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  • PANGAEA  (423,297)
  • Amsterdam : Elsevier
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  • 1
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    Unknown
    Geochemistry on sediments off NE Greenland (2015)
    PANGAEA
    In:  Supplement to: Notholt, Hanne (1998): Die Auswirkungen der NorthEastWater-Polynya auf die Sedimentation vor NO-Grönland und Untersuchungen zur Paläo-Ozeanographie seit dem Mittelweichsel (The Implication of the NorthEastWater-Polynya on the Sedimentation by NE-Greenland and Late Quaternary Paleo-oceanic Investigations). Berichte zur Polarforschung = Reports on Polar Research, 275, 183 pp, https://doi.org/10.2312/BzP_0275_1998
    Details
    Publication Date: 2024-06-28
    Description: Sedimentation and the early diagenetic processes have been studied in surface sediments from the NE-Greenland shelf and continental slope. I have used these data together with geochemical and sedimentological investigations from seven long sediment cores from the NE- and E-Greenland continental margin between 80' and 72' N for reconstructing the paleoenvironmental history of the East- Greenland-Current (ff).
    Keywords: Amdrup Land; Amdrups Land, Sophus Müllers Næs; ARK-IX/3; ARK-V/3b; AWI_Paleo; AWI_PerDyn; AWI Arctic Land Expedition; Germania Land; GIK21733-2 PS13/240; GIK21734-2 PS13/247; GIK21735-1 PS13/249; GL-Land_1993; Gravity corer (Kiel type); Greenland1993; HAND; Hertugen af Orleans Land; Holm Land; Holms Land, Eskimonæs; Holms Land, Mallemukfjeldet; Hovgaard Oe; Khatanga River; King Oskar Fjord; Kongsfjorden, Spitsbergen, Arctic; Kronprins Chr. Land, Dijmphna Sund; Lamberts Land; MUC; MultiCorer; Nakkehoved; Northeast Greenland; Notholt_A; Notholt_B; Notholt_C; Notholt_D; Notholt_E; Notholt_F; Notholt_H; Notholt_I; Notholt_J; Notholt_K; Notholt_L; Notholt_M; Notholt_N; Notholt_O; Notholt_P; Notholt_Q; Notholt_R; Notholt_S; Notholt_T; Notholt_U; Notholt_V; Notholt_W; Notholt_X; Ny-Ålesund, Spitsbergen; Ossiar Sarsfjellet; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Permafrost Research (Periglacial Dynamics) @ AWI; Polarstern; PS13 GRÖKORT; PS1733-2; PS1734-2; PS1735-1; PS2413-3; PS2415-4; PS2419-3; PS2419-4; PS2420-3; PS2422-2; PS2422-3; PS2423-3; PS2423-4; PS2424-1; PS2424-2; PS2425-3; PS2426-4; PS2427-3; PS2428-2; PS2429-4; PS2430-2; PS2432-3; PS2433-3; PS2434-3; PS2435-3; PS2437-3; PS2438-2; PS26/115; PS26/119; PS26/138; PS26/145; PS26/147; PS26/148; PS26/149; PS26/155; PS26/165; PS26/179; PS26/213; PS26/214; PS26/215; PS26/217; PS26/231; PS26/232; PS26/234; PS26/258; PS26/278; PS26 NEW; Quaternary Environment of the Eurasian North; QUEEN; Sampling by hand; SL
    Type: Dataset
    Format: application/zip, 33 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 2
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    Unknown
    Fatty acid composition, and bacteria and meiofauna abundance in sediment cores PS71/013 and PS71/085 during POLARSTERN cruise ANT-XXIV/2 (2011)
    PANGAEA
    In:  Supplement to: Veit-Köhler, Gritta; Guilini, Katja; Peeken, Ilka; Sachs, Oliver; Sauter, Eberhard-Jürgen; Würzberg, Laura (2011): Antarctic deep-sea meiofauna and bacteria react to the deposition of particulate organic matter after a phytoplankton bloom. Deep Sea Research Part II: Topical Studies in Oceanography, 58(19-20), 1983-1995, https://doi.org/10.1016/j.dsr2.2011.05.008
    Details
    Publication Date: 2024-06-28
    Description: During the RV Polarstern ANT XXIV-2 cruise to the Southern Ocean and the Weddell Sea in 2007/2008, sediment samples were taken during and after a phytoplankton bloom at 52°S 0°E. The station, located at 2960 m water depth, was sampled for the first time at the beginning of December 2007 and revisited at the end of January 2008. Fresh phytodetritus originating from the phytoplankton bloom first observed in the water column had reached the sea floor by the time of the second visit. Absolute abundances of bacteria and most major meiofauna taxa did not change between the two sampling dates. In the copepods, the second most abundant meiofauna taxon after the nematodes, the enhanced input of organic material did not lead to an observable increase of reproductive effort. However, significantly higher relative abundances of meiofauna could be observed at the sediment surface after the remains of the phytoplankton bloom reached the sea floor. Vertical shifts in meiofauna distribution between December and January may be related to changing pore-water oxygen concentration, total sediment fatty acid content, and pigment profiles measured during our study. Higher oxygen consumption after the phytoplankton bloom may have resulted from an enhanced respiratory activity of the living benthic component, as neither meiofauna nor bacteria reacted with an increase in individual numbers to the food input from the water column. Based on our results, we infer that low temperatures and ecological strategies are the underlying factors for the delayed response of benthic deep-sea copepods, in terms of egg and larval production, to the modified environmental situation.
    Keywords: ANDEEP-SYSTCO; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
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    Sedimentological analysis of sediments from Amundsen and Bellingshausen Seas, Southern Ocean (2000)
    PANGAEA
    In:  Supplement to: Hillenbrand, Claus-Dieter (2000): Glazialmarine Sedimentationsentwicklung am westantarktischen Kontinentalrand im Amundsen- und Bellingshausenmeer - Hinweise auf Paläoumweltveränderungen während der quartären Klimazyklen (Glaciomarine sedimentation on the continental margins of the Amundsen and Bellingshausen Seas, West Antarctica - indications for paleoenvironmental changes during the Quaternary climatic cycles). Berichte zur Polarforschung = Reports on Polar Research, 346, 182 pp, https://doi.org/10.2312/BzP_0346_2000
    Details
    Publication Date: 2024-06-28
    Description: Glaciomarine deposits at the Antarctic continental margin represent an important paleoglaciological and paleoceanographical record of environmental changes in both Antarctica and the adjacent Southern Ocean. In order to reconstruct the climatic-controlled sedimentation history in the Amundsen and Bellingshausen Seas during Quaternary glacial cycles, sedimentological, geochemical and clay mineralogical investigations were carried out on 34 surface sediment samples and On 7 sediment cores. The study of the surface sediment samples allows one to decipher the recent sediment supply and transportation processes. The input of glacial debris is highest in the eastern Bellingshausen Sea because of the subpolar climatic conditions prevailing over the adjacent Antarctic Peninsula. Fine sediment pathways of transport in the Amundsen and Bellingshausen Seas were recon- structed by analysing the clay mineralogical composition of the surface sediments and connecting it with specific source rocks in the West Antarctic hinterland. Grain size data show a complex dispersal Pattern of ice-rafted debris (IRD). According to these data, redeposition by currents plays a major role near the shelf break both in marginal seas and on the continental rise in the eastern Bellingshausen Sea. ff
    Keywords: Amundsen Sea; Antarctic Peninsula; ANT-VI/2; ANT-XI/3; AWI_Paleo; Bellingshausen Sea; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS12; PS12/201; PS1565-2; PS2547-1; PS2547-3; PS2548-1; PS2549-1; PS2550-1; PS2551-1; PS2552-1; PS2553-3; PS29; PS29/063; PS29/064; PS29/065; PS29/066; PS29/067; PS29/068; PS29/070; SL
    Type: Dataset
    Format: application/zip, 14 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 4
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    Unknown
    Data compilation of VEINS (2005)
    PANGAEA
    In:  International Council for the Exploration of the Sea, Copenhagen
    Details
    Publication Date: 2024-06-28
    Description: This data collection contains physical oceanographic and hydrochemistry data from 82 cruises in the frame of the project VEINS -Variability of Exchanges in the Northern Seas.
    Keywords: 06MT39_5; 06MT39_5/506-1; 06MT39_5/507-1; 06MT39_5/508-1; 06MT39_5/509-1; 06MT39_5/510-1; 06MT39_5/511-1; 06MT39_5/512-2; 06MT39_5/513-1; 06MT39_5/514-1; 06MT39_5/515-1; 06MT39_5/516-1; 06MT39_5/517-1; 06MT39_5/518-1; 06MT39_5/519-1; 06MT39_5/520-1; 06MT39_5/521-1; 06MT39_5/522-1; 06MT39_5/523-1; A09/98; A09/98_286; A09/98_288; A09/98_291; A09/98_292; A09/98_294; A09/98_296; A09/98_300; A09/98_302; A09/98_317; A09/98_319; A09/98_322; A09/98_324; A09/98_325; A09/98_327; A09/98_330; A09/98_331; A09/98_335; A09/98_356; A09/98_377; A09/98_379; A09/98_381; A09/98_383; A09/98_385; A09/98_387; A09/98_401; A09/98_424; A09/98_427; A09/98_430; A09/98_449; A09/98_451; A09/98_454; A09/98_456; A09/98_458; A09/98_461; A09/98_462; A09/98_465; A09/98_467; A09/98_470; A09/98_471; A09/98_477; A09/98_480; A09/98_483; A09/98_497; A09/98_499; A09/98_502; A09/98_504; A09/98_506; A09/98_519; A09/98_521; A09/98_522; A09/98_523; A09/98_525; A09/98_527; A09/98_534; A09/98_537; A09/98_539; A09/98_542; A09/98_544; A09/98_548; A09/98_549; A09/98_566; A09/98_569; A09/98_572; A09/98_574; A09/98_576; A09/98_578; A09/98_585; A09/98_588; A09/98_590; A09/98_591; A09/98_594; A09/98_597; A09/98_598; A09/98_599; A09/98_602; A09/98_603; A09/98_604; A09/98_606; A09/98_608; A09/98_610; A09/98_612; A10/99; A10/99_364-1; A10/99_366-1; A10/99_368-1; A10/99_370-1; A10/99_372-1; A10/99_374-1; A10/99_376-1; A10/99_379-1; A10/99_382-1; A10/99_384-1; A10/99_394-1; A10/99_396-1; A10/99_398-1; A10/99_400-1; A10/99_401-1; A10/99_403-1; A10/99_404-1; A10/99_406-1; A10/99_409-1; A10/99_444-1; A10/99_446-1; A10/99_448-1; A10/99_452-1; A10/99_454-1; A10/99_457-1; A10/99_481-1; A10/99_483-1; A10/99_486-1; A10/99_488-1; A10/99_490-1; A10/99_491-1; A10/99_509-1; A10/99_511-1; A10/99_513-1; A10/99_515-1; A10/99_517-1; A10/99_521-1; A10/99_522-1; A10/99_525-1; A10/99_529-1; A10/99_531-1; A10/99_534-1; A10/99_536-1; A10/99_551-1; A10/99_557-1; A10/99_559-1; A10/99_561-1; A10/99_564-1; A10/99_566-1; A10/99_568-1; A10/99_580-1; A10/99_582-1; A10/99_584-1; A10/99_586-1; A10/99_589-1; A10/99_592-1; A10/99_595-1; A10/99_597-1; A10/99_599-1; A10/99_600-1; A10/99_602-1; A10/99_603-1; A10/99_604-1; A10/99_606-1; A10/99_608-1; A10/99_612-1; A10/99_615-1; A10/99_618-1; A10/99_620-1; A10/99_640-1; A10/99_643-1; A10/99_646-1; A10/99_648-1; A10/99_650-1; A10/99_653-1; A10/99_655-1; A10/99_656-1; A10/99_658-1; A10/99_662-1; A10/99_664-1; A10/99_667-1; A10/99_670-1; A10/99_673-1; A10/99_676-1; A10/99_678-1; A10/99_680-1; A10/99_682-1; A10/99_685-1; A10/99_687-1; A10/99_689-1; A10/99_697-1; A10/99_698-1; A10/99_700-1; A10/99_702-1; A10/99_704-1; A10/99_705-1; A10/99_707-1; A14/97; A14/97_446; A14/97_448; A14/97_450; A14/97_452; A14/97_453; A14/97_455; A14/97_457; A14/97_458; A14/97_460; A14/97_467; A14/97_507; A14/97_509; A14/97_510; A14/97_514; A14/97_515; A14/97_517; A14/97_546; A14/97_548; A14/97_551; A14/97_556; A14/97_558; A14/97_576; A14/97_580; A14/97_582; A14/97_584; A14/97_586; A14/97_589; A14/97_592; A14/97_594; A14/97_597; A14/97_622; A14/97_624; A14/97_627; A14/97_641; A14/97_643; A14/97_644; A14/97_645; A14/97_648; A14/97_651; A14/97_658; A14/97_660; A14/97_663; A14/97_666; A14/97_668; A14/97_671; A14/97_672; A14/97_689; A14/97_691; A14/97_694; A14/97_696; A14/97_698; A14/97_700; A14/97_710; A14/97_711; A14/97_712; A14/97_714; A14/97_717; A14/97_720; A14/97_722; A14/97_723; A14/97_726; A14/97_729; A14/97_734; A14/97_739; A14/97_741; A14/97_742; A14/97_744; A14/97_746; A14/97_748; A14/97_759; ARA-12-1/97; ARA-12-1/97_398; ARA-12-1/97_399; ARA-12-1/97_400; ARA-12-1/97_401; ARA-12-1/97_402; ARA-12-1/97_403; ARA-12-1/97_404; ARA-12-1/97_405; ARA-12-1/97_406; ARA-12-1/97_407; ARA-12-1/97_408; ARA-12-1/97_409; ARA-12-1/97_410; ARA-12-1/97_411; ARA-12-1/97_412; ARA-12-1/97_413; ARA-12-1/97_414; ARA-12-1/97_415; ARA-12-1/97_416; ARA-12-1/97_417; ARA-12-1/97_418; ARA-12-1/97_419; ARA-12-1/97_420; ARA-12-1/97_421; ARA-12-1/97_422; ARA-12-1/97_423; ARA-12-1/97_424; ARA-12-1/97_425; ARA-12-2/97; ARA-12-2/97_426; ARA-12-2/97_427; ARA-12-2/97_428; ARA-12-2/97_429; ARA-12-2/97_430; ARA-12-2/97_431; ARA-12-2/97_432; ARA-12-2/97_433; ARA-12-2/97_434; ARA-12-2/97_435; ARA-12-2/97_436; ARA-12-2/97_437; ARA-12-2/97_438; ARA-12-2/97_439; ARA-12-2/97_440; ARA-12-2/97_441; ARA-12-2/97_442; ARA-12-2/97_443; ARA-12-2/97_444; ARA-12-2/97_445; ARA-12-2/97_446; ARA-12-2/97_447; ARA-12-2/97_448; ARA-12-2/97_449; ARA-12-2/97_450; ARA-12-2/97_451; ARA-12-2/97_452; ARA-12-2/97_453; ARA-12-2/97_454; ARA-12-2/97_455; ARA-12-2/97_456; ARA-12-2/97_457; ARA-12-2/97_458; ARA-12-2/97_459; ARA-12-2/97_460; ARA-12-2/97_461; ARA-12-2/97_462; ARA-12-2/97_463; ARA-12-2/97_464; ARA-12-2/97_465; ARA-12-2/97_466; ARA-12-2/97_467; ARA-12-2/97_468; ARA-12-2/97_469; ARA-12-2/97_470; ARA-12-2/97_471; ARA-12-2/97_472; ARA-12-2/97_473; ARA-12-2/97_474; ARA-12-2/97_475; ARA-12-2/97_476; ARA-12-2/97_477; ARA-12-2/97_478; ARA-12-2/97_479; ARA-12-2/97_480; ARA-12-2/97_481; ARA-12-2/97_482; ARA-12-2/97_483; ARA-12-2/97_484; ARA-12-2/97_485; ARA-12-2/97_486; ARA-12-2/97_487; ARA-12-2/97_488; ARA-12-2/97_489; ARA-12-2/97_490; ARA-12-2/97_491; ARA-12-2/97_492; ARA-12-2/97_493; ARA-12-2/97_494; ARA-12-2/97_495; ARA-12-2/97_496; ARA-12-2/97_497; ARA-12-3/97; ARA-12-3/97_498; ARA-12-3/97_499; ARA-12-3/97_500; ARA-12-3/97_501; ARA-12-3/97_502; ARA-12-3/97_503; ARA-12-3/97_504; ARA-12-3/97_505; ARA-12-3/97_506; ARA-12-3/97_507; ARA-12-3/97_508; ARA-12-3/97_509; ARA-12-3/97_510; ARA-12-3/97_511; ARA-12-3/97_512; ARA-12-3/97_513; ARA-12-3/97_514; ARA-12-3/97_515; ARA-12-3/97_516; ARA-12-3/97_517; ARA-12-3/97_518; ARA-12-3/97_519; ARA-12-3/97_521; ARA-12-3/97_522; ARA-12-3/97_523; ARA-12-3/97_524; ARA-12-3/97_525; ARA-12-3/97_526; ARA-12-3/97_527; ARA-12-3/97_528; ARA-12-3/97_529; ARA-12-3/97_530; ARA-12-3/97_531; ARA-12-3/97_532; ARA-12-3/97_533; ARA-12-3/97_534; ARA-12-3/97_535; ARA-12-3/97_536; ARA-12-3/97_537; ARA-12-3/97_538; ARA-12-3/97_539; ARA-12-3/97_540; ARA-12-3/97_541; ARA-12-3/97_542; ARA-12-3/97_543; ARA-12-3/97_544; ARA-12-3/97_545; ARA-12-3/97_546; ARA-12-3/97_547; ARA-12-3/97_548; ARA-12-3/97_549; ARA-12-3/97_550; ARA-12-3/97_551; ARA-12-3/97_552; ARA-12-3/97_553; ARA-12-3/97_554; ARA-12-3/97_555; ARA-12-3/97_556; ARA-12-3/97_557; ARA-12-3/97_558; ARA-12-3/97_559; ARA-12-3/97_560; ARA-12-3/97_561; ARA-12-3/97_562; ARA-12-3/97_563; ARA-12-3/97_564; ARA-12-3/97_565; ARA-12-3/97_566; ARA-12-3/97_567; ARA-12-3/97_568; ARA-12-3/97_569; ARA-12-3/97_570; ARA-12-3/97_571; ARA-12-3/97_572; ARA-12-3/97_573; ARA-12-3/97_574; ARA-12-3/97_575; ARA-12-3/97_576; ARA-12-3/97_577; ARA-12-3/97_578; Aranda (1989); ARK-XIV/2; ARK-XV/3; Arni Fridriksson; B02/98; B02/98-1001; B02/98-1011; B02/98-1021; B02/98-1031; B02/98-1061; B02/98-1062; B02/98-1071; B02/98-1081; B02/98-1101; B02/98-1111; B02/98-1121; B02/98-1131; B02/98-1141; B02/98-1151; B02/98-1181; B02/98-1191; B02/98-1221; B02/98-1222; B02/98-1231; B02/98-1241; B02/98-1251; B02/98-1261; B02/98-1271; B02/98-1281; B02/98-1291; B02/98-1292; B02/98-1293; B02/98-1301; B02/98-1311; B02/98-1321; B02/98-1341; B02/98-1342; B02/98-1361; B02/98-1371; B02/98-1381; B02/98-1391; B02/98-1401; B02/98-1411; B02/98-1421; B02/98-1431; B02/98-1441; B02/98-1451; B02/98-1461; B02/98-1471; B02/98-1481; B02/98-1491; B02/98-1501; B02/98-1511; B02/98-1521; B02/98-1531; B02/98-1541; B02/98-1551; B02/98-1561; B02/98-1571; B02/98-1581; B02/98-1591; B02/98-1601; B02/98-1611; B02/98-1622; B02/98-531; B02/98-541; B02/98-551; B02/98-561; B02/98-571; B02/98-581; B02/98-591; B02/98-601; B02/98-621; B02/98-622; B02/98-631; B02/98-641; B02/98-651; B02/98-661; B02/98-671; B02/98-681; B02/98-691; B02/98-701; B02/98-711; B02/98-721; B02/98-731; B02/98-741; B02/98-751; B02/98-761; B02/98-771; B02/98-781; B02/98-791; B02/98-801; B02/98-811; B02/98-821; B02/98-831; B02/98-841; B02/98-842; B02/98-843; B02/98-844; B02/98-845; B02/98-851; B02/98-861; B02/98-891; B02/98-901; B02/98-911; B02/98-921; B02/98-931; B02/98-941; B02/98-961; B02/98-971; B02/98-972; B02/98-973; B02/
    Type: Dataset
    Format: application/zip, 93 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 5
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    Ice rafted debris (〉 2 mm gravel) distribution in sediment core PS1735-1 (1996)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-06-28
    Keywords: ARK-V/3b; AWI_Paleo; DEPTH, sediment/rock; GIK21735-1 PS13/249; Gravity corer (Kiel type); Ice rafted debris, number of gravel; IRD-Counting (Grobe, 1987); King Oskar Fjord; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1735-1; Quaternary Environment of the Eurasian North; QUEEN; SL
    Type: Dataset
    Format: text/tab-separated-values, 330 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 6
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    Unknown
    Shear strength of sediment core PS1712-2 (1996)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-06-28
    Keywords: ARK-V/3b; AWI_Paleo; DEPTH, sediment/rock; GIK21712-2 PS13/160; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1712-2; Rotovisco, Haake; Scoresby Sund; Shear strength, primary; SL
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 7
    facet.materialart.
    Unknown
    Shear strenght of sediment core PS1727-1 (1996)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-06-28
    Keywords: ARK-V/3b; AWI_Paleo; DEPTH, sediment/rock; GIK21727-1 PS13/204; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1727-1; Rotovisco, Haake; Scoresby Sund; Shear strength, primary; SL
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 8
    facet.materialart.
    Unknown
    Ice rafted debris (〉 2 mm gravel) distribution in sediment core PS1733-2 (1996)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-06-28
    Keywords: ARK-V/3b; AWI_Paleo; DEPTH, sediment/rock; GIK21733-2 PS13/240; Gravity corer (Kiel type); Ice rafted debris, number of gravel; IRD-Counting (Grobe, 1987); King Oskar Fjord; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1733-2; Quaternary Environment of the Eurasian North; QUEEN; SL
    Type: Dataset
    Format: text/tab-separated-values, 401 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 9
    facet.materialart.
    Unknown
    Susceptibility raw data of sediment core PS1713-2 (1996)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Keywords: ARK-V/3b; AWI_Paleo; DEPTH, sediment/rock; GIK21713-2 PS13/161; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1713-2; Scoresby Sund; SL; Susceptibility; Susceptibility unit, AWI, MS2C [145 mm]
    Type: Dataset
    Format: text/tab-separated-values, 97 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 10
    facet.materialart.
    Unknown
    Susceptibility raw data of sediment core PS1714-2 (1996)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Keywords: ARK-V/3b; AWI_Paleo; DEPTH, sediment/rock; GIK21714-2 PS13/165; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1714-2; Scoresby Sund; SL; Susceptibility; Susceptibility unit, AWI, MS2C [145 mm]
    Type: Dataset
    Format: text/tab-separated-values, 445 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
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