Planktonic foraminifera, age of sediments and polarity reversals, New Britain, Papua New Guinea

Created 17/10/2025

Updated 17/10/2025

Samples from the Rudiger Point-Cape Ruge area, New Britain, are not from a conformable late Miocene-earliest Pliocene sequence, as was presumed by previous workers, but rather are of two age groups, one of general middle Miocene age, and a younger group of late Miocene age. A sample of volcanolithic sandstone, NG34B, is of late Pliocene-middle Pleistocene, Zone N.21-Zone N.22, age; this is the youngest marine sediment yet recognised in New Britain. Planktonic Zone N.18 is correlated, at least in part, with a normally magnetised interval.

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Title Planktonic foraminifera, age of sediments and polarity reversals, New Britain, Papua New Guinea
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/en/dataset/9a1fbc0c-0354-4e3b-b686-39a7994fc80d
Contact Point
Geoscience Australia Data
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
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      ],
      [
        152.87,
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      ],
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      ],
      [
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      ],
      [
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      ]
    ]
  ],
  "type": "Polygon"
}
Data Portal Geoscience Australia

Data Source

This dataset was originally found on Geoscience Australia "Planktonic foraminifera, age of sediments and polarity reversals, New Britain, Papua New Guinea". Please visit the source to access the original metadata of the dataset:
https://ecat.ga.gov.au/geonetwork/srv/eng/csw/dataset/planktonic-foraminifera-age-of-sediments-and-polarity-reversals-new-britain-papua-new-guinea