Data

Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14

Australian Antarctic Data Centre
NOBLE, TARYN L ; TOOZE, SIAN
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.26179/5d5df0f2bb683&rft.title=Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14&rft.identifier=10.26179/5d5df0f2bb683&rft.publisher=Australian Antarctic Data Centre&rft.description=Ice-rafted debris is characterised by coarse material with typically angular grains, transported within icebergs and deposted in the ocean as the icebergs melt. This iceberg rafted debris (IBRD) flux data submitted here, was calculated by quantifying the coarse sand fraction (CSF) as a percentage of the bulk sample (weight of grains in the 250 micron to 2 mm size fraction), the dry bulk density (DBD) and the linear sedimentation rate (LSR) (following Krissek et al., 1995, Patterson et al., 2014). A method for quantifying the IBRD flux uses the coarse sand fraction (CSF) as a percentage of the bulk sample, dry bulk density (DBD) and the linear sedimentation rate (LSR) (Krissek et al., 1995, Patterson et al., 2014): The CSF (250μm-2mm) was acquired from samples at 10cm intervals along KC14 by wet-sieving approximately 20g of sediment per sample. Authigenic grains and microfossils were removed from the samples under a microscope. The remaining material was weighed on a microbalance and calculated as a percentage of the bulk sample. The DBD was calculated by subsampling approximately 8cm3 of sediment from the same depth intervals and dividing the dry weight of the sediment by the volume of the subsampler. The LSR was approximated by dividing the distance (cm) between the calibrated bulk carbon ages by the difference in time (kyr). The IBRD flux was then quantified using the above equation for each depth interval.&rft.creator=NOBLE, TARYN L &rft.creator=TOOZE, SIAN &rft.date=2019&rft.coverage=northlimit=-63.30854; southlimit=-66.53854; westlimit=109.74805; eastLimit=125.0957; projection=WGS84&rft.coverage=northlimit=-63.30854; southlimit=-66.53854; westlimit=109.74805; eastLimit=125.0957; projection=WGS84&rft_rights=This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4419_KC14_IBRDFlux when using these data.&rft_subject=geoscientificInformation&rft_subject=oceans&rft_subject=ICEBERGS&rft_subject=EARTH SCIENCE&rft_subject=OCEANS&rft_subject=SEA ICE&rft_subject=SEDIMENT TRANSPORT&rft_subject=MARINE SEDIMENTS&rft_subject=SEDIMENT COMPOSITION&rft_subject=ICEBERG RAFTED DEBRIS&rft_subject=SEDIMENTOLOGY&rft_subject=RV INVESTIGATOR&rft_subject=ICEBERG RAFTED DEBRIS FLUX&rft_subject=SEDIMENT CORERS&rft_subject=SHIPS&rft_subject=LABORATORY&rft_subject=Paleo Start Date 2 ka&rft_subject=Paleo Stop Date 25 ka&rft_subject=PHANEROZOIC > CENOZOIC > QUATERNARY > HOLOCENE&rft_subject=CONTINENT > ANTARCTICA&rft_subject=OCEAN > SOUTHERN OCEAN > SABRINA CONTINENTAL SLOPE&rft_subject=GEOGRAPHIC REGION > POLAR&rft_place=Hobart&rft.type=dataset&rft.language=English Access the data

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This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4419_KC14_IBRDFlux when using these data.

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Brief description

Ice-rafted debris is characterised by coarse material with typically angular grains, transported within icebergs and deposted in the ocean as the icebergs melt. This iceberg rafted debris (IBRD) flux data submitted here, was calculated by quantifying the coarse sand fraction (CSF) as a percentage of the bulk sample (weight of grains in the 250 micron to 2 mm size fraction), the dry bulk density (DBD) and the linear sedimentation rate (LSR) (following Krissek et al., 1995, Patterson et al., 2014). A method for quantifying the IBRD flux uses the coarse sand fraction (CSF) as a percentage of the bulk sample, dry bulk density (DBD) and the linear sedimentation rate (LSR) (Krissek et al., 1995, Patterson et al., 2014): The CSF (250μm-2mm) was acquired from samples at 10cm intervals along KC14 by wet-sieving approximately 20g of sediment per sample. Authigenic grains and microfossils were removed from the samples under a microscope. The remaining material was weighed on a microbalance and calculated as a percentage of the bulk sample. The DBD was calculated by subsampling approximately 8cm3 of sediment from the same depth intervals and dividing the dry weight of the sediment by the volume of the subsampler. The LSR was approximated by dividing the distance (cm) between the calibrated bulk carbon ages by the difference in time (kyr). The IBRD flux was then quantified using the above equation for each depth interval.

Issued: 2019-08-21

Data time period: 2016-07-01 to 2019-06-30

This dataset is part of a larger collection

Click to explore relationships graph

125.0957,-63.30854 125.0957,-66.53854 109.74805,-66.53854 109.74805,-63.30854 125.0957,-63.30854

117.421875,-64.92354

text: northlimit=-63.30854; southlimit=-66.53854; westlimit=109.74805; eastLimit=125.0957; projection=WGS84

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