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The ontogeny of Theriosynoecum fittoni (Mantell)

The carapaces of Theriosynoecum fittoni (Mantell) from the uppermost Weald Clay (Lower Cretaceous) of four English localities have been measured. Nine growth stages were recognized and the shape and ornament of each stage recorded. Though change in shape is considerable, the tubercles are generally constant in number and relative position throughout development. A lectotype for the species is designated, figured, and described.

Tetrapterites visensis—a new spore-bearing structure from the Lower Carboniferous

Tetrapterites visensis gen. et sp. nov. is the name given to examples of a spore-bearing structure from two Lower Carboniferous shales. A spore tetrad is enclosed by a non-cellular membrane of basic tetrahedral shape with wing-like appendages at the apices. These apical modifications (herein designated skiadions) are also found as separate entities in the assemblages and resemble saccate spores. Detailed descriptions of the Tetrapterites capsule and component parts are given and an attempt is made to explain its unusual organization.

Microplankton from the Cambridge Greensand (Mid-Cretaceous)

Thirty-eight species of dinoflagellates (including hystrichospheres) and of acritarchs of uncertain systematic position are recorded from the Cambridge Greensand; eight of these are new, and several others are recorded for the first time in Europe. Rock samples studied include six from the Gault immediately below, and five from the lowest Chalk Marl which continues above the 'greensand'. Evidence for the early Cenomanian (Varians Zone) age of the Cambridge Greensand is discussed.

Taxonomic criteria in the classification of the Pennsylvanian productoid Juresania nebrascensis

Biometrical and qualitative analysis of the form of the cardinal process in a sample of 123 brachial valves of Juresania nebrascensis (Owen) indicates that this feature is more variable than the size and shape of the valve proper. This relatively greater variability suggests that the form of the cardinal process has only limited value as a taxonomic criterion in the classification of this species.

A seed megaspore from the Devonian of Canada

A megaspore tetrad, Cystosporites devonicus sp. nov., is described from the Upper Devonian of Scaumenac Bay, Quebec, Canada. Cystosporites megaspores have previously been reported only from the Carboniferous, where they have been found in the lycopod seed Lepidocarpon. The occurrence of this Canadian Cystosporites shows that a level of heterospory equivalent to that reached by Lepidocarpon had already been attained by the late Devonian.

Devonian corals and brachiopods from the Brendon Hills, west Somerset

The coral and brachiopod faunas of the Middle-Upper Devonian Ilfracombe Beds in the Brendon Hills, west Somerset, have been examined. The corals are restricted to two limestone horizons in the Ilfracombe Beds, the Rodhuish Limestone and the Roadwater Limestone; the brachiopods are sparse and more uniformly distributed throughout the succession. The rugose corals, Heterophrentis percevali sp. nov., Thamnophyllum caespitosum (Goldfuss), Acanthophyttum (Neostringophyllum) concavum (Walther) and Mesophyllum (Arcophylluni) sandhillense sp.
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