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Featured articles from Cave & Karst Science Journals
Characterization of minothems at Libiola (NW Italy): morphological, mineralogical, and geochemical study, Carbone Cristina; Dinelli Enrico; De Waele Jo
Chemistry and Karst, White, William B.
The karst paradigm: changes, trends and perspectives, Klimchouk, Alexander
Long-term erosion rate measurements in gypsum caves of Sorbas (SE Spain) by the Micro-Erosion Meter method, Sanna, Laura; De Waele, Jo; Calaforra, José Maria; Forti, Paolo
The use of damaged speleothems and in situ fault displacement monitoring to characterise active tectonic structures: an example from Zapadni Cave, Czech Republic , Briestensky, Milos; Stemberk, Josef; Rowberry, Matt D.;
Featured articles from other Geoscience Journals
Karst environment, Culver D.C.
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs, Bontognali, Tomaso R.R.; D’Angeli Ilenia M.; Tisato, Nicola; Vasconcelos, Crisogono; Bernasconi, Stefano M.; Gonzales, Esteban R. G.; De Waele, Jo
Calculating flux to predict future cave radon concentrations, Rowberry, Matt; Marti, Xavi; Frontera, Carlos; Van De Wiel, Marco; Briestensky, Milos
Microbial mediation of complex subterranean mineral structures, Tirato, Nicola; Torriano, Stefano F.F;, Monteux, Sylvain; Sauro, Francesco; De Waele, Jo; Lavagna, Maria Luisa; D’Angeli, Ilenia Maria; Chailloux, Daniel; Renda, Michel; Eglinton, Timothy I.; Bontognali, Tomaso Renzo Rezio
Evidence of a plate-wide tectonic pressure pulse provided by extensometric monitoring in the Balkan Mountains (Bulgaria), Briestensky, Milos; Rowberry, Matt; Stemberk, Josef; Stefanov, Petar; Vozar, Jozef; Sebela, Stanka; Petro, Lubomir; Bella, Pavel; Gaal, Ludovit; Ormukov, Cholponbek;
DEPT UNIV PROFESSIONNEL REVUES SCIENTIFIQUES TECHNIQUE 11 RUE GOSSIN, F-92543 MONTROUGE, FRANCE
Comptes Rendus de L Academie Des Sciences Serie Ii Fascicule A-Sciences de La Terre et Des Planetes, 1995, Vol 321, Issue 3, p. 209-214
EVIDENCE OF PALAEOSTRUCTURES RELATED TO FREEZING THROUGH SOIL MICROMORPHOLOGY IN LAZARET CAVE, NICE (FRANCE)
Laafar S. , Rousseau L. , Delumley H. ,
Abstract:
In the Lazaret cave (Nice), the study of soil micromorphology has revealed palaeostructures with a microaggregate facies as well as a round or flat morphology. Observations were performed in the middle of stratigraphic layer C of the archaeological filling which probably belongs to isotopic stage 6. The specific characteristics of these palaeostructures are compared to those observed in certain recent sites which underwent a cold and wet climate. From this comparison, it can be inferred that layer C might have been formed under similar climatic conditions
In the Lazaret cave (Nice), the study of soil micromorphology has revealed palaeostructures with a microaggregate facies as well as a round or flat morphology. Observations were performed in the middle of stratigraphic layer C of the archaeological filling which probably belongs to isotopic stage 6. The specific characteristics of these palaeostructures are compared to those observed in certain recent sites which underwent a cold and wet climate. From this comparison, it can be inferred that layer C might have been formed under similar climatic conditions
Keywords: c, cave, climate, cold, facies, france, microaggregate, micromorphology, middle, morphology, palaeostructure, paleoclimate, recent, site, sites, soil, time, times, wet,