J. Sandoval et Rb. Chandler, The Sonniniid ammonite Euhoploceras from the Middle Jurassic of south-westEngland and southern Spain, PALAEONTOL, 43, 2000, pp. 495-532
A biostratigraphical and taxonomic revision of the genus Euhoploceras is pr
esented using new material collected from the Upper Aalenian-Lower Bajocian
of south-west England and the Betic Cordillera (Spain). Euhoploceras is sh
own to range from the uppermost Aalenian (Concavum Zone, Limitatum Subzone)
to the Lower Bajocian (Laeviuscula Zone). S. S. Buckman's 69 species of So
nninia are grouped into three macroconch morphospecies: Euhoploceras acanth
odes (Buckman), strongly ornamented, with tubercles and strong ribs through
out ontogeny; Euhoploceras marginatum (Buckman) with tuberculate inner whor
ls and relatively strong ribs persisting to the outer whorls, and Euhoploce
ras modestum (Buckman) with ribbed, sometimes slightly tuberculate inner wh
orls, becoming smooth or only slightly ornamented in later stages of coilin
g. Euhoploceras adicrum (Waagen) is a younger species with a type horizon i
n the Laeviuscula Zone. Dimorphism and possible polymorphism are present in
both English and Spanish faunas. Euhoploceras subspinosum (Buckman) probab
ly represents dwarf forms of E. acanthodes [M] and is included as a junior
synonym of the latter; likewise, E. subdecoratum (Buckman) may belong with
E. marginatum [M], although they are described separately herein. Some of t
he microconchs of Euhoploceras [M] are probably represented by Nannoceras.
Similarities between English and Betic Euhoploceras confirm that during lat
e Aalenian-earliest Bajocian times, the English and Spanish palaeobiogeogra
phical regions were connected. The ammonite assemblages revised here come f
rom the Concavum to Ovalis zones.