Ooids in Purbeck limestones (lowermost Cretaceous) of the Swiss and French Jura

Abstract

Ooids occurring in the shallow‐water Purbeckian carbonate sediments of the Jura mountains can be grouped into six types. Gradations from one type to another and coexistence of the various types are common. Type 1 ooids are small and well rounded. They display fine concentric micritic laminae. In many cases their cortices are dissolved and replaced by void‐filling spar. Microsparitic neomorphic replacement occurs locally. Type 2 ooids are large and have irregular shapes. They show fine micritic laminae and occasional layers of fine‐radial crystals. They commonly evolve into oncoids. Ooids of type 3 display many fine‐radial cortical laminae and are patchily micritized. They are medium in size and mostly well rounded. This type of ooid may pass into large, irregularly shaped coated grains. Type 4 ooids have 1 to 4 cortical laminae with a fine‐radial structure and patchy micritization. They are medium in size and well rounded. Type 5 ooids have only one lamina with a coarse‐radial structure. They are small and well rounded. Associated are spherical grains containing bundles of elongate crystals. Ooids of type 6 show superpositions of two or more different, radial and or fine micritic laminae. The cortical structure may also change laterally in the same lamina. The preferential dissolution of type 1 ooid cortices to form oomoulds indicates a primary composition of unstable carbonate. Sedimentological features and comparison with modern ooid occurrences point to formation on high‐energy sandbars in normal‐marine waters. Type 2 ooids grew in marine‐lagoonal environments with quiet water and abundant cyanobacteria. The radially structured ooid cortices of types 3, 4 and 5 show no dissolution features. This implies that they were originally composed of stable carbonates, or that an unstable carbonate phase was transformed into a stable one at an early stage of diagenesis. Type 3 ooids occur together with marine faunas and indicate high water energy. Ooids of type 4 and type 5 originated probably from relatively quiet water of variable salinity. Coexistence of different ooid types and mixed forms of type 6 implies gradual or rapid changes in hydrodynamic, geochemical and microbiological conditions which were a feature of the Purbeckian depositional environments.

Formation of illitic minerals at surface temperatures in Purbeckian sediments (Lower Berriasian, Swiss and French Jura)

“…However, the higher percentages of illite are encountered in the southeastern part of the Jura Mountains, towards the open-marine subalpine basin. There, marine influences are expressed by marine high-energy ooids (Strasser, 1986) and marine-lagoonal faunas (dasycladaceans, benthic foraminifera). Consequently, K § was probably provided by marine waters during ingressions on to the Purbeckian platform (Fig.…”

Magnitude of lateral displacement on the Crevillente Fault Zone (Betic Cordillera, SE Spain): stratigraphical and sedimentological considerations

“…The second textural type has fine, though abundant, lamellae of radial microsparite. These two categories correspond to types 1 and 3 of Strasser (1986). Moreover, ooids formed of very thin micritic lamellae (third group), corresponding to type 2 of Strasser (1986), have been also found.…”

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“…El tipo de envuelta más representada es la formada por láminas micríticas inferiores y 1 ó 2 láminas esparíticas exteriores (tipo mixto 1-3: Strasser, 1986). Los bioclastos más abundantes son de equinodermos, crinoides, algas solenoporáceas y miliólidos.…”

“…Los ooides de tipo 4 que existen localmente, son característicos de medios restringidos de baja energía (Strasser, 1986), Ypor ello debieron ser resedimentados desde dominios más someros. Los abundantes intraclastos son también resedimentados ya que son similares a las facies que se desarrollan lateralmente.…”