Pre-Cambrian to Palaeozoic Palaeopalynology and Palaeobotany
3
0
0
Texte intégral
(2)
(3) Carnets de Géologie / Notebooks on Geology - Memoir 2005/02 (CG2005_M02). Contents BREUER P., AL-GHAZI A., FILATOFF J., HIGGS K.T., STEEMANS P. & WELLMAN C.H. (2005).- Stratigraphic palynology of Devonian boreholes from northern Saudi Arabia.- CG2005_M02_Abstract01, p. 3-9 FRANÇOIS L., GRARD A. & GODDÉRIS Y. (2005).- Modelling atmospheric CO2 changes at geological time scales.- CG2005_M02_Abstract02, p. 11-14 GERRIENNE P., MEYER-BERTHAUD B. & FAIRON-DEMARET M. (2005).- The significance of Runcaria (Middle Devonian, Belgium) in the evolution of seed plants.- CG2005_M02_Abstract03, p. 15-19 GOLUBKOVA E. & RAEVSKAYA E. (2005).- Main changes in microfossil communities during the Upper Proterozoic of Russia.- CG2005_M02_Abstract04, p. 21-25 JAVAUX E.J. & MARSHALL C.P. (2005).- Tracking the record of early life.- CG2005_M02_Abstract05, p. 2731 PRESTIANNI C. (2005).- Early diversification of seeds and seed-like structures.- CG2005_M02_Abstract06, p. 33-38 RAEVSKAYA E. (2005).- Diversity and distribution of Cambrian acritarchs from the Siberian and EastEuropean platforms - a generalized scheme.- CG2005_M02_Abstract07, p. 39-44 RIBECAI C., BAGNOLI G., MAZZARINI F. & MUSUMECI G. (2005).- Paleontological evidence for Late Cambrian in the Arburese area, SW Sardinia.- CG2005_M02_Abstract08, p. 45-50 RUBINSTEIN C.V. (2005).- Ordovician to Lower Silurian palynomorphs from the Sierras subandinas (Subandean ranges), northwestern Argentina: a preliminary report.- CG2005_M02_Abstract09, p. 5156 STREEL M. & HARTKOPF-FRÖDER C. (2005).- Late Famennian correlation by miospores between the Refrath 1 borehole (Bergisch Gladbach-Paffrath Syncline, Germany) and the reference section of Chanxhe (Dinant Syncline, Belgium).- CG2005_M02_Abstract10, p. 57-60 VANGUESTAINE M. & BRÜCK P.M. (2005).- A Middle Cambrian age for the Ediacara fauna from the Booley Bay Formation, County Wexford, Ireland: new acritarch data and its implications.CG2005_M02_Abstract11, p. 61-62 VANMEIRHAEGHE J., YANS J., PRÉAT A., GRASSINEAU N. & VERNIERS J. (2005).- New evidence for the Hirnantian (Upper Ordovician) in Belgium? An integrated isotopical, biostratigraphical and sedimentological approach.- CG2005_M02_Abstract12, p. 63-68 VECOLI M., LEHNERT O. & SERVAIS T. (2005).- The role of marine microphytoplankton in the Ordovician biodiversification event.- CG2005_M02_Abstract13, p. 69-70 WAUTHOZ B. (2005).- Correlation and biostratigraphy of the Kortrijk (Sint-Antonius) and Kortrijk (Lust) boreholes (early Silurian, Belgium).- CG2005_M02_Abstract14, p. 71-77. For their interest, comments and advices during the preparation of this special volume the editors thank (in alphabetic order): A. ACHAB (Quebec-Canada), C. BERRY (Cardiff-UK), B. GRANIER (BrestFrance), A. LE HÉRISSÉ (Brest-France), B. MEYER-BERTHAUD (Montpellier-France), B. OWENS (Sheffield-UK), E. RAEVSKAYA (Saint Petersburg-Russia), N. SANDER (Modesto-CA, USA), T. TYRELL (Southampton-UK), M. VANGUESTAINE (Liège-Belgium), and J. VERNIERS (Ghent-Belgium). The full version of articles presented here as extended abstracts will be published in various journals. For more details please contact the authors. 1.
(4)
Documents relatifs
Germany is thus affected by this global shortage of doctors not only as a result of the emigration of German doctors, but also in terms of recruiting foreign doctors, with both
Species Icriodus iowaensis iowaensis is known since the Frasnian and ranges till the middle part of the Palmatolepis rhomboidea conodont zone of the new global zonation,
If fractures converted into THA are considered as surgery-, patient- (three cases of early loss of fracture reduction) or trauma-related (one case of femoral head damage)
As announced above, one of the main points of the Galois-theoretic part of this paper is to try to extend Proposition 2.5 to the almost semiabelian case. Due to technical
L’analyse par la méthode du bilan azoté de surface des pratiques agricoles réelles ou préconisées par le biais de MAET (mesures agroenvironnementales territorialisées) et
LCCAs include and are not limited to the following commonly used measures: Net Present Value, Benefit to Cost Ratio, Internal Rate of Return, and Payback
Their reasoning is as follows: (1) According to Calvet [1996] (on which their comment is largely based) the high-elevation, low-relief surfaces in the Eastern Pyrenees are remnants of
Composition of Lavas from the Northern Mariana Trough: Implications for Magmagenesis in 881.
