Diameza ( Miniseraphs ) eratoides ( Cossmann, 1889 )

Caze, Bruno, Merle, Didier, Pacaud, Jean-Michel & Saint Martin, Jean-Paul, 2010, First Systematic Study using the Variability of the Residual Colour Patterns: The Case of the Paleogene Seraphsidae (Mollusca, Gastropoda, Stromboidea), Geodiversitas 32 (3), pp. 417-477 : 448-450

publication ID

https://doi.org/10.5252/g2010n3a4

persistent identifier

https://treatment.plazi.org/id/03A69848-FF88-1E7E-FD1A-FE8BFEACFCD9

treatment provided by

Marcus

scientific name

Diameza ( Miniseraphs ) eratoides ( Cossmann, 1889 )
status

 

Diameza ( Miniseraphs) eratoides ( Cossmann, 1889) ( Figs 20 View FIG F-J; 22)

Terebellum ( Seraphs) eratoides Cossmann, 1889: 98 View in CoL , 99, pl. 3, figs 7, 8;

Terebellum ( Seraphs) eratoides View in CoL – Cossmann 1904: 46. — Cossmann & Pissarro 1905: 97, pl. 16, fig. 36; 1911: pl. 32, fig. 158-7.

Seraphs ( Miniseraphs) eratoides View in CoL – Jung 1974: 30, pl. 9, figs 10-12, text-figs 19, 20. — Le Renard 1992: 6. — Le Renard & Pacaud 1995: 112. — Pacaud & Le Renard 1995: 162.

TYPE LOCALITY. — Chaussy, Les Garennes (Val d’Oise, France), Lutetian (Middle Eocene).

TYPE MATERIAL. — Lectotype designated by Jung (1974) from the Bernay collection; paralectotype ( Boutillier coll.) from Vaudancourt ( Oise), not found.

The type material of this species has not been found in the Bernay collection, now deposited at the UCBL. A neotype designation is needed to clarify the taxonomic status of this species.A neotype from the type locality ( MNHN A28932, Faullummel coll., Fig. 22 View FIG A-D) is accordingly chosen here. This initiative conforms to the rules specified by the ICZN (1999: art. 75), as regards the designation of a neotype.

OTHER MATERIAL EXAMINED. — See Appendix 1.

SHELL DESCRIPTION

Shell up to 8 mm in height and up to 5 mm in diameter, very stout with wide apical angle ( Fig. 20 View FIG F-H). Aperture long and narrow. Callus of the inner lip clearly delineated, but weakly developed.Columella slightly bent backwards near the base. Outer lip thickened and forming a small protuberance at the apex ( Fig. 20J View FIG ). Outer lip slightly sinuous for the whole height in labral view ( Fig. 20G View FIG ). Siphonal notch moderately deep on the dorsal side. Faint oblique to spiral grooves near the base ( Fig. 20I View FIG ).

COLOUR PATTERN DESCRIPTION

The residual pattern is only composed of 2 levels of residual pigmentation: dark lines on a lighter background. Th ese axial lines are wavy, but do not cover the whole shell surface. Most specimens show a combination of two morphologies: 1) dark wavy lines, sometimes forming zigzags ( Fig.22E View FIG ), which are visible on the extremities of the shell and near the outer lip; 2) on the median part of the shell, a chessboard morphology ( Fig. 22A, C, E, G, I, J View FIG ), as defined by Meinhardt (1998: fig. 5.6). Th e chessboard pattern can appear as “light dots” on a darker background on poorly preserved shells ( Fig. 22G, J View FIG ).

VARIABILITY

The intraspecific variability is weak. Some specimens show numerous continuous wavy lines near the outer lip ( Fig. 22E, F View FIG ), while others show a chessboard pattern on the whole shell surface, except for the abapical and adapical extremities ( Fig. 22G, H View FIG ).

UCBL

Centre de Paleontologie Stratigraphique et Paleoecologie

MNHN

Museum National d'Histoire Naturelle

Kingdom

Animalia

Phylum

Mollusca

Class

Gastropoda

Order

Littorinimorpha

Family

Seraphsidae

Genus

Diameza

Loc

Diameza ( Miniseraphs ) eratoides ( Cossmann, 1889 )

Caze, Bruno, Merle, Didier, Pacaud, Jean-Michel & Saint Martin, Jean-Paul 2010
2010
Loc

Seraphs ( Miniseraphs ) eratoides

LE RENARD J. & PACAUD J. - M. 1995: 112
LE RENARD J. & PACAUD J. - M. 1995: 162
LE RENARD J. 1992: 6
JUNG P. 1974: 30
1974
Loc

Terebellum ( Seraphs ) eratoides

COSSMANN M. & PISSARRO G. 1905: 97
COSSMANN M. 1904: 46
1904
Loc

Terebellum ( Seraphs ) eratoides

COSSMANN M. 1889: 98
1889
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