Central mechanisms of fever.

The possible role of various potential chemical mediators in the production of fever is reviewed. A major problem in this field is the very considerable conflict of evidence, let alone interpretation. On the existing evidence, it appears unlikely that monoamines, acetyl choline, or alterations in relative concentrations of sodium and calcium play any major role in the production of fever. Recent evidence makes it unlikely that prostaglandins have a direct role in this mechanism, though the involvement of other metabolites of arachidonic acid has not been excluded. It is possible that protein synthesis may play a part in the central action of leukocyte pyrogen.     

Botryocladius gen.n.: a new transantarctic genus of orthocladiine midge (Diptera: Chironomidae)

A new genus of orthocladiine Chironomidae, Botryocladius (type species B. grapeth sp.n. from eastern Australia) is described and illustrated in all life history stages. All thirteen included species are described as new, six from eastern Australia (B. grapeth, B. brindabella, B. mdfrc, B. collessi, B. tasmania, B. australoalpinus), two from Western Australia (B. bibulmun and B. freemani), one from ephemeral streams in Australia (B. petrophilus) and four from Patagonian Argentina and Chile (B. edwardsi, B. glacialis, B. mapuche and B. tronador). All Australian species are known from at least pupal exuviae, most from adult males and several from larvae. In contrast, only B. edwardsi amongst Neotropical species is known from the adult male; all others are described from pupal exuviae. The immature stages are lotic in Australian permanent and temporary streams and Patagonian glacial streams and rivers, and lentic in Neotropical glacial-fed and Australian subalpine lakes. Botryocladius appears to belong with a grouping centred on two formally undescribed taxa from Australia. The genus evidently demonstrates a vicariant distribution with at least two sister-group relationships between South American and Australian taxa, providing a minimum dating for the clade of 38 Ma., with apparent absence from New Zealand indicating a maximum date of 80 Ma.