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Hannibal, Joseph T. (1994) Methods for distinguishing carbonized specimens of the presumed cephalopod aptychus Sidetes (Spathiocaris) from the plant Protosalvinia (Foerstia) Journal of Paleontology, 68 (3) 671-673 doi:10.1017/s0022336000026007

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Reference TypeJournal (article/letter/editorial)
TitleMethods for distinguishing carbonized specimens of the presumed cephalopod aptychus Sidetes (Spathiocaris) from the plant Protosalvinia (Foerstia)
JournalJournal of Paleontology
AuthorsHannibal, Joseph T.Author
Year1994 (May)Volume68
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000026007Search in ResearchGate
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Mindat Ref. ID416300Long-form Identifiermindat:1:5:416300:2
GUID0
Full ReferenceHannibal, Joseph T. (1994) Methods for distinguishing carbonized specimens of the presumed cephalopod aptychus Sidetes (Spathiocaris) from the plant Protosalvinia (Foerstia) Journal of Paleontology, 68 (3) 671-673 doi:10.1017/s0022336000026007
Plain TextHannibal, Joseph T. (1994) Methods for distinguishing carbonized specimens of the presumed cephalopod aptychus Sidetes (Spathiocaris) from the plant Protosalvinia (Foerstia) Journal of Paleontology, 68 (3) 671-673 doi:10.1017/s0022336000026007
In(1994, May) Journal of Paleontology Vol. 68 (3) Cambridge University Press (CUP)
Abstract/NotesThe purpose of this note is to point out the similarities between Protosalvinia (Foerstia) and Sidetes (Spathiocaris) and to discuss characters that can be used to distinguish the two taxa. Protosalvinia Clarke, 1885 (Figure 1.1-1.4), also commonly referred to by the junior subjective synonym Foerstia, is a plant fossil that is frequently noted as occurring in Upper Devonian black shale sequences of North America. This taxon has been of great interest to stratigraphers, paleoecologists, plant taxonomists, and plant morphologists over the years (see, for example, Winslow, 1962, p. 7, p. 22, fig. 3; Barron and Ettensohn, 1981, p. 30-31; Matthews, 1983; and Romankiw et al., 1988). Most workers in recent years have considered Protosalvinia to be a marine alga, but there is also evidence for a land plant affinity (Romankiw et al., 1988).


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