Data

Sedimentary Processes in the Fjord-like Embayments of the Vestfold and Larsemann Hills

Australian Antarctic Data Centre
MCMINN, ANDREW
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=https://data.aad.gov.au/metadata/records/ASAC_705&rft.title=Sedimentary Processes in the Fjord-like Embayments of the Vestfold and Larsemann Hills&rft.identifier=https://data.aad.gov.au/metadata/records/ASAC_705&rft.publisher=Australian Antarctic Data Centre&rft.description=Ellis Fjord is a small, fjord-like marine embayment in the vestfold Hills, eastern Antarctica. Modern sediment input is dominated by a biogenic diatom rain, although aeolian, fluvial, ice-rafted, slumped and tidal sediments also make a minor contribution. In areas where bioturbation is significant relict glaciogenic sediments are reworked into the fine-grained diatomaceous sediments to produce poorly sorted fine sands and silts. Where the bottom waters are anoxic, sediments remain unbioturbated and have a high biogenic silica component. Three depositional and non-depositional facies can be recognised in the fjord: an area of non-deposition around the shoreline; a relict morainal facies in areas of low sedimentation and high bioturbation; and a basinal facies in the deeper areas of the fjord.&rft.creator=MCMINN, ANDREW &rft.date=2000&rft.coverage=northlimit=-68.0; southlimit=-68.5; westlimit=78.0; eastLimit=79.0; projection=WGS84&rft.coverage=northlimit=-68.0; southlimit=-68.5; westlimit=78.0; eastLimit=79.0; 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=ASAC_705 when using these data.&rft_subject=oceans&rft_subject=SEDIMENTATION&rft_subject=EARTH SCIENCE&rft_subject=OCEANS&rft_subject=COASTAL PROCESSES&rft_subject=DIATOMS&rft_subject=BIOLOGICAL CLASSIFICATION&rft_subject=PROTISTS&rft_subject=MICROALGAE&rft_subject=PLANTS&rft_subject=PHYTOPLANKTON&rft_subject=BIOSPHERE&rft_subject=AQUATIC ECOSYSTEMS&rft_subject=PLANKTON&rft_subject=AEOLIAN&rft_subject=ANTARCTICA&rft_subject=BIOGENIC&rft_subject=FJORD&rft_subject=FLUVIAL&rft_subject=HOLOCENE&rft_subject=ICE-RAFTING&rft_subject=SEDIMENTS&rft_subject=TIDAL&rft_subject=VESTFOLD HILLS&rft_subject=FIELD SURVEYS&rft_subject=CONTINENT > ANTARCTICA&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=ASAC_705 when using these data.

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Brief description

Ellis Fjord is a small, fjord-like marine embayment in the vestfold Hills, eastern Antarctica. Modern sediment input is dominated by a biogenic diatom rain, although aeolian, fluvial, ice-rafted, slumped and tidal sediments also make a minor contribution. In areas where bioturbation is significant relict glaciogenic sediments are reworked into the fine-grained diatomaceous sediments to produce poorly sorted fine sands and silts. Where the bottom waters are anoxic, sediments remain unbioturbated and have a high biogenic silica component. Three depositional and non-depositional facies can be recognised in the fjord: an area of non-deposition around the shoreline; a relict morainal facies in areas of low sedimentation and high bioturbation; and a basinal facies in the deeper areas of the fjord.

Issued: 2000-08-04

Data time period: 1991-10-01 to 1991-11-30

Data time period: 1995-11-01 to 1995-11-30

This dataset is part of a larger collection

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79,-68 79,-68.5 78,-68.5 78,-68 79,-68

78.5,-68.25

text: northlimit=-68.0; southlimit=-68.5; westlimit=78.0; eastLimit=79.0; projection=WGS84

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