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  • PANGAEA  (4)
  • 2010-2014  (4)
Document type
Keywords
Years
Year
  • 1
    Publication Date: 2023-02-07
    Keywords: DEPTH, sediment/rock; LATITUDE; LONGITUDE; Nickel; Potassium oxide; Rock type; trondheimsfjord; Trondheimsfjord, Norway; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator
    Type: Dataset
    Format: text/tab-separated-values, 1098 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-02-08
    Keywords: DEPTH, sediment/rock; Factor 1; Factor 2; Sample ID; trondheimsfjord; Trondheimsfjord, Norway
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
    Location Call Number Limitation Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Grøsfjeld, Kari; De Schepper, Stijn; Fabian, Karl; Husum, Katrine; Baranwal, Soma; Andreassen, Karin; Knies, Jochen (2014): Dating and palaeoenvironmental reconstruction of the sediments around the Miocene/Pliocene boundary in Yermak Plateau ODP Hole 911A using marine palynology. Palaeogeography, Palaeoclimatology, Palaeoecology, 414, 382-402, https://doi.org/10.1016/j.palaeo.2014.08.028
    Publication Date: 2024-01-09
    Description: The late Neogene evolution of the Arctic to Subarctic region is poorly understood due to few available records and poor age control. At the margin of the Arctic Ocean, Yermak Plateau Ocean Drilling Program (ODP) Hole 911A is strategically located for establishing a stratigraphic framework for the Arctic. Here we present dinoflagellate cyst and acritarch data from 24 stratigraphic levels in the lower part (474.26-505.64 metres below the seafloor (mbsf)) of ODP Hole 911A. The marine palynomorphs indicate a latest Miocene to earliest Pliocene age (between 5.8 and 5.0 Ma) for the base of the hole based on the co-occurrence of the dinoflagellate cyst Barssidinium evangelineae and acritarch Lavradosphaera crista. Our age estimate for the sediments can possibly be further refined to 5.0-5.33 Ma based on the presence of Achomosphaera andalousiensis suttonensis, which apparently has a range restricted to the Pliocene. An age close to the Miocene/Pliocene boundary agrees with the planktonic foraminifer data. Together with recently available magnetostratigraphic data, the base of the hole is likely to be placed at ~5.2 Ma. This new chronostratigraphy is a first step towards a better understanding of the late Neogene palaeoenvironment for the Yermak Plateau and also for the wider Arctic to Subarctic region. The terrestrial and fresh water palynomorphs were most likely redistributed and/or displaced from the shelf towards deeper parts of the basin during contourite deposition under the influence of the West Spitsbergen Current. The in situ marine dinoflagellate cyst assemblage contains a mixture of cool water and thermophilic taxa, indicating sea-ice free, cool-temperate, warmer than present conditions at the Yermak Plateau. Rivers were likely the source for the freshwater influence.
    Keywords: 151-911A; Achomosphaera andalousiensis andalousiensis; Achomosphaera andalousiensis suttonensis; Acritarcha; Acritarcha, standard error; Acritarcha indeterminata; Acritarcha per unit mass; Amiculosphaera umbraculum; Barssidinium evangelineae; Barssidinium graminosum; Barssidinium pliocenicum; Barssidinium spp.; Bitectatodinium raedwaldii; Bitectatodinium tepikiense; Botryococcus spp.; Brigantedinium spp.; Cymatiosphaera invaginata; Cymatiosphaera spp.; DEPTH, sediment/rock; Dinoflagellate cyst; Dinoflagellate cyst, standard error; Dinoflagellate cyst indeterminata; Dinoflagellate cyst per unit mass; Dinoflagellate cyst reworked; Dinoflagellate cyst reworked, standard error; Dinoflagellate cyst reworked per unit mass; DRILL; Drilling/drill rig; Dry mass; DSDP/ODP/IODP sample designation; Echinidinium euaxum; Filisphaera filifera; Filisphaera microornata; Foraminifera, linings; Habibacysta tectata; Impagidinium aculeatum; Impagidinium pallidum; Impagidinium patulum; Impagidinium sp.; Impagidinium spp.; Invertocysta lacrymosa; Invertocysta tabulata; Joides Resolution; Laboratory code/label; Lavradosphaera crista; Lavradosphaera lucifer; Leg151; Lejeunecysta mariae; Lejeunecysta spp.; Lingulodinium machaerophorum; Lycopodium clavatum, standard deviation; Lycopodium clavatum markers counted; Lycopodium clavatum spores per tablet; Lycopodium tablets; Nematosphaeropsis labyrinthus; North Greenland Sea; Number of taxa; Ocean Drilling Program; ODP; Operculodinium? eirikianum crebrum; Operculodinium? eirikianum eirikianum; Operculodinium centrocarpum; Operculodinium sp.; Pediastrum spp.; Pentapharsodinium dalei; Protoceratium reticulatum; Sample code/label; Selenopemphix dionaeacysta; Spiniferites elongatus; Spiniferites falcipedius; Spiniferites spp.; Sumatradinium sp.; Tasmanites; Trinovantedinium glorianum; Trinovantedinium variabile
    Type: Dataset
    Format: text/tab-separated-values, 1521 data points
    Location Call Number Limitation Availability
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Aagaard-Sørensen, Steffen; Husum, Katrine; Hald, Morten; Knies, Jochen (2010): Paleoceanographic development in the SW Barents Sea during the Late Weichselian-Early Holocene transition. Quaternary Science Reviews, 29(25-26), 3442-3456, https://doi.org/10.1016/j.quascirev.2010.08.014
    Publication Date: 2023-12-13
    Description: The Late Weichselian-Early Holocene variability of the North Atlantic Current has been studied with focus on the zonal component of this meridional transport during the transition from glacial to interglacial conditions. The investigated sediment core is from 409 m water depth in the SW Barents Sea. Eight Accelerator mass spectrometry (AMS) 14C dates show that the core covers the last 20,000 cal yr B.P. with a centennial scale resolution during Late Weichselian-Early Holocene. Planktic foraminiferal assemblages were analyzed using the 〉100 ?m size fraction and foraminiferal planktic and benthic d13C and d18O isotopes were measured. Furthermore, a range of physical and chemical analyses has been carried out on the bulk sediment samples. Four time periods have been identified which represent the varying oceanographic conditions in Ingøydjupet, a glacial trough located off the north coast of Norway in the SW Barents Sea. 1) The late glacial (before ca 15,000 cal yr B.P.) influenced by the nearby ice sheets with high amounts of sea ice- or iceberg-transported detritus. 2) The late Oldest Dryas stadial and the Bølling-Allerød interstadial (ca 15,000-12,700 cal yr B.P.) with cold surface water conditions influenced by the collapse of the nearby ice sheets, high amounts of sea ice- or iceberg-transported detritus and melt water and weak subsurface inflow of Atlantic Water. 3) The Younger Dryas cold stadial (12,700-11,650 cal yr B.P.) with low primary productivity and extensive sea ice cover and 4) The Preboreal and Early Holocene (11,650-6800 cal yr B.P. cal yr B.P.) with strong influx of Atlantic Water into the area, near absence of ice rafted debris and generally ameliorated conditions in both surface and bottom water masses as seen from a high flux of foraminifera and increased marine primary production.
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated material; Age, dated standard deviation; Age, maximum/old; Age, minimum/young; Barents Sea; Calendar age; Calendar age, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; International Polar Year (2007-2008); IPY; JM05-085-GC; Mass spectrometer Finnigan MAT 251; Reservoir effect/correction; Sample ID; Standard deviation; δ13C; δ13C, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 104 data points
    Location Call Number Limitation Availability
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