Diatom recovery from core MD88-787: Raw counts

Core MD88-787 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge, within the Polar Front Zone. \n\nA total of 69 diatom species and taxa were recorded in core MD88-787. Over time, the core indi...

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Bibliographic Details
Other Authors: Department of Biological Sciences, Macquarie University (isOwnedBy)
Format: Dataset
Language:unknown
Published: data.gov.au
Subjects:
Online Access:https://researchdata.edu.au/diatom-recovery-core-raw-counts/1935366
http://data.gov.au/dataset/9a04d643-b001-467f-bce2-b263cce0d8cd
id ftands:oai:ands.org.au::1935366
record_format openpolar
spelling ftands:oai:ands.org.au::1935366 2023-09-05T13:23:05+02:00 Diatom recovery from core MD88-787: Raw counts Department of Biological Sciences, Macquarie University (isOwnedBy) Spatial: 145.0,-56.5 145.5,-56.5 145.5,-56.0 145.0,-56.0 145.0,-56.5 Spatial: true https://researchdata.edu.au/diatom-recovery-core-raw-counts/1935366 http://data.gov.au/dataset/9a04d643-b001-467f-bce2-b263cce0d8cd unknown data.gov.au https://researchdata.edu.au/diatom-recovery-core-raw-counts/1935366 http://data.gov.au/dataset/9a04d643-b001-467f-bce2-b263cce0d8cd diatom-recovery-from-core-md88-787-raw-counts Department of Biological Sciences, Macquarie University 53001900 53120000 Biosphere Diatoms Fragilariopsis kerguelensis Fragilariopsis separanda Microbiota Thalassiosira lentiginosa dataset ftands 2023-08-14T23:01:31Z Core MD88-787 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge, within the Polar Front Zone. \n\nA total of 69 diatom species and taxa were recorded in core MD88-787. Over time, the core indicates a reduction in the number of diatom valves in the sediments for the last glacial. This trend is not observed during the previous 'glacial' period in isotope-stage 4, but is again noted in isotope-stage 6. Interglacial isotope-stages 3 and 5 indicate higher- or equivalent-diatom content comparable to isotope-stage 1. The reduced diatom signal during the glacials appears odd since the expectation was for an enhanced diatom signal produced by the northward shifting fronts. The decrease in signal could be interpreted as being affected by sea-ice cover and the resulting change towards more lightly silicified diatom species. App 1-1.pdf - App 6-6 787.pdf - aodn:bluenet_datasets_southern_indian_ocean - Core Data – Southern and Indian Ocean http://gcmd.nasa.gov/Resources/valids/keyword_list.html - http://www.marine.csiro.au/csquares/index.html - Dataset Sea ice Research Data Australia (Australian National Data Service - ANDS) Indian Tasman Fracture Zone ENVELOPE(151.000,151.000,-58.500,-58.500)
institution Open Polar
collection Research Data Australia (Australian National Data Service - ANDS)
op_collection_id ftands
language unknown
topic 53001900
53120000
Biosphere
Diatoms
Fragilariopsis kerguelensis
Fragilariopsis separanda
Microbiota
Thalassiosira lentiginosa
spellingShingle 53001900
53120000
Biosphere
Diatoms
Fragilariopsis kerguelensis
Fragilariopsis separanda
Microbiota
Thalassiosira lentiginosa
Diatom recovery from core MD88-787: Raw counts
topic_facet 53001900
53120000
Biosphere
Diatoms
Fragilariopsis kerguelensis
Fragilariopsis separanda
Microbiota
Thalassiosira lentiginosa
description Core MD88-787 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge, within the Polar Front Zone. \n\nA total of 69 diatom species and taxa were recorded in core MD88-787. Over time, the core indicates a reduction in the number of diatom valves in the sediments for the last glacial. This trend is not observed during the previous 'glacial' period in isotope-stage 4, but is again noted in isotope-stage 6. Interglacial isotope-stages 3 and 5 indicate higher- or equivalent-diatom content comparable to isotope-stage 1. The reduced diatom signal during the glacials appears odd since the expectation was for an enhanced diatom signal produced by the northward shifting fronts. The decrease in signal could be interpreted as being affected by sea-ice cover and the resulting change towards more lightly silicified diatom species. App 1-1.pdf - App 6-6 787.pdf - aodn:bluenet_datasets_southern_indian_ocean - Core Data – Southern and Indian Ocean http://gcmd.nasa.gov/Resources/valids/keyword_list.html - http://www.marine.csiro.au/csquares/index.html -
author2 Department of Biological Sciences, Macquarie University (isOwnedBy)
format Dataset
title Diatom recovery from core MD88-787: Raw counts
title_short Diatom recovery from core MD88-787: Raw counts
title_full Diatom recovery from core MD88-787: Raw counts
title_fullStr Diatom recovery from core MD88-787: Raw counts
title_full_unstemmed Diatom recovery from core MD88-787: Raw counts
title_sort diatom recovery from core md88-787: raw counts
publisher data.gov.au
url https://researchdata.edu.au/diatom-recovery-core-raw-counts/1935366
http://data.gov.au/dataset/9a04d643-b001-467f-bce2-b263cce0d8cd
op_coverage Spatial: 145.0,-56.5 145.5,-56.5 145.5,-56.0 145.0,-56.0 145.0,-56.5
Spatial: true
long_lat ENVELOPE(151.000,151.000,-58.500,-58.500)
geographic Indian
Tasman Fracture Zone
geographic_facet Indian
Tasman Fracture Zone
genre Sea ice
genre_facet Sea ice
op_source Department of Biological Sciences, Macquarie University
op_relation https://researchdata.edu.au/diatom-recovery-core-raw-counts/1935366
http://data.gov.au/dataset/9a04d643-b001-467f-bce2-b263cce0d8cd
diatom-recovery-from-core-md88-787-raw-counts
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