Descrição de uma espécie nova de Cephalosphaera Enderlein, 1936 da Amazônia (Diptera, Pipunculidae)

Cephalosphaera aurata sp. nov. é descrita, um "checklist" e uma chave de identificação para as espécies neotropicais são apresentados e novos dados de distribuição geográfica para C. miriamae Rafael, 1992 são fornecidos.

Cephalosphaera Enderlein, a genus of Pipunculidae (Diptera) new for Australia, with descriptions of four new species

Cephalosphaera Enderlein is a nearly cosmopolitan genus of big-headed flies (Pipunculidae) which was previously unknown from Australia. Four species have now been found in Australia, all of them undescribed. New species in the subgenus Neocephalosphaera include: C. eukrenaina, C. parthenopipis and C. petila. Only one new species occurs in the nominate subgenus: C. prionotaina. Descriptions and a key to these species are presented.

Pipunculidae (Diptera) da Estação Ecológica de Maracá e da localidade de Pacaraima, Roraima, Brasil.

As espécies de pipunculidae da Estação Ecológica de Maracá e de Pacaraima, Brasil, são registradas. Dezesseis espécies foram identificadas ao nível específico; dessas, dez são novas à ciência, mas apenas cinco são descritas neste trabalho: Amazunculus claripennis, Cephalosphaera pacaraima, C. semispiralis, Elmohardyia praecipuae E. raraimensis.

Pollen distribution of sediment core MD96-2048 from the Western Indian Ocean

Glacial-interglacial fluctuations in the vegetation of South Africa might elucidate the climate system at the edge of the tropics between the Indian and Atlantic Oceans. However, vegetation records covering a full glacial cycle have only been published from the eastern South Atlantic. We present a pollen record of the marine core MD96-2048 retrieved by the Marion Dufresne from the Indian Ocean ~120 km south of the Limpopo River mouth. The sedimentation at the site is slow and continuous. The upper 6 m (spanning the past 342 Ka) have been analysed for pollen and spores at millennial resolution. The terrestrial pollen assemblages indicate that during interglacials, the vegetation of eastern South Africa and southern Mozambique largely consisted of evergreen and deciduous forests. During glacials open mountainous scrubland dominated. Montane forest with Podocarpus extended during humid periods was favoured by strong local insolation. Correlation with the sea surface temperature record of the same core indicates that the extension of mountainous scrubland primarily depends on sea surface temperatures of the Agulhas Current. Our record corroborates terrestrial evidence of the extension of open mountainous scrubland (including fynbos-like species of the high-altitude Grassland biome) for the last glacial as well as for other glacial periods of the past 300 Ka.