Grain-size distribution of sediment core GeoB19905-1

doi:doi:10.1594/PANGAEA.930871

Grain-size distribution of sediment core GeoB19905-1

The disintegrated, inorganic grain-size distribution of sediment core GeoB19905-1 was determined every ten centimetres (and in parts higher resolution) to decipher patterns of sediment input to and transport on the southern west Greenland shelf. Prior to measurement, organic matter, calcium carbonate and biogenic silica were chemically removed from the bulk sediment. Measurements were then performed using a Beckman Coulter Laser Diffraction Particle Size Analyzer LS 13320.

BibTex:

@dataset{Weiser_Jens_and_Titschack_Jürgen_and_Kienast_Markus_and_McCave_I_Nick_and_Lochte_Annalena_Antonia_and_Saini_Jeetendra_and_Stein_Ruediger_and_Hebbeln_Dierk_2021,
    abstract = {The disintegrated, inorganic grain-size distribution of sediment core GeoB19905-1 was determined every ten centimetres (and in parts higher resolution) to decipher patterns of sediment input to and transport on the southern west Greenland shelf. Prior to measurement, organic matter, calcium carbonate and biogenic silica were chemically removed from the bulk sediment. Measurements were then performed using a Beckman Coulter Laser Diffraction Particle Size Analyzer LS 13320.},
    author = {Weiser, Jens and Titschack, Jürgen and Kienast, Markus and McCave, I Nick and Lochte, Annalena Antonia and Saini, Jeetendra and Stein, Ruediger and Hebbeln, Dierk},
    doi = {10.1594/PANGAEA.930871},
    institution = {PANGAEA (Land Surface)},
    keyword = {'8.2 ka event', 'Labrador Sea', 'West Greenland Current', 'sortable silt'},
    title = {Grain-size distribution of sediment core GeoB19905-1},
    url = {https://service.tib.eu/ldmservice/vdataset/png-doi-10-1594-pangaea-930871},
    year = {2021}
}