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OMIV - Time series of meteorological parameters on landslides

Database
Collected date : from 1 Sep 1992 ongoing
Labels : SNO OMIV
Creators : OMIV

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 ...

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OMIV - Time serie of seismic waveforms recorded on landslides and catalogue of endogenous seismic events

Database
Collected date : from 21 Sep 2006 ongoing
Labels : SNO OMIV
Creators : OMIV

Seismic waveforms continuous records acquired on OMIV landslides at 250 Hz in miniseed standardized file format. Instrumental catalogue of endogenous seismic events.

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OMIV - Time series of landslide surface displacements measured by GPS/GNSS

Database
Collected date : from 11 Apr 2003 ongoing
Labels : SNO OMIV
Creators : OMIV

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).

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DCF77 time of flight measurement

DCF77 is a Very Low Frequency (VLF) emitter located in Mainflingen, Germany, about 400 km away from Besançon, France. The objective of the collected data is to measure the time of flight of the 77.5 kHz signal with respect to GPS 1 PPS used as reference, and assess the dependence with ionospheric ...

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Structural dataset in the Montagne Noire migmatitic dome (French Massif Central)

Database
Collected date : from Apr 2010 ongoing

The structural dataset gives the orientation of structural elements (bedding, cleavage, foliation, lineation, etc.). The data are georeferenced in the World Geodetic System 1984.

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JURAQUAKE

Dataset
Collected date : from Jul 2018 ongoing
Labels : ZAAJ

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.

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Mesures urbaines de la température dans l’agglomération du Grand Dijon (MUSTARDijon)

Dataset
Collected date : from Sep 2014 ongoing

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)

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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

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Wetland functionning and functional traits of Nuphar lutea

Dataset
Collected date : from Apr 2015 to Mar 2016

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 ...

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Pollen analysis - Bloye (F-74), Tourbière (étang) de Beaumont

Natural site: peat bog. 8 palynological samples. Tests for a future research.

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Cholera database of Democratic Republic of Congo

Database
Collected date : from 1 Jan 2000 ongoing

This database contains information on the weekly monitoring of cholera in the health zones of the DRC since 2000.

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Pollen analysis - Puruaguita (Mexique, Guanajuato), Las Cazuelejas (CAZ-P)

Natural site: sections. 8 palynological samples. All samples are sterile except one (333 pollen grains).

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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 et locus 2 (locus 1 very poor).

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Pollen analysis - Varces-Allières-et-Risset (F-38), Lachar (Autoroute A51)

Dataset
Collected date : 1996
Creators : Hervé Richard

Natural site: section in varve. 6 poor palynological samples.

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Pollen analysis - Saint-Jorioz (F-74), Chez Le Beau

Natural site border on the Annecy lake. 16 meters drilling, with boring machine (Apageo) and "russian" corer. 183 palynological samples + 6 radiocarbon datings. Never published in its totality.

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Pollen analysis - Saint-Jeoire (F-74), Déviation de St-Jeoire

Natural site: section in glaciolacustrine sediment. One palynological sample, probably Oldest Dryas.

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Pollen analysis - Pagny-sur-Meuse (F-55), Les Marais (Morte Fontaine)

Natural site: drilling in a swamp forest. 4 palynological samples. Should be looked by new analysis.

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Pollen analysis - Luc-en-Diois (F-26), Lac du Claps (Petit Lac)

Dataset
Collected date : 1997
Creators : Hervé Richard

Natural site: lake formed in 1442 upstream a natural dam due to a rockslide. Drilling. 16 palynological samples. Opportunities to demonstrate seasonal rhythms.

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Pollen analysis - Le Miroir (F-71), La Tuilerie (La Peupleraie), A39-T2

Natural site over the alignment of the A39 motorway; drilling. 88 palynological samples + 2 radiocarbon datings. Samples often difficult to read. Publication CRAS, 1996.

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Pollen analysis - Marchamp (F-01), Lac de Cerin (MM)

Dataset
Collected date : 1987
Labels : ZAAJ
Creators : Hervé Richard

Natural site: peat bog and lake. 9 palynological samples. Geographical coordinates in the center of the residual lake.

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GPS-Jura

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.

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Jurassic Karst

Hydrogeochemical monitoring of karst springs in the Jura mountains

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Greenhouse gas emissions (CO2, CH4, N2O) in Cathedral Peak, South Africa

Monitoring of greenhouse gas emissions (CO2, CH4, N2O), using field incubation chambers, in the region Cathedral Peak (KwaZulu Natal nature reserve, South Africa)

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Pollen analysis - Plancher-les-Mines (F-70), Peat bog du Rossely

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.

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