GPS/GNSS observations acquired on OMIV landslides at 24h/30s session/frequency in Rinex standardized file format. Time series of sensor positions and baselines (E, N, Up components).
OMIV - Time serie of seismic waveforms recorded on landslides and catalogue of endogenous seismic events
Seismic waveforms continuous records acquired on OMIV landslides at 250 Hz in miniseed standardized file format. Instrumental catalogue of endogenous seismic events.
Meteorological observations acquired on OMIV landslides using a standardized protocol (6min, 15 min, 30 min, 60 min) according to the measured parameters and transfered in a Ascii standardized file format with the file database management system BD-OH OMIV. Estimation of potential evapotranspiration ...
The structural dataset gives the orientation of structural elements (bedding, cleavage, foliation, lineation, etc.). The data are georeferenced in the World Geodetic System 1984.
Eleven populations of Nuphar lutea were sampled in eleven wetlands differing in physicochemical characteristics and spread along three rivers (the Ain, the Doubs and the Loue Rivers). Fifteen traits, grouped into four sets (growth, reproduction, storage and defence), were measured during the growing ...
Section in the holocene caving of Flims. 6 sterile palynological samples.
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.
Natural site: peat bog in the north edge of the lake. 5 palynological samples. 1st half of the subatlantic period at 2.15 m depth. Should be looked by new analysis.
Archaeological site: lime mortar from a wall. Only one palynological sample. Test in the mortar of the fortified house.
Natural site: section. 6 palynological samples. Top of the section in the "argiles d'Albens" (Albens clays)
Urban archaeological excavation. 10 palynological samples. "Urban" typical results.
Archaeological excavation. 18 palynological samples + 2 radiocarbon datings. 6 acceptable samples.
Natural site: lake formed in 1442 upstream a natural dam due to a rockslide. Drilling. 16 palynological samples. Opportunities to demonstrate seasonal rhythms.
Hydrogeochemical monitoring of karst springs in the Jura mountains
Natural site: drilling in the deep levels of the lake (Edytem laboratory). 2 palynological samples.
Pollen analysis - Labergement-Sainte-Marie (F-25), Between the two lakes. M. Magny/V. Bichet Transects
Natural site. Peat bog between Saint-Point lake and Remoray lake. 10 palynological samples + 15 radiocarbon datings.
Natural site. Geological section in pleniglacial varves. 3 palynological samples.
Natural site, wet meadow. 13 palynological samples. Lacustrine chalk-peat limit. Approximate geographical coordinates.
Natural site: wetland border on the lake. 81 palynological samples by Hervé Richard and 81 samples by Jacques-Louis de Beaulieu (Marseille). No radiocarbon dating. Never published. Other analysis by Carole Bégeot (2008).
Natural site: geological section border on the Ain river. 2 palynological samples.
Natural site: lacustrine drilling. 2 palynological samples.
Natural site: travertine quarry ("Tuff of Dortan"). 3 palynological samples + 1 radiocarbon dating: 9100 ± 180 BP.
Natural site; weat meadow. 62 palynological samples. 12 meters length drilling.
Natural site; weat meadow. 16 palynological samples. Many drillings along a transect ligne: 6.0 to 12.45 meters length.