Titlebook: Microbial Mats; Structure, Developme Lucas J. Stal,Pierre Caumette Conference proceedings 1994 Springer-Verlag Berlin Heidelberg 1994 Benth

噴油井

Rutger de Wit,Joan O. Grimalt,Mariona Hernandez-Mariné

arabesque

磨坊

Ester Clavero,Joan O. Grimalt,Vidal Merino,Mariona Hernández-Mariné

fluffy

Aharon Oren,Uri Fischel,Zeev Aizenshtat,Eitan B. Krein,Robert H. Reed

神圣在玷污

LATHE

Microbial mats in coastal environmentstidal sediments (Cohen et al. 1984; Cohen and Rosenberg 1989). A noticeable similarity of these environments is their relative low species diversity. Particularly, multicellular organisms are excluded from such environments and it has been conceived that the absence or limited activity of grazing or

obstinate

etiquette

Microbial mats in a thermomineral sulfurous cave (Feru and Capotà 1991). Hydrogeologieal studies performed during the last 60 years (Macovei 1912; Cioc?rdel and Protopopescu-Pache 1955; Moissiu 1968; Feru and Capotà 1991) identified a deep captive sulfurous aquifer located in Barremian-Jurassic limestones, extending 15 km to the North and 50 km t

啞劇

Establishment of phototrophic purple sulphur bacteria in microbial mat systemsnvironments (Castenholz 1984; Cohen 1984; J?rgensen and Cohen 1977; Stal et al. 1985; Van Gemerden et al. 1989a, b). The laminated structure of these vertically stratified benthic ecosystems is the result of the development of the constituent microflora along physical and chemical gradients. Thus, i

拾落穗

Biological versus inorganic processes in stromatolite morphogenesis: Observations from mineralizing tion. In general, all sedimentary laminations reflect periodic interruptions in deposition. For example, in stromatolites formed in detrital sedimentary systems, laminations may arise through variations in current velocity and rates of sedimentation (Farmer and Des Marais 1993). In mineralizing sedi