Published July 4, 2016
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Fig. 3. A in A new sediment-dwelling pholadid bivalve from Oligocene glaciomarine sediments of King George Island, West Antarctica
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Fig. 3. A. Outcrops of glaciomarine strata of the Oligocene Polonez Cove Formation (the Siklawa Member) on King George Island, arrow indicates position on Pholadidea gradzinskii horizons at Mazurek Point (photograph by AG, January 2007). B. Diamictite from bed in Siklawa Member of the Polonez Cove Formation, with Pholadidea gradzinskii bearing moulds at the base (arrowed). The diamictite contains metamorphic (m) and granitoid (g) clasts.
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Published as part of Hryniewicz, Krzysztof & Gaździcki, Andrzej, 2016, A new sediment-dwelling pholadid bivalve from Oligocene glaciomarine sediments of King George Island, West Antarctica, pp. 885-896 in Acta Palaeontologica Polonica 61 (4) on page 887, DOI: 10.4202/app.00255.2016, http://zenodo.org/record/13264480
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- Journal article: 10.4202/app.00255.2016 (DOI)
- Journal article: urn:lsid:plazi.org:pub:987C9B4B8639FF98FFFFFFEF1F07761D (LSID)
- Journal article: http://publication.plazi.org/id/987C9B4B8639FF98FFFFFFEF1F07761D (URL)
- Journal article: https://zenodo.org/record/13264480 (URL)