SEM photo of Cretarhabdus limbicrassus from Black, 1972a (Pl. 16, Fig. 5)
Stradneria limbicrassa Reinhardt, 1964
Cretarhabdella spectabilis Black, 1971a
Cretarhabdella lateralis Black, 1972a
Cretarhabdus multiforus Black, 1972a
Cretarhabdus biseriatus Forchheimer, 1972
Cretarhabdus cantianus Black 1973
The entire species exhibits first-order, slightly greyish-white interference colours. The pelaga of Cretarhabdus limbicrassus shows a weak inclined extinction and length-fast (-) elongation in their natural settling position, in plan view under crossed polars.
Species of Cretarhabdus are constructed of cretarhabdid pelaga surrounding a large central area spanned by an axial cross that supports a distal process. The inter-cross area is occupied by lateral bars that delimit pores arranged in two or more complete concentric cycles. The number of pores in the outer cycle is typically 20 or more, a characteristic feature of Cretarhabdus limbicrassus.
Black, M. 1971a. Coccoliths of the Speeton Clay and Sutterby Marl. Proceedings of the Yorkshire Geological Society 38: 381-424.
Black, M. 1972a. British Lower Cretaceous Coccoliths. I-Gault Clay (Part 1). Palaeontographical Society Monograph. 126: 1-48.
Forchheimer, S. 1972. Scanning electron microscope studies of Cretaceous coccoliths from the Köpingsberg Borehole No. 1, SE Sweden. Sveriges Geologiska Undersökning, Series C. #668, 65: 1-141.
Reinhardt, P. 1964. Einige Kalkflagellaten-Gattungen (Coccolithophoriden, Coccolithineen) aus dem Mesozoikum Deutschlands. - Monatsberichteder Deutschen Akademieder Wissenschaftenzu Berlin. 6: 749-759.
Stradneria limbicrassa
Reinhardt, 1964
Maastrichtian
Rugen, Germany