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Upper Cretaceous foraminifera from the Ballydeenlea Chalk, County Kerry, Ireland

Twenty-three species of Upper Cretaceous foraminifera have been recovered from the newly discovered (Walsh 1960) Ballydeenlea Chalk of County Kerry, Ireland. These are the first Upper Cretaceous foraminifera reported from the Republic of Ireland and the westernmost Upper Cretaceous fauna found in Europe. This faunal assemblage shows that the Ballydeenlea Chalk can be correlated with part of the Upper Chalk (Senonian) of England and Northern Ireland.

Schizochroal eyes and vision in some phacopid trilobites

Some aspects of vision in nine species of phacopid trilobites are described. Methods of study, which primarily consist of the investigation of the morphology of the visual surface and the extent and nature of the visual field, are identical with those of previous work.Divergent interpretations of intraspecific variation in the lens number of Phacops sp. are discussed and sexual dimorphism is advanced as a tenable hypothesis.

Description of dimorphism in Striatopora flexuosa Hall

Striatopora Hall comprises branching favositoid tabulate corals with thick, dilated walls near the outer surface of the colonies. Study of serial sections of the type species, S. flexuosa Hall, shows that individuals within colonies commonly originated in one of two positions, either near the axis of the colony or near the boundary between inner thin-walled and outer thick-walled zones. Corallites originating in the two positions are morphologically distinct and were produced alternately by corallites of the first type. Corallites of the second type did not reproduce asexually.

A new productid brachiopod from the Upper Viséan of Scotland

Promarginifera trearnensis gen. et sp. nov. a productid brachiopod from the Upper Visean of Ayrshire, Scotland is described. It occurs in the Dockra Limestone 65 ft. below the Visean-Namurian junction. Morphologically the form has affinities with both the marginiferids and dictyoclostids but on the evidence of a marginiferid cardinal process and discontinuous marginal ridges it is classified as a marginiferid of the subfamily Costispiniferinae.
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