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  • PANGAEA  (60,120)
  • Blackwell Publishing Ltd  (27,294)
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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Auffret, Gérard A; Zaragosi, Sebastien; Dennielou, Bernard; Cortijo, Elsa; Van Rooij, David; Grousset, Francis E; Pujol, Claude; Eynaud, Frédérique; Siegert, Martin J (2002): Terrigenous fluxes at the Celtic Margin during the last glacial cycle. Marine Geology, 188(1-2), 79-108, https://doi.org/10.1016/S0025-3227(02)00276-1
    Publication Date: 2024-06-25
    Description: The sedimentary sections of three cores from the Celtic margin provide high-resolution records of the terrigenous fluxes during the last glacial cycle. A total of 21 14C AMS dates allow us to define age models with a resolution better than 100 yr during critical periods such as Heinrich events 1 and 2. Maximum sedimentary fluxes occurred at the Meriadzek Terrace site during the Last Glacial Maximum (LGM). Detailed X-ray imagery of core MD95-2002 from the Meriadzek Terrace shows no sedimentary structures suggestive of either deposition from high-density turbidity currents or significant erosion. Two paroxysmal terrigenous flux episodes have been identified. The first occurred after the deposition of Heinrich event 2 Canadian ice-rafted debris (IRD) and includes IRD from European sources. We suggest that the second represents an episode of deposition from turbid plumes, which precedes IRD deposition associated with Heinrich event 1. At the end of marine isotopic stage 2 (MIS 2) and the beginning of MIS 1 the highest fluxes are recorded on the Whittard Ridge where they correspond to deposition from turbidity current overflows. Canadian icebergs have rafted debris at the Celtic margin during Heinrich events 1, 2, 4 and 5. The high-resolution records of Heinrich events 1 and 2 show that in both cases the arrival of the Canadian icebergs was preceded by a European ice rafting precursor event, which took place about 1–1.5 kyr before. Two rafting episodes of European IRD also occurred immediately after Heinrich event 2 and just before Heinrich event 1. The terrigenous fluxes recorded in core MD95-2002 during the LGM are the highest reported at hemipelagic sites from the northwestern European margin. The magnitude of the Canadian IRD fluxes at Meriadzek Terrace is similar to those from oceanic sites.
    Keywords: CALYPSO; Calypso Corer; Celtic Shelf; CH-NKS12; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952002; MD95-2002; Meriadzec; NO-MKS03; PC; Piston corer
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Michels, Klaus; Kuhn, Gerhard; Hillenbrand, Claus-Dieter; Diekmann, Bernhard; Fütterer, Dieter K; Grobe, Hannes; Uenzelmann-Neben, Gabriele (2002): The southern Weddell Sea: combined contourite-turbidite sedimentation at the southeastern margin of the Weddell Gyre. In: Stow, D A V; Pudsey, C; Howe, J C; Faugères, J-C & Viana, A R (eds.), Deep-water contourite systems: modern drifts and ancient series, seismic and sedimentary characteristics. Geological Society of London, Memoirs, London, 22, 305-323, hdl:10013/epic.14690.d001
    Publication Date: 2024-06-25
    Description: Sedimentary processes in the southeastern Weddell Sea are influenced by glacial-interglacial ice-shelf dynamics and the cyclonic circulation of the Weddell Gyre, which affects all water masses down to the sea floor. Significantly increased sedimentation rates occur during glacial stages, when ice sheets advance to the shelf edge and trigger gravitational sediment transport to the deep sea. Downslope transport on the Crary Fan and off Dronning Maud and Coats Land is channelized into three huge channel systems, which originate on the eastern-, the central and the western Crary Fan. They gradually turn from a northerly direction eastward until they follow a course parallel to the continental slope. All channels show strongly asymmetric cross sections with well-developed levees on their northwestern sides, forming wedge-shaped sediment bodies. They level off very gently. Levees on the southeastern sides are small, if present at all. This characteristic morphology likely results from the process of combined turbidite-contourite deposition. Strong thermohaline currents of the Weddell Gyre entrain particles from turbidity-current suspensions, which flow down the channels, and carry them westward out of the channel where they settle on a surface gently dipping away from the channel. These sediments are intercalated with overbank deposits of high-energy and high-volume turbidity currents, which preferentially flood the left of the channels (looking downchannel) as a result of Coriolis force. In the distal setting of the easternmost channel-levee complex, where thermohaline currents are directed northeastward as a result of a recirculation of water masses from the Enderby Basin, the setting and the internal structures of a wedge-shaped sediment body indicate a contourite drift rather than a channel levee. Dating of the sediments reveals that the levees in their present form started to develop with a late Miocene cooling event, which caused an expansion of the East Antarctic Ice Sheet and an invigoration of thermohaline current activity.
    Keywords: ANT-IV/3; ANT-VI/3; ANT-VIII/5; AWI_Paleo; Camp Norway; gcmd1; Giant box corer; GKG; Gravity corer (Kiel type); Halley Bay; KL; Lyddan Island; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; PS08; PS08/333; PS12; PS12/319; PS12/340; PS12/458; PS1367-2; PS1599-1; PS1599-3; PS16; PS16/409; PS16/410; PS16/419; PS1607-3; PS1635-1; PS1789-1; PS1790-1; PS1794-2; SL; Weddell Sea
    Type: Dataset
    Format: application/zip, 13 datasets
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2024-06-25
    Description: Presented is a spatial distribution of Temperature, Salinity, Oxygen, Nitrate, Ammonia Nitrogen, Organic Nitrogen, Phosphate, Organic Phosphate, and Silicate data from the Sea of Okhotsk during the 1990 - 1997 period for the months of June - August.
    Keywords: Ak_MA_Lavrentyev_1994; Akademik A Nesmeyanov; Akademik M.A. Lavrentyev; AN_1992; AN_1993; GOFLO; Go-Flo bottles; Lavrentyev-94_10; Lavrentyev-94_100; Lavrentyev-94_102; Lavrentyev-94_103; Lavrentyev-94_105; Lavrentyev-94_107; Lavrentyev-94_108; Lavrentyev-94_109; Lavrentyev-94_11; Lavrentyev-94_110; Lavrentyev-94_111; Lavrentyev-94_113; Lavrentyev-94_114; Lavrentyev-94_115; Lavrentyev-94_119; Lavrentyev-94_12; Lavrentyev-94_120; Lavrentyev-94_121; Lavrentyev-94_122; Lavrentyev-94_123; Lavrentyev-94_124; Lavrentyev-94_125; Lavrentyev-94_126; Lavrentyev-94_127; Lavrentyev-94_128; Lavrentyev-94_129; Lavrentyev-94_13; Lavrentyev-94_130; Lavrentyev-94_131; Lavrentyev-94_132; Lavrentyev-94_133; Lavrentyev-94_134; Lavrentyev-94_135; Lavrentyev-94_136; Lavrentyev-94_137; Lavrentyev-94_138; Lavrentyev-94_14; Lavrentyev-94_140; Lavrentyev-94_141; Lavrentyev-94_142; Lavrentyev-94_143; Lavrentyev-94_144; Lavrentyev-94_145; Lavrentyev-94_146; Lavrentyev-94_147; Lavrentyev-94_148; Lavrentyev-94_149; Lavrentyev-94_15; Lavrentyev-94_150; Lavrentyev-94_16; Lavrentyev-94_17; Lavrentyev-94_18; Lavrentyev-94_19; Lavrentyev-94_2; Lavrentyev-94_20; Lavrentyev-94_21; Lavrentyev-94_22; Lavrentyev-94_23; Lavrentyev-94_24; Lavrentyev-94_25; Lavrentyev-94_26; Lavrentyev-94_27; Lavrentyev-94_28; Lavrentyev-94_29; Lavrentyev-94_3; Lavrentyev-94_30; Lavrentyev-94_32; Lavrentyev-94_33; Lavrentyev-94_34; Lavrentyev-94_35; Lavrentyev-94_37; Lavrentyev-94_38; Lavrentyev-94_39; Lavrentyev-94_4; Lavrentyev-94_41; Lavrentyev-94_42; Lavrentyev-94_43; Lavrentyev-94_44; Lavrentyev-94_45; Lavrentyev-94_46; Lavrentyev-94_47; Lavrentyev-94_48; Lavrentyev-94_49; Lavrentyev-94_5; Lavrentyev-94_50; Lavrentyev-94_51; Lavrentyev-94_52; Lavrentyev-94_53; Lavrentyev-94_54; Lavrentyev-94_55; Lavrentyev-94_56; Lavrentyev-94_57; Lavrentyev-94_58; Lavrentyev-94_59; Lavrentyev-94_6; Lavrentyev-94_60; Lavrentyev-94_61; Lavrentyev-94_63; Lavrentyev-94_65; Lavrentyev-94_66; Lavrentyev-94_67; Lavrentyev-94_68; Lavrentyev-94_69; Lavrentyev-94_7; Lavrentyev-94_70; Lavrentyev-94_71; Lavrentyev-94_72; Lavrentyev-94_73; Lavrentyev-94_76; Lavrentyev-94_77; Lavrentyev-94_79; Lavrentyev-94_8; Lavrentyev-94_80; Lavrentyev-94_81; Lavrentyev-94_82; Lavrentyev-94_83; Lavrentyev-94_84; Lavrentyev-94_85; Lavrentyev-94_87; Lavrentyev-94_89; Lavrentyev-94_9; Lavrentyev-94_90; Lavrentyev-94_91; Lavrentyev-94_92; Lavrentyev-94_94; Lavrentyev-94_96; Lavrentyev-94_97; Lavrentyev-94_99; Levanidov-97_1; Levanidov-97_100; Levanidov-97_101; Levanidov-97_102; Levanidov-97_103; Levanidov-97_104; Levanidov-97_105; Levanidov-97_107; Levanidov-97_108; Levanidov-97_109; Levanidov-97_11; Levanidov-97_110; Levanidov-97_111; Levanidov-97_112; Levanidov-97_113; Levanidov-97_114; Levanidov-97_115; Levanidov-97_116; Levanidov-97_119; Levanidov-97_12; Levanidov-97_120; Levanidov-97_121; Levanidov-97_122; Levanidov-97_123; Levanidov-97_124; Levanidov-97_125; Levanidov-97_128; Levanidov-97_129; Levanidov-97_130; Levanidov-97_131; Levanidov-97_132; Levanidov-97_133; Levanidov-97_134; Levanidov-97_135; Levanidov-97_136; Levanidov-97_137; Levanidov-97_139; Levanidov-97_14; Levanidov-97_140; Levanidov-97_141; Levanidov-97_142; Levanidov-97_143; Levanidov-97_144; Levanidov-97_145; Levanidov-97_146; Levanidov-97_147; Levanidov-97_149; Levanidov-97_15; Levanidov-97_150; Levanidov-97_151; Levanidov-97_152; Levanidov-97_154; Levanidov-97_155; Levanidov-97_156; Levanidov-97_157; Levanidov-97_158; Levanidov-97_16; Levanidov-97_160; Levanidov-97_18; Levanidov-97_19; Levanidov-97_2; Levanidov-97_20; Levanidov-97_21; Levanidov-97_22; Levanidov-97_23; Levanidov-97_25; Levanidov-97_26; Levanidov-97_27; Levanidov-97_28; Levanidov-97_29; Levanidov-97_3; Levanidov-97_30; Levanidov-97_31; Levanidov-97_32; Levanidov-97_33; Levanidov-97_34; Levanidov-97_35; Levanidov-97_36; Levanidov-97_37; Levanidov-97_38; Levanidov-97_39; Levanidov-97_4; Levanidov-97_40; Levanidov-97_41; Levanidov-97_42; Levanidov-97_43; Levanidov-97_45; Levanidov-97_46; Levanidov-97_47; Levanidov-97_48; Levanidov-97_49; Levanidov-97_51; Levanidov-97_53; Levanidov-97_54; Levanidov-97_55; Levanidov-97_56; Levanidov-97_57; Levanidov-97_58; Levanidov-97_59; Levanidov-97_6; Levanidov-97_60; Levanidov-97_61; Levanidov-97_62; Levanidov-97_64; Levanidov-97_65; Levanidov-97_66; Levanidov-97_67; Levanidov-97_68; Levanidov-97_69; Levanidov-97_7; Levanidov-97_70; Levanidov-97_71; Levanidov-97_72; Levanidov-97_73; Levanidov-97_74; Levanidov-97_75; Levanidov-97_76; Levanidov-97_77; Levanidov-97_78; Levanidov-97_79; Levanidov-97_8; Levanidov-97_80; Levanidov-97_81; Levanidov-97_82; Levanidov-97_83; Levanidov-97_84; Levanidov-97_85; Levanidov-97_86; Levanidov-97_87; Levanidov-97_88; Levanidov-97_89; Levanidov-97_9; Levanidov-97_90; Levanidov-97_91; Levanidov-97_92; Levanidov-97_93; Levanidov-97_94; Levanidov-97_95; Levanidov-97_96; Levanidov-97_97; Levanidov-97_98; Mlechniy_Put_1990; Mlechny Put; MP90_320; MP90_321; MP90_322; Nesmeyanov-92_2178; Nesmeyanov-92_2179; Nesmeyanov-92_2180; Nesmeyanov-92_2181; Nesmeyanov-92_2182; Nesmeyanov-92_2183; Nesmeyanov-92_2184; Nesmeyanov-92_2185; Nesmeyanov-92_2186; Nesmeyanov-92_2187; Nesmeyanov-92_2188; Nesmeyanov-92_2193; Nesmeyanov-92_2194; Nesmeyanov-92_2195; Nesmeyanov-92_2200; Nesmeyanov-92_2201; Nesmeyanov-92_2202; Nesmeyanov-92_2203; Nesmeyanov-92_2204; Nesmeyanov-92_2207; Nesmeyanov-92_2208; Nesmeyanov-92_2209; Nesmeyanov-92_2210; Nesmeyanov-92_2211; Nesmeyanov-92_2212; Nesmeyanov-92_2217; Nesmeyanov-92_2218; Nesmeyanov-92_2219; Nesmeyanov-92_2220; Nesmeyanov-92_2221; Nesmeyanov-92_2222; Nesmeyanov-92_2223; Nesmeyanov-92_2224; Nesmeyanov-92_2225; Nesmeyanov-92_2226; Nesmeyanov-92_2227; Nesmeyanov-92_2230; Nesmeyanov-92_2231; Nesmeyanov-92_2232; Nesmeyanov-92_2233; Nesmeyanov-92_2234; Nesmeyanov-92_2235; Nesmeyanov-92_2240; Nesmeyanov-92_2241; Nesmeyanov-92_2242; Nesmeyanov-92_2243; Nesmeyanov-92_2244; Nesmeyanov-92_2245; Nesmeyanov-92_2246; Nesmeyanov-92_2250; Nesmeyanov-92_2251; Nesmeyanov-92_2252; Nesmeyanov-92_2265; Nesmeyanov-92_2266; Nesmeyanov-93_2273; Nesmeyanov-93_2274; Nesmeyanov-93_2275; Nesmeyanov-93_2276; Nesmeyanov-93_2277; Nesmeyanov-93_2278; Nesmeyanov-93_2279; Nesmeyanov-93_2281; Nesmeyanov-93_2282; Nesmeyanov-93_2283; Nesmeyanov-93_2284; Nesmeyanov-93_2285; Nesmeyanov-93_2286; Nesmeyanov-93_2287; Nesmeyanov-93_2288; Nesmeyanov-93_2289; Nesmeyanov-93_2291; Nesmeyanov-93_2292; Nesmeyanov-93_2293; Nesmeyanov-93_2294; Nesmeyanov-93_2295; Nesmeyanov-93_2297; Nesmeyanov-93_2298; Nesmeyanov-93_2299; Nesmeyanov-93_2300; Nesmeyanov-93_2304; Nesmeyanov-93_2305; Nesmeyanov-93_2306; Nesmeyanov-93_2308; Nesmeyanov-93_2309; Nesmeyanov-93_2310; Nesmeyanov-93_2311; Nesmeyanov-93_2313; Nesmeyanov-93_2314; Nesmeyanov-93_2315; Nesmeyanov-93_2316; Nesmeyanov-93_2317; Nesmeyanov-93_2318; Nesmeyanov-93_2319; Nesmeyanov-93_2320; Nesmeyanov-93_2321; Nesmeyanov-93_2357; Nesmeyanov-93_2359; Nesmeyanov-93_2360; Nesmeyanov-93_2362; Nesmeyanov-93_2363; Nesmeyanov-93_2364; Nesmeyanov-93_2365; Nesmeyanov-93_2366; Nesmeyanov-93_2369; Nesmeyanov-93_2370; Nesmeyanov-93_2371; Nesmeyanov-93_2372; Nesmeyanov-93_2373; Nesmeyanov-93_2374; Nesmeyanov-93_2375; Nesmeyanov-93_2377; Nesmeyanov-93_2378; Nesmeyanov-93_2379; Nesmeyanov-93_2380; Nesmeyanov-93_2381; Nesmeyanov-93_2382; Nesmeyanov-93_2384; Nesmeyanov-93_2385; Nesmeyanov-93_2386; Nesmeyanov-93_2387; Nesmeyanov-93_2388; Nesmeyanov-93_2389; Nesmeyanov-93_2390; Nesmeyanov-93_2391; Nesmeyanov-93_2392; Nesmeyanov-93_2396; Nesmeyanov-93_2397; Nesmeyanov-93_2398; Nesmeyanov-93_2399; Nesmeyanov-93_2400; Nesmeyanov-93_2402; Nesmeyanov-93_2403; Nesmeyanov-93_2404; Nesmeyanov-93_2405; Nesmeyanov-93_2406; Nesmeyanov-93_2410; Nesmeyanov-93_2412; Nesmeyanov-93_2413; Nesmeyanov-93_2418; Nesmeyanov-93_2419; Nesmeyanov-93_2420; Nesmeyanov-93_2421; Nesmeyanov-93_2422; Nesmeyanov-93_2423; Nesmeyanov-93_2426; Nesmeyanov-93_2427; Nesmeyanov-93_2428; Nesmeyanov-93_2429; Nesmeyanov-93_2430; Nesmeyanov-93_2431; Okhotsk Sea; Prof_Levanidov_1997; Professor
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Esper, Oliver; Zonneveld, Karin A F; Höll, Christine; Karwath, Britta; Schneider, Ralph R; Vink, Annemiek; Weise-Ihlo, Ilka; Willems, Helmut (2000): Reconstruction of palaeoceanographic conditions in the South Atlantic Ocean at the last two Terminations based on calcareous dinoflagllate cysts. International Journal of Earth Sciences, 88(4), 680-693, https://doi.org/10.1007/s005310050297
    Publication Date: 2024-06-25
    Description: Despite the increasing interest in the South Atlantic Ocean as a key area of the heat exchange between the southern and the northern hemisphere, information about its palaeoceanographic conditions during transitions from glacial to interglacial stages, the so-called Terminations, are not well understood. Herein we attempt to increase this information by studying the calcareous dinoflagellate cysts and the shells of Thoracosphaera heimii (calcareous cysts) of five Late Quaternary South Atlantic Ocean cores. Extremely high accumulation rates of calcareous cysts at the Terminations might be due to a combined effect of increased cyst production and better preservation as result of calm, oligotrophic conditions in the upper water layers. Low relative abundance of Sphaerodinella albatrosiana compared with Sphaerodinella tuberosa in the Cape Basin may be the result of the relatively colder environmental conditions in this region compared with the equatorial Atlantic Ocean with high relative abundance of S. albatrosiana. Furthermore, the predominance of S. tuberosa during glacials and interglacials at the observed site of the western Atlantic Ocean reflects decreased salinity in the upper water layer.
    Keywords: Brazil Basin; Cape Basin; Equatorial Atlantic; GeoB; GeoB1105-4; GeoB1117-2; GeoB1214-1; GeoB2204-2; GeoB3603-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M12/1; M23/3; M34/1; M9/4; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Southern Cape Basin
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Weber, Michael E; Wiedicke-Hombach, Michael; Kudrass, Hermann-Rudolph; Erlenkeuser, Helmut (2003): Bengal Fan sediment transport activity and response to climate forcing inferred from sediment physical properties. Sedimentary Geology, 155(3-4), 361-381, https://doi.org/10.1016/S0037-0738(02)00187-2
    Publication Date: 2024-06-25
    Description: We obtained sediment physical properties and geochemical data from 47 piston and gravity cores located in the Bay of Bengal, to study the complex history of the Late Pleistocene run-off from the Ganges and Brahmaputra rivers and its imprint on the Bengal Fan. Grain-size parameters were predicted from core logs of density and velocity to infer sediment transport energy and to distinguish different environments along the 3000-km-long transport path from the delta platform to the lower fan. On the shelf, 27 cores indicate rapidly prograding delta foresets today that contain primarily mud, whereas outer shelf sediment has 25% higher silt contents, indicative of stronger and more stable transport regime, which prevent deposition and expose a Late Pleistocene relic surface. Deposition is currently directed towards the shelf canyon 'Swatch of No Ground', where turbidites are released to the only channel–levee system that is active on the fan during the Holocene. Active growth of the channel–levee system occurred throughout sea-level rise and highstand with a distinct growth phase at the end of the Younger Dryas. Coarse-grained material bypasses the upper fan and upper parts of the middle fan, where particle flow is enhanced as a result of flow-restriction in well-defined channels. Sandier material is deposited mainly as sheet-flow deposits on turbidite-dominated plains at the lower fan. The currently most active part of the fan with 10-40 cm thick turbidites is documented for the central channel including inner levees (e.g., site 40). Site 47 from the lower fan far to the east of the active channel–levee system indicates the end of turbidite sedimentation at 300 ka for that location. That time corresponds to the sea-level lowering during late isotopic stage 9 when sediment supply to the fan increased and led to channel avulsion farther upstream, probably indicating a close relation of climate variability and fan activity. Pelagic deep-sea sites 22 and 28 contain a 630-kyear record of climate response to orbital forcing with dominant 21- and 41-kyear cycles for carbonate and magnetic susceptibility, respectively, pointing to teleconnections of low-latitude monsoonal forcing on the precession band to high-latitude obliquity forcing. Upper slope sites 115, 124, and 126 contain a record of the response to high-frequency climate change in the Dansgaard–Oeschger bands during the last glacial cycle with shared frequencies between 0.75 and 2.5 kyear. Correlation of highs in Bengal Fan physical properties to lows in the d18O record of the GISP2 ice-core suggests that times of greater sediment transport energy in the Bay of Bengal are associated with cooler air temperatures over Greenland. Teleconnections were probably established through moisture and other greenhouse-gas forcing that could have been initiated by instabilities in the methane hydrate reservoir in the oceans.
    Keywords: Bay of Bengal; Bengal Fan; BENGAL FAN; Gravity corer (Kiel type); Gulf of Mannar; Indian Ocean; KL; Piston corer (BGR type); SL; SO93/1; SO93/1_01KL; SO93/1_09KL; SO93/1_19KL; SO93/1_24KL; SO93/1_27KL; SO93/1_28KL; SO93/1_29KL; SO93/1_32KL; SO93/1_34KL; SO93/2; SO93/2_36KL; SO93/2_39KL; SO93/2_42KL; SO93/2_45KL; SO93/2_46KL; SO93/2_47KL; SO93/2_49KL; SO93/2_51KL; SO93/2_54KL; SO93/2_56KL; SO93/3; SO93/3_107KL; SO93/3_114SL; SO93/3_126KL; SO93/3_66SL; SO93/3_68SL; SO93/3_69SL; SO93/3_70SL; SO93/3_71SL; SO93/3_77SL; SO93/3_78SL; SO93/3_79SL; SO93/3_80SL; SO93/3_82SL; SO93/3_83KL; SO93/3_84KL; SO93/3_85KL; SO93/3_86KL; SO93/3_87KL; SO93/3_96KL; SO93-63KL; Sonne
    Type: Dataset
    Format: application/zip, 39 datasets
    Location Call Number Expected Availability
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Pérez-Folgado, Marta; Sierro, Francisco Javier; Flores, José-Abel; Cacho, Isabel; Grimalt, Joan O; Zahn, Rainer; Shackleton, Nicholas J (2003): Western Mediterranean planktonic foraminifera events and millennial climatic variability during the last 70 kyr. Marine Micropaleontology, 48(1-2), 49-70, https://doi.org/10.1016/S0377-8398(02)00160-3
    Publication Date: 2024-06-25
    Description: Detailed study of associations of planktonic foraminifera in cores MD95-2043 and ODP 977, located in the Alboran Sea (Mediterranean Sea), has allowed the identification of 29 new faunal events,defined by abrupt changes in the abundances of Neogloboquadrina pachyderma (right and left coiling), Turborotalita quinqueloba, Globorotalia scitula, Globorotalia inflata, Globigerina bulloides and Globigerinoides ruber (white and pink varieties). The age model for ODP 977 was based on that of MD95-2043 [Cacho et al. (1999),Paleoceanogr. 14, 698-705], on the isotopic stratigraphy,and on two AMS 14C measurements. Sea Surface Temperatures (SSTs) were estimated for the last 54 kyr using the Modern Analog Technique (MAT) and were compared with the SSTs provided by the U37(k0) method. The U37(k0) record is very similar to the MAT annual mean temperature record for the last 8 kyr. However, for older times alkenone-derived temperatures are consistently higher than the annual MAT temperatures. This offset may be due to an underestimation of the SST provided by the planktonic foraminiferal method for glacial times, to an overestimation of the U37(k0) record, or to changes in the seasonal production of alkenones. Most of the variability in the fauna is related to the millennial variability of Heinrich and Dansgaard-Oeschger (D-O) events. During Heinrich events (HEs) and most of the other D-O stadials, G. bulloides, T. quinqueloba and G. scitula increased, while N. pachyderma (right coiling), G. inflata and G. ruber decreased. By contrast, N. pachyderma (left coiling) was only abundant in the HEs. The main component of the associations -N. pachyderma (right coiling) - follows a general trend similar to that of sea-level and delta18O. This species reached its highest abundance during the Last Glacial Maximum, when sea-level was at a lower position. The occurrence of a shallower nutricline owing to a shallowing of the interface between Atlantic inflowing and Mediterranean outflowing waters could have favoured the development of neogloboquadrinids in the vicinity of the Strait of Gibraltar.
    Keywords: 161-977A; Alboran Sea; CALYPSO; Calypso Corer; DRILL; Drilling/drill rig; IMAGES; IMAGES I; International Marine Global Change Study; Joides Resolution; Leg161; Marion Dufresne (1995); MD101; MD952043; MD95-2043; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 7
    Publication Date: 2024-06-25
    Description: During METEOR Cruise M 34/1 all recovered gravity cores were subject to laboratory geophysical studies. A routine shipboard measurement of three physical parameters was carried out on the segmented sediment cores, comprising the determination of - the compressional (P-) wave velocity vp, - the electric resistivity Rs, and - the magnetic volume susceptibility K. These properties are closely related to the grain size, porosity and Iithology of the sediments and provide high-resolution core logs (spacing 3, 3 and 1 cm, respectively) available prior to all other detailed investigations. In addition, oriented sampies for later shore based paleo- and rockmagnetic studies were taken at intervals of 10 cm.
    Keywords: GeoB; GeoB3602-1; GeoB3603-2; GeoB3604-3; GeoB3605-2; GeoB3606-1; GeoB3607-2; GeoB3608-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M34/1; Meteor (1986); Northern Cape Basin; SL; Southern Cape Basin
    Type: Dataset
    Format: application/zip, 23 datasets
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  • 8
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    PANGAEA
    In:  Supplement to: Koç, Nalân; Labeyrie, Laurent D; Manthé, Sandrine; Flower, Benjamin P; Hodell, David A; Aksu, Ali E (2001): The last occurrence of Proboscia curvirostris in the North Atlantic marine isotope stages 9-8. Marine Micropaleontology, 41(1-2), 9-23, https://doi.org/10.1016/S0377-8398(00)00054-2
    Publication Date: 2024-06-25
    Description: Well-preserved diatoms are present in high sedimentation rate Pleistocene cores retrieved on Ocean Drilling Program (ODP) Legs 151, 152, 162 and IMAGES cruises of R/V Marion Dufresne from the North Atlantic. Investigation of the stratigraphic occurrence of diatom species shows that the youngest diatom event observed in the area is the last occurrence (LO) of Proboscia curvirostris (Jousé) Jordan and Priddle. P. curvirostris is a robust species that can easily be identified in the sediments, and therefore can be a practical biostratigraphic tool. We have mapped its areal distribution, and found that it stretches from 40°N to 80°N in the North Atlantic. Further, we have correlated the LO P. curvirostris to the oxygen isotope records of six cores to refine the age of this biostratigraphic event. The extinction of P. curvirostris is latitudinally diachronous through Marine Isotope Stages (MIS) 9 to 8 within the North Atlantic. This is closely related to the paleoceanography of the area. P. curvirostris first disappeared within interglacial MIS 9 (324 ka) from the northern areas that are most sensitive to climatic forcing, like the East Greenland current and the sea-ice margin. It survived in mid-North Atlantic until the conditions of the MIS 8 (glaciation) became too severe (260 ka). In the North Pacific at ODP Site 883 the LO P. curvirostris falls within MIS 8. The observed overlap in age between the North Atlantic and the North Pacific strongly suggests that the extinction of P. curvirostris is synchronous between these oceans.
    Keywords: 152-919A; 162-983A; CALYPSO; Calypso Corer; DRILL; Drilling/drill rig; Greenland Sea; Iceland; IMAGES I; Joides Resolution; Leg152; Leg162; Marion Dufresne (1995); MD101; MD952014; MD95-2014; MD952027; MD95-2027; Newfoundland Slope; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Arz, Helge Wolfgang; Gerhardt, Sabine; Pätzold, Jürgen; Röhl, Ursula (2001): Millennial-scale changes of surface- and deep-water flow in the western tropical Atlantic linked to Northern Hemisphere high-latitude climate during the Holocene. Geology, 29(3), 239-242, https://doi.org/10.1130/0091-7613(2001)029%3C0239:MSCOSA%3E2.0.CO;2
    Publication Date: 2024-06-25
    Description: There is increasing evidence that the preceding Holocene climate was as unstable as the last glacial period, although variations occurred at much lower amplitudes. However, low-latitude climate records that confirm this variability are sparse. Here we present a radiocarbon-dated Holocene marine record from the tropical western Atlantic. Aragonite dissolution derived from the degree of preservation of the pteropod Limacina inflata records changes in the corrosiveness of the bottom water at the core site due to the changing influence of northern versus southern water masses. The delta18O difference between the shallow-living planktonic foraminifera Globigerinoides sacculifer and the deep-living Globorotalia tumida is used as proxy for changes in the vertical stratification of the surface water, hence the trade wind strength at this latitude. We compared our data to high-latitude records of the North Atlantic region. A good agreement is found between the aragonite dissolution and the strength in the Island-Scotland Overflow Water, which contributes significantly to the North Atlantic Deep Water. This suggests that large-scale variations in the Atlantic thermohaline circulation occurred throughout the Holocene. Concurrently, the comparison of our Delta delta18O with the GISP2 glaciochemical records points to global Holocene atmospheric reorganizations seen in both the tropics and high northern latitudes.
    Keywords: GeoB; GeoB3910-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M34/4; Meteor (1986); Northeast Brasilian Margin; SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Brathauer, Uta; Abelmann, Andrea; Gersonde, Rainer; Niebler, Hans-Stefan; Fütterer, Dieter K (2001): Calibration of Cycladophora davisiana events versus oxygen isotope stratigraphy in the subantarctic Atlantic Ocean - a stratigraphic tool for carbonate-poor Quaternary sediments. Marine Geology, 175(1-4), 167-181, https://doi.org/10.1016/S0025-3227(01)00141-4
    Publication Date: 2024-06-25
    Description: We calibrated the Cycladophora davisiana abundances versus oxygen isotope stratigraphy back to 220 ka for the subantarctic Atlantic Ocean. The relative abundances of C. davisiana and delta18O measurements of benthic and planktic foraminifera have been determined in two sediment cores. Oxygen isotope stratigraphy has been used to date the C. davisiana records and to assign SPECMAP ages to the C. davisiana events. Comparisons with an existing calibration from the subantarctic Indian Ocean show, that the C. davisiana events 'b2, c1, c2, d, e1, e2, e3, f, h, i1 and i2' occur synchronous within the errors of the oxygen isotope stratigraphy in the Indian and the Atlantic sectors of the Southern Ocean. Larger deviations occur only for events 'b1' and 'g'. Furthermore, the long-term fluctuations in C. davisiana abundances have been studied in a sediment core covering the last 700 kyr. Based on biostratigraphic extinction levels, ages for early Brunhes C. davisiana events have been estimated. Major C. davisiana abundance maxima occur approximately every 100 ka in conjunction with glacial/interglacial cycles over the entire record.
    Keywords: Agulhas Basin; ANT-IX/4; ANT-VIII/3; ANT-XI/2; AWI_Paleo; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS16; PS16/271; PS1752-1; PS18; PS18/238; PS2082-1; PS2498-1; PS28; PS28/304; SL; South Atlantic
    Type: Dataset
    Format: application/zip, 5 datasets
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