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Vertical distribution of benthic foraminifers in the Arctic Ocean (1998)

Wollenburg, Jutta Erika ; Mackensen, Andreas

PANGAEA

In: Supplement to: Wollenburg, Jutta Erika; Mackensen, Andreas (1998): On the vertical distribution of living (Rose Bengal stained) benthic foraminifers in the Arctic Ocean. Journal of Foraminiferal Research, 28(4), 268-285

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Publication Date: 2024-07-01

Description: The vertical distribution of living (Rose Bengal stained) benthic foraminifers was determined in the upper 15 cm of sediment cores taken along transects extending from the continental shelf of Spitsbergen through the Eurasian Basin of the Arctic Ocean. Cores taken by a multiple corer were raised from 50 stations with water depths between 94 and 4427 m, from areas with moderate primary production values to areas that are among the least productive ones in the world. We believe, that in the Arctic Ocean the vertical distribution of living foraminifers is determined by the restricted availability of food. Live foraminiferal faunas are dominated by potentially infaunal species or epifaunal species. Species confined to the infaunal microhabitat are absent in Arctic sediments that we examined, and predominantly infaunal living species are nowhere dominant. In general, an infaunal mode of life is restricted to the seasonally ice-free areas and thus to areas with at least moderate primary production during the summer period. Under the permanent ice cover living species are usually restricted to the top centimeter of the sediment surface, even though some are able to dwell deeper in the sediment under ice-free conditions.

Keywords: ANT-X/4; ARK-IX/4; ARK-VIII/2; ARK-VIII/3; AWI_Paleo; Barents Sea; Gakkel Ridge, Arctic Ocean; Giant box corer; GKG; Lomonosov Ridge, Arctic Ocean; MIC; MiniCorer; MUC; MultiCorer; Nansen Basin; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/111; PS19/113; PS19/114; PS19/117; PS19/150; PS19/152; PS19/154; PS19/157; PS19/175; PS19/178; PS19/190; PS19/245; PS19/246; PS19/249; PS19/252; PS19 ARCTIC91; PS19 EPOS II; PS21 06AQANTX_4; PS2137-1; PS2139-1; PS2140-1; PS2143-1; PS2157-3; PS2159-3; PS2161-1; PS2163-1; PS2177-3; PS2179-3; PS2187-5; PS2212-6; PS2213-4; PS2214-1; PS2215-1; PS2247-1; PS2445-2; PS2446-2; PS27; PS27/019; PS27/020; Quaternary Environment of the Eurasian North; QUEEN; South Atlantic; Svalbard; Yermak Plateau

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Format: application/zip, 18 datasets

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Age model and color measurements of sediment cores from the eastern equatorial Pacific (1999)

Weber, Michael E ; Pisias, Nicklas G

PANGAEA

In: Supplement to: Weber, Michael E; Pisias, Nicklas G (1999): Spatial and temporal distribution of biogenic carbonate and opal in deep-sea sediments from the eastern equatorial Pacific: implications for ocean history since 1.3 Ma. Earth and Planetary Science Letters, 174(1-2), 59-73, https://doi.org/10.1016/S0012-821X(99)00248-4

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Publication Date: 2024-07-01

Description: High-resolution records of glacial-interglacial variations in biogenic carbonate, opal, and detritus (derived from non-destructive core log measurements of density, P-wave velocity and color; r 〉= 0.9) from 15 sediment sites in the eastern equatorial (sampling resolution is ~1 kyr) clear response to eccentricity and precession forcing. For the Peru Basin, we generate a high-resolution (21 kyr increment) orbitally-based chronology for the last 1.3 Ma. Spectral analysis indicates that the 100 kyr cycle became dominant at roughly 1.2 Ma, 200-300 kyr earlier than reported for other paleoclimatic records. The response to orbital forcing is weaker since the Mid-Brunhes Dissolution Event (at 400 ka). A west-east reconstruction of biogenic sedimentation in the Peru Basin (four cores; 91-85°W) distinguishes equatorial and coastal upwelling systems in the western and eastern sites, respectively. A north-south reconstruction perpendicular to the equatorial upwelling system (11 cores, 11°N-°3S) shows high carbonate contents (〉= 50%) between 6°N and 4°S and highly variable opal contents between 2°N and 4°S. Carbonate cycles B-6, B-8, B-10, B-12, B-14, M-2, and M-6 are well developed with B-10 (430 ka) as the most prominent cycle. Carbonate highs during glacials and glacial-interglacial transitions extended up to 400 km north and south compared to interglacial or interglacial^glacial carbonate lows. Our reconstruction thus favors glacial-interglacial expansion and contraction of the equatorial upwelling system rather than shifting north or south. Elevated accumulation rates are documented near the equator from 6°N to 4°S and from 2°N to 4°S for carbonate and opal, respectively. Accumulation rates are higher during glacials and glacial-interglacial transitions in all cores, whereas increased dissolution is concentrated on Peru Basin sediments close to the carbonate compensation depth and occurred during interglacials or interglacial-glacial transitions.

Keywords: 181KL; 184KL; 189KL; 206KL; 217KL; 222SL; 229KL; 235KL; 243KL; 244KA; 249KL; 251KL; 254KL; 261KA; 268KA; 272KA; 276KL; 278KA; 286KL; ATESEPP; Gravity corer (Kiel type); KAL; Kasten corer; KL; Peru Basin; Piston corer (BGR type); SEDIPERU - TUSCH; SL; SO106/1; SO106/1_181KL; SO106/1_184KL; SO106/1_189KL; SO106/1_206KL; SO106/1_217KL; SO106/1_222SL; SO106/1_229KL; SO106/1_235KL; SO106/2; SO106/2_243KL; SO106/2_244KA; SO106/2_249KL; SO106/2_251KL; SO106/2_254KL; SO106/2_261KA; SO106/2_268KA; SO106/2_272KA; SO106/2_276KL; SO106/2_278KA; SO106/2_286KL; SO79; SO79_108KL; SO79_136KL; SO79_164KL; SO79_169KL; SO79_26KL; SO79_48KL; SO79_53KL; SO79_71KL; SO79_77KL; SO79_82KL; SO79_85KL; SO79_9KL; Sonne

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Format: application/zip, 37 datasets

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Calcareous dinoflagellates in the eastern equatorial Atlantic (1998)

Höll, Christine ; Zonneveld, Karin A F ; Willems, Helmut

PANGAEA

In: Supplement to: Höll, Christine; Zonneveld, Karin A F; Willems, Helmut (1998): On the ecology of calcareous dinoflagellates: The Quaternary Eastern Equatorial Atlantic. Marine Micropaleontology, 33(1-2), 1-25, https://doi.org/10.1016/S0377-8398(97)00033-9

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Publication Date: 2024-07-01

Description: Sediments of the Equatorial Atlantic (core GeoB 1105-4) have been investigated for both calcareous dinoflagellates and organic-walled dinoflagellate cysts. In order to determine the ecological affinity of calcareous dinoflagellates the statistical methods of Detrended Correspondence Analysis (DCA) and Redundancy Analysis (RDA) were used. Utilising DCA, distribution patterns of calcareous dinoflagellates have been compared with those of the ecologically much better known organic-walled dinoflagellate cysts. This method was also used to determine which environmental gradients have a major influence on the species composition. By using existing environmental information based on benthic and planktic foraminifera, such as Sea Surface Temperature (SST) and stable oxygen and carbon isotopes, as well as information on the amount of Calcium Carbonate and Total Organic Carbon (TOC) in bottom sediments, these gradients could be interpreted in terms of productivity and glacial-interglacial trends. Using RDA, the direct relationships between the distribution patterns of calcareous dinoflagellates with the above mentioned external variables could be determined. For the studied region and time interval (141-6.7 ka) the calcareous dinoflagellates show enhanced abundances in periods with reduced productivity most probably related to decreased divergence and relatively stratified, oligotrophic oceanic conditions.

Keywords: Equatorial Atlantic; GeoB1105-4; Gravity corer (Kiel type); M9/4; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents

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Format: application/zip, 2 datasets

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Radionuclides measured on three sediment cores from the Weddell Sea, Antarctica (1995)

Frank, Martin ; Eisenhauer, Anton ; Bonn, Wolfgang J ; [et al.]

PANGAEA

In: Supplement to: Frank, Martin; Eisenhauer, Anton; Bonn, Wolfgang J; Walter, Peter; Grobe, Hannes; Kubik, Peter W; Dittrich-Hannen, Beate; Mangini, Augusto (1995): Sediment redistribution versus paleoproductivity change: Weddell Sea margin sediment stratigraphy and biogenic particle flux of the last 250,000 years deduced from 230Thex, 10Be and biogenic barium profiles. Earth and Planetary Science Letters, 136(3-4), 559-573, https://doi.org/10.1016/0012-821X(95)00161-5

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Publication Date: 2024-07-01

Description: High resolution 230Thex and 10Be and biogenic barium profiles were measured at three sediment gravity cores (length 605-850 cm) from the Weddell Sea continental margin. Applying the 230Thex dating method, average sedimentation rates of 3 cm/kyr for the two cores from the South Orkney Slope and of 2.4 cm/kyr for the core from the eastern Weddell Sea were determined and compared to delta18O and lithostratigraphic results. Strong variations in the radionuclide concentrations in the sediments resembling the glacial/interglacial pattern of the delta18O stratigraphy and the 10Be stratigraphy of high northern latitudes were used for establishing a chronostratigraphy. Biogenic Ba shows a pattern similar to the radionuclide profiles, suggesting that both records were influenced by increased paleoproductivity at the beginning of the interglacials. However, 230Thex0 fluxes (0 stands for initial) exceeding production by up to a factor of 4 suggest that sediment redistribution processes, linked to variations in bottom water current velocity, played the major role in controlling the radionuclide and biogenic barium deposition during isotope stages 5e and 1. The correction for sediment focusing makes the 'true' vertical paleoproductivity rates, deduced from the fluxes of proxy tracers like biogenic barium, much lower than previously estimated. Very low 230Thex0 concentrations and fluxes during isotope stage 6 were probably caused by rapid deposition of older, resedimented material, delivered to the Weddell Sea continental slopes by the grounded ice shelves and contemporaneous erosion of particles originating from the water column.

Keywords: ANT-II/3; ANT-IV/3; ANT-VI/3; Atka Bay; AWI_Paleo; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS04; PS04/257; PS08; PS08/366; PS1170-3; PS12; PS12/248; PS1388-3; PS1575-1; SL; South Atlantic Ocean; South Orkney

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Format: application/zip, 6 datasets

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Sediments in arctic sea ice - entrainment, characterization and quantification (1998)

Thiede, Jörn ; Lindemann, Frank

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In: Supplement to: Lindemann, Frank (1998): Sedimente im arktischen Meereis - Eintrag, Charakterisierung und Quantifizierung (Sediments in arctic sea ice - entrainment, characterization and quantification). Berichte zur Polarforschung = Reports on Polar Research, 283, 124 pp, https://doi.org/10.2312/BzP_0283_1998

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Publication Date: 2024-07-01

Description: Sediments in Arctic sea ice are important for erosion and redistribution and consequently a factor for the sediment budget of the Arctic Ocean. The processes leading to the incorporation of sediments into the ice are not understood in detail yet. In the present study, experiments on the incorporation of sediments were therefore conducted in ice tanks of The Hamburg Ship Model Basin (HSVA) in winter 1996/1997, These experiments showed that on average 75 % of the artificial sea-ice sediments were located in the brine-channel system. The sediments were scavenged from the water column by frazil ice. Sediments functioning as a nucleus for the formation of frazil ice were less important for the incorporation. Filtration in grease ice during relatively calm hydrodynamic conditions was probably an effective process to enrich sediments in the ice. Wave fields did not play an important role for the incorporation of sediments into the artificial sea ice. During the expedition TRANSDRIFT III (TDIII, October 1995), different types of natural, newly-formed sea ice (grease ice, nilas and young ice) were sampled in the inner Laptev Sea at the time of freeze-up. The incorporation of sediments took place during calm meteorological conditions then. The characteristics of the clay mineral assemblages of these sedirnents served as references for sea-ice sediments which were sampled from first-year drift ice in the outer Laptev Sea and the adjacent Arctic Ocean during the POLARSTERN expedition ARK-XI/1 (July-September 1995). Based on the clay mineral assemblages, probable incorporation areas for the sedirnents in first-year drift ice could be statistically reconstructed in the inner Laptev Sea (eastern, central, and Western Laptev Sea) as well as in adjacent regions. Comparing the amounts of particulate organic carbon (POC) in sea-ice sediments and in surface sediments from the shelves of potential incorporation areas often reveals higher values in sea-ice sediments (TDIII: 3.6 %DM; ARK-XI/1: 2.3 %DM). This enrichment of POC is probably due to the incorporation process into the sea ice, as could be deducted from maceral analysis and Rock-Eval pyrolysis. Both methods were applied in the present study to particulate organic material (POM) from sea-ice sediments for the first time. It was shown that the POM of the sea-ice sediments from the Laptev Sea and the adjacent Arctic Ocean was dominated by reworked, strongly fragmented, allochthonous (terrigenous) material. This terrigenous component accounted for more than 75 % of all counted macerals. The autochthonous (marine) component was also strongly fragmented, and higher in the sediments from newly-formed sea ice (24 % of all counted macerals) as compared to first-year drift ice (17 % of all counted macerals). Average hydroge indices confirmed this pattern and were in the transition zone between kerogen types II and III (TDIII: 275 mg KW/g POC; ARK-XI/1: 200 mg KW/g POC). The sediment loads quantified in natural sea ice (TDIII: 33.6 mg/l, ARK-XI/1: 49.0 mg/l) indicated that sea-ice sediments are an important factor for the sediment budget in the Laptev Sea. In particular during the incorporation phase in autumn and early winter, about 12 % of the sediment load imported annually by rivers into the Laptev Sea can be incorporated into sea ice and redistributed during calm meteorological conditions. Single entrainment events can incorporate about 35 % of the river input into the sea ice (ca. 9 x 10**6 t) and export it via the Transpolar Drift from the Eurasian shelf to the Fram Strait.

Keywords: 201; 205b; 208; 209; 210; 219; 221; 228a; 228b; 229; 230; 232b; 234; 237; 239; 240; 241; 242; 246; 283-1; 283-4; 285-1; 286-1; 287-1; 287-2; 288-2; 288-4; 290-1; 291-1; 291-3; 292-1; 292-2; 293-1; 293-2; 293-3; 293-4; 293-5; 293-6; 293-7; 294-1; 294-2; 294-3; 294-4; 294-6; 295-1; 295-2; 295-3; 295-4; 295-5; 295-6; 296-1; 296-2; 296-5; 296-6; Arctic Ocean; ARK-XI/1; ARK-XI/1_201; ARK-XI/1_205b; ARK-XI/1_208; ARK-XI/1_209; ARK-XI/1_210; ARK-XI/1_219; ARK-XI/1_221; ARK-XI/1_228a; ARK-XI/1_228b; ARK-XI/1_229; ARK-XI/1_230; ARK-XI/1_232b; ARK-XI/1_234; ARK-XI/1_237; ARK-XI/1_239; ARK-XI/1_240; ARK-XI/1_241; ARK-XI/1_242; ARK-XI/1_246; East Siberian Sea; ICE; Ice station; Kapitan Dranitsyn; Laptev Sea; Polarstern; PS36; Quaternary Environment of the Eurasian North; QUEEN; TDIII_283-1; TDIII_283-4; TDIII_285-1; TDIII_286-1; TDIII_287-1; TDIII_287-2; TDIII_288-2; TDIII_288-4; TDIII_290-1; TDIII_291-1; TDIII_291-3; TDIII_292-1; TDIII_292-2; TDIII_293-1; TDIII_293-2; TDIII_293-3; TDIII_293-4; TDIII_293-5; TDIII_293-6; TDIII_293-7; TDIII_294-1; TDIII_294-2; TDIII_294-3; TDIII_294-4; TDIII_294-6; TDIII_295-1; TDIII_295-2; TDIII_295-3; TDIII_295-4; TDIII_295-5; TDIII_295-6; TDIII_296-1; TDIII_296-2; TDIII_296-5; TDIII_296-6; Transdrift-III

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Format: application/zip, 2 datasets

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Foraminiferal faunal estimates of paleotemperature: Circumventing the no-analog problem yields cool ice age tropics (1999)

Mix, Alan C ; Morey, Ann E ; Pisias, Nicklas G ; [et al.]

PANGAEA

In: Supplement to: Mix, Alan C; Morey, Ann E; Pisias, Nicklas G; Hostetler, Steven W (1999): Foraminiferal faunal estimates of paleotemperature: Circumventing the no-analog problem yields cool ice age tropics. Paleoceanography, 14(3), 350-359, https://doi.org/10.1029/1999PA900012

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Publication Date: 2024-07-01

Description: The sensitivity of the tropics to climate change, particularly the amplitude of glacial-to-interglacial changes in sea surface temperature (SST), is one of the great controversies in paleoclimatology. Here we reassess faunal estimates of ice age SSTs, focusing on the problem of no-analog planktonic foraminiferal assemblages in the equatorial oceans that confounds both classical transfer function and modern analog methods. A new calibration strategy developed here, which uses past variability of species to define robust faunal assemblages, solves the no-analog problem and reveals ice age cooling of 5° to 6°C in the equatorial current systems of the Atlantic and eastern Pacific Oceans. Classical transfer functions underestimated temperature changes in some areas of the tropical oceans because core-top assemblages misrepresented the ice age faunal assemblages. Our finding is consistent with some geochemical estimates and model predictions of greater ice age cooling in the tropics than was inferred by Climate: Long-Range Investigation, Mapping, and Prediction (CLIMAP) [1981] and thus may help to resolve a long-standing controversy. Our new foraminiferal transfer function suggests that such cooling was limited to the equatorial current systems, however, and supports CLIMAP's inference of stability of the subtropical gyre centers.

Keywords: 138-846B; A150/180; A152-84; A153-154; A15-547TW; A15-552TW; A15-558; A15-558P; A15-558TW; A15-559FF; A15-572FF; A15-585GC; A15-586TW; A15-590GC; A15-591GC; A15-592FF; A15-596FF; A15-597A; A15-597B; A15-600FF; A15-602FF; A15-612GC; A15-614TW; A15-618GC; A156-4; A157-3; A164-13; A164-15; A164-16; A164-17; A164-23; A164-24; A164-5; A164-6; A164-61; A167-12; A167-13; A167-14; A167-18TW; A167-1TW; A172-1; A172-2; A173-4; A179-13; A179-15; A179-20; A179-24; A179-6; A179-7; A180-13; A180-15; A180-16; A180-20; A180-32; A180-39; A180-47; A180-47PC; A180-48; A180-48PC; A180-56; A180-69; A180-70; A180-72; A180-73; A180-74; A180-76; A180-78; A180-9; A181/185; A181-7; A181-9; A260210A; Agassiz; AH-1; AH-4; AH-5; AH-7; AH-8; All5402P; All5423P; All5424P; All542P; also published as VM28-122; AMPH-005G; AMPH-007PG; AMPH-011P; AMPH-012G; AMPH-013G; AMPH-016G; AMPH-017G; AMPH-019G; AMPH01AR; AMPH-021G; AMPH-022G; AMPH-023G; AMPH-024G; AMPH-107G; AMPH-130G; AMPH-131G; AMPH-132G; AMPH-133G; AMPH-134G; AMPH-135GV; AMPH-137GV; AMPH-138GV; AMPH-139GV; AMPHITRITE; AR1-117; AR1-119; AR1-144; AR2-113; AR2-117; AR2-128; AR2-136; AR3-25; AR3-38; AR3-45; AR4-52; AR4-55; AR4-56; AR4-63; Argo; ARIES; ARIES-046G; ARIES-049G; Atlantic; Atlantic Ocean; Bay of Bengal; BC; Box corer; BRA-262D; BRA-91AD; BRA-91D; BRA-96D; CAP-1BG; CAP-1HG; CAP-2-1BG; CAP-32HG; CAP-3HG; CAP-42-1; CAP-44BG; CAP-48-2; CAP-48HG; CAP-49BG; CAP-4BG; CAP-50HG; CAP-5HG; CAP-6HG; CAP-8-2; CH10098P; CH10-98; CHA-164B; CHA-296; CHA-300; CHA-302; Challenger1872; CHM-5; CHU-23; CHU-23G; CHU-24; CHU-26; CHU-30; CHU-X1; CIRCE; CIRCE-21; CIRCE-239; CIRCE-24; CIRCE-26; CIRCE-27; CIRCE-32; CIRCE-36; CIRCE-38; CIRCE-42; CIRCE-44; CUS-3G; DIS-385D; DIS-386D; DODO; DODO-117PG; DODO-119PG; DODO-126P; DODO-126PG; DODO-144G; DODO-173G; DODO-191; DODO-192G; DODO-193; DODO-195G; DODO-197; DODO-200V; DODO-201G; DODO-202V; DODO-204; DODO-220V; DRILL; Drilling/drill rig; DW010; DW013; DW034; DW035; DW036; DW048; DW050; DW058; DW089; DW137; DW147B; DWD-100B; DWD-108B; DWD-10BG; DWD-10HH; DWD-11BG; DWD-12BG; DWD-12HH; DWD-137G; DWD-13BG; DWD-13HH; DWD-143; DWD-147B; DWD-149; DWD-15BG; DWD-16BG; DWD-34HG; DWD-35HH; DWD-36HG; DWD-46BG; DWD-47B; DWD-47BG; DWD-48BG; DWD-48HG; DWD-49BG; DWD-50HG; DWD-54HG; DWD-56BG; DWD-56HG; DWD-58BG; DWD-58HH; DWD-59BG; DWD-60BG; DWD-61BG; DWD-62BG; DWD-63BG; DWD-64BG; DWD-68BG; DWD-70BG; DWD-71BG; DWD-73BG; DWD-74BG; DWD-75BG; DWD-76BG; DWD-77BG; DWD-78BG; DWD-79BG; DWD-83BG; DWD-89HH; DWD-89HH-2; DWD-93BG; East Atlantic; Eastern Equatorial Pacific; ELT11.010; ELT11.064; ELT11.089; ELT-1101; ELT-1110; ELT-1164; ELT-1189; ELT-1246; ELT-1271; ELT44; ELT44.027-PC; ELT45; ELT45.027-PC; ELT45.029-PC; ELT45.070-PC; ELT45.073-PC; ELT45.077-PC; ELT45.078-PC; ELT45.081-PC; ELT48; ELT48.003-PC; ELT48.011-PC; ELT48.022-PC; ELT48.023-PC; ELT48.027-PC; ELT49; ELT49.022-PC; ELT49.023-PC; ELT49.024-PC; ELT49.025-PC; Eltanin; ELT-C100; EN06601; EN066-10GGC; Endeavor; EQA-27; FANHMS2G; FANHMS4G; FFC; Free fall corer; GC; GIK12392-1; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Horizon; Indian Ocean; JAPANYON; Joides Resolution; JSB-5P; JSB-6P; JYN2; JYN2-007G; JYN5-019G; K708-001; K708-004; K708-006; K708-007; K708-008; K714-3; KAL; Kasten corer; KM1-41; KNR073-04-003; KNR733P; Knr735P; KNR735P; Leg138; LFGS; LFGS-36G; LFGS-38G; LFGS-45G; LSDA; LSDA-103V; LSDA-106G; LSDA-107GA; LSDA-113G; LSDA-117G; LSDA-128G; LSDA-136G; LSDA-SCS; LSDA-SCS-002G; LSDA-SCS-003G; LSDA-SCS-006G; LSDA-SCS-008G; LSDA-SCS-009G; LSDA-SCS-013D; LSDH; LSDH-009G; LSDH-025V; LSDH-038V; LSDH-076PG; LSDH-077G; LSDH-078PG; LSDH-079P; LSDH-079PG; LSDH-080G; LSDH09; LSDH-093PG; LSDH-104G; LUSIAD-9; LUSIAD-A; LUSIAD-H; M12392-1; M25; M70-68; M70-PC-49; M70-PC-61; Marion Dufresne (1972); MD10; MD13; MD76-131; MD76-132; MD76-135; MD77-168; MD77-169; MD77-170; MD77-171; MD77-174; MD77-176; MD77-179; MD77-180; MD77-181; MD77-185; MD77-191; MD77-194; MD77-196; MD77-199; MD77-202; MD77-203; MD77-204; MDPC03HO-043K; Melville; MEN; MEN-08G; MEN-11G; MEN-12G; Meteor (1964); MIDPAC; MONS01AR-MONS08AR; MONSOON; MPC-0-1; MPC-0-2; MPC-10-1; MPC-1-1; MPC-11-1; MPC-43K; MPC-45; MSN-100G; MSN-103P; MSN-104P; MSN-109P; MSN-10G; MSN-135P; MSN-136G; MSN-137P; MSN-138P; MSN-141G; MSN-14G; MSN-45G; MSN-52G; MSN-55G; MSN-56PG; MSN-63G; MSN-90G; MSN-93G; mt1-gyre; MT1-gyre; mt1-mid; MT1-mid; mt1-nrsh; MT1-nrsh; MUK-19BP; MUK-20BP; MUK-27HG; NEL-394D; NZO-A106; NZO-A181; NZO-A315; OSIRIS II; OSIRIS III; Pacific Ocean; PAP-127V; PAP-14; PAP-19; PC; Piston corer; PLDS-001G; PLDS-1; Pleiades; PROA; PROA-011P; PROA-079PG; PROA-083PG; PROA-084PG; PROA-085PG-1; PROA-086P; PROA-086PG; PROA-087PG; PROA-088PG; PROA-089PG; PROA-103PG; PROA-118G; PROA-122G; PROA-124G1; PROA-146G; PROA-147G; PROA-149G; PROA-151G; PROA-155G; PROA-156G; PROA-160G; RC0-113; RC0-117; RC0-121; RC08; RC08-102; RC08-103; RC08-145; RC08-16; RC08-18; RC08-22; RC08-23; RC08-27; RC08-28; RC08-39; RC08-40; RC08-41; RC08-46; RC08-50; RC08-53; RC08-60; RC08-61; RC08-62; RC08-63; RC08-94; RC09; RC09-124; RC09-126; RC09-139; RC09-14; RC09-143; RC09-150; RC09-155; RC09-160; RC09-161; RC09-162; RC09-163; RC09-212; RC09-222; RC09-225; RC09-49; RC09-61; RC09-67; RC10; RC10-114; RC10-139; RC10-140; RC10-141; RC10-142; RC10-143; RC10-146; RC10-161; RC10-162; RC10-172; RC10-175; RC10-176; RC10-22; RC10-49; RC10-50; RC10-52; RC10-53; RC10-54; RC10-56; RC10-62; RC10-64; RC10-97; RC11; RC11-10; RC11-103; RC11-106; RC11-11; RC11-111; RC11-116; RC11-117; RC1112; RC11-12; RC11-120; RC11-121; RC11-122; RC11-128; RC11-13; RC11-134; RC11-138; RC11-139; RC11-14; RC11-141; RC11-145; RC11-146; RC11-147; RC11-15; RC11-16; RC11-160; RC11-162; RC11-21; RC11-210; RC11-213; RC11-22; RC11-220; RC11-230; RC11-238; RC11-255; RC11-26; RC11-260; RC11-35; RC11-37; RC11-78; RC11-79; RC11-80; RC11-86; RC11-9; RC12; RC12-107; RC12-121; RC12-138; RC12-139; RC12-143; RC12-146; RC12-233; RC12-234; RC12-235; RC12-241; RC12-266; RC12-268; RC12-291; RC12-292; RC12-293; RC12-294; RC12-297; RC12-298; RC12-299; RC12-300; RC12-303; RC12-304; RC12-328; RC12-33; RC12-330; RC12-331; RC12-332; RC12-333; RC12-335; RC12-339; RC12-340; RC12-341; RC12-342; RC12-343; RC12-344; RC12-347; RC12-350; RC12-361; RC12-365; RC12-366; RC12-417; RC12-418; RC12-45; RC13; RC13-108; RC13-110; RC13-113; RC13-115; RC13-122; RC13-136; RC13-138; RC13-140; RC13-151; RC13-152; RC13-153; RC13-158; RC13-159; RC13-17; RC13-184; RC13-189; RC13-190; RC13-195; RC13-196; RC13-197; RC13-199; RC13-205; RC13-209; RC13-210; RC13-227; RC13-229; RC13-242; RC13-253; RC13-275; RC13-81; RC14; RC14-29; RC14-31; RC14-31TW; RC14-33; RC14-33TW; RC14-34; RC14-34TW; RC14-35; RC14-35TW; RC14-36; RC14-37; RC14-37TW; RC14-39; RC14-39TW; RC14-44; RC14-44TW; RC14-7; RC14-79TW; RC14-9; RC14-92; RC14-93; RC14-94; RC14-97; RC15; RC15-115; RC15-143; RC15-145; RC15-151; RC15-91; RC15-93; RC15-94; RC17; RC17-101; RC17-102; RC17-103; RC17-104; RC17-105; RC17-110; RC17-113; RC17-114; RC17-116; RC17-121; RC17-123; RC17-125; RC17-126; RC17-127; RC17-132; RC17-142; RC17-144; RC17-145; RC17-176; RC17-177; RC17-178; RC17-69; RC17-73; RC17-98; RC18; RC18-47; RC24; RC24-1; RC24-16; RC24-27; RC24-7; RE009-7; RE010-002; RE5-034; RE5-036; RE5-054; RE5-057; RIS-101; RIS-103; RIS-104; RIS-105; RIS-106; RIS-108; RIS-121V; RIS-14; RIS-15G; RIS-17; RIS-17G; RIS-21G; RIS-24; RIS-29G; RIS-32; RIS-33; RIS-34; RIS-35; RIS-51G; Robert Conrad; SCAN; SCAN-015P; SCAN-022PG; SCAN-023PG; SCAN-025G; SCAN-026G; SCAN-027G; SCAN-028G; SCAN-059P; SCAN-065G; SCAN-066G; SCAN-067G; SCAN-068G; SCAN-082P; SCAN-083P; SCAN-084P; SCAN-084PG; SCAN-085P; SCAN-086P; SCAN-087P; SCAN-088P; SCAN-088PG; SCAN-091G; SCAN-094P; SCAN-095G; SCAN-096P; SDS-93P; SDS-95P; SDS-97P; SDS-98P; SOB; SOB-009G; SOB-026GA; SOB-031GA; South Atlantic Ocean; Southern Borderland; South Pacific Ocean; SP008-004; SP009-003; SP010-005; Spencer F. Baird; Stranger; STYX_III; STYX_IX; STYX03AZ; STYX09AZ; STYXIII-75G; STYXIII-77P; STYXIII-80FF-34; STYXIII-81FF-41; STYXIII-81FF-44;

Type: Dataset

Format: application/zip, 14 datasets

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Sea-surface temperature reconstructions for the Quaternary western Atlantic (1999)

Hale, Walter ; Pflaumann, Uwe

PANGAEA

In: Supplement to: Hale, Walter; Pflaumann, Uwe (1999): Sea-surface Temperature Estimations using a Modern Analog Technique with Foraminiferal Assemblages from Western Atlantic Quaternary Sediments. In: Fischer, G & Wefer, G (eds.), Use of Proxies in Paleoceanography - Examples from the South Atlantic, Springer, Berlin, Heidelberg, 69-90

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Publication Date: 2024-07-01

Description: Paleotemperature estimates calculated by the SIMMAX Modern Analog Technique are presented for two gravity cores from the Rio Grande Rise, one from the Brazil Slope, and one from the Ceara Rise. The estimates are based on comparisons between modern and fossil planktonic foraminiferal assemblages and were carried out on samples from Quaternary sediments. Estimated warm-season temperatures from the Rio Grande Rise (at approx. 30° S) range from around 19°C to 24°C, with some coincidence of warm peaks with interglacial stages. The temperature estimates (also warm-season) from the more tropical Brazil Slope (at approx. 8° S) and Ceara Rise (at approx. 4° N) cores are more stable, remaining between 26°C and 28°C throughout most of their lengths. This fairly stable situation in the tropical western Atlantic is interrupted in oxygen isotope stage 6 by a significant drop of 2-3°C in both of these cores. Temperature estimates from the uppermost samples in all cores compare very well to the modern-day measured values. Affinities of some foraminiferal species for warmer or cooler surface temperatures are identified within the temperature range of the examined samples based on their abundance values. Especially notable among the warmer species are, Globorotalia menardii, Globigerinita glutinata, Globigerinoides ruber, and Globigerinoides sacculifer. Species indicative of cooler surface temperatures include Globorotalia inflata, Globigerina bulloides, Neogloboquadrina pachyderma, and Globigerina falconensis. A cluster analysis was carried out to assist in understanding the degree of variation which occurs in the foraminiferal assemblages, and how temperature differences influence the faunal compositions of the samples. It is demonstrated that fairly similar samples may have unexpectedly different estimated temperatures due to small differences in key species and, conversely, quite different assemblages can result in similar or identical temperature estimates which confirms that other parameters than just temperature affect faunal content.

Keywords: 06MT15_2; Amazon Fan; Angola Basin; Argentine Basin; Brazil Basin; Eastern Rio Grande Rise; Equatorial Atlantic; GeoB1007-4; GeoB1105-4; GeoB1309-2; GeoB1312-2; GeoB1523-1; GeoB1701-4; GeoB2109-1; GeoB2204-2; GeoB2819-1; GeoB3808-6; Gravity corer (Kiel type); M15/2; M16/2; M20/2; M23/2; M23/3; M29/2; M34/3; M6/6; M9/4; Meteor (1986); Mid Atlantic Ridge; Niger Sediment Fan; Rio Grande Rise; SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents

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Format: application/zip, 17 datasets

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Physical properties measured on sediment cores from the Southern Ocean, Weddell Sea area (1996)

Villinger, Heinrich

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2024-07-01

Description: This collection of 359 data sets represents raw data of physical properties measurements on Polarstern sediment cores from both polar oceans, sampled and measured between 1985 and 1995.

Keywords: Agulhas Basin; Antarctic Ocean; ANT-II/3; ANT-IV/3; ANT-IV/4; ANT-IX/3; ANT-V/4; ANT-VI/3; ANT-VIII/3; ANT-VIII/5; ANT-VIII/6; ARK-IV/3; ARK-V/3b; ARK-VII/3b; Astrid Ridge; Atka Bay; Atlantic Indik Ridge; Atlantic Ridge; AWI_Paleo; Barents Sea; Camp Norway; Filchner Shelf; Filchner Trough; Fram Strait; Giant box corer; GIK21532-6 PS11/396-6; GIK21532-9 PS11/396-9; GIK21533-3 PS11/412; GIK21730-2 PS13/224; GKG; Gravity corer (Kiel type); Greenland Sea; Greenland Shelf; Greenland Slope; Gunnerus Ridge; Halley Bay; Indian-Antarctic Ridge; Kainan Maru Seamount; KAL; Kapp Norvegia; Kasten corer; KL; Lazarev Sea; Lyddan Island; Maud Rise; Meteor Rise; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; PS04; PS04/256; PS04/259; PS08; PS08/338; PS08/347; PS08/353; PS08/354; PS08/356; PS08/366; PS08/379; PS08/381; PS08/564; PS08/617; PS08/634; PS08/635; PS08/643; PS10; PS10/686; PS10/688; PS10/699; PS11; PS1169-2; PS1172-1; PS12; PS12/242; PS12/244; PS12/247; PS12/248; PS12/250; PS12/252; PS12/280; PS12/284; PS12/291; PS12/302; PS12/327; PS12/336; PS12/338; PS12/340; PS12/344; PS12/348; PS12/350; PS12/352; PS12/492; PS12/536; PS12/545; PS12/549; PS12/551; PS12/553; PS12/555; PS12/557; PS1370-2; PS1375-3; PS1377-2; PS1378-3; PS1380-3; PS1388-3; PS1396-1; PS1398-1; PS13 GRÖKORT; PS1451-1; PS1458-1; PS1461-1; PS1462-1; PS1465-1; PS1478-2; PS1479-2; PS1483-3; PS1532-6; PS1532-9; PS1533-3; PS1572-2; PS1573-1; PS1574-2; PS1575-1; PS1575-2; PS1576-2; PS1577-1; PS1584-1; PS1585-3; PS1588-1; PS1591-1; PS16; PS16/262; PS16/267; PS16/271; PS16/278; PS16/281; PS16/284; PS16/287; PS16/288; PS16/299; PS16/300; PS16/302; PS16/303; PS16/306; PS16/308; PS16/311; PS16/312; PS16/314; PS16/316; PS16/321; PS16/323; PS16/329; PS16/334; PS16/337; PS16/342; PS16/345; PS16/351; PS16/354; PS16/358; PS16/362; PS16/366; PS16/369; PS16/372; PS16/409; PS16/410; PS16/417; PS16/444; PS16/507; PS16/511; PS16/512; PS16/513; PS16/515; PS16/516; PS16/518; PS16/519; PS16/520; PS16/522; PS16/530; PS16/534; PS16/536; PS16/540; PS16/541; PS16/547; PS16/549; PS16/550; PS16/552; PS16/554; PS16/555; PS16/557; PS16/564; PS16/568; PS1603-1; PS1605-1; PS1606-3; PS1607-3; PS1609-3; PS1611-3; PS1612-2; PS1613-4; PS1640-1; PS1648-1; PS1649-2; PS1650-2; PS1651-1; PS1652-2; PS1653-1; PS1654-2; PS17; PS17/239; PS17/241; PS17/242; PS17/243; PS17/244; PS17/245; PS17/247; PS17/248; PS17/249; PS17/250; PS17/251; PS17/257; PS17/258; PS17/262; PS17/264; PS17/265; PS17/272; PS17/274; PS17/276; PS17/281; PS17/285; PS17/286; PS17/287; PS17/288; PS17/289; PS17/290; PS1730-2; PS1750-6; PS1751-7; PS1752-1; PS1754-1; PS1755-6; PS1756-5; PS1757-1; PS1758-1; PS1761-1; PS1762-1; PS1763-1; PS1764-1; PS1765-2; PS1765-3; PS1766-1; PS1767-1; PS1768-8; PS1769-1; PS1770-1; PS1771-1; PS1772-8; PS1773-1; PS1774-5; PS1775-4; PS1776-8; PS1777-6; PS1778-5; PS1779-2; PS1780-5; PS1781-1; PS1782-5; PS1783-5; PS1784-2; PS1786-1; PS1789-1; PS1790-1; PS1793-1; PS1793-2; PS1799-1; PS18; PS18/126; PS1805-6; PS1808-1; PS1809-1; PS1810-1; PS1811-8; PS1812-6; PS1813-6; PS1814-1; PS1815-1; PS1816-1; PS1820-6; PS1821-6; PS1822-6; PS1823-1; PS1823-6; PS1824-1; PS1825-6; PS1826-1; PS1827-1; PS1828-1; PS1829-6; PS1830-1; PS1831-1; PS1835-1; PS1835-2; PS1836-2; PS1836-3; PS1916-1; PS1916-2; PS1918-1; PS1918-2; PS1919-1; PS1919-2; PS1920-1; PS1920-2; PS1921-2; PS1922-1; PS1922-2; PS1923-1; PS1923-2; PS1924-1; PS1924-2; PS1925-1; PS1925-2; PS1926-1; PS1926-2; PS1927-1; PS1927-2; PS1929-2; PS1930-2; PS1932-2; PS1933-1; PS1934-1; PS1934-2; PS1937-2; PS1939-2; PS1941-3; PS1943-1; PS1946-2; PS1947-1; PS1948-2; PS1949-1; PS1949-2; PS1950-2; PS1951-1; PS1951-2; PS1990-2; Quaternary Environment of the Eurasian North; QUEEN; Scoresby Sund; Shona Ridge; SL; South Atlantic Ocean; South Orkney; South Sandwich Basin; South Sandwich Islands; South Sandwich Trough; Svalbard; Van Heesen Ridge; Weddell Sea

Type: Dataset

Format: application/zip, 268 datasets

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Living benthic foraminifers from the central Arctic Ocean (1998)

Wollenburg, Jutta Erika ; Mackensen, Andreas

PANGAEA

In: Supplement to: Wollenburg, Jutta Erika; Mackensen, Andreas (1998): Living benthic foraminifers from the central Arctic Ocean: faunal composition, standing stock and diversity. Marine Micropaleontology, 34(3-4), 153-185, https://doi.org/10.1016/S0377-8398(98)00007-3

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Publication Date: 2024-07-01

Description: Fifty short sediment cores collected with a multiple corer and five box cores from the central Arctic Ocean were analysed to study the ecology and distribution of benthic foraminifers. To work out living faunal associations, standing stock and diversity, separate analyses of living (Rose Bengal stained) and dead foraminifers were carried out for the sediment surface. The size fractions between 63 and 125 µm and 〉125 µm were counted separately to allow comparison with former Arctic studies and with studies from the adjacent Norwegian-Greenland Sea, Barents Sea and the North Atlantic Ocean. Benthic foraminiferal associations are mainly controlled by the availability of food, and competition for food, while water mass characteristics, bottom current activity, substrate composition, and water depth are of minor importance. Off Spitsbergen in seasonally ice-free areas, high primary production rates are reflected by high standing stocks, high diversities, and foraminiferal associations (〉125 µm) that are similar to those of the Norwegian-Greenland Sea. Generally, in seasonally ice-free areas standing stock and diversity increase with increasing food supply. In the central Arctic Ocean, the oligotrophic permanently ice-covered areas are dominated by epibenthic species. The limited food availability is reflected by very low standing stocks and low diversities. Most of these foraminiferal associations do not correspond to those of the Norwegian-Greenland Sea. The dominant associations include simple agglutinated species such as Sorosphaerae, Placopsilinellae, Komokiacea and Aschemonellae, as well as small calcareous species such as Stetsonia horvathi and Epistominella arctica. Those of the foraminiferal species that usually thrive under seasonally ice-free conditions in middle bathyal to lower bathyal water depth are found under permanently ice-covered conditions in water depths about 1000 m shallower, if present at all.

Keywords: Amundsen Basin; ARK-IX/4; ARK-VIII/2; ARK-VIII/3; AWI_Paleo; Barents Sea; Gakkel Ridge, Arctic Ocean; Giant box corer; GKG; Lomonosov Ridge, Arctic Ocean; Makarov Basin; MIC; MiniCorer; Morris Jesup Rise; MUC; MultiCorer; Nansen Basin; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/091; PS19/094; PS19/100; PS19/111; PS19/113; PS19/114; PS19/117; PS19/150; PS19/152; PS19/153; PS19/154; PS19/157; PS19/158; PS19/159; PS19/160; PS19/161; PS19/164; PS19/165; PS19/166; PS19/167; PS19/172; PS19/173; PS19/175; PS19/176; PS19/178; PS19/181; PS19/182; PS19/183; PS19/184; PS19/185; PS19/186; PS19/189; PS19/190; PS19/194; PS19/196; PS19/198; PS19/200; PS19/214; PS19/216; PS19/218; PS19/222; PS19/224; PS19/226; PS19/228; PS19/234; PS19/241; PS19/245; PS19/246; PS19/249; PS19/252; PS19 ARCTIC91; PS19 EPOS II; PS2125-1; PS2125-2; PS2127-1; PS2129-2; PS2137-1; PS2139-1; PS2140-1; PS2143-1; PS2157-3; PS2159-3; PS2160-3; PS2161-1; PS2163-1; PS2164-1; PS2165-5; PS2166-1; PS2167-3; PS2168-3; PS2170-4; PS2171-2; PS2172-3; PS2175-4; PS2176-2; PS2177-3; PS2178-4; PS2179-3; PS2180-1; PS2181-4; PS2182-4; PS2183-3; PS2184-3; PS2185-4; PS2186-3; PS2187-5; PS2190-5; PS2191-1; PS2192-2; PS2193-3; PS2198-4; PS2199-4; PS2200-4; PS2202-4; PS2204-3; PS2205-1; PS2206-4; PS2208-1; PS2210-3; PS2212-6; PS2213-4; PS2214-1; PS2214-4; PS2215-1; PS2445-2; PS2446-2; PS2447-3; PS2448-3; PS27; PS27/019; PS27/020; PS27/024; PS27/025; Quaternary Environment of the Eurasian North; QUEEN; Svalbard; Yermak Plateau

Type: Dataset

Format: application/zip, 5 datasets

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Sedimentation rates and geochemical analysis of surface sediments from the South Atlantic (1997)

Nürnberg, Christine Caroline ; Bohrmann, Gerhard ; Frank, Martin ; [et al.]

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In: Supplement to: Nürnberg, Christine Caroline; Bohrmann, Gerhard; Frank, Martin; Schlüter, Michael (1997): Barium accumulation in the Atlantic sector of the Southern Ocean - Results from 190,000 year records. Paleoceanography, 12(4), 594-603, https://doi.org/10.1029/97PA01130

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Publication Date: 2024-07-01

Description: Extensive investigations of sedimentary barium were performed in the southern South Atlantic in order to assess the reliability of the barium signal in Antarctic sediments as a proxy for paleoproductivity. Maximum accumulation rates of excess barium were calculated for the Antarctic zone south of the polar front where silica accumulates at high rates. The correspondence between barium and opal supports the applicability of barium as a proxy for productivity. Within the Antarctic zone north of today's average sea ice maximum, interglacial vertical rain rates of excess barium are high, with a maximum occurring during the last deglaciation and early Holocene and during oxygen isotope chronozone 5.5. During these periods, the maximum silica accumulation was supposedly located south of the polar front. Glacial paleoproductivity, instead, was low within the Antarctic zone. North of the polar front, significantly higher barium accumulation occurs during glacial times. The vertical rain rates, however, are as high as in the glacial Antarctic zone. Therefore there was no evidence for an increased productivity in the glacial Southern Ocean.

Keywords: Agulhas Basin; Agulhas Ridge; Antarctic Peninsula; ANT-IX/2; ANT-IX/3; ANT-IX/4; ANT-V/4; ANT-VI/3; ANT-VIII/3; ANT-X/4; ANT-X/5; ANT-X/6; ANT-XI/2; Atka Bay; Atlantic Indik Ridge; Atlantic Ridge; AWI_Paleo; Barents Sea; Camp Norway; Cape Basin; CTD/Rosette; CTD-RO; Eastern Weddell Sea, Southern Ocean; Falkland Islands; Filchner Trough; Giant box corer; Giant gravity corer AWI; GKG; Gravity corer (Kiel type); GSL; Halley Bay; Indian-Antarctic Ridge; Islas Orcadas; Kapp Norvegia; KL; Lazarev Sea; Lyddan Island; Maud Rise; Meteor Rise; MG; MIC; MiniCorer; MUC; Multiboxcorer; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; PS10; PS10/668; PS10/672; PS10/673; PS10/675; PS10/678; PS10/684; PS10/686; PS10/690; PS10/699; PS10/701; PS10/703; PS10/707; PS10/711; PS10/719; PS10/725; PS10/738; PS10/757; PS10/762; PS10/766; PS10/778; PS10/782; PS10/784; PS10/804; PS10/816; PS10/818; PS10/820; PS10/824; PS12; PS12/242; PS12/244; PS12/247; PS12/248; PS12/250; PS12/252; PS12/271; PS12/273+276; PS12/280; PS12/284; PS12/287; PS12/289; PS12/300; PS12/302; PS12/305; PS12/310; PS12/312; PS12/319; PS12/336; PS12/338; PS12/344; PS12/348; PS12/352; PS12/364; PS12/366; PS12/374; PS12/380; PS12/382; PS12/458; PS12/486; PS12/490; PS12/492; PS12/526; PS12/534; PS12/545; PS12/551; PS12/553; PS12/555; PS12/557; PS1471-2; PS1472-4; PS1473-1; PS1474-1; PS1475-1; PS1477-1; PS1478-1; PS1480-2; PS1483-2; PS1484-2; PS1485-1; PS1486-2; PS1487-1; PS1488-1; PS1489-3; PS1490-2; PS1493-2; PS1495-1; PS1496-2; PS1498-1; PS1499-2; PS1500-2; PS1502-1; PS1506-2; PS1507-2; PS1508-2; PS1509-2; PS1572-1; PS1573-2; PS1574-1; PS1575-2; PS1576-1; PS1577-2; PS1581-2; PS1582-1; PS1584-2; PS1585-1; PS1586-2; PS1587-1; PS1590-1; PS1591-2; PS1593-1; PS1595-2; PS1596-1; PS1599-1; PS16; PS16/267; PS16/271; PS16/278; PS16/281; PS16/284; PS16/303; PS16/306; PS16/311; PS16/316; PS16/321; PS16/323; PS16/334; PS16/342; PS16/345; PS16/351; PS16/354; PS16/362; PS16/372; PS1605-3; PS1606-1; PS1609-2; PS1611-1; PS1613-2; PS1618-1; PS1619-1; PS1622-1; PS1625-1; PS1626-1; PS1635-2; PS1638-1; PS1639-1; PS1640-3; PS1645-1; PS1647-2; PS1649-1; PS1651-2; PS1652-2; PS1653-2; PS1654-1; PS1751-2; PS1752-5; PS1754-2; PS1755-1; PS1756-5; PS1756-6; PS1764-2; PS1765-1; PS1768-1; PS1768-8; PS1771-4; PS1772-6; PS1772-8; PS1773-2; PS1775-5; PS1777-7; PS1778-1; PS1779-3; PS1780-1; PS1782-6; PS1786-2; PS18; PS18/044; PS18/048; PS18/055; PS18/056; PS18/058; PS18/059; PS18/063; PS18/065; PS18/067; PS18/075; PS18/080; PS18/081; PS18/082; PS18/084; PS18/086; PS18/088; PS18/092; PS18/094; PS18/096; PS18/100; PS18/101; PS18/102; PS18/106; PS18/108; PS18/114; PS18/118; PS18/167; PS18/186; PS18/187; PS18/196; PS18/198; PS18/199; PS18/200; PS18/201; PS18/202; PS18/203; PS18/204; PS18/218; PS18/227; PS18/229; PS18/236; PS18/237; PS18/238; PS18/241; PS18/243; PS18/244; PS18/249; PS18/250; PS18/251; PS18/252; PS18/253; PS18/254; PS18/255; PS18/256; PS18/257; PS18/261; PS18/262; PS18/263; PS18/266; PS18/267; PS18 06AQANTIX_2; PS1953-1; PS1954-1; PS1957-1; PS1958-1; PS1960-1; PS1961-1; PS1963-1; PS1964-1; PS1965-1; PS1967-1; PS1969-1; PS1970-1; PS1971-1; PS1973-1; PS1974-1; PS1975-1; PS1977-1; PS1978-1; PS1979-1; PS1981-1; PS1982-1; PS1983-1; PS1985-1; PS1986-1; PS1987-1; PS1988-1; PS2020-1; PS2039-2; PS2040-1; PS2049-3; PS2050-2; PS2051-3; PS2052-3; PS2053-1; PS2054-2; PS2055-3; PS2056-2; PS2065-1; PS2072-1; PS2073-1; PS2080-1; PS2081-1; PS2082-1; PS2084-2; PS2086-3; PS2087-1; PS2091-1; PS2092-1; PS2093-1; PS2094-1; PS2095-1; PS2096-1; PS2097-1; PS2098-1; PS2099-1; PS2103-2; PS2104-1; PS2105-2; PS21 06AQANTX_4; PS2108-1; PS2109-3; PS22; PS22/280; PS22/678; PS22/679; PS22/690; PS22/712; PS22/714; PS22/717; PS22/718; PS22/721; PS22/722; PS22/727; PS22/730; PS22/737; PS22/744; PS22/747; PS22/748; PS22/751; PS22/755; PS22/758; PS22/764; PS22/769; PS22/773; PS22/776; PS22/780; PS22/783; PS22/786; PS22/790; PS22/791; PS22/797; PS22/802; PS22/803; PS22/804; PS22/805; PS22/806; PS22/810; PS22/811; PS22/812; PS22/813; PS22/814; PS22/815; PS22/816; PS22/818; PS22/823; PS22/825; PS22/826; PS22/828; PS22/829; PS22/830; PS22/832; PS22/833; PS22/834; PS22/835; PS22/837; PS22/838; PS22/840; PS22/841; PS22/842; PS22/846; PS22/849; PS22/850; PS22/851; PS22/852; PS22/853; PS22/855; PS22/857; PS22/860; PS22/872; PS22/876; PS22/879; PS22/886; PS22/891; PS22/899; PS22/902; PS22/908; PS22/911; PS22/917; PS22/941; PS22/947; PS22/956; PS22/973; PS22 06AQANTX_5; PS2230-1; PS2231-1; PS2233-1; PS2234-1; PS2235-1; PS2237-1; PS2238-1; PS2239-1; PS2240-1; PS2241-1; PS2242-1; PS2243-1; PS2244-1; PS2245-1; PS2246-1; PS2247-1; PS2248-1; PS2250-6; PS2251-1; PS2254-1; PS2256-4; PS2257-1; PS2258-1; PS2259-1; PS2260-1; PS2262-7; PS2263-1; PS2265-2; PS2266-1; PS2267-2; PS2268-6; PS2269-5; PS2270-5; PS2271-1; PS2272-1; PS2273-1; PS2275-1; PS2276-2; PS2278-5; PS2280-1; PS2283-6; PS2285-3; PS2288-1; PS2292-1; PS2293-1; PS2299-1; PS2302-2; PS2304-2; PS2305-1; PS2306-1; PS2307-2; PS2308-1; PS2312-1; PS2313-1; PS2314-1; PS2315-1; PS2316-1; PS2317-1; PS2318-1; PS2320-1; PS2325-1; PS2327-1; PS2328-1; PS2329-1; PS2330-1; PS2331-1; PS2333-1; PS2334-1; PS2335-4; PS2336-1; PS2338-1; PS2339-1; PS2341-1; PS2342-1; PS2343-1; PS2347-1; PS2350-1; PS2351-1; PS2352-1; PS2353-2; PS2354-1; PS2355-1; PS2356-1; PS2357-2; PS2361-1; PS2362-1; PS2363-1; PS2364-1; PS2365-2; PS2366-1; PS2367-1; PS2368-4; PS2369-4; PS2370-4; PS2371-1; PS2372-1; PS2374-2; PS2376-1; PS2487-2; PS2488-1; PS2489-4; PS2489-7; PS2491-5; PS2492-1; PS2493-3; PS2494-1; PS2498-2; PS2499-1; PS2501-4; PS2502-1; PS2503-1; PS2505-2; PS2506-1; PS2507-1; PS2508-1; PS2509-2; PS2511-3; PS2512-1; PS2513-1; PS2514-3; PS2515-2; PS2516-1; PS2517-5; PS2518-2; PS2519-1; PS2520-1; PS28; PS28/236; PS28/243; PS28/256; PS28/264; PS28/277; PS28/280; PS28/289; PS28/304; PS28/314; PS28/329; PS28/334; PS28/337; PS28/342; PS28/345; PS28/347; PS28/350; PS28/352; PS28/361; PS28/367; PS28/373; PS28/375; PS28/378; PS28/385; PS28/390; PS28/395; PS28/404; PS28/408; Scotia Sea, southwest Atlantic; Shona Ridge; SL; South Atlantic; South Atlantic Ocean; South Orkney; South Sandwich; South Sandwich Basin; South Sandwich Trough; van Veen Grab; Vestkapp; VGRAB; Weddell Sea; Wegener Canyon

Type: Dataset

Format: application/zip, 5 datasets

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