Minorities in European Cities: The Dynamics of Social Integration and Social Exclusion at the Neighbourhood Level
Martiniello, Marco ;
Book published by MacMillan & St. Martin's Press (2000)Detailed reference viewed: 233 (1 ULg)
Minority Nationalism and European Integration - P. Lynch
in Nations & Nationalism (1997), 4(3), 476-478Detailed reference viewed: 42 (0 ULg)
A miospore assemblage at the Siluro-Devonian boundary from the Tawil Formation, Qatif Field, Saudi Arabia
Steemans, Philippe ; ; et al
Conference (2001)Detailed reference viewed: 7 (0 ULg)
Miospore assemblages from the Silurian-Devonian boundary, in borehole A1-61, Ghadamis Basin, Libya
; Steemans, Philippe
in Review of Palaeobotany and Palynology (2002, April), 118(1-avr Sp. Iss. SI), 397-421
Well preserved and diversified miospore assemblages have been recorded from a relatively continuous sequence in borehole A1-61 which spans the Silurian-Devonian boundary in the northwestern part of the ... [more ▼]
Well preserved and diversified miospore assemblages have been recorded from a relatively continuous sequence in borehole A1-61 which spans the Silurian-Devonian boundary in the northwestern part of the Ghadamis Basin, Libya. The sequence is represented by early Devonian Lochkovian beds of the Tadrart Formation that transgress onto the Silurian Ludlow-Pridoli beds of the upper part of the 'Alternances Argilo-greseuses' Formation. The present work demonstrates a succession of miospore assemblages from closely sampled layers that have been stratigraphically dated as Ludlow-middle Pridoli and early Lochkovian by chitinozoans and acritarchs. Over 80 species of cryptospores and trilete spores have been identified. Modified detailed morphological interpretations are given. The miospore assemblages are correlated with miospore zonation schemes established for the type sequences of the Welsh Borderland, and those previously described from Libya. Early occurrences of some species as Streelispora newportensis on the western Gondwana plate, are put forward by comparison with the Old Red Sandstone continent. Phytogeographic and palaeobotanic implications based on these observations are discussed. (C) 2002 Elsevier Science B.V. All rights reserved. [less ▲]Detailed reference viewed: 35 (5 ULg)
Miospore Biozonation in the Middle Devonian - Lower Carboniferous of Europe : its application to Western Gondwana
; Streel, Maurice
in Anais da Academia Brasileira de Ciencias (1995), 67(3), 311-312Detailed reference viewed: 8 (0 ULg)
Miospore contribution to the Upper Famennian-Strunian event stratigraphy
in Annales de la Société Géologique de Belgique (1986), 109(1), 75-92Detailed reference viewed: 15 (0 ULg)
Miospore correlation between North American, German and Uralian (Udmurtia) deep facies through Appalachian, Irish and Belgian Platform and Continental Facies near the Devonian-Carboniferous Boundary.
in Lecture note in Earth Science (1986), 8Detailed reference viewed: 1 (0 ULg)
Miospore evidence for pre-Emsian and latest Famennian sedimentation in the Devonian of the Paraná Basin, South Brazil
; ; Steemans, Philippe et al
Conference (1995)Detailed reference viewed: 8 (0 ULg)
Miospore Evolution from the Ordovician to the Silurian
in Review of Palaeobotany and Palynology (2000, December), 113(1-3), 189-196
The definition of the term cryptospore is amended to include only spores thought to be produced by embryophytes and to exclude all enigmatic palynomorphs. Cryptospores are included here in the miospore ... [more ▼]
The definition of the term cryptospore is amended to include only spores thought to be produced by embryophytes and to exclude all enigmatic palynomorphs. Cryptospores are included here in the miospore group.The oldest published assemblage of typical cryptospores is Llanvirn in age. The evolution of cryptospore assemblages is very slow from the Llanvirn to the early Llandovery. The Telychian and Sheinwoodian stages are periods of drastic impoverishment in cryptospore biodiversity, followed by an important modification in miospore assemblages. This step in the evolution of the vegetation is correlated with the rapid transgression of seas on the continent during the early Llandovery. On the other hand, the Hirnantian glaciation does not affect diversity of the miospore assemblages. [less ▲]Detailed reference viewed: 27 (6 ULg)
Miospore lateral distribution in Upper Famennian alluvial lagoonal to tidal facies from eastern United States and Belgium.
Streel, Maurice ;
in Review of Palaeobotany and Palynology (1990), 64Detailed reference viewed: 12 (1 ULg)
Miospore ranges near the D/C Boundary and extinction events.
in Newsletter. Subcommission on Devonian Stratigraphy (1996), 12Detailed reference viewed: 10 (0 ULg)
Miospore stratigraphy, the tool to link Late Devonian macrofauna, microflora and events to the standard conodont zonation.
Streel, Maurice ;
Conference (2006)Detailed reference viewed: 6 (0 ULg)
Miospore systematics and stratigraphic correlation of Devonian-Carboniferous Boundary deposits in the European part of the USSR and Western Europe.
; ; et al
in Courier Forschungsinstitut Senckenberg (1988), 100Detailed reference viewed: 1 (0 ULg)
Miospores du Dévonien Moyen et Supérieur du bassin du Parana, Brésil: systématique et stratigraphie.
; Streel, Maurice ;
in Sciences Géologiques. Bulletin (1988), 41(3/4), 351-377Detailed reference viewed: 8 (0 ULg)
Miospores et acritarches de la Formation d'Hydrequent (Frasnien Supérieur à Famennien Inférieur, Boulonnais, France).
; Streel, Maurice ;
in Annales de la Société Géologique de Belgique (1983), 106Detailed reference viewed: 2 (1 ULg)
Miospores et Foraminifères du Famennien des Massifs des Mdakra et du Khatouat (Maroc).
; ; et al
in Sciences Géologiques : Mémoire (1992), 83Detailed reference viewed: 3 (1 ULg)
Miospores from Ordovician-Silurian Argentinean basins: evolution and relationships with other South American basins
; ; Steemans, Philippe
Conference (2011, September)Detailed reference viewed: 20 (4 ULg)
Miospores from the Devonian-Carboniferous transition in Hunan, SW-China.
; Steemans, Philippe ; Streel, Maurice
Conference (1993)Detailed reference viewed: 3 (1 ULg)