Ground temperature history in central Europe from borehole temperature data     

Christoph Clauser  Jean-Claude Mareschal 《Geophysical Journal International》1995,121(3):805-817

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Impacts « multi-échelle » d'un échange (Mg,Ca)–Pb et ses conséquences sur l'augmentation de la perméabilité d'une bentonite     

Nevila Jozja  Patrick Baillif  Jean-Claude Touray  Charles-Henri Pons  Fabrice Muller  Carole Burgevin 《Comptes Rendus Geoscience》2003,335(9):729-736

The article addresses the structural effects of solutions of lead nitrate on a suspended or compacted bentonite. A permeability increase is observed on compacted clay. Investigating the composition of output solution, using X-Rays Diffusion at Small Angles and Scanning Electron Microscopy, this permeability increase is explained from structural variations at nanometric (reduction of particle size) and micrometric scales (microfissuration of aggregates). To cite this article: N. Jozja et al., C. R. Geoscience 335 (2003).  相似文献   

Professor Bastiaan Jacob Collette 1930–1991     

Jean-Claude Sibuet  Jacob Verhoef  Walter Roest 《Marine Geophysical Researches》1992,14(2):88-92

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Evolution à Long terme (1978–1986) des populations d'Amphipodes des sables fins de la pierre noire (baie de morlaix, manche occidentale) aprs̀s la catastrophe de l'Amoco Cadiz     

Jean-Claude Dauvin 《Marine environmental research》1987,21(4)

Greatly reduced in 1978 by the Amoco Cadiz oil spill, the amiphipod populations of the fine sand community of Pierre Noire in the Bay of Morlaix have not yet fully recovered 8 years after the pollution. The sublittoral sandi-mud benthic communities in the western part of the English Channel show a discontinuous distribution, occurring in isolated zones which are localized in estuaries and bays. The amphipods, which are characteristic of these communities and lack a pelagic larva, form insular populations. This insular distribution delays their re-introduction to the fine sand community of Pierre Noire. Moreover, the biological and demographic characteristics of the species entail limited periods of recolonisation and increase in population.  相似文献   

Tectonic Significance of the Taitung Canyon, Huatung Basin, East of Taiwan   总被引：1，自引：0，他引：1  

Jean-Claude Sibuet  Shu-Kun Hsu  Alain Normand 《Marine Geophysical Researches》2006,27(1):77-79

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How geographic distance and depth drive ecological variability and isolation of demersal fish communities in an archipelago system (Cape Verde, Eastern Atlantic Ocean)     

Anibal Medina  Jean-Claude Brêthes  Jean-Marie Sévigny  & Bruno Zakardjian 《Marine Ecology》2007,28(3):404-417

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Distribution of sterol and fatty alcohol biomarkers in particulate matter from the frontal structure of the Alboran Sea (S.W. Mediterranean Sea)   总被引：1，自引：0，他引：1  

Imma Tolosa  Nathalie LeBlond  Claire Copin-Montgut  Jean-Claude Marty  Stephen de Mora  Louis Prieur 《Marine Chemistry》2003,82(3-4):161-183

Sterol and fatty alcohol biomarkers were analyzed in suspended and sinking particles from the water column (20–300 m) of the Almeria–Oran frontal zone to characterize the biogenic sources and biogeochemical processes. Diatom- and haptophyte-related sterols were predominant at all sites and vertical distributions of sterol, and fatty alcohol biomarkers in sinking particles were markedly different from suspended particles. In contrast to the relatively fresh sinking particles with elevated concentrations of phyto- and zooplanktonic sterols, suspended particles were extensively degraded with increasing depth and exhibited a more terrestrial and zooplanktonic signature with depth.Sterol and alcohol biomarkers distributions and δ¹³C values from the jet core and the associated gyre of Atlantic waters showed a decoupling between the sinking particles of 100- and 300-m depth, demonstrating the influence of lateral advection in the frontal zone. In contrast, vertical transport of the particulate organic matter in Mediterranean waters was interpreted from the similar isotopic and molecular composition at both depths. The high abundance of phytosterols and phytol below the euphotic zone at 100 m signified that downwelling of biomass occurred on the downstream side of the gyre. The high concentrations of phytosterols and POC, in combination with the high phytosterols/phytol ratio, indicated the accumulation of detrital plant material in the oligotrophic Mediterranean waters near the frontal zone.A higher contribution of phytol in the sinking particles collected during the night at the surface of the jet and at the upstream side of the gyre provided evidence of diel vertical zooplankton migration and important grazing by herbivorous zooplankton.Carbon isotope ratios of sterols confirmed that the 24-ethylcholest-5-en-3β-ol, commonly associated with terrestrial sources, was a substantial constituent of the phytoplankton in this area. However, the more δ¹³C depleted values obtained for this compound in suspended particles suggested that there was some terrestrial contribution that only becomes evident after degradation of the more labile marine organic matter.  相似文献   

Continent–Ocean Transition of the Northern South China Sea and off Southwestern Taiwan     

Shu-Kun Hsu  Jean-Claude Sibuet 《Marine Geophysical Researches》2004,25(1-2):1-4

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Influence of spatial scales of observation on temporal change in diversity and trophic structure of fine-sand communities from the English Channel and the southern North Sea   总被引：2，自引：0，他引：2  

Ghertsos  Konstantinos; Luczak  Christophe; Dewarumez  Jean-Marie; Dauvin  Jean-Claude 《ICES Journal of Marine Science》2000,57(5):1481-1487

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Composition and spatial organization of a cold seep community on the South Barbados accretionary prism: Tectonic, geochemical and sedimentary context     

Didier Jollivet  Jean-Claude Faugeres  Roger Griboulard  Daniel Desbruyers  Gerard Blanc 《Progress in Oceanography》1990,24(1-4)

Deep faunal assemblages were observed on cold seeps, between 1000 and 2000m depth, along the southern termination of the Barbados accretionary prism, during the Caracolante II and Diapicar cruises. Faunal composition and microdistribution of a cold seep community were analyzed at one site using deep-sea photographs and seismic (3.5 Kz) profiles. The community is dominated by large mussels up to 20cm long (possibly related to the genus Bathymodiolus), tiny vesicomyid clams, and vestimentiferan clusters in which animals are up to 2m long. There is a high density of sponges (three species), bryozoans and gorgonians. Other taxa occasionally associated with this assemblage include galatheid crabs, anemones, holothurians and possibly pennatulaceans which are numerous at boundaries of the site. A typical deep-sea fauna of fish, asteroids and ophiuroids is also scattered about the vicinity. This seep community is distributed as a band of discontinuous colonies, 40–50m in width and more than 10km in length. Living colonies alternate with accumulations shells and bare areas. The substratum is hard mud covered by a ferrugineous crust and cemented by carbonates. The early diagenetic character of the bottom and the occurrence of biological assemblages indicate that seepages of sulphur and/or methane, which have been revealed along the decollement zone of the Barbados prism, must diffuse through the sea floor. These biological and geological features are located on the crests of NE-SW anticlinal ridges and mud volcanoes which have been built by diaprism.  相似文献