Planktonic foraminifera and age of sediments, west Tasmanian margin, South Tasman Rise and Lord Howe Rise.

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Description:

Dredge and core samples of sediments recovered from the west Tasmanian margin, South Tasman Rise and the Lord Howe Rise, on R.V. Sonne, are of possible Eocene, late Oligocene, early and late Miocene, early and late Pliocene, and Pleistocene or younger ages. Reworked Paleocene and Eocene specimens occur in some cores and dredge samples of late Oligocene age. Some cores show a major stratigraphical break from late Oligocene to Pleistocene. The coiling direction of Turborotalia pachyderma was investigated as a possible method of correlation of younger cores, and also as an indicator of palaeoclimatic changes. No correlation between cores was possible using coiling curves, which indicate rapid and irregular changes in sea-water temperatures over small areas, assuming that the coiling direction of T. pachyderma is an indication of sea-water temperature. http://datadiscoverystudio.org/geoportal/rest/metadata/item/41a9c74028c94645933cbc590d554674/html

Metadata

Name Value Last Modified
@context
  • @context:
  • @id: urn:81238
  • @type: Dataset
  • additionalType:
    • geolink:Dataset
    • vivo:Dataset
  • citation: Belford, D.J. (1989-01-01T00:00:00), Planktonic foraminifera and age of sediments, west Tasmanian margin, South Tasman Rise and Lord Howe Rise., Bureau of Mineral Resources, Geology and Geophysics, urn:81238.
  • creator:
      • @type: Role
      • creator:
        • @type: Person
        • additionalType: geolink:Person
        • name: Belford, D.J.
      • roleName: author
  • datePublished: 1989-01-01T00:00:00
  • description: Dredge and core samples of sediments recovered from the west Tasmanian margin, South Tasman Rise and the Lord Howe Rise, on R.V. Sonne, are of possible Eocene, late Oligocene, early and late Miocene, early and late Pliocene, and Pleistocene or younger ages. Reworked Paleocene and Eocene specimens occur in some cores and dredge samples of late Oligocene age. Some cores show a major stratigraphical break from late Oligocene to Pleistocene. The coiling direction of Turborotalia pachyderma was investigated as a possible method of correlation of younger cores, and also as an indicator of palaeoclimatic changes. No correlation between cores was possible using coiling curves, which indicate rapid and irregular changes in sea-water temperatures over small areas, assuming that the coiling direction of T. pachyderma is an indication of sea-water temperature.
  • distribution:
      • @id: urn:file//nas/cds/open/journals/Jou1989_v11_n1_p037/Jou1989_v11_n1_p037.pdf
      • @type: DataDownload
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            • sales@ga.gov.au
          • name: Commonwealth of Australia (Geoscience Australia)
        • roleName: distributor
      • url:
      • @id: urn:filenolongerexists
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      • description: Download the journal article (pdf).
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          • @type: Organization
          • email:
            • sales@ga.gov.au
          • name: Commonwealth of Australia (Geoscience Australia)
        • roleName: distributor
      • url:
  • identifier:
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      • propertyID: dataset identifier
      • value: urn:81238
      • @type: PropertyValue
      • propertyID: dataset identifier
      • value: urn:Product
  • includedInDataCatalog:
    • @type: DataCatalog
    • name: Name of catalog source for record being transformed
    • url: not defined
  • keywords:
    • GA Publication
    • Journal
    • Earth Sciences
    • Published_External
    • Dredge
    • Core
    • Correlation
    • Eocene
    • Oligocene
    • Miocene
    • Pliocene
    • Pleistocene
    • Paleocene
    • Geoscience Australia
    • Sea Water
    • West
    • South
    • Direction
    • Temperature
    • Earth Science
  • license:
      • @type: DigitalDocument
      • description: accessConstraints: license.
      • name: MD_LegalConstraints
      • @type: DigitalDocument
      • description: useConstraints: license. otherConstraints: Creative Commons Attribution 4.0 International Licence.
      • name: MD_LegalConstraints
      • @type: DigitalDocument
      • description: classification:
      • name: MD_SecurityConstraints
  • name: Planktonic foraminifera and age of sediments, west Tasmanian margin, South Tasman Rise and Lord Howe Rise.
  • publisher:
      • :
        • @type: Organization
        • name: Bureau of Mineral Resources, Geology and Geophysics
      • @type: Role
      • roleName: publisher
  • spatialCoverage:
    • @type: Place
    • description: Tasman
    • geo:
      • @type: GeoShape
      • box: 171.88362156900007, -42.21453141199994 173.41362156900004, -40.68453141199994
Extracted by http://clowder.ncsa.illinois.edu/extractors/deprecatedapi on Oct 11, 2020
  • @context:
  • @id: urn:81238
  • @type: Dataset
  • additionalType:
    • geolink:Dataset
    • vivo:Dataset
  • citation: Belford, D.J. (1989-01-01T00:00:00), Planktonic foraminifera and age of sediments, west Tasmanian margin, South Tasman Rise and Lord Howe Rise., Bureau of Mineral Resources, Geology and Geophysics, urn:81238.
  • creator:
      • @type: Role
      • creator:
        • @type: Person
        • additionalType: geolink:Person
        • name: Belford, D.J.
      • roleName: author
  • datePublished: 1989-01-01T00:00:00
  • description: Dredge and core samples of sediments recovered from the west Tasmanian margin, South Tasman Rise and the Lord Howe Rise, on R.V. Sonne, are of possible Eocene, late Oligocene, early and late Miocene, early and late Pliocene, and Pleistocene or younger ages. Reworked Paleocene and Eocene specimens occur in some cores and dredge samples of late Oligocene age. Some cores show a major stratigraphical break from late Oligocene to Pleistocene. The coiling direction of Turborotalia pachyderma was investigated as a possible method of correlation of younger cores, and also as an indicator of palaeoclimatic changes. No correlation between cores was possible using coiling curves, which indicate rapid and irregular changes in sea-water temperatures over small areas, assuming that the coiling direction of T. pachyderma is an indication of sea-water temperature.
  • distribution:
      • @id: urn:file//nas/cds/open/journals/Jou1989_v11_n1_p037/Jou1989_v11_n1_p037.pdf
      • @type: DataDownload
      • additionalType: dcat:distribution
      • dcat:accessURL:
      • description: Service Protocol: .
      • fileFormat:
        • pdf v.Unknown
        • pdf v.Unknown
      • provider:
        • @type: Role
        • provider:
          • @type: Organization
          • email:
            • sales@ga.gov.au
          • name: Commonwealth of Australia (Geoscience Australia)
        • roleName: distributor
      • url:
      • @id: urn:filenolongerexists
      • @type: DataDownload
      • additionalType: dcat:distribution
      • dcat:accessURL:
      • description: Download the journal article (pdf).
      • fileFormat:
        • pdf v.Unknown
        • pdf v.Unknown
      • provider:
        • @type: Role
        • provider:
          • @type: Organization
          • email:
            • sales@ga.gov.au
          • name: Commonwealth of Australia (Geoscience Australia)
        • roleName: distributor
      • url:
  • identifier:
      • @type: PropertyValue
      • propertyID: dataset identifier
      • value: urn:81238
      • @type: PropertyValue
      • propertyID: dataset identifier
      • value: urn:Product
  • includedInDataCatalog:
    • @type: DataCatalog
    • name: Name of catalog source for record being transformed
    • url: not defined
  • keywords:
    • GA Publication
    • Journal
    • Earth Sciences
    • Published_External
    • Dredge
    • Core
    • Correlation
    • Eocene
    • Oligocene
    • Miocene
    • Pliocene
    • Pleistocene
    • Paleocene
    • Geoscience Australia
    • Sea Water
    • West
    • South
    • Direction
    • Temperature
    • Earth Science
  • license:
      • @type: DigitalDocument
      • description: accessConstraints: license.
      • name: MD_LegalConstraints
      • @type: DigitalDocument
      • description: useConstraints: license. otherConstraints: Creative Commons Attribution 4.0 International Licence.
      • name: MD_LegalConstraints
      • @type: DigitalDocument
      • description: classification:
      • name: MD_SecurityConstraints
  • name: Planktonic foraminifera and age of sediments, west Tasmanian margin, South Tasman Rise and Lord Howe Rise.
  • publisher:
      • :
        • @type: Organization
        • name: Bureau of Mineral Resources, Geology and Geophysics
      • @type: Role
      • roleName: publisher
  • spatialCoverage:
    • @type: Place
    • description: Tasman
    • geo:
      • @type: GeoShape
      • box: 171.88362156900007, -42.21453141199994 173.41362156900004, -40.68453141199994

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Last Modified: Oct 11, 2020 04:17:27

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