There is a clear trend of increased cooling and the spread of tundra and steppe environments from the MP through the early Aurignacian, with a warm event in GH 11 and a cold event in GH 7a/7aa suggested by both the modified indicator species and habitat weighting methods.
← all excerpts
Did climate determine Late Pleistocene settlement dynamics in the Ach Valley, SW Germany?
1
—
—