Spatial and temporal variability of pelagic and benthic organic matter composition in lake
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 ...
Glaciological data Austre Lovén Svalbard
These data are measured in High Arctic over an observatory basin, located at 79°N on the W coast of Svalbard. Austre Lovén is a small 4.5 km² polythermal glacier in constant decline since the end of the LIA. The surrounding catchment is no more than 10 km² and exhibits a significant periglacial area ...
Physicochemical characteristics of water and sediment - floodplains of the Ain, Doubs and Loue Rivers - 2015-2016
19 sites (16 wetlands and 3 rivers) with different physicochemical characteristics and distributed along three rivers (Ain, Doubs, and Loue) were sampled. The physicochemical characteristics of the wetlands were measured in situ or after laboratory analysis.
Physicochemical characteristics of water and sediment - Ain River floodplain - 2019-2020
34 sites (16 wetland sites, 15 river sites, and 3 groundwaters) distributed along the Ain River with different physicochemical characteristics were sampled. The physicochemical characteristics of the wetlands were measured in situ or after laboratory analysis.
EBSD mapping of shear zones strain gradient - deformation mechanisms
Objective : characterize the deformation mechanisms and the crystallographic fabrics within homogeneously deformed granitic samples.
EBSD mapping of brittle shear zones precursors
Objective : microtextural characterization within a shear zone brittle precursor
EBSD mapping of shear zones strain gradient - seismic anisotropy
Objective : calculate the crystallographic preferred orientation (CPO) of each mineral phase in order to rebuild the elastic properties of the polyminéralic aggregates.
Microprobe analysis on a brittle shear zone precursor
Objective : compare the chemical compositions of minerals within the brittle precursor and in the host rock.
Quantitative X-ray mapping of brittle shear zones precursors
Objective : characterize the chemical zonings in plagioclase and garnet related to fluid-rock interactions within a shear zone precursor
Satellite images of cloud types products in West Africa from March to August in 2017
It is products developped by Meteo France through the SAF application, showing the types of clouds in function of their elevation.
Water temperature data of the Forbonnet peatland (Thermopeat project)
This describes the temperature data acquired in a range of piezometers throughout the Forbonnet peatland (Jura Mountains, Frasne-Bouverans peatland complex).
SISMEAUCLIM
This project is based on three disciplines: seismology, hydrogeology and climatology. It aims to develop a new approach to monitor hydrogeological reservoirs, in particular karst aquifers, subject to extreme climatic events. The objective is to carry out 4D imaging during floods in a watershed ...
OMIV - Time series of hydrochemical parameters on landslides
Since 2010, the monitoring network, set up within the framework of the SNO- (Multidisciplinary Observatory of Slope Instabilities). This monitoring network provides a large amount of hydrogeological data The hydrogeological monitoring is composed of a high frequency and quasi-continuous monitoring, ...
OMIV - Time series of meteorological parameters on landslides
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 ...
Noise map Besançon 2008
Urban noise (road traffic, train traffic, pedestrian area, springs)
Phytomanagement - Vieux-Charmont (F-25)
The study site is an industrial wasteland, located in the city of Vieux-Charmont in the Doubs (France). The site presents an urbanized environment with the presence of dwellings, the Belfort-Montbéliard greenway. Several wetlands are also present, in particular the gravels pond and the river "la ...
Mesures urbaines de la température dans l’agglomération du Grand Dijon (MUSTARDijon)
Air temperature and monitoring in the Dijon agglomeration for high-resolution monitoring of the urban heat island (50 stations, record sampling every 20 minutes, period June 2014 onwards)
Pollen analysis - Les Rousses (F-39), Les Rousses lake
Natural site: peat bog near the lake's outlet. 16 palynological samples. The selection was made in several drillings. Two pollen tests performed in 2021 towards the lake outlet.
Mobile temperature measurements of air temperature in Dijon
Air temperature and monitoring in the Dijon agglomeration by bike (one measurement every 5m) to characterize the urban heat island at very high resolution along constant transects
Pollen analysis - Fontenu (F-39), îlot David-1987, FG 30, 86 S-C, 86 G23
Archaeological site. Lake dwelling. 9 palynological samples (related to M. Magny PhD thesis, 1991).
Pollen analysis - Bonlieu (F-39), Le Lautrey (point 205)
Peat bog; 51 palynological samples. Other analyses on this site by Carole Bégeot and Pascale Ruffaldi (2006)
Pollen analysis - Corsier (Suisse, Genève), Marina
Lacustrin archaeological site: sub-lake drilling. 25 palynological samples in the core C1
Pollen analysis - Ponsonby (Chili, Provincia Ultima Esperenza, Patagonia Austral), Emperaire/Legoupil excavations (Riesco Island)
Sections in an archaeological site. 146 palynological samples + 7 radiocarbon datings. 3 series: pingüino, locus 1 (very poor) et locus 2.
Pollen analysis - Montlebon (F-25), La Vigne 2
Natural site: wet meadow. 22 palynological samples. From 3,90 to 18,85 meters length: extension of Morteau Stade and Sur la Seigne transect lines.
Pollen analysis - Fontenu (F-39), Lac de Chalain, Station 3-1986 (îlot David)
Archaeological site. Lake dwelling. 5 palynological samples (related to M. Magny PhD thesis, 1991).
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