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  • 2005-2009  (17)
  • 2000-2004  (15)
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Year
  • 11
    Publication Date: 2023-10-21
    Keywords: Age, 14C AMS; Age, dated; DEPTH, sediment/rock; GeoB; Geosciences, University of Bremen; NIOZ89; PC; Piston corer; SFB261; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Southeast Atlantic; T89-16; T89-16-PC; Tyro
    Type: Dataset
    Format: text/tab-separated-values, 23 data points
    Location Call Number Limitation Availability
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  • 12
    Publication Date: 2023-11-30
    Keywords: 24-Ethylcholest-5-en-3beta-ol per unit sediment mass; 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per unit sediment mass; Alkenone per unit sediment mass; Anker24; Anker26; BC; Box corer; C40 biphytanediols per unit sediment mass; Cholesterol per unit sediment mass; Delta 22-cholesterol per unit sediment mass; DEPTH, sediment/rock; Diatomsterol per unit sediment mass; Elevation of event; Event label; Gas chromatography; Gas chromatography - Mass spectrometry (GC-MS); GeoB; Geosciences, University of Bremen; Grab; GRAB; Latitude of event; Loliolide per unit sediment mass; Long-chain fatty acids C24+C26+C28 per unit sediment mass; Longitude of event; n-Alkanol long chain alcohols C24+C26+C28 per unit sediment mass; NIOZ89; Southeast Atlantic; stigmasta-5,24(28)-dien-3-ol per unit sediment mass; Sum C28-C32 diols per unit sediment mass; T89-10; T89-11; T89-12; T89-13; T89-14; T89-15; T89-16; T89-17; T89-19; T89-20; T89-21; T89-22; T89-23; T89-25; T89-28; T89-30; T89-31; T89-32; T89-33; T89-34; T89-35; T89-36; T89-40; T89-41; T89-42-1; T89-47; Tyro
    Type: Dataset
    Format: text/tab-separated-values, 303 data points
    Location Call Number Limitation Availability
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  • 13
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    Unknown
    PANGAEA
    In:  Supplement to: Schefuß, Enno; Versteegh, Gerard J M; Jansen, J H Fred; Sinninghe Damsté, Jaap S (2001): Marine and terrigenous lipids in southeast Atlantic sediments (Leg 175) as paleoenvironmental indicators: Initial results. In: Wefer, G; Berger, WH; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 175, 1-23, https://doi.org/10.2973/odp.proc.sr.175.228.2001
    Publication Date: 2024-01-09
    Description: Lipid compositions of sediments recovered during Ocean Drilling Program Leg 175 in the eastern South Atlantic reflect a variety of oceanographic and climatological environments. Most of the identified lipids can be ascribed to marine sources, notably haptophytes, eustigmatophytes, dinoflagellates, archaea, and diatoms. Elevated concentrations of cholesterol suggest zooplankton herbivory, characteristic for sites influenced by upwelling. At these sites, sulfurized highly branched isoprenoids from diatoms are also present in high amounts. Sterols, sterol ethers, hopanoids, and midchain hydroxy fatty acids could also be detected. Terrigenous lipids are n-alkanes, fatty acids, n-alcohols, and triterpenoid compounds like taraxerol and -amyrine. n-Alkanes, fatty acids, and n-alcohols are derived from leaf waxes of higher land plants and transported to the sea by airborne dust or fresh water. Triterpenoid compounds are most probably derived from mangroves and transported solely by rivers. Lipid compositions below the Congo low-salinity plume are strongly influenced by terrigenous material from the Congo River. Elevated organic carbon contents and predominantly marine lipid distributions at the Angola margin may indicate a highly productive plankton population, probably sustained by the Angola Dome. Sedimentary lipids in the Walvis Basin contain an upwelling signal, likely transported by the Benguela Current. Sedimentary lipids off Lüderitz Bay and in the southern Cape Basin are dominated by plankton lipids in high to intermediate amounts, reflecting persistent and seasonal upwelling, respectively.
    Keywords: 175-1076A; 175-1077A; 175-1079A; 175-1082A; 175-1084A; 175-1085A; Benguela Current, South Atlantic Ocean; DRILL; Drilling/drill rig; Joides Resolution; Leg175; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 14
    Publication Date: 2024-02-02
    Keywords: Age, 14C AMS; Age, 14C calibrated, CALIB 4.4 (Stuiver et al., 2003); Age, dated; Age, dated, error to older; Age, dated, error to younger; Age, maximum/old; Age, minimum/young; Calendar age; Center for Marine Environmental Sciences; Congo Fan; DEPTH, sediment/rock; GeoB6518-1; Gravity corer (Kiel type); M47/3; MARUM; Meteor (1986); Sample code/label; SL
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
    Location Call Number Limitation Availability
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  • 15
    Publication Date: 2024-02-02
    Keywords: AGE; Alkenone, unsaturation index UK'37; Calculated; Calculated, see reference(s); Calculated from C37 alkenones (Prahl & Wakeham, 1987); Center for Marine Environmental Sciences; Congo Fan; DEPTH, sediment/rock; GeoB6518-1; Globigerinoides ruber white, δ18O; Gravity corer (Kiel type); M47/3; MARUM; Mass spectrometer Finnigan MAT 251; Mass spectrometer Finnigan MAT 252; Mass spectrometer Thermo Electron Delta plus XL; Meteor (1986); n-Alkane C29, δ13C; n-Alkane C29, δ13C, standard deviation; n-Alkane C29, δD; n-Alkane C29, δD, standard deviation; Sea surface temperature, annual mean; SL; δ18O, water
    Type: Dataset
    Format: text/tab-separated-values, 989 data points
    Location Call Number Limitation Availability
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  • 16
    Publication Date: 2024-02-02
    Keywords: AEOLD; Aeolian dust sample; ALTITUDE; Center for Marine Environmental Sciences; D1; D10; D11; D12; D13; D14; D15; D16; D17; D18; D19; D20; D21; D22; D23; D24; D25; D3; D4; D5; D6; D7; D8; D9; Event label; GeoB; Geosciences, University of Bremen; LATITUDE; Latitude 2; LONGITUDE; Longitude 2; M41/1; M41/1_D1; M41/1_D10; M41/1_D11; M41/1_D12; M41/1_D13; M41/1_D14; M41/1_D15; M41/1_D16; M41/1_D17; M41/1_D18; M41/1_D19; M41/1_D2; M41/1_D20; M41/1_D21; M41/1_D22; M41/1_D23; M41/1_D24; M41/1_D25; M41/1_D3; M41/1_D4; M41/1_D5; M41/1_D6; M41/1_D7; M41/1_D8; M41/1_D9; MARUM; Meteor (1986); Pressure, at given altitude; Time in hours; Weather Balloon; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 132 data points
    Location Call Number Limitation Availability
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  • 17
    Publication Date: 2024-02-02
    Keywords: AEOLD; Aeolian dust sample; ALTITUDE; Beckman Coulter Laser diffraction particle size analyzer LS 230; Center for Marine Environmental Sciences; D1; D10; D11; D12; D13; D14; D15; D16; D17; D18; D19; D20; D21; D23; D24; D25; D3; D4; D5; D6; D7; D8; D9; Event label; GeoB; Geosciences, University of Bremen; Latitude 2; Longitude 2; M41/1; M41/1_D1; M41/1_D10; M41/1_D11; M41/1_D12; M41/1_D13; M41/1_D14; M41/1_D15; M41/1_D16; M41/1_D17; M41/1_D18; M41/1_D19; M41/1_D2; M41/1_D20; M41/1_D21; M41/1_D23; M41/1_D24; M41/1_D25; M41/1_D3; M41/1_D4; M41/1_D5; M41/1_D6; M41/1_D7; M41/1_D8; M41/1_D9; MARUM; Meteor (1986); Size fraction 0.412-0.375 µm; Size fraction 0.452-0.412 µm; Size fraction 0.496-0.452 µm; Size fraction 0.545-0.496 µm; Size fraction 0.598-0.545 µm; Size fraction 0.656-0.598 µm; Size fraction 0.721-0.656 µm; Size fraction 0.791-0.721 µm; Size fraction 0.868-0.791 µm; Size fraction 0.948-1.041 mm; Size fraction 0.953-0.868 µm; Size fraction 1.041-1.143 mm; Size fraction 1.047-0.953 µm; Size fraction 1.143-1.255 mm; Size fraction 1.149-1.047 µm; Size fraction 1.255-1.377 mm; Size fraction 1.261-1.149 µm; Size fraction 1.377-1.512 mm; Size fraction 1.384 -1.261 µm; Size fraction 1.512-1.660 mm; Size fraction 1.520-1.384 µm; Size fraction 1.668-1.520 µm; Size fraction 1.822-1.660 mm; Size fraction 1.832-1.668 µm; Size fraction 10.78-9.818 µm; Size fraction 101.1-92.09 µm; Size fraction 11.83-10.78 µm; Size fraction 111.0-101.1 µm; Size fraction 12.99-11.83 µm; Size fraction 121.8-111.0 µm; Size fraction 133.7-121.8 µm; Size fraction 14.26-12.99 µm; Size fraction 146.8-133.7 µm; Size fraction 15.65-14.26 µm; Size fraction 161.2-146.8 µm; Size fraction 17.18-15.65 µm; Size fraction 176.8-161.2 µm; Size fraction 18.86-17.18 µm; Size fraction 194.2-176.8 µm; Size fraction 2.000-1.822 mm; Size fraction 2.010-1.832 µm; Size fraction 2.207-2.010 µm; Size fraction 2.423-2.207 µm; Size fraction 2.660-2.423 µm; Size fraction 2.920-2.660 µm; Size fraction 20.70-18.86 µm; Size fraction 213.2-194.2 µm; Size fraction 213.2-234.1 µm; Size fraction 22.73-20.70 µm; Size fraction 234.1-256.8 µm; Size fraction 24.95-22.73 µm; Size fraction 256.8-282.1 µm; Size fraction 27.38-24.95 µm; Size fraction 282.1-309.6 µm; Size fraction 3.205-2.920 µm; Size fraction 3.519-3.205 µm; Size fraction 3.862-3.519 µm; Size fraction 30.07-27.38 µm; Size fraction 309.6-339.8 µm; Size fraction 33.01-30.07 µm; Size fraction 339.8-373.1 µm; Size fraction 36.24-33.01 µm; Size fraction 373.1-409.6 µm; Size fraction 39.77-36.24 µm; Size fraction 4.240-3.863 µm; Size fraction 4.655-4.240 µm; Size fraction 409.6-449.7 µm; Size fraction 43.67-39.78 µm; Size fraction 449.7-493.6 µm; Size fraction 47.94-43.67 µm; Size fraction 493.6-541.9 µm; Size fraction 5.110-4.655 µm; Size fraction 5.610-5.110 µm; Size fraction 52.62-47.94 µm; Size fraction 541.9-594.9 µm; Size fraction 57.77-52.62 µm; Size fraction 594.9-653.0 µm; Size fraction 6.158-5.611 µm; Size fraction 6.761-6.158 µm; Size fraction 63.41-57.77 µm; Size fraction 653.0-716.9 µm; Size fraction 69.62-63.41 µm; Size fraction 7.421-6.760 µm; Size fraction 716.9-786.9 µm; Size fraction 76.42-69.61 µm; Size fraction 786.9-863.9 µm; Size fraction 8.147-7.421 µm; Size fraction 8.943-8.147 µm; Size fraction 83.89-76.42 µm; Size fraction 863.9-948.2 µm; Size fraction 9.818-8.943 µm; Size fraction 92.09-83.90 µm
    Type: Dataset
    Format: text/tab-separated-values, 2256 data points
    Location Call Number Limitation Availability
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  • 18
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    Unknown
    PANGAEA
    In:  Supplement to: Scourse, James D; Marret, Fabienne; Versteegh, Gerard J M; Jansen, J H Fred; Schefuß, Enno; van der Plicht, Johannes (2005): High resolution last deglaciation record from the Congo fan reveals significance of mangrove pollen and biomarkers as indicators of shelf transgression. Quaternary Research, 64(1), 57-69, https://doi.org/10.1016/j.yqres.2005.03.002
    Publication Date: 2024-03-06
    Description: High abundances of mangrove pollen have been associated with transgressive cycles on tropical margins, but the detailed relations between systems tracts and the taphonomy of the pollen are unclear. We report here the occurrence and high abundance of Rhizophora pollen, in association with taraxerol, a Rhizophora-sourced biomarker, from a high-resolution Congo fan core covering the last deglaciation. An age model based on 14C dates enables the temporal changes in taraxerol content and the percentage frequencies and flux (pollen grains (pg)/cm**2/(10**3 yr)) of mangrove pollen to be compared quantitatively with the lateral rate of transgression across the flooding surface (derived from glacio-hydro-isostatic model output and the bathymetry of the margin). Rhizophora pollen concentrations and taraxerol content of the sediment are very strongly positively correlated with the lateral rate of transgression and indicate, independently of any sequence stratigraphic context, that mangrove pollen spikes are associated with the transgressive systems tract rather than the highstand systems tract or maximum flooding surface. Lower-resolution longer-term records from this margin indicate an association between taraxerol concentrations and transgressive rather than regressive phases. The flux of these materials to the Congo fan is interpreted as a function of the erosion of flooded mangrove swamp on the shelf and, less importantly, changing extent of mangrove habitat, during sea-level rise. Congo River palaeoflood events also result in reworking of mangrove pollen and supply to the fan, but this mechanism is subdominant. Rhizophora pollen has been underestimated in many palynological studies undertaken on cores from the African margin because of inappropriate sieve mesh size used during laboratory preparation.
    Keywords: Acacia; Alchornea; Allophylus; Altenanthera; Araliaceae; Asteraceae; Canthium; Caryophyllaceae; Cassia; Celtis; Chenopodiaceae; Cochlospermum-type; Combretaceae; Cyperaceae; DEPTH, sediment/rock; Diospyros; Dobera-type; Ebenaceae undifferentiated; Euphorbiaceae; Fagara; Ficus; Hymenocardia; Isoberlinia; Lannea; Liliaceae; Macaranga-type; Manilkara; Myrica; Myrtaceae; Nauclea; NIOZ89; Oleaceae; PC; Piston corer; Poaceae; Podocarpus; Pollen, total; Pollen indeterminata; Pseudarthria; Rhizophora; Rubiaceae; Rullia; Salvadoraceae; Sapindaceae; Schefflera; Schrebera; Securinega; Size fraction; Southeast Atlantic; Spores; Spores, monolete; Spores, trilete; Syncepalum; Syzygium; T89-16; T89-16-PC; Tamarindus; Tetrochidium; Tyro; Uapaca
    Type: Dataset
    Format: text/tab-separated-values, 423 data points
    Location Call Number Limitation Availability
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  • 19
    Publication Date: 2024-01-09
    Keywords: 175-1076A; 175-1077A; 175-1079A; 175-1082A; 175-1084A; 175-1085A; AGE; Benguela Current, South Atlantic Ocean; Carbon, organic, total; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Flash combustion at 1050°C in a Carlo Erba NA1500 Analyser; Joides Resolution; Latitude of event; Leg175; Longitude of event; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
    Location Call Number Limitation Availability
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  • 20
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    Unknown
    PANGAEA
    In:  Supplement to: Schefuß, Enno; Sinninghe Damsté, Jaap S; Jansen, J H Fred (2004): Forcing of tropical Atlantic sea surface temperatures during the mid-Pleistocene transition. Paleoceanography, 19, PA4029, https://doi.org/10.1029/2003PA000892
    Publication Date: 2024-01-09
    Description: We compare a new mid-Pleistocene sea surface temperature (SST) record from the eastern tropical Atlantic to changes in continental ice volume, orbital insolation, Atlantic deepwater ventilation, and Southern Ocean front positions to resolve forcing mechanisms of tropical Atlantic SST during the mid-Pleistocene transition (MPT). At the onset of the MPT, a strong tropical cooling occurred. The change from a obliquity- to a eccentricity-dominated cyclicity in the tropical SST took place at about 650 kyr BP. In orbital cycles, tropical SST changes significantly preceded continental ice-volume changes but were in phase with movements of Southern Ocean fronts. After the onset of large-amplitude 100-kyr variations, additional late glacial warming in the eastern tropical Atlantic was caused by enhanced return flow of warm waters from the western Atlantic driven by strong trade winds. Pronounced 80-kyr variations in tropical SST occurred during the MPT, in phase with and likely directly forced by transitional continental ice-volume variations. During the MPT, a prominent anomalous long-term tropical warming occurred, likely generated by extremely northward displaced Southern Ocean fronts. While the overall pattern of global climate variability during the MPT was determined by changes in mean state and frequency of continental ice volume variations, tropical Atlantic SST variations were primarily driven by early changes in Subantarctic sea-ice extent and coupled Southern Ocean frontal positions.
    Keywords: 175-1077B; AGE; Alkenone, unsaturation index UK'37; Benguela Current, South Atlantic Ocean; Calculated from C37 alkenones (Brassell et al., 1986); Calculated from C37 alkenones (Prahl & Wakeham, 1987); Center for Marine Environmental Sciences; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Intercore correlation; Joides Resolution; Leg175; MARUM; Ocean Drilling Program; ODP; Sample code/label; Sea surface temperature, annual mean
    Type: Dataset
    Format: text/tab-separated-values, 856 data points
    Location Call Number Limitation Availability
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