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Journal of Micropalaeontology An open-access journal of The Micropalaeontological Society
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Volume 3, issue 1
J. Micropalaeontol., 3, 9, 1984
https://doi.org/10.1144/jm.3.1.59
© Author(s) 1984. This work is distributed under
the Creative Commons Attribution 4.0 License.
J. Micropalaeontol., 3, 9, 1984
https://doi.org/10.1144/jm.3.1.59
© Author(s) 1984. This work is distributed under
the Creative Commons Attribution 4.0 License.

  01 Mar 1984

01 Mar 1984

Larger agglutinated foraminifera from the Faeroe Channel and Rockall Trough collected by W. B. Carpenter

John W. Murray and Caroline M. Taplin John W. Murray and Caroline M. Taplin
  • Department of Geology, University of Exeter, Exeter, England & Department of Geology, University College of Wales, Aberystwyth, Wales

Abstract. The Carpenter collection contains numerous slides of larger agglutinated foraminifera from the Faeroe Channel area. These have been re-identified during the preparation of a catalogue. The Faeroe Channel has a cold bottom water mass to the north (temperature ∼ 0°C) overlying sandy sediment with few larger agglutinated foraminifera, and a somewhat warmer water mass to the south (temperature > 2°C) overlying carbonate ooze with a diverse fauna of larger agglutinated foraminifera.

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