Re-analysis of faunal assemblages from the Haua Fteah and other late quaternary archaeological sites in Cyrenaican Libya

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In preliminary reports based on approximately 5000 identified bones from the Haua Fteah, Cyrenaica, E. S. Higgs concluded that changes in the abundance of bovines versus Barbary sheep reflected climatic change from drier (=last interglaciation) to wetter (=last glaciation) and back to drier (=present interglaciation). Higgs also reported the earliest occurrence of domestic caprines in Africa, in Haua Fteah “Neolithic” layers dated to about 6800 bp. A new analysis, based on roughly 9000 identified specimens, supports the broad pattern of faunal change that Higgs found, but suggests that it reflects wetter when Higgs proposed drier and vice versa. The new analysis failed to confirm the early date for domestic caprines, mainly because of uncertainty concerning the stratigraphic provenience of key specimens. Finally, the new analysis produced some additions to the species list (most notably eland) and provided previously unavailable information on skeletal part representation and on the ages of animals at time of death. With respect to skeletal parts, smaller ungulates tend to be represented by a wider variety than larger ones, a contrast that is almost universal in Stone Age sites. With regard to age profiles, the largest and most reliable one (for Barbary sheep from the “Neolithic” layers) implies the animals were captured by driving over cliffs or into other traps. Restudy of small additional samples from the Cyrenaican sites of Hagfet et Tera, Hagfet ed Dabba, and Sidi el Hajj Creiem fully supports taxonomic and paleoenvironmental conclusions drawn earlier by Higgs and Bate.