The main aim of the study of Holocene landforms and formations in Tunisia is to reconstitute morphogenic, climatic, anthropic and neotectonic conditions of their genesis. Earth, biological and historical sciences methods and technics are used. More accurate arguments can be brought into the controversy about climatic aridifïcation in North Africa since Roman age and about the causes of present desertification.L'étude des formes et formations de l'Holocêne en Tunisie a pour but principal de reconstituer les conditions morphogéniques, climatiques, anthropiques et néotectoniques de leur genèse. Elle utilise les méthodes et techniques des Sciences de la Terre, de la Vie et des Sciences historiques. Elle peut permettre d'apporter des arguments p...
International audienceThis paper is a synthesis of relations between morphogenetic activity, climati...
POLLEN IN THE CORES OF GULF OF GABES AND KERKENNAH PLATEAU (TUNISIA): CLIMATIC AND ANTHROPIC SIGNALS...
International audienceIn the Neo-Cretaceous monoclinal plateau of the Dahar, the altitude progressiv...
The main aim of the study of Holocene landforms and formations in Tunisia is to reconstitute morphog...
International audienceThe main aim of the study of Holocene landforms and formations in Tunisia is t...
In Tunisia, lunettes are characteristic in the area of Tunis and in the Central-Eastern steppes, but...
Tunisian saharian and presaharian Holocene period can be divided into four subperiods. Lower Holocen...
First studies have established that one holocene terrace and one historic terrace have been accumula...
International audienceIn the southernmost part of Tunisia, the alluvial terrace attributed to Upper ...
We present the preliminary results of a Tunisian-Italian project of scientific collaboration in the...
Le changement climatique au cours de l’Holocène est un événement majeur, qui a bien influencé sur le...
International audiencePollen and clay mineralogical analyses of a Holocene sequence from Sebkha Bouj...
International audienceTunisian saharian and presaharian Holocene period can be divided into four sub...
International audienceThis paper is a synthesis of relations between morphogenetic activity, climati...
POLLEN IN THE CORES OF GULF OF GABES AND KERKENNAH PLATEAU (TUNISIA): CLIMATIC AND ANTHROPIC SIGNALS...
International audienceIn the Neo-Cretaceous monoclinal plateau of the Dahar, the altitude progressiv...
The main aim of the study of Holocene landforms and formations in Tunisia is to reconstitute morphog...
International audienceThe main aim of the study of Holocene landforms and formations in Tunisia is t...
In Tunisia, lunettes are characteristic in the area of Tunis and in the Central-Eastern steppes, but...
Tunisian saharian and presaharian Holocene period can be divided into four subperiods. Lower Holocen...
First studies have established that one holocene terrace and one historic terrace have been accumula...
International audienceIn the southernmost part of Tunisia, the alluvial terrace attributed to Upper ...
We present the preliminary results of a Tunisian-Italian project of scientific collaboration in the...
Le changement climatique au cours de l’Holocène est un événement majeur, qui a bien influencé sur le...
International audiencePollen and clay mineralogical analyses of a Holocene sequence from Sebkha Bouj...
International audienceTunisian saharian and presaharian Holocene period can be divided into four sub...
International audienceThis paper is a synthesis of relations between morphogenetic activity, climati...
POLLEN IN THE CORES OF GULF OF GABES AND KERKENNAH PLATEAU (TUNISIA): CLIMATIC AND ANTHROPIC SIGNALS...
International audienceIn the Neo-Cretaceous monoclinal plateau of the Dahar, the altitude progressiv...