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Featured researches published by Philippe Fauré.


Cancer | 1988

Diagnostic features of primary malignant lymphomas of the thyroid with monoclonal antibodies

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

Immunohistochemical profile of cutaneous B-cell lymphoma on cryostat and paraffin sections

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

Évolution paléogéographique de la Tunisie saharienne et atlasique au cours du Jurassique

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

Datations et corrélations nouvelles dans les séquences de dépôt du Lias terminal et du Dogger des Corbières (Aude, France) grâce aux Ammonites et aux Brachiopodes

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

Le genre Prodactylioceras (Ammonitina, Pliensbachien inférieur); Biostratigraphie, paléobiogéographie et modalités évolutives. Description d'une espèce nouvelle: Prodactylioceras aurigeriense nov. SP.

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

Le Pliensbachien de Jebel Zaghouan (Tunisie). Nouvelles données fauniques. Implications biostratigraphiques et paléobiogéographiques

Philippe Fauré; Fouad Zargouni; Najla Sekatni; Yves Alméras


Geobios | 2007

Zonation des brachiopodes du jurassique moyen sur la marge sud de la Téthys occidentale (Maroc, Algérie occidentale) Comparaison avec la marge nord-téthysienne française

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

Le Jurassique et le Crétacé basal de la Tunisie atlasique nord-occidentale : essai de corrélations avec les formations de la Dorsale tunisienne et de la ride Amar-Djédeida

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

Le passage Lias–Dogger de la Dorsale de Tunisie septentrionale: Nouveaux apports biostratigraphiques. Âge Toarcien supérieur de la distension téthysienne

Nejla Sekatni; Philippe Fauré; Rabah Alouani; Fouad Zargouni


Geobios | 1995

Le toarcien inférieur, période charnière dans l'évolution des Nodosariidés (Foraminifères): L'exemple des pyrénées méridionales du Haut-Aragon

Jean-Pierre Nicollin; Philippe Fauré; Christiane Ruget

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Georges Delsol

Paul Sabatier University

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P. Caveriviere

Paul Sabatier University

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