoir age correction based on paired wood and foraminiferal samples. Small Holocene reservoir ages of 105 ± 180 years point to intense surface ocean-atmosphere interchange linked to increased monsoonal precipitation, whereas Last Glacial Maximum and deglacial reservoir ages are significantly higher. Mg/Ca derived sea surface temperature reconstructions based on Globigerinoides ruber (s. s., white) exhibit an extended plateau during the Antarctic Cold Reversal, suggesting an atmospheric connection to high-latitude Southern Hemisphere climate and a seasonal bias on G. ruber. This is in agreement with southern hemisphere sites along the track of the Indonesian Throughflow and in contrast to Northern Hemisphere records from the South China Sea, Sulu Sea and Western Pacific (off Mindanao), which exhibit warming during the Bølling-Allerød. Ice-volume corrected d18O seawater (d18Osw) increased during Heinrich Stadial 1 and the Younger Dryas, whereas the Bølling-Allerød is characterized by low d18Osw. We attribute d18Osw variability in the southern Makassar Strait during the Last Glacial Maximum and glacial termination to changes in provenance and seasonality of precipitation rather than to variability in the amount of local precipitation and runoff.
    Keywords: GIK/IfG; GIK18515-3; Institute for Geosciences, Christian Albrechts University, Kiel; KL; MAJA; Makasar Strait; Piston corer (BGR type); SO217; SO217_2-3; Sonne
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
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    PANGAEA
    In:  Department of Geosciences, Bremen University
    Publication Date: 2024-07-01
    Keywords: Center for Marine Environmental Sciences; CONDOR-Ia; DEPTH, sediment/rock; Dry mass; GeoB; GeoB3301-4; Geosciences, University of Bremen; Gravity corer (Kiel type); MARUM; Mass, tara; SL; SO101; SO101/3_1-4; Sonne; South-East Pacific; Volume; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 304 data points
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  • 6
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    PANGAEA
    In:  Department of Geosciences, Bremen University
    Publication Date: 2024-07-01
    Keywords: Center for Marine Environmental Sciences; CONDOR-Ia; DEPTH, sediment/rock; Dry mass; GeoB; GeoB3302-1; Geosciences, University of Bremen; Gravity corer (Kiel type); MARUM; Mass, tara; SL; SO101; SO101/3_2-1; Sonne; South-East Pacific; Volume; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 274 data points
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  • 7
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    PANGAEA
    In:  Department of Geosciences, Bremen University
    Publication Date: 2024-07-01
    Keywords: Center for Marine Environmental Sciences; CONDOR-Ia; DEPTH, sediment/rock; Dry mass; GeoB; GeoB3304-5; Geosciences, University of Bremen; Gravity corer (Kiel type); MARUM; Mass, tara; SL; SO101; Sonne; South-East Pacific; Volume; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 566 data points
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  • 8
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    PANGAEA
    In:  Department of Geosciences, Bremen University
    Publication Date: 2024-07-01
    Keywords: Center for Marine Environmental Sciences; CONDOR-Ia; DEPTH, sediment/rock; Dry mass; GeoB; GeoB3305-1; Geosciences, University of Bremen; Gravity corer (Kiel type); MARUM; Mass, tara; SL; SO101; Sonne; South-East Pacific; Volume; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 271 data points
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  • 9
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    PANGAEA
    In:  Department of Geosciences, Bremen University
    Publication Date: 2024-07-01
    Keywords: Center for Marine Environmental Sciences; CONDOR-Ia; DEPTH, sediment/rock; Dry mass; GeoB; GeoB3308-1; Geosciences, University of Bremen; Gravity corer (Kiel type); MARUM; Mass, tara; SL; SO101; Sonne; South-East Pacific; Volume; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 633 data points
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  • 10
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    Unknown
    PANGAEA
    In:  Department of Geosciences, Bremen University
    Publication Date: 2024-07-01
    Keywords: Center for Marine Environmental Sciences; CONDOR-Ia; DEPTH, sediment/rock; Dry mass; GeoB; GeoB3311-1; Geosciences, University of Bremen; Gravity corer (Kiel type); MARUM; Mass, tara; SL; SO101; Sonne; South-East Pacific; Volume; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 254 data points
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