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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Schlünz, Birger; Schneider, Ralph R; Müller, Peter J; Showers, William J; Wefer, Gerold (1999): Terrestrial organic carbon accumulation on the Amazon deep sea fan during the last glacial sea-level low stand. Chemical Geology, 159(1-4), 263-281, https://doi.org/10.1016/S0009-2541(99)00041-8
    Publication Date: 2024-06-25
    Description: Sediment cores from the Amazon deep sea fan recovered during R/V Meteor cruise 16-2 show in detail the modern areal distribution of sedimentary organic carbon, stable organic carbon isotopes of the organic matter (OM), as well as variations in the depositional processes. In addition, we studied up to 300 m long drilled sediment records recovered during ODP Leg 155 which allow evaluation of temporal variations on the Amazon fan. Our results reveal new evidence for a very rapid change of fan depositional processes and organic carbon source at times of sea-level change over the middle and lower Amazon fan. To estimate the amount of terrestrial organic carbon stored in sediments from the last glacial in the Amazon fan we used stable organic carbon isotopes of the OM (delta13Corg), organic carbon content (Corg), and age models based on oxygen isotopes, faunal data, and magnetic excursions. Following our results, the organic carbon accumulation on the Amazon deep sea fan is controlled by glacio-eustatic sea-level oscillations. Interglacial sea-level high stand sediments are dominated by marine OM whereas during glacial sea-level low stands terrestrial organic carbon is transported beyond the continental shelf through the Amazon canyon and deposited directly onto the Amazon deep sea fan. Glacial sediments of the Amazon fan stored approximately 73*10**15 g terrestrial Corg in 20,000 years or 3.7*10**12 g terrestrial Corg/yr (equivalent to 7-12% of the riverine organic carbon discharge; assuming constant paleo discharge), which is about the same amount of terrestrial organic carbon as deposited on the Amazon shelf today (3.1*10**12 g terrestrial Corg/yr or 6-10% of the modern riverine organic carbon discharge).
    Keywords: Amazon Fan; GeoB1511-5; GeoB1512-3; GeoB1513-1; GeoB1514-7; Gravity corer (Kiel type); M16/2; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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  • 2
    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: 2024-06-25
    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
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Vidal, Laurence; Schneider, Ralph R; Marchal, Olivier; Bickert, Torsten; Stocker, Thomas F; Wefer, Gerold (1999): Link between the North and South Atlantic during the Heinrich events of the last galcial period. Climate Dynamics, 15(12), 909-919, https://doi.org/10.1007/s003820050321
    Publication Date: 2024-06-25
    Description: High resolution benthic oxygen isotope records combined with radiocarbon datings, from cores retrieved in the North, Equatorial, and South Atlantic are used to establish a reliable cronostratigraphy for the last 60 ky. This common temporal framework enables us to study the timing of the sub-Milankovitch climate variability in the entire surface Atlantic during this period, as reflected in planktonic oxygen isotope records. Variations in sea surface temperatures in the Equatorial and South Atlantic reveal two warm periods during the mid-stage 3 which are correlated to the warming observed in the North Atlantic after Heinrich events (HL) 5 and 4. However, the records show that the warming started about 1500 y earlier in the South Atlantic. A zonally averaged ocean circulation model simulates a similar north-south thermal antiphasing between the latitudes of our coring sites, when pertubated by a freshwater flux anomaly. We infer that the observed phase relationship between the northern and the southern Atlantic is related to periods of reduced NADW production in the North Atlantic, such as during HL5 and HL4.
    Keywords: Amazon Fan; GeoB; GeoB1515-1; GeoB1515-2; GeoB1711; GeoB1711-4; Geosciences, University of Bremen; Giant box corer; GKG; Gravity corer (Kiel type); M16/2; M20/2; Meteor (1986); Namibia continental slope; SL
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Rühlemann, Carsten; Mulitza, Stefan; Müller, Peter J; Wefer, Gerold; Zahn, Rainer (1999): Warming of the tropical Atlantic Ocean and slowdown of thermohaline circulation during the last deglaciation. Nature, 402(6761), 511-514, https://doi.org/10.1038/990069
    Publication Date: 2024-06-25
    Description: Evidence for abrupt climate changes on millennial and shorter timescales is widespread in marine and terrestrial climate records (Dansgard et al., 1993, doi:10.1038/364218a0; Bond et al., 1993, doi:10.1038/365143a0; Charles et al., 1996, doi:10.1016/0012-821X(96)00083-0, Bard et al., 1997, doi:10.1038/385707a0). Rapid reorganization of ocean circulation is considered to exert some control over these changes (Broecker et al., 1985, doi:10.1038/315021a0), as are shifts in the concentrations of atmospheric greenhouse gases (Broecker, 1994, doi:10.1038/372421a0). The response of the climate system to these two influences is fundamentally different: slowing of thermohaline overturn in the North Atlantic Ocean is expected to decrease northward heat transport by the ocean and to induce warming of the tropical Atlantic (Crowley, 1992, doi:10.1029/92PA01058; Manabe and Stouffer, 1997, doi:10.1029/96PA03932), whereas atmospheric greenhouse forcing should cause roughly synchronous global temperature changes (Manabe et al., 1991, doi:10.1175/1520-0442(1991)004〈0785:TROACO〉2.0.CO;2). So these two mechanisms of climate change should be distinguishable by the timing of surface-water temperature variations relative to changes in deep-water circulation. Here we present a high-temporal-resolution record of sea surface temperatures from the western tropical North Atlantic Ocean which spans the past 29,000 years, derived from measurements of temperature-sensitive alkenone unsaturation in sedimentary organic matter. We find significant warming is documented for Heinrich event H1 (16,900-15,400 calendar years bp) and the Younger Dryas event (12,900-11,600 cal. yr bp), which were periods of intense cooling in the northern North Atlantic. Temperature changes in the tropical and high-latitude North Atlantic are out of phase, suggesting that the thermohaline circulation was the important trigger for these rapid climate changes.
    Keywords: Gravity corer (Kiel type); M35/1; M35003-4; Meteor (1986); SL
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Thomson, John; Nixon, S; Summerhayes, Colin P; Schönfeld, Joachim; Zahn, Rainer; Grootes, Pieter Meiert (1999): Implications for sedimentation changes on the Iberian margin over the last two glacial/interglacial transitions from (230Th-excess)0 systematics. Earth and Planetary Science Letters, 165(3-4), 255-270, https://doi.org/10.1016/S0012-821X(98)00265-9
    Publication Date: 2024-06-25
    Description: The Portuguese margin is well-suited for studies of the contrasts in North Atlantic circulation during glacial and interglacial times because of its rapid sediment accumulation rate. This paper reports a (230Thexcess)0-based study of sediment accumulation over the past 140 ky, a period which includes the last two glacial/interglacial transitions, in two cores at 2.4 and 3.5 km water depth on a slope transect at 40°N. Although the independently-determined mean sediment accumulation fluxes over the past 140 ky are unequivocally high with means of 13.2 and 10.5 g cm**-2 ky**-1 in the two cores, conventional application of the (230Thexcess)0 method yields consistently lower fluxes with means of 3.5 and 3.8 g cm**-2 ky**-1. These (230Thexcess)0 estimates are interpreted as representations of the regional depositional flux through time. This (230Thexcess)0 regional flux is composed of a carbonate flux of 〈1 g cm**-2 ky**-1and a larger and variable clay input which indicates the importance of the sea level control on the clay input to the basin. Clay flux dominates the regional sediment accumulation which has a total flux of ~2 g cm**-2 ky**-1and a CaCO3 content up to 50% in interglacial times, and a total flux up to ~5 g cm**-2 ky**-1and a CaCO3 content down to 10% in glacial times. This pattern of change of sediment composition through time is also typical of the NE Atlantic, and sediment focusing (contourite formation) appears responsible for the high actual fluxes observed in glacial compared with interglacial times on the Iberian margin. The inventories of (230Thexcess)0 exceed those which could have been supplied from the overlying water column alone over 140 ky by factors of *3.2 and *4.0 in the two cores. This is ascribed to preferential current focusing of fine sedimentary material in glacial times as a result of a systematic change in deep ocean circulation in response to climatic forcing. The presence of Heinrich events in the sediments is clearly evident, but at this southerly latitude they produce muted regional increases in accumulation flux (〈2 g cm**-2 ky**-1), apart from the large Heinrich event 4 which introduced an additional 10-20 g cm cm**-2 ky**-1 over ambient background levels.
    Keywords: CALYPSO; Calypso Corer; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952039; MD95-2039; MD952040; MD95-2040; Porto Seamount
    Type: Dataset
    Format: application/zip, 8 datasets
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Pacific Oceanology Institute, Far East Branch of Russian Academy of Sciences | Supplement to: Astakhova, N V; Sorochinskaya, A V (1999): Authigenic carbonates in Upper Pleistocene - Holocene deposits of marginal seas, Northwest Pacific. Tikhookeanskaya Geologiya (Pacific Geology), 18(1), 41-49
    Publication Date: 2024-06-25
    Description: The paper presents data on authigenic carbonate distribution in Holocene - Upper Pleistocene deposits of the Okhotsk, Japan, East China, Philippine and South China Seas. Description of carbonate samples, their chemical and isotope compositions are given. Chemical analysis of the samples indicates that almost all authigenic carbonates are composed of calcite or magnesian calcite; and only in one case, of siderite. Oxygen isotopic composition (d18O) ranges from +37.7 to +26.1 per mil (SMOW); it is, probably, connected with different temperatures of carbonate formation. A distinct geographic regularity is traced. Decrease in d18O values is observed from the cold Okhotsk Sea to the warm South China Sea. A very wide range of carbon isotopic composition (d13C from -42 to +3.8 per mil) indicates different sources of carbonic acid required for formation of these carbonates. As a basis for carbon isotopic composition we can distinguish three sources of carbonic acid in the studied sediments: microbiological methane oxidation, organic matter destruction during sediment diagenesis, and dissolved organogenic limestone. Thus, formation of authigenic carbonates in sediments from the marginal seas of the Northwest Pacific results from: 1) sediment diagenesis, 2) methane oxidation in zones of gas anomalies, 3) their precipitation from the supersaturated by carbonates sea shoal waters of tropical sea lagoons.
    Keywords: Akademik A Nesmeyanov; Akademik M.A. Lavrentyev; AN_1993; AN25-936; Archive of Ocean Data; ARCOD; AS-99-119; AS-99-3155; AS-99-89102; AS-99-8935; AS-99-8937; AS-99-E35; AS-99-T-03B; AS-99-T-21; Ast-82156; Ast-8785; Ast-E29; BC; Box corer; Dredge; DRG; GC; Gravity corer; Gravity corer (Kiel type); LV27/GREGORY; LV27-1-2; LV27-1-3; LV27-1A; LV27-2-3; MUC; MULT; MultiCorer; Multiple investigations; Nesmeyanov-93_9312; Obzh-89228; Okhotsk Sea; P31-3161; Sea of Okhotsk; SL; South China Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Gingele, Franz; Schmiedl, Gerhard (1999): Comparison of independant proxies on deep water advection in the southeast Atlantic off Namibia. South African Journal of Marine Science, 21, 181-190, https://doi.org/10.2989/025776199784126079
    Publication Date: 2024-06-25
    Description: Independent proxies were assessed in two Late Quaternary sediment cores from the eastern South Atlantic to compare deep-water changes during the last 400 kyr. Two cores were recovered from beneath North Atlantic Deep Water (NADW) at approximately 3 000 m depth. Late Quaternary presence of NADW is indicated by the Cibicidoides wuellerstorfi assemblage on the Walvis Ridge (Core GeoB 1214) and the Bulimina alazanensis assemblage on the Namibian continental slope (Core GeoB 1710). The propagation of NADW is exclusively observed during interglacials, with maximum factor loadings in Stages 1, 5, 7, 9 and 11. These maxima are consistent with peaks in kaolinite/chlorite ratios and maxima of poorly crystalline smectite in the clay-mineral record. Kaolinite and poorly crystalline smectite are products of intense chemical weathering. They are injected into the NADW at low latitudes, north of the study area, and advected south. Chlorite, which is stable under cold weathering regimes, is a characteristic mineral of water masses of southern origin. During glacial stages, it is advected north with Southern Component Water (SCW). Above the NADW/SCW depths, kaolinite/chlorite ratios vary only slightly without a significant glacial-interglacial pattern, as measured in a core (GeoB 1712) from 1 000 m deep on the same profile of the Namibian continental slope off Walvis Bay.
    Keywords: GeoB; GeoB1710-3; GeoB1712-4; Geosciences, University of Bremen; Gravity corer (Kiel type); M20/2; Meteor (1986); Namibia continental slope; SL
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
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    PANGAEA
    In:  Supplement to: Stein, Ruediger; Fahl, Kirsten; Niessen, Frank; Siebold, Martina (1999): Late quaternary organic carbon and biomarker records from the Laptev Sea continental margin (Arctic Ocean): implications for organic carbon flux and composition. In: Kassens, H; Bauch, H A; Dmitrenko, I A; Eicken, H; Hubberten, H-W; Melles, M; Thiede, J & Timokhov, L A (eds.), Land-ocean systems in the Siberian Arctic: dynamics and history, Springer, Berlin, Heidelberg, 635-656
    Publication Date: 2024-06-25
    Description: In order to understand the processes controlling organic carbon deposition (i.e., primary productivity vs. terrigenous supply) and their paleoceanographic significance, three sediment cores (PS2471, PS2474. and PS2476) from the Laptev Sea continental margin were investigated for their content and composition of organic carbon. The characterization of organic matter indudes the determination of buk parameters (hydrogen index values and C/N ratios) and the analysis of specific biomarkers (n-alaknes, fatty acids, alkenones, and pigments). Total organic carbon (TOC) values vary between 0.3 and 2%. In general, the organic matter from the Laptev Sea continental margin is dominated by terrigenous matter throughout. However. significant amounts of marine organic carbon occur. The turbidites, according to a still preliminary stratigraphy probably deposited during glacial Oxygen Isotope Stages 2 and 4, are characterized by maximum amounts of organic carbon of terrigenous origin. Marine organic carbon appears to show enhanced relative abundances in the Termination I (?) and early Holocene time intervals, as indicated by maximum amounts of short chain n-alkanes, short-chain fatty acids, and alkenones. The increased amounts of faity acids, however, may also have a freshwater origin due to increased river discharge at that time. The occurrence of alkenones is suggested to indicate an intensification of Atlantic water inflow along the Eurasian continental margin starting at that time. Oxygen Isotope Stage l accumutation rates of total organic carhon are 0.3, 0.17, and 0.02 C/cm**2/ky in cores PS2476, PS2474, and PS2471, respectively.
    Keywords: Amundsen Basin; ARK-IX/4; ARK-VIII/3; AWI_Paleo; Gakkel Ridge, Arctic Ocean; Giant box corer; Giant piston corer; GKG; GPC; Gravity corer (Kiel type); KAL; Kasten corer; Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/157; PS19/165; PS19 ARCTIC91; PS2163-4; PS2170-3; PS2471-4; PS2474-2; PS2474-3; PS2476-3; PS2476-4; PS27; PS27/054; PS27/059; PS27/062; Quaternary Environment of the Eurasian North; QUEEN; SL
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Dokken, Trond; Jansen, Eystein (1999): Rapid changes in the mechanism of ocean convection during the last glacial period. Nature, 401(6752), 458-461, https://doi.org/10.1038/46753
    Publication Date: 2024-06-25
    Description: High-amplitude, rapid climate fluctuations are common features of glacial times. The prominent changes in air temperature recorded in the Greenland ice cores (Dansgaard et al., 1993, doi:10.1038/339532a0; Grootes et al., 1993 doi:10.1038/366552a0) are coherent with shifts in the magnitude of the northward heat flux carried by the North Atlantic surface ocean (Bond et al., 1993, doi:10.1038/365143a0; Bond and Lotti, 1995, doi:10.1126/science.267.5200.1005); changes in the ocean's thermohaline circulation are a key component in many explanations of this climate flickering (Broecker, 1997, doi:10.1126/science.278.5343.1582). Here we use stable-isotope and other sedimentological data to reveal specific oceanic reorganizations during these rapid climate-change events. Deep water was generated more or less continuously in the Nordic Seas during the latter part of the last glacial period (60 to 10 thousand years ago), but by two different mechanisms. The deep-water formation occurred by convection in the open ocean during warmer periods (interstadials). But during colder phases (stadials), a freshening of the surface ocean reduced or stopped open-ocean convection, and deep-water formation was instead driven by brine-release during sea-ice freezing. These shifting magnitudes and modes nested within the overall continuity of deep-water formation were probably important for the structuring and rapidity of the prevailing climate changes.
    Keywords: CALYPSO; Calypso Corer; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952010; MD95-2010; Voring Plateau
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Cacho, Isabel; Grimalt, Joan O; Pelejero, Carles; Canals, Miquel; Sierro, Francisco Javier; Flores, José-Abel; Shackleton, Nicholas J (1999): Dansgaard-Oeschger and Heinrich event imprints in the Alboran Sea paleotemperature record. Paleoceanography, 14(6), 698-705, https://doi.org/10.1029/1999PA900044
    Publication Date: 2024-06-25
    Description: Past sea surface temperature (SST) evolution in the Alboran Sea (western Mediterranean) during the last 50,000 years has been inferred from the study of C37 alkenones in International Marine Global Change Studies MD952043 core. This record has a time resolution of ~200 years allowing the study of millennial-scale and even shorter climatic changes. The observed SST curve displays characteristic sequences of extremely rapid warming and cooling events along the glacial period. Comparison of this Alboran record with delta18O from Greenland ice (Greenland Ice Sheet Project 2 core) shows a strong parallelism between these SST oscillations and the Dansgaard-Oeschger events. Five prominent cooling episodes standing out in the SST profile are accompanied by an anomalous high abundance of Neogloboquadrina pachyderma sinistral which is confined to the duration of these cold intervals. These features and the isotopic record reflect drastic changes in the surface hydrography of the Alboran Sea in association with Heinrich events Hl-5.
    Keywords: Alboran Sea; CALYPSO; Calypso Corer; IMAGES I; Marion Dufresne (1995); MD101; MD952043; MD95-2043
    Type: Dataset
    Format: application/zip, 2 datasets
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