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  • 2005-2009  (15)
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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: de Vernal, Anne; Eynaud, Frédérique; Henry, Maryse; Hillaire-Marcel, Claude; Londeix, Laurent; Mangin, Sylvie; Matthiessen, Jens; Marret, Fabienne; Radi, Taoufik; Rochon, André; Solignac, Sandrine; Turon, Jean-Louis (2005): Reconstruction of sea-surface conditions at middle to highlatitudes of the Northern Hemisphere during the Last Glacial Maximum(LGM) based on dinoflagellate cyst assemblages. Quaternary Science Reviews, 24(7-9), 897-924, https://doi.org/10.1016/j.quascirev.2004.06.014
    Publication Date: 2023-10-21
    Description: A new calibration database of census counts of organic-walled dinoflagellate cyst (dinocyst) assemblages has been developed from the analyses of surface sediment samples collected at middle to high latitudes of the Northern Hemisphere after standardisation of taxonomy and laboratory procedures. The database comprises 940 reference data points from the North Atlantic, Arctic and North Pacific oceans and their adjacent seas, including the Mediterranean Sea, as well as epicontinental environments such as the Estuary and Gulf of St. Lawrence, the Bering Sea and the Hudson Bay. The relative abundance of taxa was analysed to describe the distribution of assemblages. The best analogue technique was used for the reconstruction of Last Glacial Maximum (LGM) sea-surface temperature and salinity during summer and winter, in addition to sea-ice cover extent, at sites from the North Atlantic (n=63), Mediterranean Sea (n=1) and eastern North Pacific (n=1). Three of the North Atlantic cores, from the continental margin of eastern Canada, revealed a barren LGM interval, probably because of quasi-permanent sea ice. Six other cores from the Greenland and Norwegian seas were excluded from the compilation because of too sparse assemblages and poor analogue situation. At the remaining sites (n= 54), relatively close modern analogues were found for most LGM samples, which allowed reconstructions. The new LGM results are consistent with previous reconstructions based on dinocyst data, which show much cooler conditions than at present along the continental margins of Canada and Europe, but sharp gradients of increasing temperature offshore. The results also suggest low salinity and larger than present contrasts in seasonal temperatures with colder winters and more extensive sea-ice cover, whereas relatively warm conditions may have prevailed offshore in summer. From these data, we hypothesise low thermal inertia in a shallow and low-density surface water layer.
    Keywords: LIT; Literary studies; MARGO; MARGO_0000; Multiproxy Approach for the Reconstruction of the Glacial Ocean surface
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-11-28
    Keywords: 286; 287; 288; 289; 290; 291; 293; 295; 297; 298; 300; 301; 302; 303; 304; 305; 306; 307; 310; 311; 312; 313; 314; 316; 317; 318; 319; 320; 321; 322; 323; 324; 326; 327; 329; 330; 331; Bitectatodinium spongium; Brigantedinium spp.; Center for Marine Environmental Sciences; Counting, palynology; DEPTH, sediment/rock; Dinoflagellate cyst; Dinoflagellate cyst indeterminata; Dubridinium spp.; Echinidinium aculeatum; Echinidinium delicatum; Echinidinium granulatum; Echinidinium spp.; Echinidinium transparantum; Elevation of event; Event label; GeoB9501-4; GeoB9502-5; GeoB9503-3; GeoB9504-4; GeoB9505-3; GeoB9506-3; GeoB9508-4; GeoB9510-3; GeoB9512-4; GeoB9513-5; GeoB9515-2; GeoB9516-4; GeoB9517-5; GeoB9518-4; GeoB9519-6; GeoB9520-4; GeoB9521-3; GeoB9522-2; GeoB9525-5; GeoB9526-4; GeoB9527-6; GeoB9528-1; GeoB9529-1; GeoB9531-2; GeoB9532-1; GeoB9533-3; GeoB9534-4; GeoB9535-5; GeoB9536-4; GeoB9537-4; GeoB9538-5; GeoB9539-1; GeoB9541-1; GeoB9542-1; GeoB9544-1; GeoB9545-1; GeoB9546-1; Impagidinium aculeatum; Impagidinium paradoxum; Impagidinium patulum; Impagidinium spp.; Latitude of event; Leujeunocysta oliva; Lingulodinium machaerophorum; Longitude of event; M65/1; MARUM; Mauritania Canyon; Meteor (1986); MUC; MultiCorer; Nematosphaeropsis labyrinthus; Operculodinium centrocarpum; Operculodinium israelianum; Pentapharsodinium dalei; Polykrikos kofoidii; Polysphaeridium zoharyi; Protoperidinium americanum; Protoperidinium monospinum; Protoperidinium spp.; Protoperidinium stellatum; Quinquecuspis concreta; Selenopemphix nephroides; Selenopemphix quanta; Spiniferites bentori; Spiniferites bulloides; Spiniferites hyperacanthus; Spiniferites mirabilis; Spiniferites pachydermus; Spiniferites ramosus; Spiniferites spp.; Stelladinium spp.; Trinovantedinium applanatum; Tuberculodinium vancampoae; Votadinium calvum; Votadinium spinosum; Xandarodinium xanthum
    Type: Dataset
    Format: text/tab-separated-values, 1591 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-02-02
    Keywords: 286; 287; 288; 289; 290; 291; 293; 295; 297; 298; 300; 301; 302; 303; 304; 305; 306; 307; 310; 311; 312; 313; 314; 316; 317; 318; 319; 320; 321; 322; 323; 324; 326; 327; 329; 330; 331; 371; 376; 388; Atlantic Ocean; Calculated, see reference(s); Center for Marine Environmental Sciences; Chlorophyll a; Counting, palynology; DEPTH, sediment/rock; Dinoflagellate cyst; Dinoflagellate cyst per unit mass; Eckernfoerder Bay; Elevation of event; Event label; GeoB9501-4; GeoB9502-5; GeoB9503-3; GeoB9504-4; GeoB9505-3; GeoB9506-3; GeoB9508-4; GeoB9510-3; GeoB9512-4; GeoB9513-5; GeoB9515-2; GeoB9516-4; GeoB9517-5; GeoB9518-4; GeoB9519-6; GeoB9520-4; GeoB9521-3; GeoB9522-2; GeoB9525-5; GeoB9526-4; GeoB9527-6; GeoB9528-1; GeoB9529-1; GeoB9531-2; GeoB9532-1; GeoB9533-3; GeoB9534-4; GeoB9535-5; GeoB9536-4; GeoB9537-4; GeoB9538-5; GeoB9539-1; GeoB9541-1; GeoB9542-1; GeoB9544-1; GeoB9545-1; GeoB9546-1; GEOTROPEX 83, NOAMP I; Giant box corer; GIK16402-1; GIK16404-1; GIK16405-1; GIK16407-1; GIK16414-1; GIK16421-1; GIK16425-1; GIK16437-3; GIK16558-1; GIK16755-1; GIK16764-1; GIK16765-1; GIK16766-1; GIK16767-1; GIK16768-1; GIK16769-1; GKG; Gravity corer (Kiel type); Latitude of event; LI198x; Littorina; Longitude of event; M6/5; M65; M65/1; MARUM; Mauritania Canyon; Meteor (1964); Meteor (1986); MUC; MultiCorer; Nitrate; off Guinea; Oxygen; Phosphate; Pollen, per unit sediment mass; Sea surface salinity; Sea surface temperature, autumn; Sea surface temperature, spring; Sea surface temperature, summer; Sea surface temperature, winter; see reference(s); SL; van Veen Grab; VGRAB
    Type: Dataset
    Format: text/tab-separated-values, 923 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-02-02
    Keywords: Algidasphaeridium minutum; ANT-IV/4; ANT-VI/3; ANT-X/4; ANT-X/6; ANT-XVIII/5a; APSARA4; Atlantic Indik Ridge; AWI_Paleo; BC; Bitectatodinium tepikiense; Bounty Trough, Southwest Pacific; Box corer; Brazil Basin; Brigantedinium spp.; Cape Basin; Central South Atlantic; Counting, dinoflagellate cysts; Dalella chathamensis; Date/Time of event; DEPTH, sediment/rock; Elevation of event; ELT27; ELT27.030-PC; ELT29; ELT29.001-PC; ELT29.002-PC; ELT29.070-PC; ELT34; ELT34.006-PC; ELT34.007-PC; ELT34.009-PC; ELT34.011-PC; ELT36; ELT36.023-PC; ELT36.025-TC; ELT36.027-PC; ELT36.043-PC; ELT43; ELT43.005-PC; ELT44; ELT44.005-PC; ELT44.006-PC; ELT53; ELT53.022-PC; ELT53.023-PC; ELT53.025-PC; ELT55; ELT55.001-PC; ELT55.002-PC; ELT55.003-PC; ELT55.004-PC; ELT55.005-PC; ELT55.006-PC; ELT55.007-PC; ELT55.008-PC; ELT55.009-PC; ELT55.010-PC; Eltanin; Event label; GC; GeoB2001-1; GeoB2007-1; GeoB2008-1; GeoB2009-1; GeoB2011-1; GeoB2018-1; GeoB2019-2; GeoB2021-4; GeoB2022-3; GeoB3601-1; GeoB3602-2; GeoB3603-1; GeoB3604-4; GeoB3605-1; GeoB3809-1; GeoB3810-2; GeoB3812-2; GeoB6407-2; GeoB6409-2; GeoB6413-4; GeoB6414-1; GeoB6416-2; GeoB6417-2; GeoB6418-3; GeoB6419-2; GeoB6421-1; GeoB6422-5; GeoB6423-2; GeoB6425-1; GeoB6427-1; GeoB6429-1; Giant box corer; GKG; Gravity corer; Gravity corer (Kiel type); Gymnodinium catenatum; Impagidinium aculeatum; Impagidinium pallidum; Impagidinium paradoxum; Impagidinium patulum; Impagidinium plicatum; Impagidinium sphaericum; Impagidinium spp.; Impagidinium strialatum; Impagidinium variaseptum; Impagidinium velorum; Indian Ocean; KAL; Kasten corer; KC029; KC032; KC046; KC064; KC073; KC075; KC078; KC081; KC083; KC084; KC090; KC095; KC098; KC100; KR88-01; KR88-02; KR88-03; KR88-04; KR88-07; KR88-08; KR88-09; KR88-13; KR88-15; KR88-16; KR88-18; KR88-25; KR88-29; KR88-30; Latitude of event; Lingulodinium machaerophorum; Longitude of event; M23/1; M34/1; M34/3; M46/4; Marion Dufresne (1972); Maud Rise; MD94-02; MD94-04; MD94-06; MD94-07; Meteor (1986); MIC; Mid Atlantic Ridge; MiniCorer; MUC; MultiCorer; Nematosphaeropsis labyrinthus; Nematosphaeropsis rigida; Operculodinium centrocarpum; Operculodinium israelianum; Operculodinium janduchenei; Operculodinium spp.; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; PC; Pentapharsodinium dalei; Piston corer; Polarstern; Polykrikos kofoidii; Polykrikos schwarzii; Polysphaeridium zoharyi; Protoperidinium americanum; Protoperidinium spp.; PS08; PS08/621; PS12; PS12/284; PS12/549; PS12/551; PS12/557; PS1459-4; PS1585-1; PS1650-1; PS1651-2; PS1654-1; PS21 06AQANTX_4; PS22; PS22/899; PS22/902; PS22/947; PS22/973; PS2230-1; PS2366-1; PS2367-1; PS2372-1; PS2376-2; PS58; PS58/251-1; PS58/254-2; PS58/256-1; PS58/258-1; PS58/265-1; PS58/266-4; PS58/267-4; PS58/268-1; PS58/269-4; PS58/270-1; PS58/272-4; PS58/274-4; PS58/276-1; PS58/280-1; PS58/290-1; PS58/291-3; PS58/292-1; Pyxidinopsis psilata; Pyxidinopsis reticulata; Q215; Q219; Q575; Q861; R657; Reference/source; S924; Selenopemphix antarcticum; Selenopemphix nephroides; Selenopemphix quanta; SL; South African margin; South Atlantic; South Atlantic Ocean; Southeast Pacific; Southern Cape Basin; South Pacific; South Pacific Ocean; Spiniferites bentori; Spiniferites membranaceus; Spiniferites mirabilis; Spiniferites pachydermus; Spiniferites ramosus; Spiniferites spp.; TAS_67GC01; TAS_67GC18; TAS_67GC44; TAS_67GC45; TAS_67GC46; TAS_67GC47; TAS_67GC49; TAS_67GC50; TAS_67GC51; TAS_67PC02; TAS_67PC03; TAS_67PC04; Trinovantedinium applanatum; Tuberculodinium vancampoae; U938; U950
    Type: Dataset
    Format: text/tab-separated-values, 5934 data points
    Location Call Number Limitation Availability
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-03-06
    Keywords: Acacia; Acalypha; Acanthaceae; Ageratum-type conyzoides; Aizoaceae; Alchornea; Allophylus; Alternanthera; Amaranthaceae/Chenopodiaceae; Anacardiaceae; Angola Basin; Antidesma-type; Araliaceae; Artemisia (Africa); Balanites; Baphia-type; Bauhinia; Blighia-type; Burkea; Butyrospermum; Caesalpinioideae; Calpocalyx-type; Canarium; Canthium; Capparidaceae; Caryophyllaceae; Cassia-type; Celastraceae/Hippocrateaceae; Celtis; Cissus; Clausena; Cnestis-type; Combretaceae/Melastomataceae; Combretum-type; Compositae Liguliflorae; Compositae Tubuliflorae; Counting, palynology; Crossopteryx; Cuticles, charred; Cuticles, stomata; Cuticles, stomata Gramineae-type; Cuviera; Cyperaceae undifferentiated; DEPTH, sediment/rock; Diospyros; Dobera-type; Dodonaea viscosa; Dry mass; Ebenaceae undifferentiated; Ephedra; Erica (Africa); Euclea; Eugenia-type; Euphorbiaceae undifferentiated; Ficus (Africa); Gaertnera; GeoB; GeoB1007-4; Geosciences, University of Bremen; Gilbertiodendron; Gravity corer (Kiel type); Gymnosporia; Hippocratea-type; Hygrophila-type; Hymenocardia; Hypoestes type; Ilex cf.. mitis; Indeterminata; Juniperus (Africa); Justicia-type; Khaya; Labiatae; Lannea; Liliaceae undifferentiated; Lophira; M6/6; Macaranga-type; Maerua-type; Manilkara; Marker, added; Marker, found; Martretia; Maytenus; Meliaceae; Meteor (1986); Mimosaceae undifferentiated; Mimosa pigra; Mitracarpus; Mitragyna; Myrica; Nauclea/Mitragyna; Nitraria; Olea capensis; Oleaceae (Africa); Ormocarpum; Papilionoideae; Paullinia; Poaceae undifferentiated; Podocarpus; Pollen, total; Polycarpaea-type; Polycarpon; Polygala; Polygonum; Pseudarthria; Pteris; Rhizophora; Rubiaceae undifferentiated; Ruellia; Rutaceae; Salvadora persica; Sapindaceae; Sapium-type; Sapotaceae; Schefflera; Schrebera; Sherbournea; SL; Solanum; Spores; Spores, monolete; Spores, monolete scabrate; Spores, monolete verrucate; Spores, trilete echinate; Spores, trilete scabrate; Spores, trilete verrucate; Synsepalum-type; Syzygium-type guineense; Tamarindus-type indica; Tapinanthus; Teclea-type; Tetrorchidium; Trichilia; Typha angustifolia-type; Uapaca; Umbelliferae; undetermined; Urticaceae; Volume; Zanthoxylum; Ziziphus-type; Zygophyllum
    Type: Dataset
    Format: text/tab-separated-values, 1360 data points
    Location Call Number Limitation Availability
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  • 6
    facet.materialart.
    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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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Esper, Oliver; Zonneveld, Karin A F (2007): The potential of organic-walled dinoflagellate cysts for the reconstruction of past sea-surface conditions in the Southern Ocean. Marine Micropaleontology, 65(3-4), 185-212, https://doi.org/10.1016/j.marmicro.2007.07.002
    Publication Date: 2024-02-02
    Description: In this study we investigate the potential of organic-walled dinoflagellate cysts (dinocysts) as tools for quantifying past sea-surface temperatures (SST) in the Southern Ocean. For this purpose, a dinocyst reference dataset has been formed, based on 138 surface sediment samples from different circum-Antarctic environments. The dinocyst assemblages of these samples are composed of phototrophic (gonyaulacoid) and heterotrophic (protoperidinioid) species that provide a broad spectrum of palaeoenvironmental information. The relationship between the environmental parameters in the upper water column and the dinocyst distribution patterns of individual species has been established using the statistical method of Canonical Correspondence Analysis (CCA). Among the variables tested, summer SST appeared to correspond to the maximum variance represented in the dataset. To establish quantitative summer SST reconstructions, a Modern Analogue Technique (MAT) has been performed on data from three Late Quaternary dinocyst records recovered from locations adjacent to prominent oceanic fronts in the Atlantic sector of the Southern Ocean. These dinocyst time series exhibit periodic changes in the dinocyst assemblage during the last two glacial/interglacial-cycles. During glacial conditions the relative abundance of protoperidinioid cysts was highest, whereas interglacial conditions are characterised by generally lower cyst concentrations and increased relative abundance of gonyaulacoid cysts. The MAT palaeotemperature estimates show trends in summer SST changes following the global oxygen isotope signal and a strong correlation with past temperatures of the last 140,000 years based on other proxies. However, by comparing the dinocyst results to quantitative estimates of summer SSTs based on diatoms, radiolarians and foraminifer-derived stable isotope records it can be shown that in several core intervals the dinocyst-based summer SSTs appeared to be extremely high. In these intervals the dinocyst record seems to be highly influenced by selective degradation, leading to unusual temperature ranges and to unrealistic palaeotemperatures. We used the selective degradation index (kt-index) to determine those intervals that have been biased by selective degradation in order to correct the palaeotemperature estimates. We show that after correction the dinocyst based SSTs correspond reasonably well with other palaeotemperature estimates for this region, supporting the great potential of dinoflagellate cysts as a basis for quantitative palaeoenvironmental studies.
    Keywords: Agulhas Basin; ANT-IV/4; ANT-IX/4; ANT-VI/3; ANT-VIII/3; ANT-X/4; ANT-X/6; ANT-XVIII/5a; APSARA4; Atlantic Indik Ridge; AWI_Paleo; BC; Bounty Trough, Southwest Pacific; Box corer; Brazil Basin; Cape Basin; Central South Atlantic; ELT27; ELT27.030-PC; ELT29; ELT29.001-PC; ELT29.002-PC; ELT29.070-PC; ELT34; ELT34.006-PC; ELT34.007-PC; ELT34.009-PC; ELT34.011-PC; ELT36; ELT36.023-PC; ELT36.025-TC; ELT36.027-PC; ELT36.043-PC; ELT43; ELT43.005-PC; ELT44; ELT44.005-PC; ELT44.006-PC; ELT53; ELT53.022-PC; ELT53.023-PC; ELT53.025-PC; ELT55; ELT55.001-PC; ELT55.002-PC; ELT55.003-PC; ELT55.004-PC; ELT55.005-PC; ELT55.006-PC; ELT55.007-PC; ELT55.008-PC; ELT55.009-PC; ELT55.010-PC; Eltanin; GC; GeoB2001-1; GeoB2007-1; GeoB2008-1; GeoB2009-1; GeoB2011-1; GeoB2018-1; GeoB2019-2; GeoB2021-4; GeoB2022-3; GeoB3601-1; GeoB3602-2; GeoB3603-1; GeoB3604-4; GeoB3605-1; GeoB3809-1; GeoB3810-2; GeoB3812-2; GeoB6407-2; GeoB6409-2; GeoB6413-4; GeoB6414-1; GeoB6416-2; GeoB6417-2; GeoB6418-3; GeoB6419-2; GeoB6421-1; GeoB6422-5; GeoB6423-2; GeoB6425-1; GeoB6427-1; GeoB6429-1; Giant box corer; GKG; Gravity corer; Gravity corer (Kiel type); Indian Ocean; KAL; Kasten corer; KC029; KC032; KC046; KC064; KC073; KC075; KC078; KC081; KC083; KC084; KC090; KC095; KC098; KC100; KR88-01; KR88-02; KR88-03; KR88-04; KR88-07; KR88-08; KR88-09; KR88-13; KR88-15; KR88-16; KR88-18; KR88-25; KR88-29; KR88-30; M23/1; M34/1; M34/3; M46/4; Marion Dufresne (1972); Maud Rise; MD94-02; MD94-04; MD94-06; MD94-07; Meteor (1986); Meteor Rise; MIC; Mid Atlantic Ridge; MiniCorer; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; PC; Piston corer; Polarstern; PS08; PS08/621; PS12; PS12/284; PS12/549; PS12/551; PS12/557; PS1459-4; PS1585-1; PS16; PS16/284; PS16/311; PS1650-1; PS1651-2; PS1654-1; PS1756-5; PS1768-8; PS18; PS18/238; PS2082-1; PS21 06AQANTX_4; PS22; PS22/899; PS22/902; PS22/947; PS22/973; PS2230-1; PS2366-1; PS2367-1; PS2372-1; PS2376-2; PS58; PS58/251-1; PS58/254-2; PS58/256-1; PS58/258-1; PS58/265-1; PS58/266-4; PS58/267-4; PS58/268-1; PS58/269-4; PS58/270-1; PS58/272-4; PS58/274-4; PS58/276-1; PS58/280-1; PS58/290-1; PS58/291-3; PS58/292-1; Q215; Q219; Q575; Q861; R657; S924; Shona Ridge; SL; South African margin; South Atlantic; South Atlantic Ocean; Southeast Pacific; Southern Cape Basin; South Pacific; South Pacific Ocean; TAS_67GC01; TAS_67GC18; TAS_67GC44; TAS_67GC45; TAS_67GC46; TAS_67GC47; TAS_67GC49; TAS_67GC50; TAS_67GC51; TAS_67PC02; TAS_67PC03; TAS_67PC04; U938; U950
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Bouimetarhan, Ilham; Marret, Fabienne; Dupont, Lydie M; Zonneveld, Karin A F (2009): Dinoflagellate cyst distribution in marine surface sediments off West Africa (6-17°N) in relation to sea-surface conditions, freshwater input and seasonal coastal upwelling. Marine Micropaleontology, 71(3-4), 113-130, https://doi.org/10.1016/j.marmicro.2009.02.001
    Publication Date: 2024-02-02
    Description: An organic-walled dinoflagellate cyst analysis was carried out on 53 surface sediment samples from West Africa (17-6°N) to obtain insight in the relationship between their spatial distribution and hydrological conditions in the upper water column as well as marine productivity in the study area. Multivariate analysis of the dinoflagellate cyst relative abundances and environmental parameters of the water column shows that sea-surface temperature, salinity, marine productivity and bottom water oxygen are the factors that relate significantly to the distribution patterns of individual species in the region. The composition of cyst assemblages and dinoflagellate cyst concentrations allows the identification of four hydrographic regimes; 1) the northern regime between 17 and 14°N characterized by high productivity associated with seasonal coastal upwelling, 2) the southern regime between 12 and 6°N associated with high-nutrient waters influenced by river discharge 3) the intermediate regime between 14 and 12°N influenced mainly by seasonal coastal upwelling additionally associated with fluvial input of terrestrial nutrients and 4) the offshore regime characterized by low chlorophyll-a concentrations in upper waters and high bottom water oxygen concentrations. Our data show that cysts of Polykrikos kofoidii, Selenopemphix quanta, Dubridinium spp., Echinidinium species, cysts of Protoperidinium monospinum and Spiniferites pachydermus are the best proxies to reconstruct the boundary between the NE trade winds and the monsoon winds in the subtropical eastern Atlantic Ocean. The association of Bitectatodinium spongium, Lejeunecysta oliva, Quinquecuspis concreta, Selenopemphix nephroides, Trinovantedinium applanatum can be used to reconstruct past river outflow variations within this region.
    Keywords: 286; 287; 288; 289; 290; 291; 293; 295; 297; 298; 300; 301; 302; 303; 304; 305; 306; 307; 310; 311; 312; 313; 314; 316; 317; 318; 319; 320; 321; 322; 323; 324; 326; 327; 329; 330; 331; 371; 376; 388; Atlantic Ocean; Center for Marine Environmental Sciences; Eckernfoerder Bay; GeoB9501-4; GeoB9502-5; GeoB9503-3; GeoB9503-5; GeoB9504-4; GeoB9505-3; GeoB9506-3; GeoB9508-4; GeoB9510-3; GeoB9512-4; GeoB9513-5; GeoB9515-2; GeoB9516-4; GeoB9517-5; GeoB9518-4; GeoB9519-6; GeoB9520-4; GeoB9521-3; GeoB9522-2; GeoB9525-5; GeoB9526-4; GeoB9527-6; GeoB9528-1; GeoB9529-1; GeoB9531-2; GeoB9532-1; GeoB9533-3; GeoB9534-4; GeoB9535-5; GeoB9536-4; GeoB9537-4; GeoB9538-5; GeoB9539-1; GeoB9541-1; GeoB9542-1; GeoB9544-1; GeoB9545-1; GeoB9546-1; GEOTROPEX 83, NOAMP I; Giant box corer; GIK16402-1; GIK16404-1; GIK16405-1; GIK16407-1; GIK16414-1; GIK16421-1; GIK16425-1; GIK16437-3; GIK16558-1; GIK16755-1; GIK16764-1; GIK16765-1; GIK16766-1; GIK16767-1; GIK16768-1; GIK16769-1; GKG; Gravity corer (Kiel type); LI198x; Littorina; M6/5; M65; M65/1; MARUM; Mauritania Canyon; Meteor (1964); Meteor (1986); MUC; MultiCorer; off Guinea; SL; van Veen Grab; VGRAB
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-02-02
    Keywords: Celtic_Sea; Center for Marine Environmental Sciences; GeoB; Geosciences, University of Bremen; Laboratory; Lycopodium marker-grain method; MARUM; MUC; MultiCorer; Species
    Type: Dataset
    Format: text/tab-separated-values, 2754 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-02-02
    Keywords: Center for Marine Environmental Sciences; GeoB; Geosciences, University of Bremen; Laboratory; Lycopodium marker-grain method; MARUM; North_Sea; North Sea; see reference(s); Species
    Type: Dataset
    Format: text/tab-separated-values, 1969 data points
    Location Call Number Limitation Availability
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