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PollenChrono
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Données de thèse
Single-crystal X-ray structures
Calculated spectroscopic databases
Chimie des eaux-basse vallée de l'Ain
Complex directed networks
Microma
Données de thèse de Thomas Leydier
Gaia
CNR Echinococcoses
OMIV
Inorganic synthesis
Phytomanagement-Chrono
Road-side counts
TNOs
Organic synthesis
Paleoparasitology
Star formation
Organometallic complexes with metal-metal bonds
AVKs
Piézométrie Chrono-Environnement
All pollen analysis (pollens and spores) made since 1981 by the laboratory of Besançon (today "Laboratoire Chrono-environnement") on the lake, marshy and peaty sediments, and on the archeological sites.
Creation of collection : 4 Nov 2016
Natural site: drilling in a wetland. 76 palynological samples + 12 radiocarbon datings. Very complex age-depth model due to an irregular sedimentation caused by the shifting of the creek.
Archaeological excavations. 18 palynological samples. Pollen not very well preserved, some acceptable samples.
Archaeological excavation (content of a Neolithic ceramic). Only one palynological sample. Very poor: very bad conservation.
Urban archaeological excavation. 46 palynological samples + 3 radiocarbon datings. Interesting results: should be published.
Natural site: drilling. 27 palynological samples + 6 radiocarbon datings. To publish in its entirety.
Archaeological excavation. 4 palynological samples. Good conservation. Sedimentary infil of an ancient meander (other ancient meanders are visible on aerial photographs). One 14C : 10120 +/- 50 BP.
Archaeological excavation. 6 palynological samples. Only one just positive sample.
Archaeological excavation in entrance of a cave served as a sheepfold. 53 palynological samples + 10 radiocarbon datings. Several series: 1985, 1988, 1994. Only some acceptable samples.
Natural site: section. 6 palynological samples. Top of the section in the "argiles d'Albens" (Albens clays)
Natural site: section in glaciolacustrine sediment. One palynological sample, probably Oldest Dryas.
Archaeological excavation. 2 palynological samples; one very rich.
Two palynological samples from moss used to fill the gaps between the construction elements of an alpine chalet. Dendrochronological date: 1750 AD.
Five palynological samples from moss used to fill the gaps between the construction elements of an alpine chalet. Dendrochronological date: between 1608 and 1700 AD.
Archaeological site: lime mortar from a wall. Only one palynological sample. Test in the mortar of the fortified house.
Archaeological site: stone sarcophagus. 6 palynological samples. Very bad conservation.
Urban archaeological excavation. 2 palynological samples. Negative.
Archaeological site: excavation in Roman camp. 2 palynological samples. Nearly sterile samples.
Natural site, drilling. 6 palynological samples. Very bad conservation. Approximate geographical coordinates (village center).
Natural site: meadow near an archaeological site. 10 palynological samples. Nearly sterile samples.
Natural site near tumulus. 6 palynological samples + 2 radiocarbon datings. Poor. 2 acceptable samples.
Archaeological excavation. Only one palynological sample. Positive but with some bad conservation problems.
Archaeological site. Lake dwelling. 135 palynological samples. Drilling of 7.50 m. 2 radiocabon datings on the oldest human impacts + archaeological dating (cultural phases) and dendrochronological dating on the neolithic levels crossed by this drilling.
Archaeological site, urban excavation. 21 palynological samples. 4 positive samples.
Archaeological excavation. 5 palynological samples. Poor.
Archaeological digs. 40 palynological samples. Lorraine airport site: in fact on three municipalities (Goin, Vigny, Liéhon): geographical coordinates on the main building of this airport (municipality of Goin). 6 positive samples.
