Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14
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...
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Online Access: | https://researchdata.edu.au/iceberg-rafted-debris-slope-a042kc14/1425329 https://doi.org/10.26179/5d5df0f2bb683 https://data.aad.gov.au/metadata/records/AAS_4419_KC14_IBRDFlux http://nla.gov.au/nla.party-617536 |
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ftands:oai:ands.org.au::1425329 2023-05-15T14:02:37+02:00 Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14 NOBLE, TARYN L (hasPrincipalInvestigator) NOBLE, TARYN L (processor) TOOZE, SIAN (hasPrincipalInvestigator) Australian Antarctic Data Centre (publisher) Spatial: northlimit=-63.30854; southlimit=-66.53854; westlimit=109.74805; eastLimit=125.0957; projection=WGS84 Temporal: From 2016-07-01 to 2019-06-30 https://researchdata.edu.au/iceberg-rafted-debris-slope-a042kc14/1425329 https://doi.org/10.26179/5d5df0f2bb683 https://data.aad.gov.au/metadata/records/AAS_4419_KC14_IBRDFlux http://nla.gov.au/nla.party-617536 unknown Australian Antarctic Data Centre https://researchdata.edu.au/iceberg-rafted-debris-slope-a042kc14/1425329 7806acad-cc66-4f27-a369-239afae595c6 doi:10.26179/5d5df0f2bb683 AAS_4419_KC14_IBRDFlux https://data.aad.gov.au/metadata/records/AAS_4419_KC14_IBRDFlux http://nla.gov.au/nla.party-617536 Australian Antarctic Data Centre geoscientificInformation oceans ICEBERGS EARTH SCIENCE SEA ICE SEDIMENT TRANSPORT MARINE SEDIMENTS SEDIMENT COMPOSITION ICEBERG RAFTED DEBRIS SEDIMENTOLOGY RV INVESTIGATOR ICEBERG RAFTED DEBRIS FLUX SEDIMENT CORERS SHIPS LABORATORY Paleo Start Date 2 ka Paleo Stop Date 25 ka PHANEROZOIC > CENOZOIC > QUATERNARY > HOLOCENE CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN > SABRINA CONTINENTAL SLOPE GEOGRAPHIC REGION > POLAR dataset ftands https://doi.org/10.26179/5d5df0f2bb683 2020-06-29T22:23:30Z 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. Dataset Antarc* Antarctica Sea ice Southern Ocean Research Data Australia (Australian National Data Service - ANDS) Southern Ocean ENVELOPE(109.74805,125.0957,-63.30854,-66.53854) |
institution |
Open Polar |
collection |
Research Data Australia (Australian National Data Service - ANDS) |
op_collection_id |
ftands |
language |
unknown |
topic |
geoscientificInformation oceans ICEBERGS EARTH SCIENCE SEA ICE SEDIMENT TRANSPORT MARINE SEDIMENTS SEDIMENT COMPOSITION ICEBERG RAFTED DEBRIS SEDIMENTOLOGY RV INVESTIGATOR ICEBERG RAFTED DEBRIS FLUX SEDIMENT CORERS SHIPS LABORATORY Paleo Start Date 2 ka Paleo Stop Date 25 ka PHANEROZOIC > CENOZOIC > QUATERNARY > HOLOCENE CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN > SABRINA CONTINENTAL SLOPE GEOGRAPHIC REGION > POLAR |
spellingShingle |
geoscientificInformation oceans ICEBERGS EARTH SCIENCE SEA ICE SEDIMENT TRANSPORT MARINE SEDIMENTS SEDIMENT COMPOSITION ICEBERG RAFTED DEBRIS SEDIMENTOLOGY RV INVESTIGATOR ICEBERG RAFTED DEBRIS FLUX SEDIMENT CORERS SHIPS LABORATORY Paleo Start Date 2 ka Paleo Stop Date 25 ka PHANEROZOIC > CENOZOIC > QUATERNARY > HOLOCENE CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN > SABRINA CONTINENTAL SLOPE GEOGRAPHIC REGION > POLAR Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14 |
topic_facet |
geoscientificInformation oceans ICEBERGS EARTH SCIENCE SEA ICE SEDIMENT TRANSPORT MARINE SEDIMENTS SEDIMENT COMPOSITION ICEBERG RAFTED DEBRIS SEDIMENTOLOGY RV INVESTIGATOR ICEBERG RAFTED DEBRIS FLUX SEDIMENT CORERS SHIPS LABORATORY Paleo Start Date 2 ka Paleo Stop Date 25 ka PHANEROZOIC > CENOZOIC > QUATERNARY > HOLOCENE CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN > SABRINA CONTINENTAL SLOPE GEOGRAPHIC REGION > POLAR |
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. |
author2 |
NOBLE, TARYN L (hasPrincipalInvestigator) NOBLE, TARYN L (processor) TOOZE, SIAN (hasPrincipalInvestigator) Australian Antarctic Data Centre (publisher) |
format |
Dataset |
title |
Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14 |
title_short |
Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14 |
title_full |
Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14 |
title_fullStr |
Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14 |
title_full_unstemmed |
Iceberg rafted debris flux on the Sabrina continental slope - for A042_KC14 |
title_sort |
iceberg rafted debris flux on the sabrina continental slope - for a042_kc14 |
publisher |
Australian Antarctic Data Centre |
url |
https://researchdata.edu.au/iceberg-rafted-debris-slope-a042kc14/1425329 https://doi.org/10.26179/5d5df0f2bb683 https://data.aad.gov.au/metadata/records/AAS_4419_KC14_IBRDFlux http://nla.gov.au/nla.party-617536 |
op_coverage |
Spatial: northlimit=-63.30854; southlimit=-66.53854; westlimit=109.74805; eastLimit=125.0957; projection=WGS84 Temporal: From 2016-07-01 to 2019-06-30 |
long_lat |
ENVELOPE(109.74805,125.0957,-63.30854,-66.53854) |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Antarc* Antarctica Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctica Sea ice Southern Ocean |
op_source |
Australian Antarctic Data Centre |
op_relation |
https://researchdata.edu.au/iceberg-rafted-debris-slope-a042kc14/1425329 7806acad-cc66-4f27-a369-239afae595c6 doi:10.26179/5d5df0f2bb683 AAS_4419_KC14_IBRDFlux https://data.aad.gov.au/metadata/records/AAS_4419_KC14_IBRDFlux http://nla.gov.au/nla.party-617536 |
op_doi |
https://doi.org/10.26179/5d5df0f2bb683 |
_version_ |
1766272952143183872 |