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Summary During the uppermost Carboniferous and lowermost Permian algal mounds were formed in inner shelf settings of the Carnic Alps (Austria/Italy). A specific mound type, characterized by the dominance of the dasyclad green alga Anthracoporella was studied in detail with regard to geometry, relationship between mound and intermound rocks, composition of the sediment, biota and diagenetic criteria...
Summary Large cyanoliths reaching up to 12 cm in size and mainly prolate, discoidal and spheroidal in shape occur in early Serpukhovian rocks from the San Antonio-La Juliana Unit (Guadiato Area, SW Spain). The main component in the cyanoliths is Girvanella, but other important components are the problematic-algae Sparaphralysia, Calcifolium and crustose Fasciella. A diverse assemblage of invertebrates,...
Summary From spring 1997 to winter 2000, the composition and structure of epibenthic bivalve clusters and patches on a backbarrier tidal flat of the East Frisian Wadden Sea were continoously analyzed. The studied bivalve aggregates developed from intense and approximately simultaneous spatfalls of Mytilus edulis and Cerastoderma edule in 1996, after a severe winter (1995/96) with 64 days of driftice...
Summary The Carboniferous, particularly during the Serpukhovian and Bashkirian time, was a period of scarce shallow-water calcimicrobial-microbialite reef growth. Organic frameworks developed on high-rising platforms are, however, recorded in the Precaspian Basin subsurface, Kazakhstan, Russia, Japan and Spain and represent uncommon occurrences within the general trend of low accumulation rates and...
Summary During Givetian times, the Jebel Rheris area was situated in a transitional zone at the northern margin of Gondwana, between the emerged Ougnate High in the north and the Mader Basin in the south. A facies pattern developed from stacked or amalgamated coral-stromatoporoid biostromes in the northern near-shore area to an alternating biostrome–crinoidal grainstone succession, which passed over...
Summary East of Cave del Predil (formerly Raibl), a platform-basin transition of the Dolomia Principale (Hauptdolomit) is spectacularly exposed at a seismic scale. Therefore, the eastern margin of the vast domain of the Dolomia Principale, facing the Slovenian Basin, is documented. Despite of strong dolomitization of the massive margin, some sedimentary structures and fossils have been recognized...
Summary The object of this paper is to provide a facies guide that helps subsequent workers recognizing different facies and palaeoenvironments of the terrestrial old Red Sandstone exposed in central N Spitsbergen. Sediments of the Early Devonian Wood Bay Formation represent continental molasse deposition under arid to semi-arid climatic conditions in three main depositional environments (rivers,...
Summary In the florigemma-Bank Member of the Late Jurassic (Oxfordian) NW German Korallenoolith Formation moderately diverse assemblages of calcareous algae are present. The following taxa have been identified: “Porostromata”, Solenopora jurassica Brown, Solenopora helvetica Peterhans, Pycnoporidium lobatum Yabe and Toyama, Otternstella cf. lemmensis (Bernier), Salpingoporella? suentelensis n. sp...
Summary This paper is focused on the facies associations of an Early-Middle Norian stratigraphic succession cropping outin the Northern Calabria (Buonvicino, Cosenza). These carbonate deposits, pertaining to the Verbicaro Unit, represent a dolomitized platform characterized by a clear dominance of automicrites over skeletal metazoans. On the basis of the chronostatigraphic data and sedimentary evolution,...
Summary The Holkerian(?)/early Asbian succession of Blue Pool (northwestern end of Gower Peninsula, southern Wales) includes two individual, decameter-sized, low relief bioconstructions: (a) a microbe-bryozoan-coral reefmound and (b) an overlying coral reef. The bioconstructions are embedded within a grainy, bioclastic and oolitic inner shelf facies. They occur in two successive shallowing upward...
Summary Microfacies analysis of over 1800 standard thin-sections of upper Viséan and Pendleian-aged platform limestones from southwestern Spain (Guadiato area) shows that foraminiferal assemblages contain many allochthonous specimens. The analysis of the cementation, recrystallization, abrasion, bioerosion, encrustation, dissolution, taphonomic distortion, orientation and sorting allow the recognition...
Summary Detailed analysis of microfabrics in Hamelin Pool stromatolites leads to reinterpretation of the origins of these structures. Previous studies have concluded that Shark Bay stromatolites form primarily as a result of sediment trapping and binding by microorganisms. Our results suggest that microbial precipitation of microcrystalline carbonate (micrite), as both framework and cement in these...
Summary The type upper Moscovian-basal Kasimovian argillaceous-carbonate succession of central European Russia contains regionally traced cyclothem-bounded subaerial exposure horizons (geosols) represented mainly by rendzina-type palaeosols. Palaeokarst profiles occurrarely and grade laterally to palaeosols. Composite subaerial profiles divided by one or two thin marine beds are called ‘multiple geosols’...
Summary Benthic coral reef communities were investigated on the Sanganeb-Atoll, 28 km off the coast of Port Sudan (Sudan, central Red Sea). Four test areas (5×5 m) were selected and marked in approx. 10 m depth along a transect running in SSW-NNE direction over the atoll and were mapped in 1980 and 1991. Detailed photographs were used for in situ verification of taxonomic composition of communities...
Summary Smaller benthic and planktonic foraminifera from the clastic sediments of the Pazin Basin (Istria, Croatia) were studied in order to obtain more data about paleoceanographic conditions that existed in the Middle Eocene Dinaric foreland basin. The succession investigated corresponds to the Middle Eocene planktonic foraminiferal zones Globigerapsis kugleri/Morozovella aragonensis (P11), Morozovella lehneri...
Summary An Early Cretaceous mass-occurrence of ammonites in the Ternberg Nappe of the Northern Calcareous Alps (Upper Austria) is described for the first time. The mass-occurrence (section KB1-B=Klausrieglerbach 1, section B) dominated by Karsteniceras ternbergense Lukeneder is of Early Barremian age (Moutoniceras moutonianum Zone). The Karsteniceras mass-occurrence comprises eight different genera,...
Summary A study of fossils in thin sections of a sample from the uppermost Krol E Member in the Mussoorie Hills of the Lesser Himalaya, India, proves the existence of morphologically differentiated calcified sponges within the Precambrian-Cambrian boundary time interval. The sponges, described as Mussooriella kroli n.g., n.sp. and Maldeotaina composita n.g., n.sp. indicate the presence of different...
Summary The internal construction and biotic communities of the Uzunbulak reef of the northwestern Tarim Basin are studied for the first time. The reef was built during the Sakmarian, while the reef substrate and capping beds are of latest Asselian and earliest Artinskian ages, respectively. The reef substrate beds are composed of skeletal and oncoid grainstone. Those fusulinid-dominated skeletal...
Vengono presentati i risultati di uno studio sistematico condotto sulle alghe calcaree del Norico dei Monti del Matese (Campania settentrionale), per la prima volta segnalate in Italia. La ricca associazione composta da prevalenti pseudoudoteacee e precisamente: Garwoodia maxima, Garwoodia toomeji, Pseudoudotea magna, Jabrianella sp., oltre a Asterocalculus heraki, Heteroporella zankli eProbolocuspis...
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