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Saunders, W. B., Ramsbottom, W. H. C. (1993) Re-evaluation of two Early Pennsylvanian (Middle Namurian) ammonoids and their bearing on mid-Carboniferous correlations. Journal of Paleontology, 67 (6) 993-999 doi:10.1017/s0022336000025300

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Reference TypeJournal (article/letter/editorial)
TitleRe-evaluation of two Early Pennsylvanian (Middle Namurian) ammonoids and their bearing on mid-Carboniferous correlations
JournalJournal of Paleontology
AuthorsSaunders, W. B.Author
Ramsbottom, W. H. C.Author
Year1993 (November)Volume67
Issue6
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000025300Search in ResearchGate
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Mindat Ref. ID416097Long-form Identifiermindat:1:5:416097:1
GUID0
Full ReferenceSaunders, W. B., Ramsbottom, W. H. C. (1993) Re-evaluation of two Early Pennsylvanian (Middle Namurian) ammonoids and their bearing on mid-Carboniferous correlations. Journal of Paleontology, 67 (6) 993-999 doi:10.1017/s0022336000025300
Plain TextSaunders, W. B., Ramsbottom, W. H. C. (1993) Re-evaluation of two Early Pennsylvanian (Middle Namurian) ammonoids and their bearing on mid-Carboniferous correlations. Journal of Paleontology, 67 (6) 993-999 doi:10.1017/s0022336000025300
In(1993, November) Journal of Paleontology Vol. 67 (6) Cambridge University Press (CUP)
Abstract/NotesReticuloceras (Swintoceras) n. subgen. unites an early group of the mid-Carboniferous goniatite family Reticulocertidae, in which reticulate sculpture is weakly developed or lacking and the typically reticuloceratid suture has slightly expanded ventral prongs. The type species, Reticuloceras (S.) spiraloides (Bisat and Hudson, 1943), is a rare, poorly known species from the British Namurian. Two additional species, R. (S.) wainwrighti (Quinn, 1966) and R. (S.) tiro (Gordon, 1969), are common in the basal type Morrowan Series, Lower Pennsylvanian, of Arkansas. Swintoceras occurs with two distinctive, late forms of the ammonoid, Hudsonoceras: Hd. ornatum (Foord and Crick, 1897) in Britain and Hd. moorei Quinn and Saunders, 1968, in Arkansas. The cooccurrence of these taxa correlates the basal Morrowan in its type region with the Namurian Reticuloceras nodosum (R1b) Zone of Britain and thereby also dates the close of the Mid-Carboniferous Eustatic Event in the North American Midcontinent.


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