Abstract
Sediments of two filled-in lakes (Terres Plaines, altitude 2100 m; Restefond, altitude 2400 m, Alpes-de-Haute-Provence) from the intra-alpine part of the Southern French Alps were pollen-analytically investigated. The palynological data indicate that in a SW-exposed valley (Restefond) deglaciation at 2400 m altitude took place already before the Allerod interstadial, clearly earlier than in a N-exposed valley (Terres Plaines) at 2100 m. -from Authors
Original language | English |
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Pages (from-to) | 123-137 |
Number of pages | 15 |
Journal | Quaternaire |
Volume | 1 |
Issue number | 2 |
DOIs | |
Publication status | Published - 1990 |