S. Laafar et al., EVIDENCE OF PALAEOSTRUCTURES RELATED TO F REEZING THROUGH SOIL MICROMORPHOLOGY IN LAZARET CAVE, NICE (FRANCE), Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 321(3), 1995, pp. 209-214
In the Lazaret cave (Nice), the study of soil micromorphology has reve
aled palaeostructures with a microaggregate facies as well as a round
or flat morphology. Observations were performed in the middle of strat
igraphic layer C of the archaeological filling which probably belongs
to isotopic stage 6. The specific characteristics of these palaeostruc
tures are compared to those observed in certain recent sites which und
erwent a cold and wet climate. From this comparison, it can be inferre
d that layer C might have been formed under similar climatic condition
s.