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  • 2015-2019  (56)
  • 2005-2009  (15)
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  • 1
    Publication Date: 2016-10-25
    Description: We establish the cyst-theca relationship of the cyst species Trinovantedinium pallidifulvum Matsuoka 1987 based on germination experiments of specimens isolated from the Gulf of Mexico. We show that the motile stage is a new species, designated as Protoperidinium louisianensis. We also determine its phylogenetic position based on single-cell PCR of a single cell germinated from the Gulf of Mexico cysts. To further refine the phylogeny, we determined the LSU sequence through single-cell PCR of the cyst Selenopemphix undulata isolated from Brentwood Bay (Saanich Inlet, BC, Canada). The phylogeny shows that P. louisianensis is closest to P. shanghaiense, the motile stage of T. applanatum, and is consistent with the monophyly of the genus Trinovantedinium. Selenopemphix undulata belongs to a different clade than Selenopemphix quanta (alleged cyst of P. conicum), suggesting that the genus Selenopemphix is polyphyletic.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 2
    Publication Date: 2020-06-10
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
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    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
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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
    Publication Date: 2024-02-21
    Description: Data set of dinocyst assemblages (% of 71 taxa) and corresponding location and sea-surface parameters.
    Keywords: Achomosphaera andalousiensis; Arctic; Ataxiodinium choane; Atlanticodinium striaticonulum; Bitectatodinium spongium; Bitectatodinium tepikiense; Brigantedinium spp.; Dalella chathamensis; Depth, bathymetric; Dinocysts; Distance; Dubridinium spp.; Echinidinium aculeatum; Echinidinium delicatum; Echinidinium granulatum; Echinidinium karaense; Echinidinium spp.; Echinidinium transparantum; Gymnodinium sp. cyst; Impagidinium aculeatum; Impagidinium japonicum; Impagidinium pallidum; Impagidinium paradoxum; Impagidinium patulum; Impagidinium plicatum; Impagidinium sphaericum; Impagidinium strialatum; Impagidinium velorum; Islandinium? cezare; Islandinium brevispinosum; Islandinium minutum; LATITUDE; Lejeunecysta spp.; Lingulodinium machaerophorum; LONGITUDE; Melitasphaeridium choanophorum; Nematosphaeropsis labyrinthus; Nematosphaeropsis rigida; Net primary production of carbon; Nitrate; North Atlantic; North Pacific; Operculodinium centrocarpum sensu Wall and Dale (1966); Operculodinium giganteum; Operculodinium israelianum; Operculodinium longispinigerum; Oxygen; Oxygen, dissolved; Pentapharsodinium dalei cyst; Phosphate; Polykrikos kofoidii cyst; Polykrikos schwartzii cyst; Polykrikos var. arctica cyst; Polysphaeridium zoharyi; Primary production of carbon per area, yearly; productivity; Protoperidinioid cyst; Protoperidinium americanum cyst; Protoperidinium fukuyoi cyst; Protoperidinium nudum cyst; Protoperidinium stellatum cyst; Pyxidinopsis reticulata; Quinquecuspis concreta; Recalculated from ml/l by using (ml/l)*44.66; Sample code/label; Scrippsiella trifida cyst; sea-ice; Sea ice concentration; Sea ice cover duration; sea-surface salinity; sea-surface temperature; Selenopemphix nephroides; Selenopemphix quanta; Silicate; Spiniferites belerius; Spiniferites bentori; Spiniferites bulloideus; Spiniferites delicatus; Spiniferites elongatus; Spiniferites lazus; Spiniferites membranaceus; Spiniferites mirabilis-hyperacanthus; Spiniferites pachydermus; Spiniferites ramosus; Spiniferites sp.; Spiniferites spp.; Stelladinium bifurcatum; Surface salinity; Surface sediment; Surface temperature; Tectatodinium pellitum; Trinovantedinium applanatum; Trinovantedinium variabile; Tuberculodinium vancampoae; Votadinium calvum; Votadinium spinosum; Xandarodinium xanthum
    Type: Dataset
    Format: text/tab-separated-values, 232224 data points
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  • 6
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    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
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  • 7
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    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
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  • 8
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    PANGAEA
    In:  Supplement to: Hötzel, Sebastian; Dupont, Lydie M; Marret, Fabienne; Jung, Gerlinde; Wefer, Gerold (2016): Steps in the intensification of Benguela upwelling over the Walvis Ridge during Miocene and Pliocene. International Journal of Earth Sciences, 1-13, https://doi.org/10.1007/s00531-016-1309-0
    Publication Date: 2024-03-06
    Description: Using the Late Miocene to Pliocene organic-walled dinoflagellate cyst record of ODP Site 1081 we reconstruct and discuss the early upwelling history over the Walvis Ridge with a special focus on the movement of the Angola-Benguela Front (ABF). We suggest that during the Late Miocene the Angola Current flowed southwards over the Walvis Ridge more frequently than today because the ABF was probably located further south as a result of a weaker meridional temperature gradient. A possible strengthening of the meridional gradient during the latest Miocene to early Pliocene in combination with uplift of south-western Africa intensified the upwelling along the coast and increased the upwelling's filaments over the Walvis Ridge. An intermediate period from 6.2 to 5.5 Ma is shown by the dominance of Habibacysta tectata, cysts of a cool-tolerant dinoflagellate known from the northern Atlantic, indicating changing oceanic conditions contemporaneous with the Messinian Salinity Crisis. From 4.3 Ma on, the upwelling signal got stronger again and waters were well-mixed and nutrient-rich. Our results indicate a northward migration of the ABF as early as 7 Ma and the initial stepwise intensification of the BUS.
    Keywords: 175-1081A; Acomosphaera spp.; AGE; Ataxiodinium confusum; Ataxiodinium zevenboomii; Batiacasphaera hirsuta; Batiacasphaera micropapillata; Benguela Current, South Atlantic Ocean; Brigantedinium spp.; Counting, dinoflagellate cysts; DEPTH, sediment/rock; Dinoflagellate cyst indeterminata; Dinoflagellates, total; DRILL; Drilling/drill rig; Habibacysta tectata; Impagidinium aculeatum; Impagidinium paradoxum; Impagidinium patulum; Impagidinium species 2 after De Schepper & Head (2009); Impagidinium sphaericum; Impagidinium spp.; Impagidinium strialatum; Joides Resolution; Leg175; Lejeunecysta oliva; Lejeunecysta sabrina; Lejeunecysta spp.; Lingulodinium machaerophorum; Marker, added; Marker, found; Nematosphaeropsis labyrinthus; Ocean Drilling Program; ODP; Operculodinium centrocarpum; Operculodinium israelianum; Operculodinium janduchenei; Operculodinium spp.; Pentapharsodinium dalei; Pyxidinopsis reticulata; Quinquecuspis concreta; Sample code/label; Selenopemphix armageddonensis; Selenopemphix brevispinosa; Selenopemphix brevispinosa conspicua; Selenopemphix nephroides; Selenopemphix quanta; Spiniferites cf. mirabilis; Spiniferites membranaceus; Spiniferites mirabilis; Spiniferites ramosus; Spiniferites spp.; Sumatradinium soucouyantiae; Trinovantedinium applanatum; Trinovantedinium ferugnomatum; Trinovantedinium glorianum; Trinovantedinium papula; Tuberculodinium vancampoae; Volume
    Type: Dataset
    Format: text/tab-separated-values, 3408 data points
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  • 9
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    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
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  • 10
    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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