Natural site; lacustrine drilling. 153 palynological samples + 19 radiocarbon datings.
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 border on the Ain river. 2 palynological samples.
Natural site, wet meadow. 13 palynological samples. Lacustrine chalk-peat limit.
Natural site: lignite level in the foundations of the lycée building. 2 palynological samples; only 8/9 pollen grains.
Natural site: peat bog border on the lake. 9 palynological samples.
Natural site: peat bog border on the lake. Two series: Narlay II (NY II) and Narlay 2003. 63 palynological samples in Narlay II; 25 in Narlay 2003 (18 by S. Guillon) + 19 radiocarbon datings. Unpublished data in its entirety. Ancient analysis by S. Wegmüller in 1966.
Natural site; marsh. 8 palynological samples. Bad conservation. See F. Firtion, 1950.
Natural site; marsh. 4 palynological samples. Very bad conservation. Deep drilling in clay levels.
Natural site. Organic level into the lower river terrace of the Ain river. 3 palynological samples. Presence of Fagus and Juglans pollen grains (= pollution).
Natural site: peat bog near the lake's outlet. 16 palynological samples. The selection was made in several drillings.
Natural site. Geological section in pleniglacial varves. 3 palynological samples.
Objective : characterize the deformation mechanisms and the crystallographic fabrics within homogeneously deformed granitic samples.
Objective : microtextural characterization within a shear zone brittle precursor
Objective : calculate the crystallographic preferred orientation (CPO) of each mineral phase in order to rebuild the elastic properties of the polyminéralic aggregates.
Objective : compare the chemical compositions of minerals within the brittle precursor and in the host rock.
Objective : characterize the chemical zonings in plagioclase and garnet related to fluid-rock interactions within a shear zone precursor
GNSS time-series on 6 sites in the French JURA arc, located taking into account a tectonic-neotectonic strategy. The GPS-JURA network is integrated in the French national RENAG network (CNRS-INSU) for research geodesy.
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 ...
As part of the QUALILAC project (Influence of the watershed on the functioning of lakes: importance of nutritional quality for couplings between benthic and pelagic environments), monitoring of the origin, quantity and quality of organic matter (OM) available at the water column and benthic level ...
Sampling of Mediterranean fan mussel specimens (Pinna nobilis) for molecular analyses of the byssus and of the shell matrix
This document describes a field mission carried out in May 2017, at the Observatoire Océanologique de Villefranche-sur-Mer. This mission aimed at collecting live specimens as well as dead shells from the Mediterranean fan mussel, Pinna nobilis, an endemic species protected by European Directive ...
The structural dataset gives the orientation of structural elements (bedding, cleavage, foliation, lineation, etc.). The data are georeferenced in the World Geodetic System 1984.
Data from the JURAQUAKE seismological network. This temporary network is currently composed of 6 seismic stations located north of Besançon and aims to record microseismicity in the area for research purpose.