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Large Scaphitid Ammonites (Hoploscaphites) from the Upper Cretaceous (Upper Campanian–Lower Maastrichtian) of North America

Endless Variation on a Single Theme

Dados Bibliográficos

ID19259863
AutoresNeil H Landman (0000-0003-0038-8079, American Museum of Natural History), W James Kennedy (Oxford University Museum of Natural History, Oxford), Joyce C Grier (North Dakota State University), Joyce Grier (Larson Paleontology Unlimited, Keystone, South Dakota), Neal L Larson (Larson Paleontology Unlimited, Keystone, South Dakota), James W Grier (0000-0002-2416-7134, North Dakota State University), Thomas Linn (Early Earth Enterprises, Glendive, Montana), Lydia Tackett (North Dakota State University), Lydia S Tackett (0000-0003-4125-4907, North Dakota State University), Brian R Jicha (0000-0002-1228-515X, Department of Geoscience, University of Wisconsin, Madison)
Ano2020
Volume441
Fascículo1
Páginas1
Data de publicação2020-09-09
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoBulletin of the American Museum of Natural History (BOOK_SERIES)
Identificadores do periódicoISSN: 0003-0090 • E-ISSN: 1937-3546
EditoraAmerican Museum of Natural History (BioOne sponsored) (PUBLISHER)
DOI10.1206/0003-0090.441.1.1
OpenAlexW3084209899
IdiomaEN
Referências citadas64

We describe three species of large scaphitid ammonites (Ammonoidea: Ancyloceratina) from the Upper Cretaceous (upper Campanian–lower Maastrichtian) of the Western Interior of North America. Each species occurs as two dimorphs, referred to as macroconch and microconch. All three species share a similar pattern of ornamentation consisting of long, thin, nonbifurcating ribs on the adoral part of the phragmocone, suggesting that they constitute a single monophyletic clade. Macroconchs of Hoploscaphites crassus (Coryell and Salmon, 1934) are characterized by a globose whorl section, with closely spaced ventrolateral tubercles on the body chamber, usually persisting to the aperture. Macroconchs of Hoploscaphites plenus (Meek and Hayden, 1860) differ from those of H. crassus in having a more subquadrate whorl section with flatter flanks, and fewer, larger, and more widely spaced ventrolateral tubercles. Macroconchs of Hoploscaphites peterseni, n. sp., closely resemble those of H. crassus, but differ in being nearly circular in side view with a more compressed whorl section. All three species lived at approximately the same time in the same general area and depositional environment. They are abundant in the Baculites baculus Zone but also occasionally occur in the B. eliasi Zone and possibly lower part of the B. grandis Zone. They are present in the Pierre Shale of east-central Montana and east-central Wyoming, the Lewis Shale of south-central Wyoming, and the Bearpaw Shale of northeast Montana. It is possible that these three species represent subspecies within a single species or a “flock” of very closely related species, similar to the “species flocks” observed in modern cichlid fishes

Cenomanian · Cretaceous · Gastropoda · Sedimentary depositional environment · Structural basin · Whorl (mollusc) · Geology · Ichthyology and Marine Biology · Marine Biology and Ecology Research · Paleontology · Paleontology and Stratigraphy of Fossils

  • Oxygen and carbon isotope fractionation in biogenic aragonite

    Open Access•Ethan L Grossman, Teh-Lung Ku•Chemical Geology: Isotope…•1986

  • Description of Two Species of Hoploscaphites (Ammonoidea

    Open Access•Neil H Landman, William J Kennedy et al.•Bulletin of the American Museum…•2019

  • Scaphites of the “Nodosus Group” from the Upper Cretaceous (Campanian) of the Western Interior of North America

    Open Access•Neil H Landman, W James Kennedy et al.•Bulletin of the American Museum…•2010

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