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Morphology and evolution of the eye in Upper Cambrian Olenidae (Trilobita)

The eyes of selected olenid species from Scandinavian concretionary shales were examined with the scanning electron microscope. Though these eyes are small, many previously unknown details were visible, including the 'peripheral zone' of Olenus wahlenbergi and other genera. Reconstructions, prepared by camera-lucida techniques, show the eye and the whole cephalon of certain species.In early olenids the visual surface was dehiscent in the adults and is preserved only in meraspids; in later genera the ocular suture became fused and the visual surface was retained.

Combined transmission and scanning electron microscopy of in situ Palaeozoic spores

This paper discusses pollen and spores isolated from Carboniferous reproductive organs, including fructifications belonging to lycopods, cordaites, and seed ferns. Microspores of the monosaccate genus Endosporites were macerated from sporangia of a single cone. Morphological variability ranges from grains still within the tetra-hedral arrangement to solitary spores. Information is provided concerning saccus-corpus organization and exine infrastructure, ornamentation, and stages of saccus ontogeny.

A problematical dinoflagellate from the Tertiary of Virginia and Maryland

Inversidinium exilimurum, gen. et sp. nov., a problematical dinoflagellate recovered from the Aquia Formation (Upper Paleocene) of the Virginia-Maryland Coastal Plain, displays an atypical peridinioid outline characterized by a truncated antapex which ruptures to form a hitherto unreported type of antapical excystment apparatus; antapical archeopyles are exceedingly rare among the dinoflagellates.

Dinoflagellate cysts and acritarchs from the Bearpaw Formation (Upper Campanian) of southern Alberta, Canada

Fifty-three species of dinoflagellate cysts and six species of acritarchs are reported from the upper Campanian Bearpaw Formation of southern Alberta. These include Diconodinium firmum sp. nov., Lejeunia parva sp. nov., L. ampla sp. nov., Spinidinium clavum sp. nov. and Hystrichosphaeridium dowlingii sp. nov. The Bearpaw Formation is divided into three informal assemblage zones. A parameter called the gonyaulacacean ratio is used as a possible guide to the salinity of the Bearpaw sea or to the proximity of the coastline. Three periods of open marine conditions are postulated.
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