DIMORPHISM IN CARBONIFEROUS AMMONOIDS FROM THE SOUTHERN MIDCONTINENT, UNITED STATES
Before its destruction, the type section of the Rockford Limestone, (Early Mississippian - Osagean), southeastern Indiana, yielded abundant ammonoid specimens of several species, including Muensteroceras oweni (Hall), and M. parallelum (Hall). The two species of Muensteroceras at this locality differ only slightly in suture pattern, while the conch of M. parallelum is relatively compressed with a narrow umbilicus, compared to M. oweni with a wider, more openly umbilicate conch. These characters suggest that M. oweni and M. parallelum represent a single dimorphic species.
To test this hypothesis, conch dimensions (maximum diameter, whorl width, whorl height, and umbilical diameter) in Muensteroceras oweni and M. parallelum were measured and compared to the Carboniferous antidimorphic ammonoid Arkanites relictus (Quinn, McCaleb and Webb. Dimorphism in each measurement, estimated by the ‘mean method’ of Plavcan (2004), is expressed as ln(mean subglobose)-ln(mean subdiscoidal) (see table below). M. oweni/M. parallelum displays less pronounced dimorphism than A. relictus, supporting the hypothesis that the former two forms are antidimorphs of a single species. If analogy to the dimorphism in Nautilus applies, the subglobose forms (M. oweni) are male; the subdiscoidal forms (M. parallelum) are female.
W/D H/D U/D
M. oweni/M.parallelum 0.25 -0.24 0.58
Arkanites r. relictus 0.24 -0.39 0.63
A. r. redivivus 0.24 -0.42 0.60