56 NATURAL SCIENCE. July, 



2. Of Cevcophonius (a genus of Scorpions) in South East Aus- 



tralia and South America. 



3. Of Buprestidae and Longicovnia in South America, Australia, 



and New Zealand. 



IV. — Among Plants. 



1. Saxafrageae — Escalonieae (17 genera) and Cunonieae (18 genera) 



in New Caledonia, Australia, Tasmania, New Zealand, 

 Mascarene Islands, South Africa, South America. Only two 

 of these 35 genera cross the Equator. 



I in South America, 



-d , / • v South Africa, 



2. Proteaceae (49 genera, 950 species) Madagascar' 



,/r • • / 1 • \ Tasmania, New 



■\. Monimiaceae (22 genera and 250 species) ^ 1 j *t 



J v • e j f j 1 Zealand, New 



\ Caledonia. 



4. Of the Cupressinae (Coniferae), Callitvis in Africa, Madagascar, 



Australia ; Fitzroya in Chili and Tasmania. 



5. Of the Verbenaceae, Petvcea typically South American, in Java 



and Timor, and Petvceovitcx nearly related to Petraa in Buru 

 and Amboina. 



6. Of Senecio appendiculaiiis ; Fevnelia buxifolia ; Chasalia capitata ; 



Pouzolzia lavigata, Cyperus scopavius in Timor and in the 

 Mascarene Islands. 



7. Of Ranunculus trullifolius, R. Mosleyi (allied), Lyallia, in Ker- 



guelen and in Fuegia. 



8. Of Polypodium vulgare in Kerguelen, South Africa, South 



America, and Marion Islands. Cotula plumosa, Uncinia compacta 

 in Kerguelen and Australasian region. Pvinglea in Kerguelen 

 and Marion Islands. 



9. From the remains of buried forests, and the occurrence of 



lignite beds, and of enormous deposits of Peat in the 

 Chatham Islands, in Kerguelen and in other Antarctic Islands, 

 indicating a former forest-clad region. 



The development of the Southern fauna and flora occurred, Mr. 

 Forbes believes, during the Ice Age of the Northern Hemisphere 

 when "Antarctica" rejoiced in a semi-tropical climate. Their dispersion 

 occurred during the slow oncome of the partial glaciation of the 

 Southern Hemisphere, which exists now. 



The occurrence of many southern forms of life in the Miocene of 

 France and other parts of Europe is explained, according to the 

 author, by their having been driven north during a cold, or perhaps 

 glacial, period in the Southern Hemisphere in that age, of which 

 there are evidences in various parts of South Africa, Australia, and 

 South America, corresponding to the warm epoch in the Miocene age 

 in northern latitudes. 



