Pollen analysis - Montlebon (F-25), Sur la Vigne 1 (Morteau A)
Natural site: wet meadow. 99 palynological samples + 4 radiocarbon datings. Drilling of 28.10 meters length.
Pollen analysis - Morteau (F-25), Moulin Bournez
Natural site; weat meadow. 126 palynological samples + 2 radiocarbon datings. 33,57 meters length drilling.
Pollen analysis - Morteau (F-25), Stade
Natural site; weat meadow. 62 palynological samples. 12 meters length drilling.
Pollen analysis - Autun (F-71), Cathédrale Saint Nazaire, cloister
Sections in archaeological excavations. 32 palynological samples. Very bad conservation: nearly sterile samples.
Pollen analysis - Arcenant (F-21), Les Berthières (Merovingian necropolis)
Archaeological site: Merovingian tombs. 2 palynological samples.
Pollen analysis - Mâcon (F-71), Cathédrale
Archaeological site: stone sarcophagus. 6 palynological samples. Very bad conservation.
Pollen analysis - Clessé (F-71), Germolles
Archaeological site. Castle moats. Only one palynological sample.
Pollen analysis - Gevrey-Chambertin (F-21), ADDB 1
Archaeological site, pit. Only one palynological sample.
Pollen analysis - Couchey (F-21), La Platelle (Champs perdrix)
Natural site: soil section. Only one palynological sample. Differential conservation problem (disproportionate number of cichorioidae pollen).
Pollen analysis - Vosnes-Romanée (F-21), Romanée-Conti
Natural site: soil section. Only one palynological sample. Differential conservation problem (disproportionate number of cichorioidae pollen).
Pollen analysis - Pont-du-Navoy (F-39), lower river terrace of the Ain river
Natural site. Geological section in pleniglacial varves. 3 palynological samples.
Pollen analysis - Ranchot (F-39), Abri des Cabones 1984 + Châteauneuf
Archaeological excavation: rock shelter. 5 palynological samples. 1 sample in "Abri de Chateauneuf" (47°09'13.28/5°54'14.05). First analysis: J. Heim, 1979.
Pollen analysis - Plancher-les-Mines (F-70), Peat bog du Rosely
Natural site: peat bog. 64 palynological samples + 6 radiocarbon datings. The results are difficult to interpret due to a possible inversion of a core depth levels.
