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Clarke, A. H., Grant, D. R., Macpherson, Elizabeth (1972) The Relationship of Atractodon stonei (Pilsbry) (Mollusca, Buccinidae) to the Pleistocene Stratigraphy and Paleoecology of Southwestern Nova Scotia. Canadian Journal of Earth Sciences, 9 (8) 1030-1038 doi:10.1139/e72-086

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Reference TypeJournal (article/letter/editorial)
TitleThe Relationship of Atractodon stonei (Pilsbry) (Mollusca, Buccinidae) to the Pleistocene Stratigraphy and Paleoecology of Southwestern Nova Scotia
JournalCanadian Journal of Earth Sciences
AuthorsClarke, A. H.Author
Grant, D. R.Author
Macpherson, ElizabethAuthor
Year1972 (August 1)Volume9
Issue8
PublisherCanadian Science Publishing
DOIdoi:10.1139/e72-086Search in ResearchGate
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Mindat Ref. ID473434Long-form Identifiermindat:1:5:473434:9
GUID0
Full ReferenceClarke, A. H., Grant, D. R., Macpherson, Elizabeth (1972) The Relationship of Atractodon stonei (Pilsbry) (Mollusca, Buccinidae) to the Pleistocene Stratigraphy and Paleoecology of Southwestern Nova Scotia. Canadian Journal of Earth Sciences, 9 (8) 1030-1038 doi:10.1139/e72-086
Plain TextClarke, A. H., Grant, D. R., Macpherson, Elizabeth (1972) The Relationship of Atractodon stonei (Pilsbry) (Mollusca, Buccinidae) to the Pleistocene Stratigraphy and Paleoecology of Southwestern Nova Scotia. Canadian Journal of Earth Sciences, 9 (8) 1030-1038 doi:10.1139/e72-086
In(1972, August) Canadian Journal of Earth Sciences Vol. 9 (8) Canadian Science Publishing
Abstract/Notes The extinct Pleistocene buccinid gastropod Atractodon stonei (Pilsbry 1893), formerly known as Neptunea stonei (Pilsbry), has been found in a southern Nova Scotian deposit. The species had been previously reported only from (presumably) Sangamon deposits at Nantucket Island, Massachusetts and at other locations south to Cape Hatteras, North Carolina. Associated molluscs from all A. stonei deposits show that it probably lived in about 5 to 20 fm and in a climate like that of the present Acadian marine zoogeographic region.Although the Nova Scotian specimens produced radiocarbon ages of 38 000 years B.P. stratigraphic and paleoclimatological data indicate Sangamon age and the radiocarbon dates are presumed to be too young. Atractodon stonei may qualify as a useful Pleistocene (Sangamon) index fossil representative of relatively specific paleoecological conditions.


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