Published January 12, 2022 | Version v1
Taxonomic treatment Open

Spiroplectammina undetermined

  • 1. Marine Research Institute and Department of Geological Sciences, University of Cape Town, Private Bag X 3, Rondebosch, 7701, South Africa. & Department of Environmental and Geographical Sciences, University of Cape Town, Private Bag X 3, Rondebosch, 7701, South Africa; & Invertebrate palaeontology and Geology, Iziko South African Museum, P. O. Box 61, Cape Town 8000, South Africa. john. compton @ uct. ac. za; https: // orcid. org / 0000 - 0002 - 0765 - 4141
  • 2. Marine Research Institute and Department of Geological Sciences, University of Cape Town, Private Bag X 3, Rondebosch, 7701, South Africa.

Description

Spiroplectammina sp. Pl. 1, figs. 1a–b

Description: The chamber walls are agglutinated and well cemented. The test is flattened and broad, with the margins sub-rounded. In cross section, the test is trapezoid in shape. Chambers are initially planispiral, becoming biserial, with flush sutures. The arched aperture is situated along the margin of the terminal chamber.

Remarks: Only a few tests were identified (not exceeding 5% in samples) in core 2670, measuring up to 0.4x 0.6 mm. The tests are commonly broken or have predatory holes.

Life strategy: Species of the genus Spiroplectammina are infaunal in low oxygen environments (Hallam & Wignall, 1997) of increased food availability (Alegret & Thomas, 2007).

Regional occurrence: This species is recorded to occur in the middle Miocene sediments of the Namibian outer continental shelf, south of the Kunene River mouth.

Notes

Published as part of Bergh, Eugene W. & Compton, John S., 2022, Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf, pp. 1-55 in Zootaxa 5091 (1) on page 6, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434

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Linked records

Additional details

Biodiversity

References

  • Hallam, A. & Wignall, P. B. (1997) Mass extinctions and their aftermath. Oxford University Press, Oxford, 328 pp.
  • Alegret, L. & Thomas, E. (2007) Deep-Sea environments across the Cretaceous / Paleogene boundary in the eastern South Atlantic Ocean (ODP Leg 208, Walvis Ridge). Marine Micropalaeontology, 64, 1 - 17. https: // doi. org / 10.1016 / j. marmicro. 2006.12.003