F
Frédéric Fluteau
Researcher at Institut de Physique du Globe de Paris
Publications - 92
Citations - 5274
Frédéric Fluteau is an academic researcher from Institut de Physique du Globe de Paris. The author has contributed to research in topics: Climate change & Earth's magnetic field. The author has an hindex of 33, co-authored 82 publications receiving 4565 citations. Previous affiliations of Frédéric Fluteau include Pierre-and-Marie-Curie University & IPG Photonics.
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Effect of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years
Gilles Ramstein,Frédéric Fluteau,Frédéric Fluteau,Jean Besse,Sylvie Joussaume,Sylvie Joussaume +5 more
TL;DR: This paper used an atmospheric general circulation model that incorporates realistic continental geography and epicontinental sea distributions to simulate the Eurasian climate of today, 10 million and 3O million years ago.
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Tectonic Uplift and Eastern Africa Aridification
Pierre Sepulchre,Gilles Ramstein,Frédéric Fluteau,Mathieu Schuster,Jean-Jacques Tiercelin,Michel Brunet +5 more
TL;DR: This work suggests that the uplift of eastern African topography led to a drastic reorganization of atmospheric circulation, engendering the strong aridification and paleoenvironmental changes suggested by the data.
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40K–40Ar dating of the Main Deccan large igneous province: Further evidence of KTB age and short duration
TL;DR: In this article, a new geochronological study was conducted using the 40K-40Ar Cassignol-Gillot technique for the Deccan Traps of the Krishna-Godavari Basin of southeastern India.
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Determination of rapid Deccan eruptions across the Cretaceous-Tertiary boundary using paleomagnetic secular variation: 2. Constraints from analysis of eight new sections and synthesis for a 3500-m-thick composite section
Anne-Lise Chenet,V. Courtillot,Frédéric Fluteau,Martine Gérard,Xavier Quidelleur,S. F. R. Khadri,K. V. Subbarao,Thor Thordarson +7 more
TL;DR: In this article, Chenet et al. reported the lower two thirds of the 3500m-thick composite section of the Deccan flood basalt province of India.
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Determination of rapid Deccan eruptions across the Cretaceous‐Tertiary boundary using paleomagnetic secular variation: Results from a 1200‐m‐thick section in the Mahabaleshwar escarpment
TL;DR: In this paper, a flow-by-flow reanalysis of the Mahabaleshwar escarpment was performed to identify four directional groups, implying very large (40 to 180 m thick) single eruptive events (SEEs) having occurred in a few decades.