Enoploclytia M’Coy, 1849

Devillez, Julien & Charbonnier, Sylvain, 2021, Review of the Late Jurassic erymoid lobsters (Crustacea: Decapoda), Geodiversitas 43 (2), pp. 25-73 : 64

publication ID

https://doi.org/ 10.5252/geodiversitas2021v43a2

publication LSID

urn:lsid:zoobank.org:pub:6EF0DFAC-609D-407D-B4CC-CB985C3295FC

DOI

https://doi.org/10.5281/zenodo.4498639

persistent identifier

https://treatment.plazi.org/id/29758789-0751-FFCA-122A-0538FC2DAA2B

treatment provided by

Felipe

scientific name

Enoploclytia M’Coy, 1849
status

 

Genus Enoploclytia M’Coy, 1849

( Fig. 1 View FIG M-N)

Enoploclytia M’Coy, 1849: 330 ; 1854: 137. — Zittel 1885: 694. — Fritsch & Kafka 1887: 27. — Van Straelen 1925: 278. — Beurlen 1928: 164. — Rathbun 1926: 128. — Secrétan 1964: 81. — Förster 1966: 146. — Taylor 1979: 25. — Aguirre-Urreta 1989: 514. — Feldmann et al. 2015: 3. — Devillez et al. 2016: 530 View Cited Treatment , fig. 1I-J; 2017: 786, fig. 4A-B; 2018: 144, fig. 2A-B.

Enoploclytia Enoploclytia – Mertin 1941: 160. — Glaessner 1969: 455.

TYPE SPECIES. — Astacus leachii Mantell, 1822 , by original designation.

DIAGNOSIS BY Devillez et al. (2018). — Fusiform intercalated plate; wide, deep cervical groove, joined to dorsal margin and to antennal groove; long, wide gastro-orbital groove originating as a median inflexion of cervical groove, delimiting two gastroorbital lobes; sinuous postcervical groove, joined to dorsal margin and to hepatic groove, with ventral extension at carapace mid-height; short branchio-cardiac groove, interrupted in upper part of carapace, joined to dorsal margin, not joined to postcervical groove; concavo-convex hepatic groove, joined to cervical groove; prominent ω and χ bulges; inferior groove convex posteriorly, joined to hepatic groove; carapace with heterogeneous coarse ornamentation; massive globose P1 propodus, rounded in transversal section; long and thin P1 fingers (straight in dorsal view); occlusal margins armed with sharp and slender tooth; P1 merus with strong, prominent distal process at extern side of its ventral extremity.

DISCUSSION

Recently, Devillez et al. (2018) reported a specimen identified as Enoploclytia sp. from the Oxfordian of France ( Fig. 18 View FIG ). Despite its poor preservation, this fossil exhibits the typical carapace groove pattern of the genus: elongated gastro-orbital groove, with two divergent distal branches, a sinuous postcervical groove joined to the posterior extremity of the hepatic groove and not joined to the branchiocardiac groove, which is short and interrupted in the branchial region ( Fig. 18C View FIG ). This specimen is the oldest occurrence of Enoploclytia , and the only known in the Jurassic. Indeed, Enoploclytia is more typical of the Cretaceous.

Kingdom

Animalia

Phylum

Arthropoda

Class

Malacostraca

Order

Decapoda

Family

Erymidae

Loc

Enoploclytia M’Coy, 1849

Devillez, Julien & Charbonnier, Sylvain 2021
2021
Loc

Enoploclytia Enoploclytia

GLAESSNER M. F. 1969: 455
MERTIN H. 1941: 160
1941
Loc

Enoploclytia M’Coy, 1849: 330

DEVILLEZ J. & CHARBONNIER S. & HYZNY M. & LEROY L. 2016: 530
FELDMANN R. M. & SCHWEITZER C. E. & KARASAWA H. 2015: 3
TAYLOR B. J. 1979: 25
FORSTER R. 1966: 146
SECRETAN S. 1964: 81
BEURLEN K. 1928: 164
RATHBUN M. J. 1926: 128
VAN STRAELEN V. 1925: 278
FRITSCH A. & KAFKA J. 1887: 27
ZITTEL K. A. VON 1885: 694
M'COY F. 1854: 137
M'COY F. 1849: 330
1849
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