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 ...
The dataset is composed of several hundreds of primate skulls. They have been scanned with micro CT scanner and surface scanners. The region of interest of this dataset is the cranial base so the muzzle and the anterior part could be missing.
Natural site: drilling. 15 palynological samples.
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 ...
Natural site, wetland near La Creuse river. Located in the earth of "Grand Pressigny" neolithic sites. 26 palynological samples + 4 radiocarbon datings. First drilling in 1985 (by A. Marguet, M. Magny, H. Richard)
Individual genotypes from 210 samples arising from 165 individuals of a maternity roost located in Le Bourg d'Oisans (French Alps), hosting Myotis myotis and Myotis blythii individuals. Num = sample identifier, ID = individual identifier, Sampling = Sampling date, Type = bat type (Myotis myotis, ...
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.
Field survey of extant gastropods occurring along the western edge of the Jura Mountains
The excel file contains the schedule of the longest dry sequences over the Mediterranean basin, detected during the season from September to April, between 1957 and 2013.
Natural site: section in varve. 6 poor palynological samples.
Natural site. Drilling. 40 palynological samples + 2 radiocabon datings. Often poor conservation. The two radiocarbon datings are in the biginnig of the Subatlantic pollen zone.
Natural site: drilling. 27 palynological samples + 6 radiocarbon datings. To publish in its entirety.
Natural site: section in glaciolacustrine sediment. One palynological sample, probably Oldest Dryas.
Natural site: peat bog. 63 palynological samples. A reanalysis was taken by Elena Ortu while in the Edytem laboratory in Chambéry, and then by Fernand David (Aix-Marseille University).
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.
Natural site: drilling in an ancient meander of the Rhône river. 17 palynological samples. Site included and completed in the HDR of Emilie Gauthier (2012).
Natural site. Core in a wet meadow border on northeast of the "l'étang de Mauguio". 41 palynological samples + 3 radiocarbon datings. Aroud 40 further samples have been read by Didier Galop (GEODE, Toulouse). Pollen diagram never published.
Natural site: peat bog border on the lake. 106 palynological samples (18 by S. Guillon) + 21 radiocarbon datings. Unpublished data in its entirety.
Natural site: high lacustrine terrace on the right bank of the Doubs river. 102 palynological samples + 1 radiocarbon dating. 10,30 meters length core. 1 radiocarbon dating between 5,90 and 6,00 m = 8250 ± 50 BP (too old : Hard Water Effect ?).