" (8) S. Brélade ImS Cave ? Asa {Reindeer {Bos ? sp. {Rhinoceros tichorhinus Nai Mousterian " (9) Krapina ImS Cave (Rock-shelter) Asa {Rhinoceros merckii {Cave Bear {Bos primigenius {Marmot (Arctomys) Nai Mousterian " (10) Taubach ImS Alluvial Deposit[4] No Asa {Elephas antiquus interment {Rhinoceros merckii {Felis leo {No Hippopotamus Nai {? Mousterian {? Upper Acheulean { = Levallois {? Chellean Division I (11) Mauer ImS Alluvial deposit No Asa {Elephas antiquus interment {Rhinoceros etruscus(5) {Ursus arvernensis {No Hippopotamus Nai None found " (12) Trinil ImS Alluvial deposit No Asa {Hippopotamus? interment {Rhinoceros sivasoudaicus {Other Sivalik types Nai None found by Dubois [1] South American remains and some others are omitted owing to insufficiency of data relating to their surroundings. [2] Names of fossil varieties of Rhinoceros. These are very confused. The term R. _leptorhinus_ should be avoided altogether. R. _megarhinus_ represents the R. _leptorhinus_ of Falconer and Cuvier. R. _merckii_ represents R. _hemitoechus_ of Falconer, which is the R. _leptorhinus_ of Owen and Boyd Dawkins. R. _tichorhinus_ is R. _antiquitatis_ of Falconer and some German writers. [3] The formation of the High Terrace drift is earlier than the date of arrival of the 'Siberian' invasion of Britain by certain Voles. Already in Pliocene times, some Voles had come into Britain from the south-east of Europe. But the Galley Hill man, if contemporary with the High Terrace drift, had arrived in Britain ages before the appearance of _Homo aurignacensis_ supposed by Klaatsch to be closely allied, and to have come into Europe through Central if not Northern Asia. The 'High Terrace' mammals have a 'Pliocene' facies.