Acanthoscaphites
Encyclopedia
Acanthoscaphites is an extinct genus of cephalopod belonging to the Ammonite
subclass. The average diameter of its shell was approximately three fourths of an inch, but some specimens have been found with a diameter of slightly over two inches.
and Maastrichtian
times, approximately 80 million years ago. Its remains can be found in rocks of that age from many countries, such as:
Ammonite
Ammonite, as a zoological or paleontological term, refers to any member of the Ammonoidea an extinct subclass within the Molluscan class Cephalopoda which are more closely related to living coleoids Ammonite, as a zoological or paleontological term, refers to any member of the Ammonoidea an extinct...
subclass. The average diameter of its shell was approximately three fourths of an inch, but some specimens have been found with a diameter of slightly over two inches.
Classification
Acanthoscaphites was first described by Schluter in 1872. Subsequent taxonomic revisions may have rendered Acanthoscaphites synonymous with Scaphites and Trachyscaphites. Little information is available regarding the validity or synonymy of the Acanthoscaphites genus, so this page may be inaccurate. Please use caution when referring to this article.Species
Note: A. nodosa and A. nodosus may be misspellings of the same name.- A. gibbus
- A. nodosa
- A. nodosus
- A. praequadrispinosus
- A. spiniger
- A. schmidi
- A. tridens
Subgenus Euroscaphites
- A. (Euroscaphites) varians blaszkiewiczi
- A. (Euroscaphites) varians
- A. (Euroscaphites) varians varians
Biogeography
Acanthoscaphites was a widespread genus during CampanianCampanian
The Campanian is, in the ICS' geologic timescale, the fifth of six ages of the Late Cretaceous epoch . The Campanian spans the time from 83.5 ± 0.7 Ma to 70.6 ± 0.6 Ma ...
and Maastrichtian
Maastrichtian
The Maastrichtian is, in the ICS' geologic timescale, the latest age or upper stage of the Late Cretaceous epoch or Upper Cretaceous series, the Cretaceous period or system, and of the Mesozoic era or erathem. It spanned from 70.6 ± 0.6 Ma to 65.5 ± 0.3 Ma...
times, approximately 80 million years ago. Its remains can be found in rocks of that age from many countries, such as:
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