Data

Diatom recovery from core MD88-779: Raw counts

Australian Ocean Data Network
Armand, Leanne ; De Deckker, Patrick ; Pichon, Jean-Jacques
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=http://catalogue-aodn.prod.aodn.org.au/geonetwork/srv/eng/search?uuid=c091c950-5a9c-11dc-bd3f-00188b4c0af8&rft.title=Diatom recovery from core MD88-779: Raw counts&rft.identifier=http://catalogue-aodn.prod.aodn.org.au/geonetwork/srv/eng/search?uuid=c091c950-5a9c-11dc-bd3f-00188b4c0af8&rft.description=Core MD88-779 was taken during the 1988 French ASPARA IV cruise in the South East Indian Ocean aboard the Marion Dufresne. The core is situated on the South Tasman Rise (47º50.690S, 146º32.750E) at a depth of 2260m. Although the core recovered was 6.7m long, only the top 2.6m were studied as preliminary investigations had indicated that this section covered the last two glacial cycles. A total of 37 diatom species and taxa were observed in the core samples, comprising predominantly warm-water fauna. The majority of samples were poorly preserved and showed high levels of dissolution making identification to species level often difficult. Species with greatest abundances were those more heavily silicified (e.g. Fragilariopsis kerguelansis), and to a lesser extent the warm-water forms (e.g. Fragilariopsis doliolu). The complete loss of a diatom record at 170cm and 210/220cm in the core is extremely unusual. The diatom signal is interpreted as having been removed by increased water mass velocity, extreme post-depositional silica dissolution or decreased productivity. There is no sedimentological evidence from the core which provides further interpretation. The diatom recovery from this core is considerably low when compared to samples from the Southern Ocean.Maintenance and Update Frequency: notPlannedStatement: Material was recovered using a Kullenberg core. The method used to produce diatom slides from the sediment sample is described in the 'methodology' document uploaded within this record.Statement: The core was sampled every 10cm from the sediment surface down to a depth of 260cm. The majority of samples were poorly preserved and showed high levels of dissolution making identification to species level often difficult. Parameters: Core depth (cm), diatom species, diatom subtotal and silica subtotal.&rft.creator=Armand, Leanne &rft.creator=De Deckker, Patrick &rft.creator=Pichon, Jean-Jacques &rft.date=2007&rft.coverage=westlimit=130; southlimit=-48.00; eastlimit=155; northlimit=-35.00&rft.coverage=westlimit=130; southlimit=-48.00; eastlimit=155; northlimit=-35.00&rft.coverage=uplimit=2266.7; downlimit=2260&rft.coverage=uplimit=2266.7; downlimit=2260&rft_rights= http://creativecommons.org/licenses/by/2.5/au/&rft_rights=http://i.creativecommons.org/l/by/2.5/au/88x31.png&rft_rights=WWW:LINK-1.0-http--related&rft_rights=License Graphic&rft_rights=Creative Commons Attribution 2.5 Australia License&rft_rights=http://creativecommons.org/international/au/&rft_rights=WWW:LINK-1.0-http--related&rft_rights=WWW:LINK-1.0-http--related&rft_rights=License Text&rft_rights=The citation in a list of references is: citation author name/s (year metadata published), metadata title. Citation author organisation/s. File identifier and Data accessed at (add http link).&rft_rights=Users are kindly requested to contact the principal investigator for authorisation before utilising or reproducing any material&rft_rights=Creative Commons Attribution 2.5 Australia License http://creativecommons.org/licenses/by/2.5/au&rft_subject=DIATOMS&rft_subject=EARTH SCIENCE&rft_subject=BIOLOGICAL CLASSIFICATION&rft_subject=PLANTS&rft_subject=MICROALGAE&rft_subject=Fragilariopsis doliolus&rft_subject=Roperia tesselata&rft_subject=Hemidiscus cuneiformis&rft_subject=Azpeitia tabularis&rft_subject=Thalassiosira lineata&rft_subject=Thalassionema nitzschioides&rft_subject=53120000&rft_subject=53001900&rft_subject=53150900&rft_subject=core_depth&rft_subject=taxonomic_name&rft_subject=taxonomic_group_count&rft.type=dataset&rft.language=English Access the data

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The citation in a list of references is: citation author name/s (year metadata published), metadata title. Citation author organisation/s. File identifier and Data accessed at (add http link).

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Brief description

Core MD88-779 was taken during the 1988 French ASPARA IV cruise in the South East Indian Ocean aboard the Marion Dufresne. The core is situated on the South Tasman Rise (47º50.690S, 146º32.750E) at a depth of 2260m. Although the core recovered was 6.7m long, only the top 2.6m were studied as preliminary investigations had indicated that this section covered the last two glacial cycles.

A total of 37 diatom species and taxa were observed in the core samples, comprising predominantly warm-water fauna. The majority of samples were poorly preserved and showed high levels of dissolution making identification to species level often difficult. Species with greatest abundances were those more heavily silicified (e.g. Fragilariopsis kerguelansis), and to a lesser extent the warm-water forms (e.g. Fragilariopsis doliolu).

The complete loss of a diatom record at 170cm and 210/220cm in the core is extremely unusual. The diatom signal is interpreted as having been removed by increased water mass velocity, extreme post-depositional silica dissolution or decreased productivity. There is no sedimentological evidence from the core which provides further interpretation.

The diatom recovery from this core is considerably low when compared to samples from the Southern Ocean.

Lineage

Maintenance and Update Frequency: notPlanned
Statement: Material was recovered using a Kullenberg core.

The method used to produce diatom slides from the sediment sample is described in the 'methodology' document uploaded within this record.
Statement: The core was sampled every 10cm from the sediment surface down to a depth of 260cm.

The majority of samples were poorly preserved and showed high levels of dissolution making identification to species level often difficult.

Parameters: Core depth (cm), diatom species, diatom subtotal and silica subtotal.

Notes

Credit
Mountain Mass Spectrometry Laboratory (Colorado)
Credit
Institute of Antarctic and Southern Ocean Studies (IASOS)
Credit
Institut Français pour la Recherche et Technologie Polaires (IFRTP)
Credit
Terres Australes et Antarctiques Françaises (TAAF)
Credit
Australian Postgraduate Research Award (APRA)
Purpose
To reconstruct the first sea-surface temperature and sea-ice record history of the Southern Ocean south of Australia.

Issued: 29 08 2007

Data time period: 1988 to 1988

This dataset is part of a larger collection

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155,-35 155,-48 130,-48 130,-35 155,-35

142.5,-41.5

text: westlimit=130; southlimit=-48.00; eastlimit=155; northlimit=-35.00

text: uplimit=2266.7; downlimit=2260

Identifiers
  • global : c091c950-5a9c-11dc-bd3f-00188b4c0af8