Philippe Fauré
Paul Sabatier University
Network
Latest external collaboration on country level. Dive into details by clicking on the dots.
Publication
Featured researches published by Philippe Fauré.
Cancer | 1988
Philippe Fauré; Shashikant Chittal; Francoise Woodman-Měmeteau; P. Caveriviere; Bernadette Gorguet; Jean-Jacques Voigt; Georges Delsol
Primary malignant lymphomas (ML) of the thyroid are rare and their conclusive morphologic diagnosis is not always possible. The authors report diagnostic features of 11 cases of ML and one case of plasmacytoma of thyroid compared with chronic lymphocytic thyroiditis and undifferentiated carcinomas of thyroid in an immunohistochemical study using monoclonal antibodies (MoAb). The lymphoid nature of tumors could be identified in all cases with three MoAb on paraffin sections. In ML, tumor cells expressed leucocyte common antigen (Dako‐LC+) with negativity for epithelial membrane antigen (Dako‐EMA—) and cytokeratin (KL1—). Newer MoAb identifying B‐cell (LN‐1, LN‐2, MB2) and T‐cell‐associated antigens (MT1, UCHL1) not denatured by fixation, revealed B‐cell nature of tumor cells in all cases of ML. Among anti‐B MoAb, LN‐1 and MB2 were most consistent in their reactivity. In cryostat sections of three ML cases, the tumor cells expressed one or more B‐cell‐associated antigens. Plasmacytoma was negative for Dako‐LC and KL1 but positive for Dako‐EMA and monotypic cytoplasmic Ig.
American Journal of Dermatopathology | 1990
Philippe Fauré; Shashikant Chittal; Bernadette Gorguet; P. Caveriviere; Pierre Brousset; Rolland Viraben; Catherine Mazerolles; Georges Delsol
Thirty cases of primary (23 cases) and secondary (seven cases) cutaneous B-cell lymphoma (CBCL) were studied by immunohistochemistry using a selected monoclonal antibody (MoAb) panel on both cryostat and paraffin sections. On cryostat sections all CBCL so tested were positive for surface membrane immunoglobulins (IgMk most often) and B-cell antigens (CD22+, CD37+ ) with a variable T-cell-reactive component identified by MoAbs against T-cell antigens (CD2, CD3, CD4, CD5, CD8). CD4-positive stromal T-cells were usually more numerous than CDS-positive cells. A strong (50–75% of total cells) stromal T-cell (CD2+, CD3+ ) reaction was found in centroblastic-centrocytic lymphoma. Small numbers of CD1+ Langerhans cells were found in most cases, but they were present in large numbers in follicular lymphoma. On paraffin sections, a combination of MoAbs against B-associated antigens (LN-1, MB2) identified B-cell lineage in virtually all cases of CBCL. CBCL was negative for MoAbs against T-associated antigens (MT1, UCHL1) with rare exceptions (two cases). However, MT1 and UCHL1 combined identified the T-cell nature of all cases of nonepidermotropic, nonmycosis T-cell lymphoma, which were initially predictive of B-lineage by histologic pattern.
Comptes Rendus De L Academie Des Sciences Serie Ii Fascicule A-sciences De La Terre Et Des Planetes | 1999
Fekri Kamoun; Bernard Peybernès; Philippe Fauré
Abstract By means of palaeontologic data, the differert Jurassic formations of Tunisia are correlated along a north-south transect, from the Saharan Platform to the Northern Atlas, across the successive steps of the South-Tethyan stable palaeomargin. A palaeogeographic synthesis of the country is herein proposed, based on 11 maps established for the most important stages of this preoceanic rifting phase which is characterized by particularly active transtensional tectonics.
Comptes Rendus De L Academie Des Sciences Serie Ii Fascicule A-sciences De La Terre Et Des Planetes | 1999
Bernard Peybernès; Philippe Fauré; Yves Alméras
Abstract By means of supplementary datings of new Ammonites and particularly Brachiopods, the stratigraphy of the Uppermost Liassic and Mid-Jurassic carbonates from Corbieres is reviewed with distinction of new depositional sequences and separation in the time of the “calcaires a chaules” (Bouquignan Formation) from the “calcaires a oncolithes” (Feuilla Formation). We also give evidence of the main gap occurring just before the deposition of the Feuilla Formation (lateral pinching out) and, particularly, of the Villedaigne Formation. This last one, Mid-Upper Bathonian in age, overlies either the Bizanet Formation (Toarcian), the Bouquignan Formation (Mid Aalenian to Lower Bajocian) or the Feuilla Formation (Lower Bathonian).
Geobios | 1984
Jean-Louis Dommergues; Philippe Fauré; René Mouterde
Resume La biostratigraphie des Prodactylioceras est ici precisee.Ce groupe Nord-Ouest europeen bien represente dans le Carixien superieur a la base de la souszone a Figulinum par P. davoei ( Sow. ), apparait des la base de la sous-zone a Capricornus avec deux formes originales a repartitions geographiques limitees et bien distinctes. La premiere P. rectiradiatum ( Wingrave ) caracterise la region anglo-lusitanienne; la seconde est une espece nouvelle: P. aurigeriense essentiellement presente dans la region aquitanoiberique.
Geodiversitas | 2007
Philippe Fauré; Fouad Zargouni; Najla Sekatni; Yves Alméras
Geobios | 2007
Yves Alméras; Philippe Fauré; Serge Elmi; Raymond Enay; Charles Mangold
Comptes rendus de l'Académie des sciences. Série 2. Sciences de la terre et des planètes | 1996
Bernard Peybernès; Fekri Kamoun; M. Durand-Delga; J. Thierry; Philippe Fauré; J.-L. Dommergues; Jean-Marie Vila; P. Cugny; Mohamed Ben Youssef
Comptes Rendus Palevol | 2008
Nejla Sekatni; Philippe Fauré; Rabah Alouani; Fouad Zargouni
Geobios | 1995
Jean-Pierre Nicollin; Philippe Fauré; Christiane Ruget