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 ...
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 ...
Peat bog. 11 palynological samples. Stratifical limit between lacustrin chalk and peat.
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)
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 et locus 2 (locus 1 very poor).
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 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.
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.
Natural site: section. 6 palynological samples. Top of the section in the "argiles d'Albens" (Albens clays)
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: peat bog and lake. 9 palynological samples. Geographical coordinates in the center of the residual lake.
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.
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: peat bog near the lake's outlet. 16 palynological samples. The selection was made in several drillings.
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, wet meadow. 13 palynological samples. Lacustrine chalk-peat limit. Approximate geographical coordinates.
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 ?).