. Bulletin of the British Museum (Natural History), Geology. Vrba (1973 : 309 footnote) has made the tentative suggestion that G. gracilior may turn out to be an Antidorcas, but we prefer to maintain our existing opinion. Gazelle horn cores from Langebaanweg (, , , and ) are mediolaterally compressed and curve backwards quite strongly. They are large for their geological age (Pliocene), and could be ancestral to G. vanhoepeni. Genus INDETERMINATE Antilopini sp. 1 A number of small horn cores from Olduvai can perhaps be placed in the Antilopini. These are. Plate
. Bulletin of the British Museum (Natural History), Geology. Vrba (1973 : 309 footnote) has made the tentative suggestion that G. gracilior may turn out to be an Antidorcas, but we prefer to maintain our existing opinion. Gazelle horn cores from Langebaanweg (, , , and ) are mediolaterally compressed and curve backwards quite strongly. They are large for their geological age (Pliocene), and could be ancestral to G. vanhoepeni. Genus INDETERMINATE Antilopini sp. 1 A number of small horn cores from Olduvai can perhaps be placed in the Antilopini. These are. Plate 41 ? Caprinae sp. Fig. 1 Supposed dorsal view of right horn core from Bed I, BM(NH) M 14531. Fig. 2 Supposed anterior view of same horn core. Fig. 3 Supposed posterior view of same horn core. 444 (Scale marked in cm and mm). Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original British Museum (Natural History). London : BM(NH)
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