In the eastern part of the Paris Basin, the «Rhaetian » is usually defined and subdivided by means of purely lithostratigraphical criteria whose chronostratigraphical value has still to be demonstrated. Therefore, several new sections in Lorraine have been palynologically analysed. From the top of the «Marnes irisées supérieures » (Upper Keuper) to the Lower Hettangian, five successive palynological episodes are distinguished. This microfloristic evolution is firstly compared to the palaeoenvironment evolution. Moreover, the chronostratigraphical interpretations of these palynological data are discussed and compared to those proposed for other fossils (Rhaetavicula contorta, Vertebrates), in order to clear up the dating problems of the tran...
International audienceThe final buildup of Pangea at the end of the Palaeozoic led to the formation ...
Palynological data from the carbonatic and siliciclastic sediments in the Central System and western...
The two samples yielded similar palynological signatures. Low levels of Carboniferous (Namurian and/...
International audienceA new description and sampling campaign of the Sancerre-Couy core has been ach...
International audienceA new description and sampling campaign of the Sancerre-Couy core has been ach...
International audienceA new description and sampling campaign of the Sancerre-Couy core has been ach...
International audienceThe aim of this study is to define the depositional environment of the Permian...
International audienceThe aim of this study is to define the depositional environment of the Permian...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
International audienceThe beginnings of Mesozoic sedimentation in north and east of France are locat...
The overarching aim of this thesis was to integrate the Bonenburg section and its extremely well- pr...
The Triassic-Jurassic (T-J) boundary, ~200 Ma, is known as one of the ‘big five’ mass extinctions in...
International audienceThe final buildup of Pangea at the end of the Palaeozoic led to the formation ...
International audienceThe final buildup of Pangea at the end of the Palaeozoic led to the formation ...
Palynological data from the carbonatic and siliciclastic sediments in the Central System and western...
The two samples yielded similar palynological signatures. Low levels of Carboniferous (Namurian and/...
International audienceA new description and sampling campaign of the Sancerre-Couy core has been ach...
International audienceA new description and sampling campaign of the Sancerre-Couy core has been ach...
International audienceA new description and sampling campaign of the Sancerre-Couy core has been ach...
International audienceThe aim of this study is to define the depositional environment of the Permian...
International audienceThe aim of this study is to define the depositional environment of the Permian...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
International audienceThe beginnings of Mesozoic sedimentation in north and east of France are locat...
The overarching aim of this thesis was to integrate the Bonenburg section and its extremely well- pr...
The Triassic-Jurassic (T-J) boundary, ~200 Ma, is known as one of the ‘big five’ mass extinctions in...
International audienceThe final buildup of Pangea at the end of the Palaeozoic led to the formation ...
International audienceThe final buildup of Pangea at the end of the Palaeozoic led to the formation ...
Palynological data from the carbonatic and siliciclastic sediments in the Central System and western...
The two samples yielded similar palynological signatures. Low levels of Carboniferous (Namurian and/...