Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Annik Brun"'
Publikováno v:
Vegetation History and Archaeobotany. 18:441-458
The layers studied, parts of banquettes, consist of limnic clayey-silty fine sediments with some intercalated horizons of shaly coal and lacustrine mud flow rubble. In the lower part of the record the Bornette interglacial has been established. This
Autor:
Annik Brun
Publikováno v:
Geobios. 25:585-594
Resume L'etude palynologique des sediments marins du golfe de Gabes et du plateau des Kerkennah permet de retracer l'histoire de la vegetation tunisienne et l'evolution des paleoclimats depuis 30 000 ans au moins. La comparaison des evenements botani
Autor:
Annik Brun
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
The past studies carried by the French Quaternarists on the Bas-Chablais Pleistocene deposits recognized in the Dranse Valley sections and also by bores and drill cores over the Gavot Plateau - sedimentary faciès, hydrological and hydrochimical cont
Autor:
Annik Brun
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
A palynological study has been carried out on clayey and lignite deposits outcroping along the Nanceau and Bornette rivulets in the south of the Annecy lake. The Bornette section which first shows a cool episode, then a cold and dry one, has an uncer
Autor:
Annik Brun
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
POLLEN IN THE CORES OF GULF OF GABES AND KERKENNAH PLATEAU (TUNISIA): CLIMATIC AND ANTHROPIC SIGNALS Pollen analysis of marine cores from Gulf of Gabes and Kerkennah Plateau shows the changes of vegetation landscape in Tunisia during the last 20, 000
Autor:
Annik Brun
Publikováno v:
L'Anthropologie. 105:442
Autor:
Annik Brun
Publikováno v:
L'Anthropologie. 104:480
Autor:
Annik Brun
Publikováno v:
L'Anthropologie. 104:174
Autor:
Christian Hannss, Annik Brun
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Monatshefte. 1987:129-145
Autor:
Carla Müller, Annik Brun, R. Desprat, Laure Blanc-Vernet, Marie Morzadec-Kerfourn, R.S.M. Templeton
Publikováno v:
Géologie Méditerranéenne. 6:290-296
Micropaleontological studies of late-Quaternary sediments show the importance of the 27 000 B.P. transgression which is almost up to the actual shoreline and also of the 1 7 000 regression. The Versilian transgression moves from East to West on the G