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  • 1
    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
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-02-05
    Description: Palmitic acid (PA) is ubiquitous in the biosphere and its hydrogen isotopic composition (δ2HPA) was proposed as a potential paleoenvironmental proxy for salinity, with δ2HPA values increasing with salinity. In this study, we analyzed 40 surface sediment samples from Baffin Bay and the Labrador Sea to examine the isotopic composition of PA in relation to local environmental variables, including salinity. In contrast to expectations, our results show a negative relationship between the δ2HPA and sea-surface salinity, raising questions about its pertinence/usefulness as a salinity proxy. Instead, our results suggest that the relative abundance of distinct organisms that employ different metabolisms is key in determining the hydrogen isotopic fractionations in PA. Whereas we show that PA is mostly produced through photoautotrophic metabolisms by diatoms and dinoflagellates, varying contributions from heterotrophic metabolisms may obscure the stable isotope composition of PA. Surprisingly, we found no correlation between the stable carbon isotopic composition of the sedimentary organic matter (δ13Corg) and palmitic acid (δ13CPA), implying major differences in either the dominant organisms producing sedimentary PA or in carbon isotope fractionation during lipid biosynthesis. We also found that the presence of extended sea-ice cover leads to enriched carbon and hydrogen isotopic compositions in PA. These enriched values suggest heterotrophic biodegradation in the water column and/or in the sediment as well as an increase in grazing activities. We propose that sea-ice cover and surface water oxygenation modulate the relative impact of phototrophic and heterotrophic metabolisms, and therefore the isotopic composition of marine sedimentary PA.
    Keywords: Average chain length; Baffin Bay; BC; Bottom water salinity, annual mean; Bottom water temperature; Box corer; Carbon; Carbon, inorganic, total; Carbon, organic; Carbon isotopes; Carbon organic/Nitrogen, molar ratio; Carbon Preference Index; Davis Strait; DB3.02; DB3.08; DB3.10; DB3.14; DB3.31; DB3.32; DB3.34; DB3.35; DB6.02; DB6.04; DB6.05; DB6.07; DB6.08; DB6.09; DEPTH, sediment/rock; Dinoflagellate cyst, heterotrophic; Dinoflagellate cyst, per unit sediment mass; Dinoflagellate cyst, phototrophic; Event label; FB1.02; FB1.07; GeoB22315-3; GeoB22318-1; GeoB22319-1; GeoB22344-2; GeoB22350-2; GeoB22353-2; GeoB22356-2; GeoB22358-2; Grab; GRAB; HB2.04; Hexadecanoic acid, δ13C; Hexadecanoic acid, δ13C, standard deviation; Hudson Strait; Hydrogen isotopes; Labrador Sea; lipid biomarkers; Maria S. Merian; MSM45; MSM45_002-4; MSM45_009-3; MSM45_030-3; MSM45_401-4; MSM45_408-3; MSM45_417-3; MSM45_424-3; MSM45_430-3; MSM45-018-3; MSM45-024-3; MSM46; MSM46_11-5; MSM46_14-2; MSM46_25-1; MSM46_28-3; MSM66; MSM66/15-3; MSM66/18-1; MSM66/19-1; MSM66/44-2; MSM66/50-2; MSM66/53-2; MSM66/56-2; MSM66/58-2; MUC; MultiCorer; n-fatty acid C16, per unit mass total organic carbon; n-fatty acid C16, per unit sediment mass; n-fatty acid C16:1, per unit mass total organic carbon; n-fatty acid C16:1, per unit sediment mass; n-fatty acid C18, per unit mass total organic carbon; n-fatty acid C18, per unit sediment mass; n-fatty acid C18:1, per unit mass total organic carbon; n-fatty acid C18:1, per unit sediment mass; n-fatty acid C18:2, per unit mass total organic carbon; n-fatty acid C18:2, per unit sediment mass; Nitrate; Nitrogen; Oxygen, apparent utilization; Oxygen saturation; Paamiut; Paamiut2014; Palmitic acid; Palynomorpha, reworked per unit sediment mass; Phosphate; Pollen, per unit sediment mass; Primary production of carbon per area, yearly; Q7.03; Q7.04; Ratio; Saturated fatty acids, per unit mass total organic carbon; Saturated fatty acids, per unit sediment mass; Sea ice cover duration; Sea surface salinity, annual mean; Sea surface salinity, summer; Sea surface salinity, winter; Sea surface temperature, annual mean; Sea surface temperature, summer; Sea surface temperature, winter; Silicate; Site; Spores per unit sediment mass; U5.04; U5.10; U5.14; V4.03; δ13C, organic carbon; δ18O, water; δ Deuterium, palmitic acid; δ Deuterium, palmitic acid, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 2194 data points
    Location Call Number Limitation Availability
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Allan, Estelle; de Vernal, Anne; Knudsen, Mads Faurschou; Hillaire-Marcel, Claude; Moros, Matthias; Ribeiro, Sofia; Ouellet‐Bernier, Marie‐Michèle; Seidenkrantz, Marit-Solveig (2018): Late Holocene sea surface instabilities in the Disko Bugt Area, West Greenland, in phase with δ18O oscillations at Camp Century. Paleoceanography and Paleoclimatology, 33(2), 227-243, https://doi.org/10.1002/2017PA003289
    Publication Date: 2024-02-02
    Description: Palynological analyses of sediment core MSM343310 from Disko Bugt (68°38.861' N, 53°49.493' W) document decadal‐ to centennial‐scale variability of sea surface conditions during the last ~3,600 years. Dinocyst fluxes (〉10⁴ cysts/cm² yr⁻¹) indicate a very high productivity. Dinocyst assemblages dominated by Islandinium minutum, Brigantedinium spp., Islandinium? cezare, and the cyst of Pentapharsodinium dalei suggest low surface salinity and marked shifts in summer sea surface temperature. The application of the modern analog technique to dinocyst assemblages, using an updated reference data set with new sites from the West Greenland margin, led to reconstruct decadal‐centennial‐scale variations in sea surface salinity and temperature, in phase with the δ18O variations in the Camp Century ice core. At ~1.5 ka BP, the seasonal sea ice cover records an important regime change, from winter‐only sea ice to more unstable conditions marked by successive cooling pulses with sea ice cover of up to 8 months/yr. The data suggest a close relationship between hydrographic conditions and regional climate over Greenland. Our record shows variations with a mean 200 years periodicity until ~2 ka BP, which supports the hypothesis of climate variations driven by solar variability. After 1.5 ka BP, our data show a variability characterized by a 60-70 year periodicity, which suggests linkages with the Atlantic Multidecadal Oscillation and southwestward migration of the atmospheric polar front. The most recent part of the record, from ~1900 CE to 2007 CE, is characterized by assemblages reflecting warmer surface conditions and reduced sea ice cover.
    Keywords: Achomosphaera spp.; Age; AGE; Arctic climate change; Arctic sea ice reconstructions; Baffin Bay; Bitectatodinium tepikiense; Brigantedinium spp.; Counting, palynology; Dinocyst database; Dubridinium spp.; Echinidinium spp.; Event label; GC; Gravity corer; Impagidinium aculeatum; Impagidinium pallidum; Islandinium? cezare; Islandinium brevispinosum; Islandinium minutum; Late Holocene; Lejeunecysta spp.; Maria S. Merian; MSM05/3; MSM05/3_343310-2-2; MSM05/3_343310-5-1; MUC; MultiCorer; Nematosphaeropsis labyrinthus; Operculodinium centrocarpum; Pentapharsodinium dalei cyst; Protoperidinium americanum; Protoperidinium nudum cyst; Selenopemphix quanta; Spiniferites belerius; Spiniferites bentori; Spiniferites elongatus; Spiniferites ramosus; Spiniferites spp.; Votadinium calvum; West Greenland
    Type: Dataset
    Format: text/tab-separated-values, 5064 data points
    Location Call Number Limitation Availability
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Allan, Estelle; de Vernal, Anne; Knudsen, Mads Faurschou; Hillaire-Marcel, Claude; Moros, Matthias; Ribeiro, Sofia; Ouellet‐Bernier, Marie‐Michèle; Seidenkrantz, Marit-Solveig (2018): Late Holocene sea surface instabilities in the Disko Bugt Area, West Greenland, in phase with δ18O oscillations at Camp Century. Paleoceanography and Paleoclimatology, 33(2), 227-243, https://doi.org/10.1002/2017PA003289
    Publication Date: 2024-02-02
    Description: Palynological analyses of sediment core MSM343310 from Disko Bugt (68°38.861' N, 53°49.493' W) document decadal‐ to centennial‐scale variability of sea surface conditions during the last ~3,600 years. Dinocyst fluxes (〉10⁴ cysts/cm² yr⁻¹) indicate a very high productivity. Dinocyst assemblages dominated by Islandinium minutum, Brigantedinium spp., Islandinium? cezare, and the cyst of Pentapharsodinium dalei suggest low surface salinity and marked shifts in summer sea surface temperature. The application of the modern analog technique to dinocyst assemblages, using an updated reference data set with new sites from the West Greenland margin, led to reconstruct decadal‐centennial‐scale variations in sea surface salinity and temperature, in phase with the δ18O variations in the Camp Century ice core. At ~1.5 ka BP, the seasonal sea ice cover records an important regime change, from winter‐only sea ice to more unstable conditions marked by successive cooling pulses with sea ice cover of up to 8 months/yr. The data suggest a close relationship between hydrographic conditions and regional climate over Greenland. Our record shows variations with a mean 200 years periodicity until ~2 ka BP, which supports the hypothesis of climate variations driven by solar variability. After 1.5 ka BP, our data show a variability characterized by a 60-70 year periodicity, which suggests linkages with the Atlantic Multidecadal Oscillation and southwestward migration of the atmospheric polar front. The most recent part of the record, from ~1900 CE to 2007 CE, is characterized by assemblages reflecting warmer surface conditions and reduced sea ice cover.
    Keywords: Achomosphaera spp.; Age; AGE; Arctic climate change; Arctic sea ice reconstructions; Baffin Bay; Bitectatodinium tepikiense; Brigantedinium spp.; Counting, palynology; Dinocyst database; Dubridinium spp.; Echinidinium spp.; Event label; GC; Gravity corer; Impagidinium aculeatum; Impagidinium pallidum; Islandinium? cezare; Islandinium brevispinosum; Islandinium minutum; Late Holocene; Lejeunecysta spp.; Maria S. Merian; MSM05/3; MSM05/3_343310-2-2; MSM05/3_343310-5-1; MUC; MultiCorer; Nematosphaeropsis labyrinthus; Operculodinium centrocarpum; Pentapharsodinium dalei cyst; Protoperidinium americanum; Protoperidinium nudum cyst; Selenopemphix quanta; Spiniferites belerius; Spiniferites bentori; Spiniferites elongatus; Spiniferites ramosus; Spiniferites spp.; Votadinium calvum; West Greenland
    Type: Dataset
    Format: text/tab-separated-values, 5064 data points
    Location Call Number Limitation Availability
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Allan, Estelle; de Vernal, Anne; Knudsen, Mads Faurschou; Hillaire-Marcel, Claude; Moros, Matthias; Ribeiro, Sofia; Ouellet‐Bernier, Marie‐Michèle; Seidenkrantz, Marit-Solveig (2018): Late Holocene sea surface instabilities in the Disko Bugt Area, West Greenland, in phase with δ18O oscillations at Camp Century. Paleoceanography and Paleoclimatology, 33(2), 227-243, https://doi.org/10.1002/2017PA003289
    Publication Date: 2024-02-02
    Description: Palynological analyses of sediment core MSM343310 from Disko Bugt (68°38.861' N, 53°49.493' W) document decadal‐ to centennial‐scale variability of sea surface conditions during the last ~3,600 years. Dinocyst fluxes (〉10⁴ cysts/cm² yr⁻¹) indicate a very high productivity. Dinocyst assemblages dominated by Islandinium minutum, Brigantedinium spp., Islandinium? cezare, and the cyst of Pentapharsodinium dalei suggest low surface salinity and marked shifts in summer sea surface temperature. The application of the modern analog technique to dinocyst assemblages, using an updated reference data set with new sites from the West Greenland margin, led to reconstruct decadal‐centennial‐scale variations in sea surface salinity and temperature, in phase with the δ18O variations in the Camp Century ice core. At ~1.5 ka BP, the seasonal sea ice cover records an important regime change, from winter‐only sea ice to more unstable conditions marked by successive cooling pulses with sea ice cover of up to 8 months/yr. The data suggest a close relationship between hydrographic conditions and regional climate over Greenland. Our record shows variations with a mean 200 years periodicity until ~2 ka BP, which supports the hypothesis of climate variations driven by solar variability. After 1.5 ka BP, our data show a variability characterized by a 60-70 year periodicity, which suggests linkages with the Atlantic Multidecadal Oscillation and southwestward migration of the atmospheric polar front. The most recent part of the record, from ~1900 CE to 2007 CE, is characterized by assemblages reflecting warmer surface conditions and reduced sea ice cover.
    Keywords: Age; AGE; Arctic climate change; Arctic sea ice reconstructions; Baffin Bay; Calculated; Dinocyst database; Event label; GC; Gravity corer; Late Holocene; Maria S. Merian; MSM05/3; MSM05/3_343310-2-2; MSM05/3_343310-5-1; MUC; MultiCorer; Paleoproductivity as carbon; Sea ice cover duration; Sea surface salinity, summer; Sea surface salinity, winter; Sea surface temperature, summer; Sea surface temperature, winter; West Greenland
    Type: Dataset
    Format: text/tab-separated-values, 1477 data points
    Location Call Number Limitation Availability
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  • 6
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