ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Oxford University Press  (34,067)
  • International Union of Crystallography  (13,434)
  • PANGAEA
  • 1995-1999  (51,828)
  • 1950-1954  (4,168)
Collection
Keywords
Publisher
Years
Year
  • 101
    Publication Date: 2024-07-01
    Keywords: Amazon Fan; Angola Diapir Field; Brazil Basin; Calcium carbonate; Calculated, see reference(s); Carbon, organic, total; Congo Fan; DEPTH, sediment/rock; East Brazil Basin; Element analyser CHN; Element analyser CHN, LECO; Elevation of event; Equatorial Atlantic; Event label; Fragmentation index, planktic foraminifera; GeoB; GeoB1000-1; GeoB1001-2; GeoB1005-2; GeoB1006-2; GeoB1007-2; GeoB1008-6; GeoB1009-3; GeoB1010-3; GeoB1011-2; GeoB1012-1; GeoB1013-2; GeoB1014-2; GeoB1015-2; GeoB1016-2; GeoB1017-3; GeoB1039-1; GeoB1040-3; GeoB1041-1; GeoB1043-2; GeoB1044-3; GeoB1048-2; GeoB1101-4; GeoB1102-3; GeoB1103-3; GeoB1104-5; GeoB1105-3; GeoB1106-5; GeoB1108-6; GeoB1109-4; GeoB1110-3; GeoB1111-5; GeoB1112-3; GeoB1113-7; GeoB1114-3; GeoB1115-4; GeoB1116-1; GeoB1117-3; GeoB1118-2; GeoB1119-2; GeoB1120-3; GeoB1401-1; GeoB1403-2; GeoB1405-7; GeoB1405-8; GeoB1407-7; GeoB1421-1; GeoB1501-1; GeoB1503-2; GeoB1504-1; GeoB1505-3; GeoB1506-1; GeoB1508-1; GeoB1509-2; GeoB1510-1; GeoB1511-6; GeoB1512-2; GeoB1513-2; GeoB1514-4; GeoB1515-2; GeoB1516-1; GeoB1517-2; GeoB1518-1; GeoB1519-2; GeoB1520-1; GeoB1521-2; GeoB1522-1; GeoB1523-2; GeoB1606-7; GeoB1607-8; GeoB1608-9; GeoB1609-9; GeoB1612-9; GeoB1613-10; GeoB1701-1; GeoB1702-6; GeoB1901-1; GeoB1902-3; GeoB1903-1; GeoB2201-1; GeoB2202-5; GeoB2204-1; GeoB2205-4; GeoB2206-1; GeoB2207-2; GeoB2208-1; GeoB2212-1; GeoB2213-1; GeoB2215-8; GeoB2216-2; GeoB2301-1; GeoB2302-1; GeoB2303-1; GeoB2304-1; GeoB2305-1; GeoB2306-1; Geosciences, University of Bremen; Giant box corer; GIK17836-1; GIK17843-1; GKG; Guinea Basin; Kongo delta; Latitude of event; Longitude of event; M16/1; M16/2; M20/1; M20/2; M23/3; M6/6; M9/4; Meteor (1986); Mid Atlantic Ridge; MUC; MultiCorer; Northern Guinea Basin; PROBOSWA; Romanche fracture zone; SFB261; SO84; SO86; Sonne; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Southwest Guinea Basin; ST. HELENA HOTSPOT; Walvis Ridge
    Type: Dataset
    Format: text/tab-separated-values, 113 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 102
    Publication Date: 2024-07-01
    Keywords: Age model; Age model, lithological correlation; Antarctic Peninsula; ANT-VI/2; AWI_Paleo; DEPTH, sediment/rock; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS12; PS12/201; PS1565-2; SL
    Type: Dataset
    Format: text/tab-separated-values, 5 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 103
    Publication Date: 2024-07-01
    Keywords: AGE; ARK-VIII/3; Counting 〉63 µm fraction; DEPTH, sediment/rock; Foraminifera, planktic indeterminata; Giant box corer; GKG; Lomonosov Ridge, Arctic Ocean; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; Polarstern; PS19/186; PS19 ARCTIC91; PS2185-3; Quaternary Environment of the Eurasian North; QUEEN
    Type: Dataset
    Format: text/tab-separated-values, 57 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 104
    Publication Date: 2024-07-01
    Keywords: Arctic Ocean; ARK-XI/1; AWI_Paleo; Density, dry bulk; Density, wet bulk; DEPTH, sediment/rock; KAL; Kasten corer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2757-8; PS36; PS36/052; Quaternary Environment of the Eurasian North; QUEEN; Shear strength, remanent; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 340 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 105
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Alexandrova, Olga A; Shevchenko, Vladimir P; Fahl, Kirsten; Stein, Ruediger (1999): The lipid composition of particulate matter from the transitional zone between Kara and Laptev Seas. In: Stein, R; Fahl, K; Ivanov, G I; Levitan, M A; Tarasov, G (eds.), Modern and Late Quaternary depositional environment of the St. Anna Trough area, northern Kara Sea, Reports on Polar Research, 244 pp, 342, 93-102, hdl:10013/epic.10345.d001
    Publication Date: 2024-07-01
    Description: The lipid composition of particulate matter in oceanic environments can provide informations on the nature and origin of the organic matter as well as on their transformation processes. Molecular characteristics for lipids in the Arctic environment have been used as indicators of the sources and transformation of organic particulate matter (Smith et al., 1997; Fahl and Stein, 1997, 1999). However, the features of the lipid composition of particulate matter in the Arctic with its high seasonality of ice Cover and primary productivity has been studied insufficiently. Lipids are one of the most important compounds of organic matter. On the one hand, the composition of lipids is a result of the variability of biological sources (phyto- and zooplankton, higher plants, bacteria etc.). On the other hand, the lipid composition of particulate matter is undergone significant alteration during vertical transport. The organic matter balance in the Arctic marginal seas, such as the Kara and Laptev seas, is characterized by the significant supply of dissolved and particulate material by the major Eurasian rivers - Ob, Yenisei and Lena (Cauwet and Sidorov, 1996; Gordeev et al., 1996, Martin et al., 1993). In relation to the world's ocean the primary productivity values are lower in the Arctic seas due to the ice-cover. However local increased values of primary productivity can be connected with the melting processes inducing increased phytoplankton growth near ice-edge (Nelson et al., 1989; Fahl and Stein, 1997) and enhanced river supply of nutrients, These features can influence the proportion of allochtonous and autochtonous components of the organic matter in the Arctic marginal seas (Fahl and Stein, 1997; Stein and Fahl, 1999). Furthermore, increased lipid contents in aquatic environments were found near density discontinuities (Parish et al., 1988). Although being less informative than lipid studies on the molecular level the character of lipid composition analysis on the group could also be used for studying of particulate organic matter and its transformation in sedimentation processes in the Arctic. In this paper the investigation of the characteristics of lipid composition performed by Alexandrova and Shevchenko (1997) in Arctic seas was continued.
    Keywords: Arctic Ocean; ARK-XI/1; AWI_Paleo; Chromatographic; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Fatty acid esters; Fatty acids; Hydrocarbons; Kara Sea; Latitude of event; Lipids; Lipids, polar; Longitude of event; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS36; PS36/088-1; PS36/089-1; PS36/091-1; PS36/092-1; PS36/094-1; PS36/095-1; PS36/096-1; Quaternary Environment of the Eurasian North; QUEEN; Sterol esters; Triacylglycerols; Wax esters
    Type: Dataset
    Format: text/tab-separated-values, 191 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 106
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wahsner, Monika; Müller, Claudia; Stein, Ruediger; Ivanov, Gennadiy I; Levitan, Mikhail A; Shelekhova, E S; Tarasov, Gennadiy A (1999): Clay-mineral distribution in surface sediments of the Eurasian Arctic Ocean and continental margin as indicator for source areas and transport pathways - a synthesis. Boreas, 28(1), 215-233, https://doi.org/10.1111/j.1502-3885.1999.tb00216.x
    Publication Date: 2024-07-01
    Description: Clay-mineral distributions in the Arctic Ocean and the adjacent Eurasian shelf areas are discussed to identify source areas and transport pathways of terrigenous material in the Arctic Ocean. The main clay minerals in Eurasian Arctic Ocean sediments are illite and chlorite. Smectite and kaolinite occur in minor amounts in these sediments, but show strong variations in the shelf areas. These two minerals are therefore reliable in reconstructions of source areas of sediments from the Eurasian Arctic. The Kara Sea and the western part of the Laptev Sea are enriched in smectite, with highest values of up to 70% in the deltas of the Ob and Yenisey rivers. Illite is the dominant clay mineral in all the investigated sediments except for parts of the Kara Sea. The highest concentrations with more than 70% illite occur in the East Siberian Sea and around Svalbard. Chlorite represents the clay mineral with lowest concentration changes in the Eastern Arctic, ranging between 10 and 25%. The main source areas for kaolinite in the Eurasian Arctic are Mesozoic sedimentary rocks on Franz-Josef Land islands. Based on clay-mineral data, transport of the clay fraction via sea ice is of minor importance for the modern sedimentary budget in the Arctic basins.
    Keywords: 41; 42; 4381-1; 4387-1; 4397-1; 4399-1; 4403-1; 4404-1; 4405-1; 4411-1; 4413-1; 4414-1; 4416-1; 4418-1; AG80; AG80/10-1; AG80/1-1; AG80/11-1; AG80/12-1; AG80/13-1; AG80/14-1; AG80/15-1; AG80/16-1; AG80/17-1; AG80/2-1; AG80/3-1; AG80/4-1; AG80/5-1; AG80/6-1; AG80/7-1; AG80/8-1; AG80/9-1; Akademik Golitsyn; Amundsen Basin; Arctic Ocean; ARK-IV/3; ARK-IX/4; ARK-VIII/2; ARK-VIII/3; ARK-XI/1; AWI_Paleo; Barents Sea; BC; BCR; Bear Island Trough; Box corer; Box corer (Reineck); Calculated; Chlorite; Chuk17; Chuk181; Chuk183; Chuk184; Chuk186; Chuk189; Chuk201; Chuk21; Chuk223; Chuk226; Chuk30; Chuk49; Chuk50; Chuk53; Chuk56; Chuk8; Chuk9; CTD/Rosette; CTD-RO; DEPTH, sediment/rock; DM49; Dmitry Mendeleev; East Siberian Sea; Elevation of event; ES281; ES282; ES284; ES285; ES286; ES288; ES289; ES290; ES291; ES292; ES293; ES295; ES314; ES315; ES316; ES317; ES318; ES320; ES323; ES326; Event label; Fram Strait; Franz Joseph Land/St. Anna Trough; Gakkel Ridge, Arctic Ocean; Giant box corer; Giant piston corer; GIK21520-10 PS11/310-10; GIK21521-13 PS11/340-13; GIK21522-19 PS11/358-19; GIK21523-14 PS11/362-14; GIK21524-1 PS11/364-1; GIK21525-2 PS11/365-2; GIK21526-5 PS11/370-5; GIK21527-18 PS11/371-18; GIK21528-7 PS11/372-7; GIK21529-7 PS11/376-7; GIK21530-3 PS11/382-3; GIK21532-1 PS11/396-1; GIK21534-6 PS11/423-6; GIK21535-5 PS11/430-5; GKG; GPC; Gravity corer (Kiel type); Gravity corer (Russian type); Illite; Jenissei; KAL; KAL_R; Kaolinite; Kaolinite/Chlorite ratio; Kara Sea; Kara Sea/St. Anna Trough; Kasten corer; Kasten corer RUS; Laptev Sea; Laptev Sea, Taymyr Island; LATITUDE; Lomonosov Ridge, Arctic Ocean; LONGITUDE; Makarov Basin; Men4376-1; Men4377-1; Men4378-1; Men4379-1; Men4380-1; Men4381-1; Men4382-1; Men4383-1; Men4384-1; Men4385-1; Men4386-1; Men4387-1; Men4390-1; Men4391-1; Men4394-1; Men4395-1; Men4397-1; Men4398-1; Men4399-1; Men4400-1; Men4401-1; Men4402-1; Men4403-1; Men4404-1; Men4405-1; Men4406-1; Men4409-1; Men4410-1; Men4411-1; Men4413-1; Men4414-1; Men4416-1; Men4417-1; Men4418-1; Mooring (long time); MOORY; Morris Jesup Rise; MUC; MULT; MultiCorer; Multiple investigations; Nansen Basin; Ob; OD-006-06; OD-007-02; OD-008-05; OD-009-08; OD-010-06; OD-011-03; OD-017-01; OD-024-06; OD-025-05; OD-026-09; OD-027-03; OD-031-03; OD-032-04; OD-035-02; OD-036-04; OD-041-04; OD-042-01; Oden; ODEN-96; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; PL-1994; PL94-01; PL94-02; PL94-03; PL94-04; PL94-05; PL94-07; PL94-08; PL94-09; PL94-10; PL94-11; PL94-12; PL94-13; PL94-16; PL94-18; PL94-19; PL94-20; PL94-22; PL94-23; PL94-25; PL94-26; PL94-28; PL94-30; PL94-31; PL94-32; PL94-34; PL94-35; PL94-37; PL94-38; PL94-39; PL94-40; PL94-41; PL94-42; PL94-44; PL94-46; PL94-50; PL94-51; PL94-53; PL94-54; PL94-55; PL94-56; PL94-57; PL94-58; PL94-60; PL94-62; PL94-63; PL94-64; PL94-65; PL94-67; PL94-68; PL94-70; Polarstern; Professor Logachev; PS11; PS11/269-12; PS1511-12; PS1520-10; PS1521-13; PS1522-19; PS1523-14; PS1524-1; PS1525-2; PS1526-5; PS1527-18; PS1528-7; PS1529-7; PS1530-3; PS1532-1; PS1534-6; PS1535-5; PS19/040; PS19/045; PS19/050; PS19/055; PS19/070; PS19/078; PS19/080; PS19/081; PS19/082; PS19/084; PS19/086; PS19/090; PS19/091; PS19/094; PS19/098; PS19/100; PS19/101; PS19/102; PS19/104; PS19/105; PS19/108; PS19/110; PS19/111; PS19/112; PS19/116; PS19/117; PS19/119; PS19/124; PS19/126; PS19/132; PS19/134; PS19/136; PS19/143; PS19/148; PS19/150; PS19/151; PS19/152; PS19/153; PS19/155; PS19/157; PS19/158; PS19/159; PS19/160; PS19/161; PS19/164; PS19/165; PS19/166; PS19/167; PS19/171; 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; PS19/192; PS19/194; PS19/198; PS19/200; PS19/204; PS19/206; PS19/210; PS19/214; PS19/216; PS19/218; PS19/222; PS19/226; PS19/239; PS19/241; PS19/245; PS19/246; PS19/249; PS19/252; PS19 ARCTIC91; PS19 EPOS II; PS2111-2; PS2113-1; PS2114-1; PS2115-1; PS2116-1; PS2117-1; PS2119-2; PS2120-1; PS2121-1; PS2122-1; PS2123-3; PS2124-1; PS2125-2; PS2127-1; PS2128-1; PS2129-2; PS2130-2; PS2131-1; PS2132-3; PS2133-1; PS2134-1; PS2136-3; PS2137-4; PS2138-2; PS2142-3; PS2143-1; PS2144-3; PS2147-3; PS2148-1; PS2149-1; PS2150-1; PS2151-1; PS2153-1; PS2156-1; PS2157-1; PS2158-1; PS2159-6; PS2160-1; PS2162-1; PS2163-1; PS2164-6; PS2165-1; PS2166-3; PS2167-1; PS2168-1; PS2170-1; PS2171-1; PS2172-1; PS2174-1; PS2175-5; PS2176-4; PS2177-1; PS2178-1; PS2179-3; PS2180-1; PS2181-4; PS2182-1; PS2183-4; PS2184-1; PS2185-7; PS2186-1; PS2187-5; PS2189-1; PS2190-5; PS2192-3; PS2193-1; PS2194-1; PS2195-1; PS2196-2; PS2198-4; PS2199-1; PS2200-6; PS2202-11; PS2205-3; PS2209-3; PS2210-1; PS2212-1; PS2213-6; PS2214-1; PS2215-4; PS2439-1; PS2440-5; PS2441-1; PS2442-1; PS2443-3; PS2444-1; PS2445-4; PS2446-1; PS2447-5; PS2448-1; PS2449-3; PS2450-2; PS2451-2; PS2452-2; PS2453-2; PS2455-3; PS2456-2; PS2457-1; PS2458-3; PS2459-2; PS2460-3; PS2461-2; PS2462-3; PS2463-3; PS2466-3; PS2467-3; PS2468-3; PS2469-3; PS2470-4; PS2471-3; PS2472-3; PS2473-3; PS2474-2; PS2475-1; PS2476-3; PS2477-3; PS2478-3; PS2481-2; PS2482-3; PS2483-2; PS2484-2; PS2486-2; PS27; PS27/001; PS27/006; PS27/007; PS27/014; PS27/016; PS27/017; PS27/019; PS27/020; PS27/024; PS27/025; PS27/027; PS27/028; PS27/029; PS27/030; PS27/031; PS27/033; PS27/034; PS27/035; PS27/038; PS27/039; PS27/040; PS27/041; PS27/043; PS27/044; PS27/048; PS27/049; PS27/050; PS27/052; PS27/053; PS27/054; PS27/056; PS27/058; PS27/059; PS27/060; PS27/062; PS27/064; PS27/065; PS27/068; PS27/069; PS27/070; PS27/071; PS27/073; PS2718-6; PS2721-6; PS2722-1; PS2723-4; PS2724-4; PS2725-5; PS2726-1; PS2727-7; PS2728-2; PS2729-6; PS2730-3; PS2740-1; PS2741-1; PS2742-3; PS2744-6; PS2745-7; PS2749-3; PS2750-1; PS2752-1; PS2753-1; PS2755-1; PS2756-1; PS2757-8; PS2758-1; PS2759-1; PS2760-6; PS2761-1; PS2762-6; PS2763-1; PS2764-8; PS2765-1; PS2767-1; PS2768-4; PS2773-1; PS2774-2; PS2775-1; PS2778-2; PS2779-1; PS2780-6; PS2781-1; PS2787-1; PS2791-1; PS2792-6; PS36; PS36/002; PS36/004; PS36/006; PS36/007; PS36/008; PS36/009; PS36/010; PS36/011; PS36/012; PS36/016; PS36/017; PS36/027; PS36/028; PS36/030; PS36/032; PS36/033; PS36/044; PS36/045; PS36/047; PS36/048a; PS36/050; PS36/051LOMO-2; PS36/052; PS36/053; PS36/055; PS36/056; PS36/057; PS36/059; PS36/060; PS36/062; PS36/064; PS36/066; PS36/067; PS36/075; PS36/076; PS36/079; PS36/082; PS36/083; PS36/084; PS36/085; PS36/091; PS36/095; PS36/096; Quaternary Environment of the Eurasian North; QUEEN; RGC; RUS_unspec; SL; Smectite; Smectite/Illite ratio; SPASIBAIII; Svalbard; van Veen Grab; VGRAB; Vilkitsky Strait; Water sample; WS; X-ray diffraction TEXTUR, clay fraction; Yermak Plateau
    Type: Dataset
    Format: text/tab-separated-values, 2010 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 107
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: DEPTH, sediment/rock; GeoB; GeoB1120-2; Geosciences, University of Bremen; Gravity corer (Kiel type); Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; M9/4; Meteor (1986); Romanche fracture zone; SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 108
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Ito, Takashi; Usui, Akira; Kajiwara, Yoshimichi; Nakano, Takanori (1998): Strontium isotopic compositions and paleoceanographic implication of fossil manganese nodules in DSDP/ODP cores, Leg 1-126. Geochimica et Cosmochimica Acta, 62(9), 1545-1554, https://doi.org/10.1016/S0016-7037(98)00051-9
    Publication Date: 2024-07-01
    Description: Strontium isotopic compositions of acetic acid (HOAc) leachate fractions of eight manganese oxide deposits from the modern seafloor, and of twenty-one buried manganese nodules from Cretaceous to Recent sediments in DSDP/ODP cores were measured. ratios of HOAc leachates in all modern seafloor manganese oxides of various origins are identical with present seawater. The ratios of the HOAc leachates of buried nodules from DSDP/ODP cores are significantly lower than those of nodules from the modern seafloor and are mostly identical with coeval seawater values estimated from the age of associated sediments. It is suggested that the buried nodules in DSDP/ODP cores are not artifacts transported from the present seafloor during the drilling process, but are in situ fossil deposits from the past deep-sea floor during Cretaceous to Quaternary periods. The formation of deep-sea fossil nodules prior to the formation of Antarctic Bottom Water (AABW) indicates that the circulation of oxygenated deep seawaters have activately deposited manganese oxides since the Eocene Epoch, or earlier.
    Keywords: 108-661A; 114-699A; 122-760A; 15-150; 32-303; 36-328; 5-37; 62-464; 81-554A; 86-578; 93-603B; Caribbean Sea/BASIN; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epoch; Event label; Glomar Challenger; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Interval comments; Iron; Joides Resolution; Latitude of event; Leg108; Leg114; Leg122; Leg15; Leg32; Leg36; Leg5; Leg62; Leg81; Leg86; Leg93; Longitude of event; Manganese; Mass spectrometer Finnigan MAT 262 RPQ Plus; Minerals; North Atlantic/PLATEAU; North Pacific; North Pacific/BASIN; North Pacific/CONT RISE; North Pacific/HILL; Rubidium; Sample code/label; Sample code/label 2; South Atlantic/BASIN; South Atlantic Ocean; South Indian Ridge, South Indian Ocean; Strontium; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error
    Type: Dataset
    Format: text/tab-separated-values, 257 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 109
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Peucker-Ehrenbrink, Bernhard; Ravizza, Gregory E; Hofmann, Albrecht W (1995): The marine 187Os/186Os record of the past 80 million years. Earth and Planetary Science Letters, 130(1-4), 155-167, https://doi.org/10.1016/0012-821X(95)00003-U
    Publication Date: 2024-07-01
    Description: We report new 187Os/186Os data and Re and Os concentrations in metalliferous sediments from the Pacific to construct a composite Os isotope seawater evolution curve over the past 80 m.y. Analyses of four samples of upper Cretaceous age yield 187Os/186Os values of between 3 and 6.5 and 187Re/186Os values below 55. Mass balance calculations indicate that the pronounced minimum of about 2 in the Os isotope ratio of seawater at the K-T boundary probably reflects the enormous input of cosmogenic material into the oceans by the K-T impactor(s). Following a rapid recovery to 187Os/186Os of 3.5 at 63 Ma, data for the early and middle part of the Cenozoic show an increase in 187Os/186Os to about 6 at 15 Ma. Variations in the isotopic composition of leachable Os from slowly accumulating metalliferous sediments show large fluctuations over short time spans. In contrast, analyses of rapidly accumulating metalliferous carbonates do not exhibit the large oscillations observed in the pelagic clay leach data. These results together with sediment leaching experiments indicate that dissolution of non-hydrogenous Os can occur during the hydrogen peroxide leach and demonstrate that Os data from pelagic clay leachates do not always reflect the Os isotopic composition of seawater. New data for the late Cenozoic further substantiate the rapid increase in the 187Os/186Os of seawater during the past 15 Ma. We interpret the correlation between the marine Sr and Os isotope records during this time period as evidence that weathering within the drainage basin of the Ganges-Brahmaputra river system is responsible for driving seawater Sr and Os toward more radiogenic isotopic compositions. The positive correlation between 87Sr/86Sr and U concentration, the covariation of U and Re concentrations, and the high dissolved Re, U and Sr concentrations found in the Ganges-Brahmaputra river waters supports this interpretation. Accelerating uplift of many orogens worldwide over the past 15 Ma, especially during the last 5 Ma, could have contributed to the rapid increase in 187Os/186Os from 6 to 8.5 over the past 15 Ma. Prior to 15 Ma the marine Sr and Os record are not tightly coupled. The heterogeneous distribution of different lithologies within eroding terrains may play an important role in decoupling the supplies of radiogenic Os and Sr to the oceans and account for the periods of decoupling of the marine Sr and Os isotope records.
    Keywords: 129-801A; 16-162; 20-196; 34-319; 35-323; 5-39; 8-74; 91-596; 92-597; 9-77B; AGE; Antarctic Ocean/PLAIN; Calculated; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Inductively coupled plasma - mass spectrometry (ICP-MS); Joides Resolution; Latitude of event; Leg129; Leg16; Leg20; Leg34; Leg35; Leg5; Leg8; Leg9; Leg91; Leg92; Longitude of event; North Pacific/ABYSSAL FLOOR; North Pacific/CONT RISE; North Pacific/HILL; North Pacific Ocean; Ocean Drilling Program; ODP; Osmium; Osmium-187/Osmium-186, error; Osmium-187/Osmium-186 ratio; Osmium-187/Osmium-188, error; Osmium-187/Osmium-188 ratio; Rhenium; Rhenium-187/Osmium-186 ratio; Sample code/label; Sample comment; South Pacific; South Pacific/BASIN; Thermal Ionization Mass Spectrometry (TIMS)
    Type: Dataset
    Format: text/tab-separated-values, 321 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 110
    Publication Date: 2024-07-01
    Keywords: 06MT41_3; Angola Basin; DEPTH, sediment/rock; GeoB; GeoB5121-2; Geosciences, University of Bremen; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; M41/3; Mass spectrometer Finnigan MAT 251; Meteor (1986); MUC; MultiCorer
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 111
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; ARK-IV/3; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK21524-2 PS11/364-2; Isotopic event; KAL; Kasten corer; Polarstern; PS11; PS1524-2; Ratio; Svalbard; Thorium-230 excess, depositional, flux; Thorium-230 excess, depositional, flux, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 112
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; ARK-IV/3; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK21521-15 PS11/340-15; Isotopic event; KAL; Kasten corer; Nansen Basin; Polarstern; PS11; PS1521-15; Ratio; Thorium-230 excess, depositional, flux; Thorium-230 excess, depositional, flux, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 113
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; Antarctic Ocean; ARK-IV/3; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK21533-3 PS11/412; Gravity corer (Kiel type); Isotopic event; Polarstern; PS11; PS1533-3; Ratio; SL; Thorium-230 excess, depositional, flux; Thorium-230 excess, depositional, flux, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 114
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; Arctic Ocean; ARK-XI/1; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Isotopic event; KAL; Kasten corer; Polarstern; PS2757-8; PS36; PS36/052; Ratio; Thorium-230 excess, depositional, flux; Thorium-230 excess, depositional, flux, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 78 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 115
    Publication Date: 2024-07-01
    Keywords: ARK-IX/4; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Gravity corer (Kiel type); Laptev Sea; Polarstern; PS2471-4; PS27; PS27/054; SL; Thorium-230; Thorium-230, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 374 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 116
    Publication Date: 2024-07-01
    Keywords: ARK-IX/4; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; KAL; Kasten corer; Laptev Sea; Polarstern; PS2474-3; PS27; PS27/059; Thorium-230; Thorium-230, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 196 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 117
    Publication Date: 2024-07-01
    Keywords: Agassiz Trawl; AGT; Arctic Ocean; ARK-VIII/2; Barents Sea; Bottom trawl; BT; Date/Time of event; Date/Time of event 2; Elevation of event; Elevation of event 2; EPOS; European Polarstern Study; Event label; Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; Method/Device of event; North Greenland Sea; Norwegian Sea; Polarstern; PS19/040-2; PS19/042-1; PS19/045-2; PS19/050-2; PS19/055-2; PS19/070-2; PS19/076-2; PS19/077-2; PS19/078-2; PS19/082-2; PS19/084-2; PS19/086-2; PS19/090-3; PS19/100-2; PS19/101-2; PS19/104-2; PS19/105-2; PS19/107-2; PS19/108-2; PS19/112-2; PS19/119A-1; PS19/125-1; PS19/134-2; PS19/136-2; PS19/141-2; PS19 EPOS II; South Atlantic Ocean; Station label; Topography
    Type: Dataset
    Format: text/tab-separated-values, 50 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 118
    Publication Date: 2024-07-01
    Keywords: Abietinaria abietina; Acanthostepheia sp.; Aceroides latipes; Acryptolaria borealis; Admete viridula; Agassiz Trawl; Aglaophamus sp.; AGT; Alcyonidium gelatinosum anderssoni; Alcyonidium mamillatum; Alcyonidium radicellatum; Allantactis parasitica; Amathillopsis spinosa; Ampelisca eschrichti; Ampharete sp.; Amphianthus aff. margaritaceus; Amphicteis gunneri; Amphicteis sundevalli; Amphilochus sp.; Amphitrite cirrata; Amphiura sundevalli; Anarhichas minor; Anisarchus medius; Anomalosipho altus; Anonyx nugax; Apomatus globifer; Arctic Ocean; Arctinula greenlandicus; ARK-VIII/2; Artacama proboscidea; Artediellus atlanticus; Ascidiacea sp.; Astarte acuticostata; Astarte borealis placenta; Astarte crenata crenata; Astarte montagui striata; Austrosyrrhoe fimbriatus; Balanus balanus; Barents Sea; Bathyarca glacialis; Bathyarca pectunculoides; Bathybiaster vexillifer; Bathycrinus carpenterii; Bathypolypus arcticus; Bispira sp.; Boreogadus saida; Boreonymphon abyssorum; Boreonymphon ossiansarsi; Boreotrophon truncatus; Bottom trawl; Brada cf. villosa; Brada inhabilis; BT; Buccinum hydrophanum; Buccinum nivale; Byblis gaimardi; Byblis longicornis; Bythocaris leucopis; Cactosoma abyssorum; Calathura brachiata; Careproctus reinhardti; Careproctus spp.; Caulophacus arcticus; Cellepora canaliculata; Cellepora nodulosa; Cellepora pumicosa; Ceramaster granularis; Chitonidae sp.; Chlamys islandica; Ciliatocardium ciliatum; Cladorhiza gelida; Cleippides quadricuspis; Colossendeis angusta; Colossendeis proboscidea; Colus islandicus; Colus latericeus; Colus sabini; Colus turgidulus; Cottunculus microps; Cribrilina watersi; Crisia eburneo-denticulata; Crisiella sp.; Cryptonatica clausa; Ctenodiscus crispatus; Cucumaria cf. frondosa; Curtitoma trevelliana; Cuspidaria arctica; Cuspidaria subtorta; Cyclopecten imbrifer; Cylichna sp.; Cystisella saccata; Dacrydium vitreum; Date/Time of event; Date/Time of event 2; Defrancia lucernaria; Diastylis goodsiri; Diastylis lepechini; Diastylis spinulosa; Diplosolen intricarius; Diplosolen obelia arctica; Disporella hispida; Dulichia macera; Edwardsia sp.; Ekmania sp.; Elevation of event; Elevation of event 2; Elpidia glacialis; Epimeria loricata; Epizoanthus incrustatus; EPOS; Escharoides jacksoni; Eucratea loricata; Eudendrium capillare; Eudendrium ramosum; Eumicrotremus spinosus; Eupyrgus scaber; European Polarstern Study; Eusirus cuspidatus; Eusirus longipes; Event label; Frigidoalvania janmayeni; Gadus morhua; Gattyana cirrosa; Geodia sp.; Glandulactis spetsbergensis; Glyphanostomum sp.; Gnathia stygia; Gorgonocephalus spp.; Grammaria abietina; Gymnelus retrodorsalis; Gymnocanthus tricuspis; Halecium beanii; Halecium labrosum; Halecium muricatum; Haploops cf. sibirica; Haploops tubicola; Harmothoe (Eunoe) nodosa; Heliometra glacialis; Henricia spp.; Hiatella arctica; Hippasteria phrygiana; Hippoglossoides platessoides; Hippoglossus hippoglossus; Hormathia digitata; Hormathia nodosa; Hornera lichenoides; Hyas sp.; Hydractinia carica; Hymenaster pellucidus; Hymenodora glacialis; Icasterias panopla; Icelus bicornis; Idmidronea atlantica gracillima; Idunella cf. aequicornis; Ischyrocerus sp.; Kadosactis rosea; Kinetoskias smitti; Korethraster hispidus; Lafoea dumosa; Lafoea grandis; Laonice cf. sarsi; Laonice spirata; Latitude of event; Latitude of event 2; Lebbeus polaris; Leionucula belloti; Leionucula corticata; Lepeta coeca; Lepidepecreum umbo; Leptagonus decagonus; Leptasterias sp.; Leptoclinus maculatus; Leptychaster arcticus; Lichenopora verrucaria; Liljeborgia fissicornis; Liljeborgia sp.; Liparis fabricii; Liparis gibbus; Liponema multicornis; Lissodendoryx spp.; Longitude of event; Longitude of event 2; Lophaster furcifer; Lumbrineris fragilis; Lumbrineris sp.; Lumpenus lampretaeformis; Lunatia pallida; Lycenchelys kolthoffi; Lycodes esmarkii; Lycodes eudipleurostictus; Lycodes frigidus; Lycodes pallidus; Lycodes reticulatus; Lycodes rossi; Lycodes seminudus; Lycodes squamiventer; Lycodes vahlii gracilis; Lycodonus flagellicauda; Lycodonus sp.; Macandrevia cranium; Macoma calcarea; Macrourus berglax; Maldane sarsi; Mallotus villosus; Margarites costalis sordida; Margarites sp.; Melanogrammus aeglefinus; Melinna cristata; Melinnopsis arctica; Melita dentata; Method/Device of event; Metopa cf. borealis; Modeeria plicatile; Modeeria rotunda; Mohnia parva; Molpadia sp.; Munnopsurus giganteus; Musculus niger; Mya truncata; Myriapora coarctata; Myriapora subgracilis; Myriochele sp.; Myriotrochus rinkii; Neoamphitrite affinis; Neohela monstrosa; Nephtys caeca; Nereis zonata; Nicomache lumbricalis; Nolella dilatata; North Greenland Sea; Norwegian Sea; Notoplites sibirica; Nuculana pernula; Nymphon cf. gracile; Nymphon elegans; Nymphon grossipes; Nymphon hirtipes; Nymphon sluiteri; Nymphon stroemi; Oenopota cinerea; Oenopota pyramidalis; Onchidiopsis sp.; Onogadus argentatus; Onuphis conchylega; Ophelia cf. rathkei; Ophelina acuminata; Ophiacantha bidentata; Ophiocten sericeum; Ophiopholis aculeata; Ophiopleura borealis; Ophiopus arcticus; Ophioscolex glacialis; Ophiura robusta; Ophiura sarsi; Owenia fusiformis; Pagurus pubescens; Palmicellaria skenei bicornis; Pandalus borealis; Panomya arctica; Paraliparis bathybius; Paramphithoe hystrix; Parasmittina jeffreysi; Pardaliscidae; Parerythrops spectabilis; Pasiphaea tarda; Phascolion strombi; Pherusa plumosa; Phoxocephalidae sp.; Phylactella labiata; Phyllodoce groenlandica; Pista maculata; Podoceridae sp.; Polarstern; Poliometra prolixa; Polycirrus medusa; Polymastia mamillaris; Pontaster tenuispinus; Poraniomorpha bidens; Poraniomorpha hispida; Poraniomorpha tumida; Porella minuta; Pourtalesia sp.; Priapulus bicaudatus; Prionospio cf. malmgreni; Protula tubularia; PS19/040-2; PS19/042-1; PS19/045-2; PS19/050-2; PS19/055-2; PS19/070-2; PS19/076-2; PS19/077-2; PS19/078-2; PS19/082-2; PS19/084-2; PS19/086-2; PS19/090-3; PS19/100-2; PS19/101-2; PS19/104-2; PS19/105-2; PS19/107-2; PS19/108-2; PS19/112-2; PS19/119A-1; PS19/125-1; PS19/134-2; PS19/136-2; PS19/141-2; PS19 EPOS II; Pseudoflustra birulai; Pseudoflustra hincksi; Pseudoflustra sinuosa; Pseudoflustra solida; Pseudomma roseum; Psolus sp.; Pteraster obscurus; Ptychogastria polaris; Pycnanthus densus; Radiella sol; Ragionula rosacea; Raja hyperborea; Raja radiata; Reinhardtius hippoglossoides; Retepora beaniana; Rhachotropis aculeata; Rhizocaulus verticillatus; Rozinante fragilis; Sabellidae sp.; Sabinea septemcarinata; Saduria megalura; Saduria sabini; Sagartia splendens; Sample code/label; Sarsiflustra abyssicola; Scalpellum sp.; Sclerocrangon cf. boreas; Sclerocrangon ferox; Sebastes mentella; Securiflustra securifrons; Serpulidae sp.; Sertularella tenella; Sertularia tenera; Siphonodentalium lobatum; Smittina glaciata; Socarnes bidenticulatus; Solaster spp.; South Atlantic Ocean; Spiochaetopterus typicus; Spirontocaris spinus; Staurophora mertensii; Stegocephalopsis ampulla; Stegocephalus inflatus; Stomphia coccinea; Strongylocentrotus pallidus; Tachyrhynchus erosus; Tealia felina lofotensis; Tentorium semisuberites; Terebellidae sp.; Terebratulina retusa; Tetilla polyura; Thelepus cincinnatus; Thracia myopsis; Tiron spiniferum; Tmetonyx cicada; Tremaster mirabilis; Tricellaria gracilis; Tricellaria ternata; Trichobranchidae sp.; Triglops murrayi; Triglops nybelini; Tubulipora fruticosa; Turrisipho voeringi; Umbellula encrinus; Unciola cf. planipes; Unciola leucopis; Urasterias lincki; Velutina sp.; Volutopsius norwegicus; Yoldia hyperborea; Yoldiella intermedia; Yoldiella lenticula; Yoldiella lucida; Zygophylax pinnatus
    Type: Dataset
    Format: text/tab-separated-values, 8425 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 119
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; ARK-VIII/3; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Isotopic event; KAL; Kasten corer; Makarov Basin; Polarstern; PS19/176; PS19 ARCTIC91; PS2178-5
    Type: Dataset
    Format: text/tab-separated-values, 49 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 120
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; ARK-IX/4; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Gravity corer (Kiel type); Isotopic event; Laptev Sea; Polarstern; PS2471-4; PS27; PS27/054; Ratio; SL; Thorium-230 excess, depositional, flux; Thorium-230 excess, depositional, flux, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 121
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; ARK-VIII/3; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Isotopic event; KAL; Kasten corer; Lomonosov Ridge, Arctic Ocean; Polarstern; PS19/186; PS19 ARCTIC91; PS2185-6
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 122
    Publication Date: 2024-07-01
    Keywords: Age, maximum/old; Age, minimum/young; ARK-IX/4; Beryllium-10, depositional, flux; Beryllium-10, depositional, flux, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Isotopic event; KAL; Kasten corer; Laptev Sea; Polarstern; PS2456-3; PS27; PS27/034; Ratio; Thorium-230 excess, depositional, flux; Thorium-230 excess, depositional, flux, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 39 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 123
    Publication Date: 2024-07-01
    Keywords: ARK-VIII/3; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; KAL; Kasten corer; Morris Jesup Rise; Polarstern; PS19/218; PS19 ARCTIC91; PS2200-5; Thorium-230; Thorium-230, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 380 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 124
    Publication Date: 2024-07-01
    Keywords: ARK-IX/4; Beryllium-10; Beryllium-10, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Gravity corer (Kiel type); Laptev Sea; Polarstern; PS2471-4; PS27; PS27/054; SL
    Type: Dataset
    Format: text/tab-separated-values, 224 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 125
    Publication Date: 2024-07-01
    Keywords: ARK-VIII/3; Beryllium-10; Beryllium-10, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; KAL; Kasten corer; Lomonosov Ridge, Arctic Ocean; Polarstern; PS19/186; PS19 ARCTIC91; PS2185-6
    Type: Dataset
    Format: text/tab-separated-values, 444 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 126
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hulth, Stefan; Hall, Per; Blackburn, T H; Landén, A (1996): Arctic sediments (Svalbard): pore water and solid phase distributions of C, N, P and Si. Polar Biology, 16(6), 447-462, https://doi.org/10.1007/BF02390426
    Publication Date: 2024-07-01
    Description: Pore water and solid phase distributions of C, N, P and Si in sediments of the Arctic Ocean (Svalbard area) have been investigated. Concentrations of organic carbon (Corg) in the solid phase of the sediment varied from 1.3 to 2.8% (mean 1.9%), with highest concentrations found at shallow stations south/southwest of Svalbard. Relatively low concentrations were obtained at the deeper stations north/northeast of Svalbard. Atomic carbon to nitrogen ratios in the surface sediment ranged from below 8 to above 10. For some stations, high C/N ratios together with high concentrations of Corg suggest that sedimentary organic matter is mainly of terrigenous origin and not from overall biological activity in the water column. Organic matter reactivity (defined as the total sediment oxygen consumption rate normalized to the organic carbon content of the surface sediment) correlated with water depth at all investigated stations. However, the stations could be divided into two separate groups with different reactivity characteristics, representing the two most dominant hydrographic regimes: the region west of Svalbard mainly influenced by the West Spitsbergen Current, and the area east of Svalbard where Arctic polar water set the environmental conditions. Decreasing sediment reactivity with water depth was confirmed by the partitioning between organic and inorganic carbon of the surface sediment. The ratio between organic and inorganic carbon at the sediment-water interface decreased exponentially with water depth: from indefinite values at shallow stations in the central Barents Sea, to approximately 1 at deep stations north of Svalbard. At stations east of Svalbard there was an inverse linear correlation between the organic matter reactivity (as defined above) and concentration of dissolved organic carbon (DOC) in the pore water. The more reactive the sediment, the less DOC existed in the pore water and the more total carbonate (Ct or Sum CO2) was present. This observation suggests that DOC produced in reactive sediments is easily metabolizable to CO2. Sediment accumulation rates of opaline silica ranged from 0.35 to 5.7 µmol SiO2 m**-2 d**-1 (mean 1.3 µmol SiO2 m**-2d**-1), i.e. almost 300 times lower than rates previously reported for the Ross Sea, Antarctica. Concentrations of ammonium and nitrate in the pore water at the sediment-water interface were related to organic matter input and water depth. In shallow regions with highly reactive organic matter, a pool of ammonium was present in the pore water, while nitrate conoentrations were low. In areas where less reactive organic matter was deposited at the sediment surface, the deeper zone of nitrification caused a build-up of nitrate in the pore water while ammonium was almost depleted. Nitrate penetrated from 1.8 to 〉= 5.8 cm into the investigated sediments. Significantly higher concentrations of 'total' dissolved nitrogen (defined as the sum of NO3, NO2, NH4 and urea) in sediment pore water were found west compared to east of Svalbard. The differences in organic matter reactivity, as well as in pore water distribution patterns of 'total' dissolved nitrogen between the two areas, probably reflect hydrographic factors (such as ice coverage and production/import of particulate organic material) related to the dominant water mass (Atlantic or Arctic Polar) in each of the two areas.
    Keywords: ARK-VIII/2; AWI; AWI_Paleo; Barents Sea; Giant box corer; GKG; MUC; MULT; MultiCorer; Multiple investigations; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/040; PS19/045; PS19/050; PS19/055; PS19/078; PS19/082; PS19/084; PS19/086; PS19/098; PS19/100; PS19/101; PS19/105; PS19/108; PS19/112; PS19/119; PS19/134; PS19/143; PS19/146; PS19 EPOS II; PS2111-2; PS2113-2; PS2114-2; PS2115-1; PS2117-1; PS2121-3; PS2122-1; PS2123-4; PS2128-1; PS2129-3; PS2130-2; PS2133-1; PS2134-1; PS2138-5; PS2144-3; PS2150-1; PS2153-1; PS2154-1; Silicon Cycling in the World Ocean; SINOPS; Svalbard; Yermak Plateau
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 127
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Petschick, Rainer; Kuhn, Gerhard; Gingele, Franz (1996): Clay mineral distribution in surface sediments of the South Atlantic: sources, transport, and relation to oceanography. Marine Geology, 130(3-4), 203-229, https://doi.org/10.1016/0025-3227(95)00148-4
    Publication Date: 2024-07-01
    Description: Surface samples, mostly from abyssal sediments of the South Atlantic, from parts of the equatorial Atlantic, and of the Antarctic Ocean, were investigated for clay content and clay mineral composition. Maps of relative clay mineral content were compiled, which improve previous maps by showing more details, especially at high latitudes. Large-scale relations regarding the origin and transport paths of detrital clay are revealed. High smectite concentrations are observed in abyssal regions, primarily derived from southernmost South America and from minor sources in Southwest Africa. Near submarine volcanoes of the Antarctic Ocean (South Sandwich, Bouvet Island) smectite contents exhibit distinct maxima, which is ascribed to the weathering of altered basalts and volcanic glasses. The illite distribution can be subdivided into five major zones including two maxima revealing both South African and Antarctic sources. A particularly high amount of Mg- and Fe-rich illites are observed close to East Antarctica. They are derived from biotite-bearing crystalline rocks and transported to the west by the East Antarctic Coastal Current. Chiorite and well-crystallized dioctaedral illite are typical minerals enriched within the Subantarctic and Polarfrontal-Zone but of minor importance off East Antarctica. Kaolinite dominates the clay mineral assemblage at low latitudes, where the continental source rocks (West Africa, Brazil) are mainly affected by intensive chemical weathering. Surprisingly, a slight increase of kaolinite is observed in the Enderby Basin and near the Filchner-Ronne Ice shelf. The investigated area can be subdivided into ten, large-scale clay facies zones with characteristic possible source regions and transport paths. Clay mineral assemblages of the largest part of the South Atlantic, especially of the western basins are dominated by chlorite and illite derived from the Antarctic Peninsula and southernmost South America and supported by advection within the Circumantarctic Deep Water flow. In contrast, the East Antarctic provinces are relatively small. Assemblages of the eastern basins north of 30°S are strongly influenced by African sources, controlled by weathering regimes on land and by a complex interaction of wind, river and deep ocean transport. The strong gradient in clay mineral composition at the Brazilian slope indicate a relatively low contribution of tropically derived assemblages to the western basins.
    Keywords: 06MT15_2; Adelaide Island; Agulhas Basin; Agulhas Ridge; Amazon Fan; Angola Basin; Antarctic Peninsula; ANTARTIDA8611; ANT-I/2; ANT-II/3; ANT-II/4; ANT-III/3; ANT-IV/2; ANT-IV/3; ANT-IV/4; ANT-IX/2; ANT-IX/3; ANT-IX/4; ANT-V/4; ANT-VI/2; ANT-VI/3; ANT-VIII/3; ANT-VIII/5; ANT-VIII/6; ANT-X/2; ANT-X/4; ANT-X/5; ANT-X/6; ANT-XI/2; ANT-XI/4; ANT-XII/4; Anvers Island; Argentine Basin; Argentine Islands; Astrid Ridge; Atka Bay; Atlantic Indik Ridge; Atlantic Ridge; AWI_Paleo; Barents Sea; BC; Box corer; Bransfield Strait; Brazil Basin; Camp Norway; Cape Basin; Cape Blanc; Cape Fiske; Congo Fan; Conrad Rise; Cosmonauts Sea; CTD/Rosette; CTD-RO; D-DCP-1; D-EL-1; DGS-13; DGS-14; DGS-15; DGS-16; DGS-18; Discovery Seamount; D-ORC-013; D-ORC-015; D-ORC-017; D-ORC-023; D-ORC-024; D-ORC-025; D-PA-1; Drake Passage; Dredge; DRG; D-ST-1B; D-ST-2; D-ST-3; D-ST-4; East Brazil Basin; Eastern Rio Grande Rise; Eastern Weddell Sea, Southern Ocean; EL-443; EL-444; EL-445; EL-446; EL-447; EL-448; EL-449; Equatorial Atlantic; Falkland Islands; Filchner Shelf; Filchner Trough; Fram Strait; GeoB1000-1; GeoB1000-2; GeoB1001-1; GeoB1001-2; GeoB1004-2; GeoB1004-3; GeoB1005-2; GeoB1005-3; GeoB1006-2; GeoB1006-3; GeoB1007-2; GeoB1007-3; GeoB1008-6; GeoB1010-3; GeoB1011-2; GeoB1012-1; GeoB1012-2; GeoB1013-2; GeoB1013-3; GeoB1014-2; GeoB1015-2; GeoB1016-2; GeoB1019-2; GeoB1019-3; GeoB1020-1; GeoB1021-3; GeoB1022-2; GeoB1022-3; GeoB1023-2; GeoB1024-3; GeoB1025-2; GeoB1026-3; GeoB1027-2; GeoB1028-4; GeoB1029-1; GeoB1031-1; GeoB1032-2; GeoB1033-3; GeoB1034-1; GeoB1035-3; GeoB1036-3; GeoB1037-1; GeoB1037-2; GeoB1039-1; GeoB1040-3; GeoB1041-1; GeoB1043-2; GeoB1044-3; GeoB1046-2; GeoB1048-2; GeoB1101-4; GeoB1102-3; GeoB1103-3; GeoB1104-5; GeoB1105-3; GeoB1106-5; GeoB1108-6; GeoB1109-4; GeoB1110-3; GeoB1111-5; GeoB1112-3; GeoB1113-7; GeoB1114-3; GeoB1115-4; GeoB1116-1; GeoB1117-3; GeoB1118-2; GeoB1119-2; GeoB1120-3; GeoB1121-1; GeoB1122-2; GeoB1203-2; GeoB1204-3; GeoB1205-2; GeoB1206-1; GeoB1207-2; GeoB1208-1; GeoB1209-1; GeoB1210-3; GeoB1211-1; GeoB1212-2; GeoB1213-2; GeoB1215-1; GeoB1216-2; GeoB1217-1; GeoB1218-1; GeoB1220-2; GeoB1306-1; GeoB1307-2; GeoB1308-1; GeoB1309-3; GeoB1310-1; GeoB1313-1; GeoB1314-1; GeoB1401-1; GeoB1403-2; GeoB1405-7; GeoB1407-7; GeoB1413-2; GeoB1414-2; GeoB1415-1; GeoB1417-2; GeoB1418-1; GeoB1419-1; GeoB1420-1; GeoB1421-1; GeoB1501-3; GeoB1503-2; GeoB1504-1; GeoB1505-3; GeoB1506-1; GeoB1508-1; GeoB1509-2; GeoB1510-1; GeoB1511-6; GeoB1512-2; GeoB1513-2; GeoB1514-4; GeoB1515-2; GeoB1516-1; GeoB1517-1; GeoB1518-1; GeoB1519-2; GeoB1520-1; GeoB1521-2; GeoB1522-1; GeoB1523-2; GeoB1601-6; GeoB1613-1; GeoB1701-1; GeoB1702-6; GeoB1703-5; GeoB1704-1; GeoB1705-2; GeoB1706-1; GeoB1707-2; GeoB1709-3; GeoB1710-2; GeoB1711-5; GeoB1712-2; GeoB1713-6; GeoB1714-1; GeoB1715-1; GeoB1716-2; GeoB1717-2; GeoB1718-1; GeoB1719-5; GeoB1720-4; GeoB1721-4; GeoB1722-3; GeoB1724-3; GeoB1725-1; GeoB1726-1; GeoB1726-2; GeoB1728-3; GeoB1729-1; GeoB1901-1; GeoB1902-3; GeoB1903-1; GeoB1904-1; GeoB1905-1; GeoB1906-1; GeoB1907-1; GeoB1908-1; GeoB2002-2; GeoB2004-1; GeoB2007-1; GeoB2008-1; GeoB2009-1; GeoB2010-1; GeoB2011-1; GeoB2016-3; GeoB2018-1; GeoB2019-2; GeoB2021-4; GeoB2022-3; GeoB2101-1; GeoB2102-1; GeoB2104-1; GeoB2105-3; GeoB2106-1; GeoB2107-5; GeoB2108-1; GeoB2109-3; GeoB2110-1; GeoB2111-2; GeoB2112-1; GeoB2113-1; GeoB2116-2; GeoB2117-4; GeoB2118-1; GeoB2119-2; GeoB2120-1; GeoB2121-1; GeoB2122-1; GeoB2123-1; GeoB2124-1; GeoB2125-2; GeoB2126-1; GeoB2127-1; GeoB2128-1; GeoB2130-1; GeoB2201-1; GeoB2202-5; GeoB2204-1; GeoB2205-4; GeoB2206-1; GeoB2207-2; GeoB2208-1; GeoB2212-1; GeoB2213-1; GeoB2214-2; GeoB2215-8; GeoB2216-2; GeoB2701-2; GeoB2703-6; GeoB2704-1; GeoB2705-7; GeoB2706-6; GeoB2708-5; GeoB2712-1; GeoB2714-5; GeoB2715-1; GeoB2717-8; GeoB2718-1; GeoB2719-1; GeoB2721-2; GeoB2722-1; GeoB2722-2; GeoB2723-1; GeoB2724-6; GeoB2725-1; GeoB2726-3; GeoB2727-1; GeoB2729-1; GeoB2730-1; GeoB2731-1; GeoB2801-1; GeoB2802-1; GeoB2803-1; GeoB2804-2; GeoB2805-1; GeoB2806-6; GeoB2808-3; GeoB2809-2; GeoB2810-2; GeoB2811-1; GeoB2813-1; GeoB2814-3; GeoB2817-3; GeoB2822-3; GeoB2824-1; GeoB2825-3; GeoB2826-1; GeoB2828-1; GeoB2829-3; GeoB2903-1; GeoB2904-11; GeoB2905-1; GeoB2906-3; GeoB2907-1; GeoB2908-8; GeoB2909-1; GeoB2911-2; GeoB2912-1; Giant box corer; GIK17836-1; GIK17843-1; GIK17851-1; GIK17862-1; GIK17866-1; GIK17884-1; GIK17912-1; GKG; Gould Bay; Gravity corer (Kiel type); Greenland Slope; GS-051; GS-053; GS-060; GS-061; GS-073; GS-074; GS-076; GS-083; GS-103; GS-105; GS-136; GS-139; GS-140; GS-142; GS-152; Guinea Basin; Halley Bay; Hope Bay; Hunter Channel; Indian-Antarctic Ridge; Islas Orcadas; Kapp Norvegia; King George Island, Antarctic Peninsula; KL; Kongo delta; Lazarev Sea; Lyddan Island; M12/1; M15/2; M16/1; M16/2; M20/1; M20/2; M23/1; M23/2; M23/3; M29/1; M29/2; M29/3; M6/6; M9/4; Maud Rise; Meteor (1986); Meteor Rise; MG; MIC; Mid Atlantic Ridge; MiniCorer; Mooring (long time); MOORY; MSN; MUC; Multiboxcorer; MultiCorer; Multiple opening/closing net; Namibia Continental Margin; Namibia continental slope; Northern Brasil-Basin; Northern Guinea Basin; Nuevo Alcocero; off Cape Blanc; off Gran Canaria; off Kunene; ORC-301; ORC-312; ORC-313; ORC-329; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); PLA; Plankton net; Polarstern; Polarstern Kuppe; PS01; PS01/154; PS01/155; PS01/156; PS01/161; PS01/162; PS01/168; PS01/177; PS01/184; PS01/186; PS01/189; PS04; PS04/225; PS04/254; PS04/257; PS04/260; PS04/262; PS04/266; PS04/271; PS04/273; PS04/318; PS04/334; PS04/335; PS04/340; PS04/346; PS04/351; PS04/357; PS04/367; PS04/370; PS04/380; PS04/382; PS04/389; PS04/414; PS04/423; PS04/429; PS04/433; PS04/440; PS04/447; PS04/449; PS04/472; PS04/477; PS04/481; PS04/484; PS04/495; PS04/500; PS04/508; PS04/509; PS04/540; PS06/288; PS06/289; PS06/301; PS06/302; PS06/303; PS06/304; PS06/306; PS06/311; PS06/313; PS06 SIBEX; PS08; PS08/284; PS08/289; PS08/321; PS08/324; PS08/327; PS08/333; PS08/335; PS08/336; PS08/338; PS08/340; PS08/344; PS08/345; PS08/346; PS08/347; PS08/350; PS08/353; PS08/354; PS08/355; PS08/356; PS08/357; PS08/358; PS08/359; PS08/360; PS08/361; PS08/364; PS08/365; PS08/366; PS08/367; PS08/368; PS08/369; PS08/374; PS08/375; PS08/379; PS08/380; PS08/381; PS08/382; PS08/384; PS08/385; PS08/386; PS08/387; PS08/394; PS08/396; PS08/401; PS08/402; PS08/410; PS08/428; PS08/430; PS08/432; PS08/438; PS08/439; PS08/440; PS08/442; PS08/445; PS08/449; PS08/450; PS08/452; PS08/480; PS08/481; PS08/482; PS08/483; PS08/504; PS08/507; PS08/509; PS08/529; PS08/533; PS08/564; PS08/585; PS08/601; PS08/607; PS08/610; PS08/621; PS08/627; PS10; PS10/668; PS10/672; PS10/673; PS10/675; PS10/678; PS10/682; PS10/684; PS10/686; PS10/688; PS10/690; PS10/694; PS10/697; PS10/699; PS10/701; PS10/703; PS10/707; PS10/711; PS10/719; PS10/725; PS10/738; PS10/740; PS10/748; PS10/757; PS10/760; PS10/762; PS10/766; PS10/768; PS10/778; PS10/782; PS10/784; PS10/794; PS10/804; PS10/809; PS10/813; PS10/816; PS10/818; PS10/820; PS10/824; PS1010-1; PS1011-1; PS1012-1; PS1013-1; PS1014-1; PS1015-1; PS1016-1; PS1017-1; PS1018-1; PS1019-1; PS1138-8; PS1167-5; PS1170-4; PS1173-6; PS1175-1; PS1179-1; PS1184-6; PS1186-3; PS1194-1; PS1196-1; PS1197-1; PS1198-1; PS1199-1; PS12; PS12/116; PS12/117; PS12/119; PS12/122; PS12/127; PS12/128; PS12/129; PS12/130; PS12/132; PS12/133; PS12/185; PS12/186; PS12/193; PS12/194; PS12/195; PS12/196; PS12/199; PS12/200; PS12/238; PS12/242; PS12/244; PS12/247; PS12/248; PS12/250; PS12/252; PS12/260; PS12/266; PS12/271; PS12/273+276; PS12/280; PS12/284; PS12/287; PS12/289; PS12/291; PS12/298; PS12/300; PS12/302; PS12/305; PS12/308; PS12/310; PS12/312; PS12/314; PS12/316; PS12/319; PS12/321; PS12/323; PS12/325; PS12/327; PS12/333; PS12/336; PS12/338; PS12/340; PS12/342; PS12/344; PS12/346; PS12/348; PS12/350; PS12/352; PS12/354; PS12/356; PS12/358; PS12/360; PS12/364; PS12/366; PS12/368; PS12/372; PS12/374; PS12/376; PS12/378; PS12/380; PS12/382; PS12/384; PS12/387;
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 128
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Diekmann, Bernhard; Kuhn, Gerhard (1999): Provenance and dispersal of glacial-marine surface sediments in the Weddell Sea and adjoining areas, Antarctica: ice-rafting versus current transport. Marine Geology, 158(1-4), 209-231, https://doi.org/10.1016/S0025-3227(98)00165-0
    Publication Date: 2024-07-01
    Description: Mineralogical and granulometric properties of glacial-marine surface sediments of the Weddell Sea and adjoining areas were studied in order to decipher spatial variations of provenance and transport paths of terrigenous detritus from Antarctic sources. The silt fraction shows marked spatial differences in quartz contents. In the sand fractions heavy-mineral assemblages display low mineralogical maturity and are dominated by garnet, green hornblende, and various types of clinopyroxene. Cluster analysis yields distinct heavy-mineral assemblages, which can be attributed to specific source rocks of the Antarctic hinterland. The configuration of modern mineralogical provinces in the near-shore regions reflects the geological variety of the adjacent hinterland. In the distal parts of the study area, sand-sized heavy minerals are good tracers of ice-rafting. Granulometric characteristics and the distribution of heavy-mineral provinces reflect maxima of relative and absolute accumulation of ice-rafted detritus in accordance with major iceberg drift tracks in the course of the Weddell Gyre. Fine-grained and coarse-grained sediment fractions may have different origins. In the central Weddell Sea, coarse ice-rafted detritus basically derives from East Antarctic sources, while the fine-fraction is discharged from weak permanent bottom currents and/or episodic turbidity currents and shows affinities to southern Weddell Sea sources. Winnowing of quartz-rich sediments through intense bottom water formation in the southern Weddell Sea provides muddy suspensions enriched in quartz. The influence of quartz-rich suspensions moving within the Weddell Gyre contour current can be traced as far as the continental slope in the northwestern Weddell Sea. In general, the focusing of mud by currents significantly exceeds the relative and absolute contribution of ice-rafted detritus beyond the shelves of the study area.
    Keywords: Adelaide Island; Antarctic Peninsula; ANTARTIDA8611; ANT-I/2; ANT-II/3; ANT-II/4; ANT-III/3; ANT-IV/2; ANT-IV/3; ANT-IV/4; ANT-IX/2; ANT-IX/3; ANT-V/4; ANT-VI/2; ANT-VI/3; ANT-VIII/5; ANT-VIII/6; ANT-X/2; ANT-X/4; ANT-X/5; ANT-X/6; ANT-XI/2; ANT-XI/4; ANT-XIV/3; Anvers Island; Argentine Islands; Astrid Ridge; Atka Bay; AWI_Paleo; Barents Sea; BC; Box corer; Bransfield Strait; Camp Norway; Cape Fiske; Cosmonauts Sea; CTD/Rosette; CTD-RO; D-EL-1; D-ORC-011; D-ORC-013; D-ORC-015; D-ORC-017; D-ORC-023; D-ORC-024; D-ORC-025; D-ORC-142; D-PA-1; Drake Passage; Dredge; DRG; D-ST-2; D-ST-3; D-ST-4; Eastern Weddell Sea, Southern Ocean; EL-443; EL-444; EL-445; EL-446; EL-447; EL-448; EL-449; Filchner Shelf; Filchner Trough; Fram Strait; Giant box corer; GKG; Gould Bay; Gravity corer (Kiel type); Greenland Slope; GS-053; GS-076; GS-152; Halley Bay; Hope Bay; Islas Orcadas; Kapp Norvegia; King George Island, Antarctic Peninsula; KL; Lazarev Sea; Lyddan Island; Maud Rise; MG; MIC; MiniCorer; MUC; Multiboxcorer; MultiCorer; Nuevo Alcocero; ORC-301; ORC-312; ORC-313; ORC-329; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; Polarstern Kuppe; PS01; PS01/154; PS01/155; PS01/156; PS01/161; PS01/162; PS01/177; PS01/184; PS01/186; PS01/189; PS04; PS04/225; PS04/254; PS04/256; PS04/257; PS04/258; PS04/260; PS04/261; PS04/262; PS04/263; PS04/264; PS04/265; PS04/266; PS04/271; PS04/273; PS04/318; PS04/334; PS04/335; PS04/340; PS04/346; PS04/351; PS04/357; PS04/367; PS04/370; PS04/380; PS04/382; PS04/389; PS04/414; PS04/423; PS04/429; PS04/433; PS04/440; PS04/447; PS04/449; PS04/472; PS04/477; PS04/481; PS04/484; PS04/495; PS04/500; PS04/508; PS04/509; PS06/288; PS06/289; PS06/301; PS06/302; PS06/303; PS06/304; PS06/306; PS06/311; PS06/313; PS06 SIBEX; PS08; PS08/284; PS08/289; PS08/321; PS08/324; PS08/327; PS08/333; PS08/335; PS08/336; PS08/338; PS08/340; PS08/344; PS08/345; PS08/346; PS08/347; PS08/350; PS08/353; PS08/354; PS08/355; PS08/356; PS08/357; PS08/358; PS08/359; PS08/360; PS08/361; PS08/364; PS08/365; PS08/366; PS08/367; PS08/368; PS08/369; PS08/374; PS08/375; PS08/379; PS08/380; PS08/381; PS08/382; PS08/384; PS08/385; PS08/386; PS08/387; PS08/394; PS08/396; PS08/397; PS08/401; PS08/402; PS08/410; PS08/428; PS08/430; PS08/432; PS08/438; PS08/439; PS08/440; PS08/442; PS08/445; PS08/449; PS08/450; PS08/452; PS08/480; PS08/481; PS08/482; PS08/483; PS08/564; PS08/585; PS08/601; PS08/607; PS08/610; PS08/621; PS08/627; PS10; PS10/668; PS10/672; PS10/673; PS10/675; PS10/678; PS10/682; PS10/684; PS10/686; PS10/688; PS10/690; PS10/694; PS10/697; PS10/699; PS10/701; PS10/703; PS10/707; PS10/711; PS10/719; PS10/725; PS10/738; PS10/740; PS10/748; PS10/757; PS10/760; PS10/762; PS10/766; PS10/768; PS10/778; PS10/782; PS10/784; PS10/794; PS10/804; PS10/813; PS10/816; PS10/818; PS10/820; PS10/824; PS1010-1; PS1011-1; PS1012-1; PS1013-1; PS1014-1; PS1016-1; PS1017-1; PS1018-1; PS1019-1; PS1138-8; PS1167-5; PS1169-1; PS1170-4; PS1171-1; PS1173-6; PS1174-2; PS1175-1; PS1176-3; PS1177-1; PS1178-4; PS1179-1; PS1184-6; PS1186-3; PS1194-1; PS1196-1; PS1197-1; PS1198-1; PS1199-1; PS12; PS12/116; PS12/117; PS12/119; PS12/122; PS12/127; PS12/128; PS12/129; PS12/130; PS12/132; PS12/133; PS12/185; PS12/186; PS12/193; PS12/194; PS12/195; PS12/196; PS12/199; PS12/200; PS12/238; PS12/242; PS12/244; PS12/247; PS12/248; PS12/250; PS12/252; PS12/260; PS12/266; PS12/271; PS12/273+276; PS12/280; PS12/284; PS12/287; PS12/289; PS12/291; PS12/298; PS12/300; PS12/302; PS12/305; PS12/308; PS12/310; PS12/312; PS12/314; PS12/316; PS12/319; PS12/321; PS12/323; PS12/325; PS12/327; PS12/333; PS12/336; PS12/338; PS12/340; PS12/342; PS12/344; PS12/346; PS12/348; PS12/350; PS12/352; PS12/354; PS12/356; PS12/358; PS12/360; PS12/364; PS12/366; PS12/368; PS12/372; PS12/374; PS12/376; PS12/378; PS12/380; PS12/382; PS12/384; PS12/387; PS12/396; PS12/418; PS12/437; PS12/458; PS12/465; PS12/472; PS12/486; PS12/490; PS12/492; PS12/503; PS12/504; PS12/510; PS12/526; PS12/534; PS12/536; PS1200-4; PS1201-1; PS1202-1; PS1203-1; PS1204-1; PS1205-1; PS1206-1; PS1207-1; PS1207-2; PS1208-1; PS1209-1; PS1210-1; PS1211-1; PS1212-1; PS1213-1; PS1214-1; PS1215-1; PS1216-1; PS1217-1; PS1219-1; PS1220-3; PS1222-1; PS1223-1; PS1272-1; PS1273-1; PS1275-1; PS1276-1; PS1277-1; PS1278-1; PS1279-1; PS1281-1; PS1282-1; PS1333-2; PS1338-1; PS1363-3; PS1364-1; PS1366-2; PS1367-1; PS1368-1; PS1369-1; PS1370-1; PS1371-1; PS1372-2; PS1373-2; PS1374-2; PS1375-2; PS1376-2; PS1377-1; PS1378-1; PS1379-1; PS1380-1; PS1381-1; PS1382-1; PS1383-1; PS1384-1; PS1385-1; PS1386-1; PS1387-1; PS1388-1; PS1389-1; PS1390-1; PS1391-1; PS1394-1; PS1395-1; PS1396-1; PS1397-1; PS1398-2; PS1399-1; PS1400-4; PS1401-2; PS1402-2; PS1403-1; PS1405-1; PS1406-1; PS1407-1; PS1410-1; PS1411-1; PS1412-1; PS1414-1; PS1415-1; PS1416-1; PS1417-1; PS1418-1; PS1419-1; PS1420-1; PS1421-1; PS1422-1; PS1423-1; PS1424-1; PS1425-1; PS1426-1; PS1427-1; PS1428-1; PS1451-2; PS1452-1; PS1453-1; PS1454-1; PS1455-4; PS1459-4; PS1460-1; PS1471-1; PS1472-4; PS1473-1; PS1474-1; PS1475-1; PS1476-1; PS1477-1; PS1478-1; PS1479-1; PS1480-2; PS1481-2; PS1482-2; PS1483-2; PS1484-2; PS1485-1; PS1486-2; PS1487-1; PS1488-2; PS1489-3; PS1490-2; PS1491-3; PS1492-1; PS1493-2; PS1494-2; PS1495-1; PS1496-2; PS1497-1; PS1498-1; PS1499-2; PS1500-2; PS1501-1; PS1502-1; PS1505-1; PS1506-1; PS1507-2; PS1508-2; PS1509-2; PS1537-1; PS1538-1; PS1539-1; PS1540-1; PS1542-1; PS1543-1; PS1544-1; PS1545-1; PS1546-2; PS1547-1; PS1554-1; PS1555-1; PS1557-1; PS1558-1; PS1559-1; PS1560-1; PS1563-1; PS1564-1; PS1569-1; PS1572-1; PS1573-2; PS1574-1; PS1575-1; PS1575-2; PS1576-1; PS1577-2; PS1578-1; PS1579-1; PS1581-2; PS1582-1; PS1584-1; PS1585-1; PS1586-2; PS1587-1; PS1588-2; PS1589-1; PS1590-1; PS1591-2; PS1593-1; PS1594-1; PS1595-2; PS1596-1; PS1597-1; PS1598-2; PS1599-1; PS16; PS16/403; PS16/405; PS16/410; PS16/413; PS16/415; PS16/417; PS16/419; PS16/425; PS16/427; PS16/430; PS16/432; PS16/446; PS16/472; PS16/499; PS16/507; PS16/509; PS16/510; PS16/515; PS16/516; PS16/518; PS16/525; PS16/526; PS16/528; PS16/530; PS16/534; PS16/536; PS16/540; PS16/541; PS16/547; PS16/549; PS16/552; PS16/554; PS16/557; PS1600-2; PS1601-1; PS1602-1; PS1603-2; PS1604-1; PS1605-3; PS1606-1; PS1607-1; PS1608-1; PS1609-2; PS1610-3; PS1611-1; PS1612-1; PS1613-2; PS1614-1; PS1615-2; PS1616-1; PS1617-2; PS1618-2; PS1619-1; PS1620-2; PS1621-2; PS1622-1; PS1623-2; PS1624-1; PS1625-1; PS1626-1; PS1627-1; PS1628-2; PS1629-1; PS1631-1; PS1632-1; PS1635-2; PS1636-1; PS1637-1; PS1638-1; PS1639-1; PS1640-3; PS1641-1; PS1642-1; PS1643-3; PS1645-1; PS1647-2; PS1648-2; PS1787-1; PS1788-1; PS1790-2; PS1791-1; PS1792-2; PS1793-1; PS1794-2; PS1795-1; PS1796-2; PS1797-1; PS1798-2; 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; PS18/083; PS18/084; PS18/086; PS18/088; PS18/092; PS18/094; PS18/096; PS18/100; PS18/101; PS18/102; PS18/106; PS18/108; PS18/114; PS18/126; PS18/127; PS18/129; PS18/135; PS18/141; PS18/142; PS18/143; PS18/144; PS18/145; PS18/146; PS18/147; PS18/148; PS18/149; PS18/150; PS18/151; PS18/152; PS18/153; PS18/154; PS18/161; PS18/165; PS18/166; PS18/167; PS18/169; PS18/170; PS18/171; PS18/172; PS18/173; PS18/175; PS18/177; PS18/178; PS18/179; PS18/180; PS18/181; PS18/182; PS18/183; PS18/184; PS18/185; PS18/186; PS18/187; PS18/189; PS18/190; PS18/191; PS18/192; PS18/193; PS18/194; PS18/196; PS18/198; PS18/199; PS18/200; PS18/201; PS18/202; PS18/203; PS18/204; PS18/208; PS18/210; PS18/211; PS18/212; PS18/214; PS18/216; PS18/217; PS18/218; PS18/219; PS18/221; PS18/222; PS18/227; PS1800-2; PS1802-2; PS1803-2; PS1805-5; PS1806-5; PS18 06AQANTIX_2; PS1807-1; PS1811-7; PS1812-5; PS1813-5; PS1817-5; PS1818-1; PS1819-5; PS1820-5; PS1821-5; PS1822-1; PS1823-1; PS1824-2; PS1825-5; PS1826-2; PS1828-2; PS1829-1; PS1831-5; PS1953-1; PS1954-1; PS1957-1; PS1958-1; PS1960-1; PS1961-1; PS1963-1; PS1964-1; PS1965-1; PS1967-
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 129
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Fahl, Kirsten; Stein, Ruediger (1999): Biomarkers as organic-carbon-source and environmental indicators in the Late Quaternary Arctic Ocean: Problems and Perspectives. Marine Chemistry, 63(3-4), 293-309, https://doi.org/10.1016/S0304-4203(98)00068-1
    Publication Date: 2024-07-01
    Description: In order to examine the variation in marine and terrigenous sources of the organic matter during the last 15,000 Cal. yr BP, hydrogen index values, C/N ratios, and specific biomolecules (short- and long-chain n-alkanes, short-chain fatty acids, sterols, alkenones, and pigments) were determined in three sediment cores from the Laptev Sea continental margin. The results show that the interpretation of the biomarker data is much more complicated and less definitive in comparison to similar data sets from low-latitude open-ocean environments. This is mainly caused by the complexity of the Arctic Ocean system, which is characterized by a high seasonality of sea-ice cover and primary productivity, sea-ice sediment transport and a high fluvial supply of freshwater (aquatic) organic matter. A combination of organic geochemical, organic petrographic and micropaleontological data may yield to a more precise identification of organic-carbon sources for these complex systems. On the Laptev Sea shelf (cores KD9502-14 and PS2725-5), terrigenous organic-carbon input controlled by river discharge seems to be predominant during the last about 10,000 Cal. yr BP. Maximum supply of terrigenous organic carbon was reached in the Early Holocene (i.e., about 9000-10,000 Cal. yr BP). Further offshore at the upper continental slope (core PS2458-4), a major change in organic-composition occurred near 10,000 Cal. yr BP. During this period hydrogen indices as well as the amounts of short-chain n-alkanes, short-chain fatty acids, dinosterol and brassicasterol significantly increased, indicating increased relative proportions of marine organic matter preserved in the later time interval.
    Keywords: Arctic Ocean; ARK-IX/4; ARK-XI/1; AWI_Paleo; Gravity corer (Kiel type); KAL; Kapitan Dranitsyn; Kasten corer; KD9502-14; Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2458-4; PS27; PS27/038; PS2725-5; PS36; PS36/009; Quaternary Environment of the Eurasian North; QUEEN; SL; Transdrift-III; VC; Vibro corer
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 130
    facet.materialart.
    Unknown
    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
    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
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 131
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Catubig, Nina R; Archer, David E; Francois, Roger; deMenocal, Peter B; Howard, William R; Yu, Ein-Fen (1998): Global deep-sea burial rate of calcium carbonate during the last glacial maximum. Paleoceanography, 13(3), 298-310, https://doi.org/10.1029/98PA00609
    Publication Date: 2024-07-01
    Description: Global databases of calcium carbonate concentrations and mass accumulation rates in Holocene and last glacial maximum sediments were used to estimate the deep-sea sedimentary calcium carbonate burial rate during these two time intervals. Sparse calcite mass accumulation rate data were extrapolated across regions of varying calcium carbonate concentration using a gridded map of calcium carbonate concentrations and the assumption that accumulation of noncarbonate material is uncorrelated with calcite concentration within some geographical region. Mean noncarbonate accumulation rates were estimated within each of nine regions, determined by the distribution and nature of the accumulation rate data. For core-top sediments the regions of reasonable data coverage encompass 67% of the high-calcite (〉75%) sediments globally, and within these regions we estimate an accumulation rate of 55.9 ± 3.6 x 10**11 mol/yr. The same regions cover 48% of glacial high-CaCO3 sediments (the smaller fraction is due to a shift of calcite deposition to the poorly sampled South Pacific) and total 44.1 ± 6.0 x 10**11 mol/yr. Projecting both estimates to 100 % coverage yields accumulation estimates of 8.3 x 10**12 mol/yr today and 9.2 x 10**12 mol/yr during glacial time. This is little better than a guess given the incomplete data coverage, but it suggests that glacial deep sea calcite burial rate was probably not considerably faster than today in spite of a presumed decrease in shallow water burial during glacial time.
    Keywords: 0055PG; 0082PG; 0091PG; 113-694; 113-697; 114-699; 114-701; 114-702; 114-704; 115-708A; 115-716B; 117-722B; 117-728A; 119-737; 119-739; 119-740; 119-741; 119-742; 119-743; 119-745; 120-751A; 19-183; 19-193; 20-194; 20-195; 20-196; 21-204; 22-211; 22-213; 22-215; 26-256; 26-257; 280; 28-267; 28-268; 28-269; 28-270; 30-285; 31-290; 31-291; 31-298; 32-307; 32-311; 34-321; 5-32; 56-434; 60-452; 60-460; 60-461; 63-472; 63-473; 6-45A; 6-46; 6-52; 6-59; 7-65; 7-66; 7-67; 85-572_Site; 85-572A; 85-574; 86-576; 86-578; 86-579; 86-580; 86-581; A150/180; A152-118; A156-3; A156-4; A164-24; A164-5; A164-6; A16-46; A164-61; A16-461; A167-13; A167-14; A173-13; A173-4; A179-15; A180-15; A180-16; A180-32; A180-39; A180-47; A180-48; A180-56; A180-72; A180-73; A180-74; A180-76; A180-9; A18-39; A18-72; A18-73; A240-ML; Albatross IV (1963); Antarctic Ocean; Antarctic Ocean/BASIN; Antarctic Ocean/CONT RISE; Antarctic Ocean/PLAIN; APSARA1; APSARA2; APSARA4; Arabian Sea; AT_II-107_65; ATII_USA; Atlantic Ocean; Atlantis II (1963); BC; Box corer; CH8X; CHN82-04; CHN82-11; CHN82-15; CHN82-20; COMPCORE; Composite Core; core_59; core_60; DRILL; Drilling/drill rig; ELT14; ELT14.006-PC; ELT17; ELT17.009-PC; ELT45; ELT45.009-PC; ELT45.024-PC; ELT45.027-PC; ELT45.029-PC; ELT45.032-PC; ELT45.063-PC; ELT45.064-PC; ELT45.071-PC; ELT45.074-PC; ELT48; ELT48.003-PC; ELT48.006-PC; ELT48.011-PC; ELT48.013-PC; ELT48.022-PC; ELT48.027-PC; ELT48.029-PC; ELT49; ELT49.008-PC; ELT49.017-PC; ELT49.018-PC; ELT49.021-PC; ELT49.023-PC; ELT50; ELT50.013-PC; ELT50.017-PC; Eltanin; EN06601; EN066-10GGC; EN066-16GGC; EN066-17GGC; EN066-21GGC; EN066-23PG; EN066-24PG; EN066-26GGC; EN066-29GGC; EN066-32GGC; EN066-36GGC; EN066-39GGC; EN066-39PG; EN066-43GGC; EN066-44GGC; EN066-47PG; EN77-29; Endeavor; ENXX; Equatorial Pacific; ERDC; ERDC-079BX; ERDC-092BX; ERDC-102BX; ERDC-129BX; GC; Glomar Challenger; Gravity corer; IC-5; India; Indian Ocean; Indian Ocean//BASIN; IO1578-4; Jean Charcot; Joides Resolution; KN11002; KN708-1; Knorr; KNR110-55; KNR110-82; KNR110-91; KS7703; Lakshadweep Sea; Leg113; Leg114; Leg115; Leg117; Leg119; Leg120; Leg19; Leg20; Leg21; Leg22; Leg26; Leg28; Leg30; Leg31; Leg32; Leg34; Leg5; Leg56; Leg6; Leg60; Leg63; Leg7; Leg85; Leg86; Marion Dufresne (1972); MD13; MD38; MD77-202; MD82-424; MD84-527; MD84-529; MD84-551; MD84-552; MD84-562; MD88-769; MD88-770; MD88-773; MD88-787; Melville; MN76-01, Pleiades; NGR9; NODC-0418; North Atlantic; North Pacific; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; North Pacific/CONT RISE; North Pacific/Gulf of California/CONT RISE; North Pacific/Philippine Sea/RIDGE; North Pacific/Philippine Sea/TRENCH; North Pacific/Philippine Sea/TROUGH; North Pacific/PLAIN; North Pacific/PLATEAU; North Pacific/RIDGE; North Pacific/SEAMOUNT; North Pacific/SEDIMENT POND; North Pacific/TRENCH; North Pacific/TROUGH; off NW Africa; OSIRIS III; Pacific Ocean; PC; Piston corer; PLDS-130P; PLDS-130PG; PLDS-4; Prydz Bay; RAMA; RAMA03WT; RAMA-44P; RC01; RC0101-RC0102; RC01-2; RC08; RC08-145; RC08-18; RC08-39; RC08-43; RC08-48; RC08-63; RC08-71; RC08-78; RC08-79; RC08-89; RC08-92; RC08-94; RC09; RC09-110; RC09-124; RC09-126; RC09-129; RC09-139; RC09-161; RC09-162; RC09-225; RC09-49; RC10; RC10-139; RC10-140; RC10-159; RC10-160; RC10-161; RC10-171; RC10-179; RC10-181; RC10-182; RC10-203; RC10-206; RC10-216; RC10-288; RC10-289; RC10-50; RC10-97; RC11; RC11-114; RC11-118; RC11-119; RC1112; RC11-120; RC11-121; RC11-170; RC11-171; RC11-172; RC11-179; RC11-193; RC11-195; RC11-209; RC11-21; RC11-210; RC11-213; RC11-220; RC11-230; RC11-26; RC11-76; RC11-77; RC11-78; RC11-80; RC11-83; RC11-86; RC11-91; RC11-94; RC11-96; RC11-97; RC12; RC12-103; RC12-107; RC12-109; RC12-121; RC12-176; RC12-179; RC12-225; RC12-227; RC12-234; RC12-241; RC12-267; RC12-289; RC12-291; RC12-294; RC12-328; RC12-340; RC12-341; RC12-343; RC12-344; RC12-361; RC12-401; RC12-412; RC12-413; RC12-416; RC12-419; RC12-63; RC12-65; RC12-66; RC13; RC13-113; RC13-151; RC13-152; RC13-153; RC13-159; RC13-189; RC13-190; RC13-205; RC13-210; RC13-227; RC13-228; RC13-229; RC13-243; RC13-251; RC13-253; RC13-254; RC13-255; RC13-256; RC13-259; RC13-261; RC13-263; RC13-271; RC13-273; RC13-275; RC13-38; RC13-63; RC13-81; RC14; RC14-106; RC14-11; RC14-29; RC14-35; RC14-39; RC14-7; RC14-9; RC14-99; RC15; RC15-23; RC15-52; RC15-61; RC15-93; RC15-94; RC15-98; RC17; RC17-113; RC17-184; RC17-194; RC17-196; RC17-197; RC17-60; RC17-61; RC17-63; RC17-69; RC17-73; RC17-98; RC23; RC23-50BX1; RC23-52BX1; RC23-53BX1; RC23-54BX1; RC23-61BX1; RE05; RE05-34; RE05-36; RE05-54; RE5-034; RE5-036; RE5-054; Rehoboth; RIVER; Robert Conrad; Sampling river; SDSE_090; SDSE_092; South Atlantic; South Atlantic Ocean; Southern East Pacific Rise; South Indian Ocean; South Indian Ridge, South Indian Ocean; South Pacific; South Pacific/BASIN; South Pacific/TRENCH; SP8-4; SwedishDeepSeaExpedition; TC; Thomas Washington; Trigger corer; V04; V04-1; V04-32; V04-8; V12; V12-122; V14; V14-101; V14-102; V14-77; V14-81; V15; V15-157; V15-168; V16; V16-114; V16-115; V16-122; V16-205; V16-25; V16-36; V17; V17-165; V17-178; V17-42; V17-43; V17-44; V18; V18-110; V18-222; V18-312; V18-318; V18-337; V18-68; V19; V19-178; V19-185; V19-188; V19-19; V19-201; V19-202; V19-204; V19-21; V19-240; V19-248; V19-25; V19-27; V19-28; V19-281; V19-282; V19-283; V19-291; V19-30; V19-305; V19-309; V19-41; V19-53; V19-55; V19-65; V19-96; V20; V20-102; V20-103; V20-104; V20-105; V20-107; V20-108; V20-109; V20-119; V20-121; V20-122; V20-123; V20-124; V20-126; V20-129; V20-170; V20-175; V20-212; V20-227; V20-228; V20-241; V20-242; V20-68; V20-74; V20-79; V20-81; V20-82; V20-85; V20-86; V20-87; V20-88; V20-92; V20-95; V20-96; V20-97; V20-98; V21; V21-145; V21-146; V21-148; V21-150; V21-151; V21-171; V21-173; V21-174; V21-175; V21-178; V21-212; V21-214; V21-29; V21-30; V21-33; V21-59; V22; V22-108; V22-168; V22-171; V22-172; V22-174; V22-177; V22-182; V22-186; V22-188; V22-196; V22-197; V22-219; V22-222; V22-234; V22-26; V22-38; V22-83; V22-86; V23; V23-100; V23-145; V23-23; V23-42; V23-58; V23-59; V23-60; V23-73; V23-74; V23-81; V23-82; V23-83; V23-84; V23-91; V23-98; V24; V24-1; V24-109; V24-166; V24-203; V24-221; V24-229; V24-235; V24-237; V24-240; V24-55; V24-58; V24-59; V24-62; V25; V25-21; V25-42; V25-44; V25-56; V25-59; V25-60; V25-75; V26; V26-104; V26-175; V26-176; V26-177; V26-37; V26-41; V26-46; V26-63; V26-82; V27; V27-110; V27-116; V27-17; V27-171; V27-175; V27-178; V27-19; V27-20; V27-221; V27-228; V27-232; V27-238; V27-239; V27-240; V27-248; V27-263; V27-264; V27-265; V27-267; V27-269; V27-46; V27-47; V27-60; V27-84; V27-85; V27-86; V28; V28-108; V28-129; V28-14; V28-177; V28-179; V28-185; V28-203; V28-229; V28-230; V28-235; V28-238; V28-239; V28-249; V28-255; V28-294; V28-304; V28-35; V28-38; V28-56; V28-59; V28-89; V29; V29-105; V29-144; V29-15; V29-153; V29-172; V29-173; V29-174; V29-177; V29-178; V29-179; V29-180; V29-183; V29-192; V29-206; V29-210; V29-219; V29-29; V29-30; V29-48; V29-84; V29-86; V29-87; V29-89; V29-90; V30; V30-100; V30-101; V30-36; V30-40; V30-41; V30-41k; V30-49; V30-51; V30-51k; V30-88; V30-93; V30-96; V30-97; V30-99; V31; V31-166; V31-178; V32; V32-102; V32-109; V32-126; V32-8; V34; V34-101; V34-109; V34-111; V34-34; V34-48; V34-51; V34-53; V34-54; V34-55; V34-87; V34-89; V34-91; V34-92; Vema; VNTR01; VNTR01-49GC; W12; W26; W48K; W53K; W8402A; W8402A-14; W8709A; W8709A-1; W8709A-13; W8709A-8; W8803B; W8803B-51GC; WAH-8-2; Wecoma; Weddell Sea; WW21; X164021; X164032; X164041; X164051; X164061; X164071; X164081; X164101; X164111; X164121; X164131; X164151; X164161; X164171; X164222; X164241; X164251; X164263; X164282; X164291; X164301; X164311; X164321; Y70-5; Y70-5-64; Yaquina
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 132
    Publication Date: 2024-07-01
    Description: The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.
    Keywords: 1; 10; 101; 11; 12; 13; 14; 15; 16; 162; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 262; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 362; 37; 38; 39; 4; 40; 41; 42; 43; 44; 45; 46; 462; 47; 48; 49; 5; 50; 51; 52; 53; 54; 55; 56; 57; 58; 59; 6; 60; 61; 62; 63; 64; 65; 66; 67; 68; 69; 7; 70; 71; 72; 73; 74; 75; 76; 77; 78; 79; 8; 80; 81; 82; 83; 84; 85; 87; 88; 89; 9; 90; 91; 92; 93; ARK-XIII/3; 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; B02/98-1361; 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; B02/98-751; B02/98-761; B02/98-771; B02/98-781; B02/98-791; B02/98-801; B02/98-811; B02/98-821; B02/98-831; B02/98-843; 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; B02/98-981; B02/98-991; B03/97; B03/97-531; B03/97-532; B03/97-551; B03/97-552; B03/97-711; B03/97-712; B03/97-751; B03/97-752; B03/97-753; B03/97-771; B03/97-772; B03/97-781; B03/97-782; B03/97-931; B03/97-932; B05/96; B05/96-1252; B05/96-252; B05/96-253; B05/96-254; B05/96-263; B05/96-278; B05/96-293-2; B06/97; B06/97-1431; B06/97-1441; B06/97-1451; B06/97-1461; B06/97-1471; B06/97-1481; B06/97-1492; B06/97-1501; B06/97-1511; B06/97-1512; B06/97-1513; B06/97-1521; B06/97-1531; B06/97-1541; B06/97-1551; B06/97-1561; B06/97-1571; B06/97-1581; B06/97-1591; B06/97-1601; B06/97-1611; B06/97-1621; B06/97-1631; B06/97-1643; B06/97-1644; B06/97-1651; B06/97-1661; B06/97-1671; B06/97-1681; B06/97-1691; B06/97-1701; B06/97-1711; B06/97-1721; B06/97-1731; B06/97-1741; B06/97-1751; B06/97-1761; B06/97-1772; B06/97-1773; B06/97-1781; B06/97-1791; B06/97-1801; B06/97-1811; B06/97-1821; B06/97-1831; B06/97-1841; B06/97-1851; B06/97-1861; B06/97-1871; B06/97-1881; B06/97-1891; B06/97-1901; B06/97-1911; B06/97-1912; B06/97-1921; B06/97-1931; B06/97-1941; B06/97-1951; B06/97-1971; B06/97-1981; B06/97-1991; B06/97-2001; B06/97-2011; B06/97-2021; B06/97-2031; B06/97-2041; B06/97-2051; B06/97-2061; B06/97-2071; B06/97-2081; B06/97-2091; B06/97-2101; B06/97-2121; B06/97-2122; B06/97-2131; B06/97-2141; B06/97-2142; B06/97-2151; B06/97-2161; B06/97-2171; B06/97-2181; B06/97-2191; B06/97-2211; B06/97-2221; B06/97-2231; B06/97-2241; B06/97-2251; B06/97-2261; B06/97-2271; B06/97-2281; B06/97-2291; B06/97-2301; B06/97-2311; B06/97-2321; B06/97-2331; B06/97-2341; B06/97-2351; B06/97-2361; B06/97-2371; B06/97-2381; B06/97-2391; B06/97-2401; B06/97-2411; B06/97-2421; B06/97-2431; B06/97-2441; B06/97-2451; B06/97-2461; B06/98; B06/98-2531; B06/98-2541; B06/98-2551; B06/98-2561; B06/98-2571; B06/98-2581; B06/98-2582; B06/98-2591; B06/98-2592; B06/98-2601; B06/98-2611; B06/98-2612; B06/98-2621; B06/98-2631; B06/98-2641; B06/98-2642; B06/98-2651; B06/98-2652; B06/98-2661; B06/98-2671; B06/98-2672; B06/98-2681; B06/98-2691; B06/98-2701; B06/98-2711; B06/98-2721; B06/98-2741; B06/98-2751; B06/98-2761; B06/98-2771; B06/98-2781; B06/98-2791; B06/98-2801; B06/98-2811; B06/98-2821; B06/98-2831; B06/98-2841; B06/98-2851; B06/98-2861; B06/98-2871; B06/98-2881; B06/98-2891; B06/98-2901; B06/98-2911; B06/98-2921; B06/98-2931; B06/98-2941; B06/98-2951; B06/98-2961; B06/98-2971; B06/98-2981; B06/98-2991; B06/98-3001; B06/98-3002; B06/98-3003; B06/98-3004; B06/98-3011; B06/98-3012; B06/98-3021; B06/98-3031; B06/98-3041; B06/98-3051; B06/98-3081; B06/98-3101; B06/98-3102; B06/98-3103; B06/98-3104; B06/98-3121; B06/98-3141; B06/98-3142; B06/98-3143; B06/98-3144; B06/98-3161; B06/98-3171; B06/98-3181; B06/98-3191; B06/98-3201; B06/98-3211; B06/98-3221; B06/98-3231; B06/98-3241; B06/98-3251; B06/98-3261; B06/98-3271; B06/98-3321; B06/98-3331; B06/98-3341; B06/98-3351; B06/98-3361; B06/98-3371; B06/98-3381; B06/98-3391; B06/98-3401; B06/98-3441; B06/98-3451; B06/98-3461; B06/98-3481; B06/98-3482; B06/98-3483; B06/98-3511; B06/98-3522; B06/98-3531; B06/98-3541; B06/98-3551; B06/98-3561; B06/98-3581; B06/98-3591; B06/98-3611; B06/98-3621; B06/98-3631; B06/98-3641; B06/98-3651; B06/98-3661; B06/98-3671; B06/98-3681; B06/98-3691; B06/98-3701; B06/98-3711; B06/98-3731; B06/98-3741; B06/98-3751; B06/98-3761; B06/98-3771; B06/98-3781; B06/98-3791; B09/96; B09/96-5311; B09/96-5312; B09/96-5321; B09/96-5322; B09/96-5351; B09/96-5352; B09/96-5353; B09/96-5451; B09/96-5452; B09/96-5481; B09/96-5482; B09/96-5511; B09/96-5512; B09/96-5521; B09/96-5522; B09/96-5531; B09/96-5532; B09/98; B09/98-5432; B09/98-5433; B09/98-5434; B09/98-5441; B09/98-5451; B09/98-5461; B09/98-5471; B09/98-5481; B09/98-5491; B09/98-5501; B09/98-5511; B09/98-5531; B09/98-5541; B09/98-5551; B09/98-5561; B09/98-5581; B09/98-5601; B09/98-5631; B09/98-5641; B09/98-5651; B09/98-5661; B09/98-5671; B09/98-5681; B09/98-5711; B09/98-5731; B09/98-5732; B09/98-5741; B09/98-5751; B09/98-5771; B09/98-5791; B09/98-5792; B09/98-5801; B09/98-5804; B09/98-5805; B10/97; B10/97-3601; B10/97-3602; B10/97-3851; B10/97-3871; B10/97-3881; B10/97-3891; B10/97-3892; B10/97-3911; B10/97-3912; B10/97-3921; B10/97-3922; B10/97-3923; B10/97-3931; B10/97-3932; B10/97-3941; B10/97-4011; B10/97-4012; B10/97-4031; B10/97-4032; B10/97-4041; B10/97-4042; B12/96; B12/96-7210; B12/96-7220; B12/96-7230; B12/96-7240; B12/96-8520; B12/96-8540; B12/96-8550; B12/98; B12/98-7811; B12/98-7812; B12/98-7813; B12/98-8391; B12/98-8392; B12/98-8393; B12/98-8394; B12/98-8621; B12/98-8622; B15/97; B15/97-6761; B15/97-6771; B15/97-6781; B15/97-6791; B15/97-6801; B15/97-6811; B15/97-6821; B15/97-6831; B15/97-6841; B15/97-6851; B15/97-6861; B15/97-6871; B15/97-6881; B15/97-6891; B15/97-6892; B15/97-6901; B15/97-6902; B15/97-6912; B15/97-6921; B15/97-6931; B15/97-6951; B15/97-6961; B15/97-6971; B15/97-6981; B15/97-6991; B15/97-7001; B15/97-7011; B15/97-7021; B15/97-7031; B15/97-7041; B15/97-7051; B15/97-7061; B15/97-7071; B15/97-7081; B15/97-7091; B15/97-7101; B15/97-7111; B15/97-7121; B15/97-7131; B15/97-7141; B15/97-7151; B15/97-7161; B15/97-7171; B15/97-7181; B15/97-7182; B15/97-7191; B15/97-7201; B15/97-7211; B15/97-7221; B15/97-7231; B15/97-7241; B15/97-7251; B15/97-7261; B15/97-7271; B15/97-7281; B15/97-7291; B15/97-7301; B15/97-7311; B15/97-7321; B15/97-7331; B15/97-7341; B15/97-7351; B15/97-7361; B15/97-7371; B15/97-7381; B15/97-7391; B15/97-7401; B15/97-7411; B15/97-7421; B15/97-7431; B15/97-7441; B15/97-7451; B15/97-7461; B15/97-7471; B15/97-7481; B15/97-7491; B15/97-7501; B15/97-7511; B15/97-7512; B15/97-7513; B15/97-7521; B15/97-7531; B15/97-7532; B15/97-7533; B15/97-7541; B15/97-7551; B15/97-7561; B15/97-7571; B15/97-7581; B15/97-7591; B15/97-7601; B15/97-7611; B15/97-7621; B15/97-7631; B15/97-7641; B15/97-7651; B15/97-7661; B15/97-7671; B15/97-7681; B15/97-7691; B15/97-7692; B15/97-7701; B15/97-7711; B15/97-7721; B15/97-7731; B15/97-7741; B15/97-7751; Bjarni Saemundsson; CARDEEP1/93; CARDEEP1/93-161; CARDEEP1/93-162; CARDEEP1/93-171; CARDEEP1/93-181; CARDEEP1/93-182; CARDEEP1/93-201; CARDEEP1/93-211; CARDEEP1/93-212; CARDEEP1/93-231; CARDEEP1/93-232; CARDEEP1/93-261; CARDEEP1/93-271; CARDEEP1/93-281; CARDEEP1/93-291; CARDEEP1/93-301; CARDEEP1/93-311; CARDEEP1/93-312; CARDEEP1/93-331; CARDEEP1/93-341; CARDEEP1/93-351; CARDEEP1/93-361;
    Type: Dataset
    Format: application/zip, 51 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 133
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Budéus, Gereon; Schneider, Wolfgang; Krause, Gunther (1998): Winter convective events and bottom water warming in the Greenland Sea. Journal of Geophysical Research: Oceans, 103(C9), 18513-18527, https://doi.org/10.1029/98JC01563
    Publication Date: 2024-07-01
    Description: From observations on yearly cruises to the central Greenland Sea between 1993 and 1996, conclusions are drawn with respect to winter convection and bottom water renewal. The data indicate that winter convection was extremely weak after 1993, not even ventilating the intermediate waters. This is remarkable, since the salinities in the upper layers increased considerably between 1993 and 1995, thus providing presumably favorable conditions for winter convection. With the absence of deep reaching winter convective events, the temperatures in the deeper waters of the Greenland Gyre increased steadily by about 0.03 K between 1993 and 1996. We conclude from the development of mainly the thermal structure on a zonal transect that an explanation for the temperature increase can be given by a large-scale downward water movement of about 150 m/yr in the central Greenland Sea. The data indicate that this process is independent of changes in the dynamically induced density distribution. It is therefore possible that a downward movement, perhaps masked by other processes, may continue for many years. If this is the case, resulting flushing times would be of the order of 20-30 years only. The presence of a large-scale circulation cell with downward movement in the central Greenland Gyre would explain the observed warming of the bottom waters without the demand for an actually active heat source. It is also in accordance with the observed increase of chemical tracer concentrations in the deep waters.
    Keywords: ARK-IX/1b; ARK-X/1; ARK-XI/2; AWI_PhyOce; CTD/Rosette; CTD-RO; ESOP; European subpolar ocean programme : sea ice-ocean interactions; JGOFS; Joint Global Ocean Flux Study; MULT; Multiple investigations; North Greenland Sea; Norwegian Sea; Petr Kottsov; Physical Oceanography @ AWI; PK-ARK-XII; PK-XII/01-1; PK-XII/01-2; PK-XII/02; PK-XII/03; PK-XII/04; PK-XII/05; PK-XII/06; PK-XII/07; PK-XII/08-1; PK-XII/08-2; PK-XII/09; PK-XII/10; PK-XII/11; PK-XII/12; PK-XII/13; PK-XII/14; PK-XII/15; PK-XII/16; PK-XII/17; PK-XII/18; PK-XII/19; PK-XII/20; PK-XII/21; PK-XII/22; PK-XII/23; PK-XII/24; PK-XII/25; PK-XII/26; PK-XII/27; PK-XII/28; PK-XII/29; PK-XII/33; PK-XII/34; PK-XII/35; PK-XII/36; PK-XII/37; PK-XII/38; PK-XII/39; PK-XII/40; PK-XII/41; PK-XII/42; PK-XII/43; PK-XII/44; PK-XII/45; PK-XII/46; PK-XII/47; PK-XII/48; PK-XII/49; PK-XII/50; PK-XII/51; PK-XII/52; Polarstern; PS24; PS24/036; PS24/037; PS24/038; PS24/039; PS24/040; PS24/041; PS24/043; PS24/044; PS24/045; PS24/046; PS24/047; PS24/048; PS24/049; PS24/050; PS24/051; PS24/053; PS24/054; PS24/055; PS24/056; PS24/057; PS24/061; PS24/062; PS24/063; PS24/064; PS24/065; PS24/066; PS24/067; PS24/068; PS24/069; PS24/070; PS31; PS31/026; PS31/026a; PS31/027; PS31/028; PS31/029; PS31/030; PS31/031; PS31/032; PS31/033; PS31/034; PS31/035; PS31/036; PS31/037; PS31/038; PS31/039; PS31/040; PS31/041; PS31/042; PS31/043; PS31/044; PS31/045; PS31/046; PS31/048; PS31/049; PS31/050; PS31/051; PS31/052; PS31/053; PS31/054; PS31/055; PS31/056; PS31/057; PS31/058; PS31/059; PS31/060; PS31/061; PS31/062; PS31/063; PS31/064; PS31/065; PS31/066; PS31/067; PS31/068; PS31/069; PS31/070; PS31/071; PS31/072; PS31/073; PS31/074; PS31/075; PS31/076; PS31/077; PS31/078; PS31/079; PS31/080; PS31/081; PS31/082; PS31/083; PS31/084; PS31/085; PS31/087; PS31/089; PS31/090; PS31/091; PS31/092; PS31/093; PS31/094; PS31/095; PS31/096; PS31/096a; PS31/097; PS31/098; PS31/099; PS31/100; PS31/101; PS31/102; PS31/103; PS31/104; PS31/105; PS31/106; PS31/107; PS31/108; PS31/109; PS31/110; PS31/111; PS37; PS37/001-1; PS37/006-1; PS37/006-2; PS37/008-2; PS37/008-4; PS37/010; PS37/014-3; PS37/014-4; PS37/015; PS37/016-4; PS37/016-5; PS37/017; PS37/018; PS37/019; PS37/020-6; PS37/020-7; PS37/021-3; PS37/021-4; PS37/022-3; PS37/022-4; PS37/023; PS37/024; PS37/025-1; PS37/025-2; PS37/026-1; PS37/026-2; PS37/028; PS37/029; PS37/033; PS37/035; PS37/036; PS37/037; PS37/038; PS37/039; PS37/040; PS37/041; PS37/042; PS37/043; PS37/044; PS37/045; PS37/046; PS37/047; PS37/048; PS37/049; PS37/050; PS37/052; PS37/053; PS37/056; PS37/057; PS37/058; PS37/059; PS37/060; PS37/061; PS37/062; PS37/063; PS37/064; PS37/065; PS37/066; PS37/067; PS37/068; PS37/069; PS37/070; PS37/071; PS37/072; PS37/073; PS37/074; PS37/075; PS37/076; PS37/077; PS37/078; PS37/079; PS37/080; PS37/081; PS37/082; PS37/083; PS37/084; PS37/085; PS37/086; PS37/087; PS37/088; PS37/089; PS37/090; PS37/091; PS37/092; PS37/093; PS37/094; PS37/095; PS37/096; PS37/097; PS37/098; PS37/099; PS37/100; PS37/101; PS37/102; PS37/103; PS37/104; PS37/105; PS37/106; PS37/107; PS37/108; PS37/109; PS37/110; PS37/111; PS37/112; PS37/113; PS37/114; PS37/115; PS37/116; PS37/117
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 134
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Zielinski, Ulrich; Gersonde, Rainer; Sieger, Rainer; Fütterer, Dieter K (1998): Quaternary surface water temperature estimations: calibration of a diatom transfer funtion for the Southern Ocean. Paleoceanography, 13(4), 365-383, https://doi.org/10.1029/98PA01320
    Publication Date: 2024-07-01
    Description: The quantitative diatom analysis of 218 surface sediment samples recovered in the Atlantic and western Indian sector of the Southern Ocean is used to define a base of reference data for paleotemperature estimations from diatom assemblages using the Imbrie and Kipp transfer function method. The criteria which justify the exclusion of samples and species out of the raw data set in order to define a reference database are outlined and discussed. Sensitivity tests with eight data sets were achieved evaluating the effects of overall dominance of single species, different methods of species abundance ranking, and no-analog conditions (e.g., Eucampia Antarctica) on the estimated paleotemperatures. The defined transfer functions were applied on a sediment core from the northern Antarctic zone. Overall dominance of Fragilariopsis kerguelensis in the diatom assemblages resulted in a close affinity between paleotemperature curve and relative abundance pattern of this species downcore. Logarithmic conversion of counting data applied with other ranking methods in order to compensate the dominance of F. kerguelensis revealed the best statistical results. A reliable diatom transfer function for future paleotemperature estimations is presented.
    Keywords: Adelaide Island; Agulhas Basin; Agulhas Ridge; Antarctic Peninsula; ANT-II/3; ANT-II/4; ANT-III/3; ANT-IV/3; ANT-IV/4; ANT-IX/2; ANT-IX/4; ANT-V/4; ANT-VI/2; ANT-VI/3; ANT-VIII/3; ANT-VIII/5; ANT-X/4; ANT-X/5; ANT-XI/2; ANT-XI/4; Argentine Islands; Atka Bay; Atlantic Indik Ridge; Atlantic Ridge; AWI_Paleo; Barents Sea; Bransfield Strait; Camp Norway; Cape Basin; Cape Fiske; Conrad Rise; Cosmonauts Sea; CTD/Rosette; CTD-RO; Drake Passage; Elephant Island; Filchner Shelf; Filchner Trough; Giant box corer; GKG; Gould Bay; Gravity corer (Kiel type); Halley Bay; Indian-Antarctic Ridge; Islas Orcadas; Joinville Island; Kapp Norvegia; King George Island, Antarctic Peninsula; Lyddan Island; Maud Rise; Meteor Rise; MIC; MiniCorer; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS04; PS04/247; PS04/248; PS04/249; PS04/250; PS04/261; PS04/263; PS04/264; PS04/265; PS04/266; PS04/268; PS04/269; PS04/270; PS04/271; PS04/277; PS04/302; PS04/304; PS04/331; PS04/335; PS04/346; PS04/351; PS04/380; PS04/414; PS04/423; PS04/429; PS04/433; PS04/440; PS04/447; PS04/472; PS04/508; PS04/509; PS04/540; PS06/289; PS06/303; PS06/304; PS06/311; PS06/313; PS06 SIBEX; PS08; PS08/321; PS08/324; PS08/327; PS08/333; PS08/338; PS08/344; PS08/345; PS08/346; PS08/347; PS08/350; PS08/356; PS08/357; PS08/358; PS08/359; PS08/360; PS08/361; PS08/365; PS08/366; PS08/367; PS08/368; PS08/369; PS08/374; PS08/375; PS08/379; PS08/380; PS08/381; PS08/382; PS08/384; PS08/385; PS08/386; PS08/387; PS08/396; PS08/397; PS08/401; PS08/402; PS08/410; PS08/440; PS08/445; PS08/452; PS08/480; PS08/482; PS08/483; PS08/585; PS08/601; PS08/607; PS08/610; PS08/621; PS08/627; PS10; PS10/672; PS10/675; PS10/684; PS10/686; PS10/699; PS10/701; PS10/703; PS10/707; PS10/820; PS1160-2; PS1161-1; PS1162-1; PS1163-2; PS1174-2; PS1176-3; PS1177-3; PS1178-4; PS1179-1; PS1181-2; PS1182-2; PS1183-4; PS1184-6; PS1190-1; PS1192-1; PS1193-2; PS1195-2; PS1197-1; PS1199-1; PS12; PS12/116; PS12/119; PS12/122; PS12/127; PS12/128; PS12/129; PS12/186; PS12/195; PS12/196; PS12/199; PS12/250; PS12/545; PS12/551; PS12/553; PS12/557; PS1200-4; PS1204-1; PS1207-1; PS1208-1; PS1209-1; PS1210-1; PS1211-1; PS1212-1; PS1214-1; PS1222-1; PS1223-1; PS1225-2; PS1273-1; PS1277-1; PS1278-1; PS1281-1; PS1282-1; PS1363-3; PS1364-1; PS1366-2; PS1367-1; PS1370-1; PS1372-2; PS1373-2; PS1374-2; PS1375-2; PS1376-2; PS1380-1; PS1381-1; PS1382-1; PS1383-1; PS1384-1; PS1385-1; PS1387-1; PS1388-1; PS1389-1; PS1390-1; PS1391-1; PS1394-1; PS1395-1; PS1396-1; PS1397-1; PS1398-2; PS1399-1; PS1400-4; PS1401-2; PS1402-2; PS1403-1; PS1406-1; PS1407-1; PS1410-1; PS1411-1; PS1412-1; PS1419-1; PS1421-1; PS1424-1; PS1425-1; PS1427-1; PS1428-1; PS1452-1; PS1453-1; PS1454-1; PS1455-4; PS1459-4; PS1460-1; PS1472-4; PS1474-1; PS1477-1; PS1478-1; PS1483-2; PS1484-2; PS1485-1; PS1486-2; PS1508-2; PS1537-2; PS1539-1; PS1540-1; PS1542-1; PS1543-1; PS1544-1; PS1555-1; PS1559-1; PS1560-1; PS1563-1; PS1576-1; PS16; PS16/267; PS16/271; PS16/281; PS16/284; PS16/294; PS16/303; PS16/306; PS16/311; PS16/316; PS16/321; PS16/323; PS16/329; PS16/334; PS16/337; PS16/342; PS16/345; PS16/351; PS16/354; PS16/362; PS16/366; PS16/372; PS16/403; PS16/419; PS16/425; PS16/432; PS16/446; PS16/472; PS16/499; PS1649-1; PS1651-2; PS1652-1; PS1654-1; PS1751-2; PS1752-5; PS1755-1; PS1756-6; PS1759-1; PS1764-2; PS1765-1; PS1768-1; PS1768-8; PS1771-4; PS1772-6; PS1773-2; PS1774-1; PS1775-5; PS1776-6; PS1777-7; PS1778-1; PS1779-3; PS1780-1; PS1782-6; PS1783-1; PS1786-2; PS1787-1; PS1794-2; PS1795-1; PS1798-2; PS18; PS18/059; PS18/075; PS18/084; PS18/088; PS18/092; PS18/094; PS18/096; PS18/100; PS18/106; PS18/114; PS18/118; PS18/229; PS18/231; PS18/232; PS18/236; PS18/237; PS18/238; PS18/244; PS18/249; PS18/251; PS18/253; PS18/254; PS18/257; PS18/260; PS18/261; PS18/262; PS18/263; PS18/266; PS18/267; PS1800-2; PS1802-2; PS1803-2; PS18 06AQANTIX_2; PS1961-1; PS1967-1; PS1973-1; PS1975-1; PS1977-1; PS1978-1; PS1979-1; PS1981-1; PS1985-1; PS1987-1; PS1988-1; PS2073-1; PS2075-3; PS2076-1; PS2080-1; PS2081-1; PS2082-3; PS2087-1; PS2091-1; PS2093-1; PS2095-1; PS2096-1; PS2099-1; PS2102-1; PS2103-2; PS2104-1; PS2105-2; PS21 06AQANTX_4; PS2108-1; PS2109-3; PS22/714; PS22/717; PS22/718; PS22/720; PS22/722; PS22/727; PS22/737; PS22/744; PS22/748; PS22/764; PS22/769; PS22/797; PS22/805; PS22 06AQANTX_5; PS2230-1; PS2231-1; PS2233-1; PS2258-1; PS2259-1; PS2260-1; PS2261-1; PS2263-1; PS2265-2; PS2267-2; PS2268-6; PS2270-5; PS2275-1; PS2276-1; PS2299-1; PS2307-2; PS2491-5; PS2492-1; PS2493-3; PS2494-1; PS2495-1; PS2496-2; PS2498-2; PS2499-1; PS2500-7; PS2501-4; PS2502-3; PS2503-1; PS2504-1; PS2505-1; PS2506-1; PS2507-1; PS2508-1; PS2509-1; PS2511-1; PS2512-1; PS2513-1; PS2514-3; PS2561-1; PS2562-1; PS2563-3; PS2564-2; PS2566-1; PS2567-1; PS2600-1; PS2602-3; PS2604-4; PS2605-1; PS2606-3; PS2607-1; PS2609-2; PS2610-2; PS2611-3; PS28; PS28/264; PS28/277; PS28/280; PS28/289; PS28/293; PS28/298; PS28/304; PS28/314; PS28/316; PS28/329; PS28/334; PS28/337; PS28/339; PS28/342; PS28/345; PS28/347; PS28/350; PS28/352; PS28/361; PS28/367; PS28/373; PS28/375; PS30; PS30/030; PS30/038; PS30/043; PS30/048; PS30/055; PS30/097; PS30/137; PS30/139; PS30/141; PS30/143; PS30/144; PS30/145; PS30/147; PS30/155; PS30/156; Scotia Sea, southwest Atlantic; Shona Ridge; SL; South Atlantic; South Atlantic Ocean; South Orkney; South Sandwich; South Sandwich Basin; South Sandwich Islands; South Sandwich Trough; van Veen Grab; Vestkapp; VGRAB; Weddell Sea; Wegener Canyon
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 135
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Niebler, Hans-Stefan (1995): Rekonstruktionen von Paläo-Umweltparametern anhand von stabilen Isotopen und Faunen-Vergesellschaftungen planktischer Foraminiferen im Südatlantik = Reconstruction of paleo-environmental parameters using stable isotopes and faunal assemblages of planktonic foraminifera in the South Atlantic Ocean. Berichte zur Polarforschung = Reports on Polar Research, 167, 198 pp, https://doi.org/10.2312/BzP_0167_1995
    Publication Date: 2024-07-01
    Description: Changes in surface water hydrography in the Southern Ocean (eastern Atlantic sector) could be reconstructed on the basis of isotope-geochemical and micropaleontological studies. A total of 75 high quality multicorer sediment surface samples from the southern South Atlantic Ocean and three Quaternary sediment cores, taken on a meridional transect across the Antarctic Circumpolar Current, have been investigated. The results of examining stable oxygen isotope compositions of 24 foraminiferal species and morphotypes were compared to the near-surface hydrography. The different foraminifera have been divided into four groups living at different depths in the upper water column. The 8180 differences between shallow-living (e.g. G. bulloides, N. pachyderma) and deeper-dwelling (e. g. G. inflata) species reflect the measured temperature gradient of the upper 250 m in the water column. Thus, the 6180 difference between shallow-living and deeper-living foraminifera can be used as an indicator for the vertical temperature gradient in the surface water of the Antarctic Circumpolar Current, which is independent of ice volume. All planktonic foraminifera in the surface sediment samples have been counted. 27 species and morphotypes have been selected, to form a reference data Set for statistical purposes. By using R- and Q-mode principal component analysis these planktonic foraminifera have been divided into four and five assemblages, respectively. The geographic distribution of these assemblages is mainly linked to the temperature of sea-surface waters. The five assemblages (factors) of the Q-mode principal component analysis account for 97.l % of the variance of original data. Following the transferfunction- technique a multiple regression between the Q-mode factors and the actual mean sea-surface environmental parameters resulted in a set of equations. The new transfer function can be used to estimate past sea-surface seasonal temperatures for paleoassemblages of planktonic foraminifera with a precision of approximately ±1.2°C. This transfer function F75-27-5 encompasses in particular the environmental conditions in the Atlantic sector of the Antarctic Circumpolar Current. During the last 140,000 years reconstructed sea-surface temperatures fluctuated in the present northern Subantarctic Zone (PS2076-1/3) at an amplitude of up to 7.5°C in summer and of up to 8.5°C in winter. In the present Polarfrontal Zone (PS1754-1) these fluctuations between glacials and interglacials show lower temperatures from 2.5 to 8.5°C in summer and from 1.0 to 5.0°C in winter, respectively. Compared to today, calculated oxygen isotope temperature gradients in the present Subantarctic Zone were lower during the last 140,000 years. This is an indicator for a good mixing of the upper water column. In the Polarfrontal Zone also lower oxygen isotope temperature gradients were found for the glacials 6, 4 and 2. But almost similar temperature gradients as today were found during the interglacial stages 5, 3 and the Holocene, which implicates a mixing of the upper water column compared to present. Paleosalinities were reconstructed by combining d18O-data and the evaluated transfer function paleotemperatures. Especially in the present Polarfrontal Zone (PS1754-1) and in the Antarctic Zone (PS1768-8), a short-term reduction of salinity up to 4 %o, could be detected. This significant reduction in sea-surface water salinity indicates the increased influx of melt-water at the beginning of deglaciation in the southern hemisphere at the end of the last glacial, approximately 16,500-13,000 years ago. The reconstruction of environmental Parameters indicates only small changes in the position of the frontal Systems in the eastern sector of the Antarctic Circumpolar Current during the last 140,000 years. The average position of the Subtropical Front and Subantarctic Front shifted approximately three latitudes between interglacials and glacials. The Antarctic Polar Front shifted approximately four latitudes. But substantial modifications of this scenario have been interpreted for the reconstruction of cold sea-surface temperatures at 41Â S during the oxygen isotope stages 16 and 14 to 12. During these times the Subtropical Front was probably shified up to seven latitudes northwards.
    Keywords: Agulhas Basin; ANT-IX/4; ANT-VI/3; ANT-VIII/3; ANT-X/4; ANT-X/5; ANT-X/6; Atlantic Indik Ridge; Atlantic Ridge; AWI_Paleo; Brazil Basin; Cape Basin; CTD/Rosette; CTD-RO; Discovery Seamount; GeoB1716-2; GeoB1717-2; GeoB1718-1; GeoB1719-5; GeoB1720-4; GeoB1721-4; GeoB1726-2; GeoB1728-3; GeoB1729-1; GeoB2002-2; GeoB2003-1; GeoB2004-1; GeoB2007-1; GeoB2008-1; GeoB2009-1; GeoB2016-3; GeoB2018-1; GeoB2019-2; GeoB2021-4; GeoB2022-3; Giant box corer; GKG; Gravity corer (Kiel type); KL; M20/2; M23/1; Meteor (1986); Meteor Rise; MIC; MiniCorer; MUC; MultiCorer; Namibia Continental Margin; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; PS12; PS12/557; PS16; PS16/262; PS16/267; PS16/271; PS16/278; PS16/281; PS16/284; PS16/294; PS16/303; PS16/311; PS16/312; PS16/334; PS16/337; PS16/342; PS16/345; PS16/351; PS1654-1; PS1750-7; PS1751-2; PS1752-5; PS1754-1; PS1754-2; PS1755-1; PS1756-6; PS1759-1; PS1764-2; PS1768-8; PS1769-1; PS1775-5; PS1776-6; PS1777-7; PS1778-1; PS1779-3; PS18; PS18/229; PS18/231; PS18/232; PS18/236; PS18/237; PS18/238; PS18/239; PS18/241; PS18/242; PS18/243; PS18/244; PS18/260; PS18/261; PS18/262; PS18/263; PS18/264; PS18/269; PS2073-1; PS2075-3; PS2076-1; PS2076-3; PS2080-1; PS2081-1; PS2082-3; PS2083-1; PS2084-2; PS2085-1; PS2085-2; PS2086-3; PS2087-1; PS2102-1; PS2102-2; PS2103-2; PS2104-1; PS2105-2; PS2106-1; PS21 06AQANTX_4; PS2110-1; PS22; PS22/678; PS22/755; PS22/840; PS22/841; PS22/842; PS22/850; PS22/851; PS22/852; PS22/853; PS22/879; PS22/899; PS22/902; PS22/908; PS22/947; 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; PS2250-5; PS2250-6; PS2272-1; PS2341-1; PS2342-1; PS2343-1; PS2351-1; PS2352-1; PS2353-2; PS2354-1; PS2363-1; PS2366-1; PS2367-1; PS2368-1; PS2372-1; PS2376-1; Shona Ridge; SL; South African margin; South Atlantic; South Atlantic Ocean; Van Heesen Ridge; Walvis Ridge
    Type: Dataset
    Format: application/zip, 22 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 136
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bollhöfer, A; Frank, Norbert; Rohloff, S; Mangini, Augusto; Scholten, Jan Christoph (1999): A record of changing redox conditions in the northern Peru Basin during the Late Quaternary deduced from Mn/Fe and growth rate variations in two diagenetic manganese nodules. Earth and Planetary Science Letters, 170(4), 403-415, https://doi.org/10.1016/S0012-821X(99)00126-0
    Publication Date: 2024-07-01
    Description: Two diagenetic manganese nodules from the Peru Basin were investigated by thermal ionization mass spectrometry and high resolution alpha spectrometry for uranium and thorium. The TIMS concentrations for nodule 62KD (63KG) vary as follows: 0.12-1.01 ppb (0.06-0.59) 230Th, 0.51-1.98 ppm (0.43-1.40) 232Th, 0.13-0.80 ppb (0.09-0.49) 234U, and 1.95-13.47 ppm (1.66-8.24) 238U. Both nodules have average growth rates of ~110 mm per million years. However, from the variations of excess 230Th with depth we estimate partial accumulation rates which range from 50 to 400 mm per million years. The 234U dating method cannot be applied due to remobilization of U from the sediment and subsequent incorporation into the nodules' crystal lattice, reflected by decay corrected 234U values far above the ocean water value. Sections of fast nodule growth are related to those layers having high Mn/Fe ratios (up to 200) and higher densities. As a possible explanation we develop a scenario that describes similar glacial/interglacial trends in both nodules as a record of regional changes of sediment and/or deep water chemistry.
    Keywords: Dredge, box; DRG_B; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Peru Basin; SEDIPERU - TUSCH; SO79; SO79_62KD; Sonne
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 137
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bollhöfer, A; Eisenhauer, Anton; Frank, Norbert; Pech, D; Mangini, Augusto (1996): Thorium and uranium isotopes in a manganese nodule from the Peru basin determined by alpha spectrometry and thermal ionization mass spectrometry (TIMS): Are manganese supply and growth related to climate? Geologische Rundschau, 85(3), 577-585, https://doi.org/10.1007/BF02369012
    Publication Date: 2024-07-01
    Description: Thorium and uranium isotopes were measured in a diagenetic manganese nodule from the Peru basin applying alpha- and thermal ionization mass spectrometry (TIMS). Alpha-counting of 62 samples was carried out with a depth resolution of 0.4 mm to gain a high-resolution Th-230(excess) profile. In addition, 17 samples were measured with TIMS to obtain precise isotope concentrations and isotope ratios. We got values of 0.06-0.59 ppb (Th-230), 0.43-1.40 ppm (Th-232), 0.09-0.49 ppb (U-234) and 1.66-8.24 ppm (U-238). The uranium activity ratio in the uppermost samples (1-6 mm) and in two further sections in the nodule at 12.5+/-1.0 mm and 27.3-33.5 mm comes close to the present ocean wa ter value of 1.144+/-0.004. In two other sections of the nodule, this ratio is significantly higher, probably reflecting incorporation of diagenetic uranium. The upper 25 mm section of the Mn nodule shows a relatively smooth exponential decrease in the Th-230(excess) concentration (TIMS). The slope of the best fit yields a growth rate of 110 mm/Ma up to 24.5 mm depth. The section from 25 to 30.3 mm depth shows constant Th-230(excess) concentrations probably due to growth rates even faster than those in the top section of the nodule. From 33 to 50 mm depth, the growth rate is approximately 60 mm/Ma. Two layers in the nodule with distinct laminations (11-15 and 28-33 mm depth) probably formed during the transition from isotopic stage 8 to 7 and in stage 5e, respectively. The Mn/Fe ratio shows higher values during interglacials 5 and 7, and lower ones during glacials 4 and 6. A comparison of our data with data from adjacent sediment cores suggests (a) a variable sb supply of hydrothermal Mn to sediments and Mn nodules of the Peru basin or (b) suboxic conditions at the water sediment interface during periods with lower Mn/Fe ratios.
    Keywords: BCR; Box corer (Reineck); GIK15561-1; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Peru Basin; SEDIPERU - TUSCH; SO79; SO79_63KG; Sonne
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 138
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-XI/1; AWI_Paleo; Density, wet bulk; Density Measuring System (DMS); DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; Porosity; PS2734-5; PS36; PS36/021; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Susceptibility unit, AWI, MS2C [145 mm]; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 2173 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 139
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-XI/1; AWI_Paleo; Density, wet bulk; Density Measuring System (DMS); DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; Porosity; PS2736-6; PS36; PS36/023; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Susceptibility unit, AWI, MS2C [145 mm]; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 2170 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 140
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-XI/1; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; Event label; Giant box corer; GKG; Laptev Sea; Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; Porosity; PS2737-4; PS36; PS36/024; Quaternary Environment of the Eurasian North; QUEEN; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 228 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 141
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Hochstetter Bugten, East Greenland; Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2621-4; PS31; PS31/127; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1566 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 142
    Publication Date: 2024-07-01
    Keywords: ARK-XI/1; AWI_Paleo; Density, wet bulk; Density Measuring System (DMS); DEPTH, sediment/rock; Gravity corer (Kiel type); Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; Porosity; PS2743-9; PS36; PS36/031; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Susceptibility unit, AWI, MS2C [145 mm]; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 543 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 143
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; East Greenland Sea; Event label; Gravity corer (Kiel type); Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2627-7; PS31; PS31/135; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1458 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 144
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; East Greenland Sea; Event label; Gravity corer (Kiel type); Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2641-4; PS31; PS31/154; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1513 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 145
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2640-6; PS31; PS31/152; Quaternary Environment of the Eurasian North; QUEEN; SL; Sofia Sund, East Greenland; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1513 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 146
    Publication Date: 2024-07-01
    Keywords: ARK-IX/4; AWI_Paleo; Barents Sea; DEPTH, sediment/rock; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2443-3; PS27; PS27/016; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Susceptibility unit, AWI, MS2C [145 mm]
    Type: Dataset
    Format: text/tab-separated-values, 207 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 147
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; East Greenland Sea; Event label; Gravity corer (Kiel type); Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2620-4; PS31; PS31/123; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1999 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 148
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Multi-Sensor Core Logger 14, GEOTEK; Norwegian-Greenland Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2616-4; PS31; PS31/116; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1232 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 149
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Greenland Sea; Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2618-4; PS31; PS31/121; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 4043 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 150
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-07-01
    Keywords: ARK-X/2; AWI_Paleo; Density, wet bulk; DEPTH, sediment/rock; Event label; Gravity corer (Kiel type); Hochstetter Bugten, East Greenland; Multi-Sensor Core Logger 14, GEOTEK; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2624-3; PS31; PS31/130; Quaternary Environment of the Eurasian North; QUEEN; SL; Susceptibility; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 2088 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...