Ontogeny and phylogeny of Upper Cenomanian rotaliporids (Foraminifera)

The fossil record of planktonic foraminifera is a key source of data on the evolution of marine plankton. One of the most distinctive groups of Cretaceous foraminifera, the rotaliporids, widely used as a stratigraphic index, has always been considered to be a monophyletic clade. New data on the coiling direction and persistent morphological features of the late rotaliporids from the Upper Cenomanian of the Western Interior Seaway, USA, and the Vocontian Basin of southeast France is used as a phylogenetic proxy. Dealing with key morphological features, the coiling pattern of these keeled morphotypes proves that the rotaliporids group is polyphyletic and composed of Thalmanninella, that displays a dextral-coiling preference, and Rotalipora s.s., that have a proportionate-coiling mode. The stratigraphically youngest rotaliporids with keels co-occur with globular forms; and all morphologies transitional between these morphotypes are observed. The ontogenetic relationships between them are investigated, indicating that loss of the keel was a selective advantage that enabled those rotaliporids to remain in the surface water, thereby avoiding the expansion of the oxygen minimum zone. Two species are observed: Thalmanninella multiloculata and Rotalipora planoconvexa. These species are interpreted as having arisen by neoteny from Thalmanninella greenhornensis and Rotalipora cushmani respectively.     

Cultivation of avian malaria parasites in mammalian liver cells

The exoerythrocytic stages of Plasmodium lophurae and P. fallax were grown in cell cultures derived from embryonic mouse livers. Liver cell monolayers were maintained in continuous culture with frequent subculturing for extended periods of time. Morphologically, the main cell type was a large, flat cell which closely resembled in shape the mouse parenchymal cell, although small colonies of spindle-shaped cells could also be found. Mammalian cells were labelled with thymidine-³H prior to infection with avian merozoites so they could be positively distinguished from any avian cells which might be present in the merozoite inoculum as contaminants. Merozoites were observed inside the labelled mammalian cells within three hours and large forms were seen at 48 hr. The mammalian cells supported parasite growth comparable to that observed in avian cell cultures.