By E. Insalaco, P. W. Skelton, T. J. Palmer
Carbonate Platform platforms: elements and interactions is a suite of thirteen papers, plus an creation, about the results of organism-environment interactions in smooth and historical carbonate structures, bobbing up from the Lyell assembly on 'Organism-Environment Feedbacks in Carbonate systems and Reefs' held on the Geological Society, united kingdom. The papers offered the following offer an built-in view of carbonate structures, emphasizing dynamic interactions in any respect hierarchical degrees and revealing the constraints of uniformitarian analogy in biotically prompted sedimentary platforms. chosen case reviews from worldwide illustrate points starting from the genesis of progress materials to altering styles of carbonate platform improvement. The textual content should be of curiosity to sedimentologists, palaeontologists and marine ecologists alike.
Readership: Sedimentologists, Palaeontologists, Marine Ecologists, Petroleum Exploration & construction Geologists and Marine Environmental Conservationists.
Cool-Water Carbonates: Depositional platforms and Palaeoenvironmental Controls (Geological Society distinct booklet) - ISBN 1862391939
The way forward for Geological Modelling in Hydrocarbon improvement - particular book no 309 - ISBN 1862392668
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Extra resources for Carbonate Platform Systems Components and Interactions
Calcium carbonate budget of a fringing reef on the west coast of Barbados. Part I - Zonation and productivity. Bulletin of Marine Science, 27, 479-510. STEUBER, T. 1996. Stable isotope sclerochronology of rudist bivalves: Growth rates and Late Cretaceous seasonality. Geology, 24,315-318. 1997. Hippuritid rudist bivalves in siliciclastic settings - functional adaptations, growth rates and strategies. Proceedings of the 8th International Coral Reef Symposium, Vol. II. 1761-1766. 1999a. Isotopic and chemical intra-shell variations in low-Mg calcite of rudist bivalves (Mollusca: Hippuritacea) - disequilibrium fractionations and late Cretaceous seasonality.
Comparable high rates of substrate infestation were noted at deep fore-reef sites in Jamaica by Goreau & Hartman (1963). By contrast, more diverse boring assemblages characterize the back-reef and lagoon. g. g. Eunice mutilata) are also common (Fig. 1). Similar diverse assemblages of 37 sponges, bivalves and worms characterize lagoon patch reef frameworks. Studies undertaken across the very different reef system of the Great Barrier Reef (Risk et al 1995) using samples of Acropora formosa also document a macroboring community dominated by sponges (Table 2, Fig.
8. Plenum, New York, 239-265. Ross, D. J. & SKELTON, P. W. 1993. Rudist formations of the Cretaceous: a palaeoecological, sedimentological and stratigraphic review. In: Wright, P. ) Sedimentology Review/1. Blackwell, London, 73-91. SANDERS, D. & PONS, J. M. 1999. Rudist formations in mixed siliciclastic-carbonate depositional environments, Upper Cretaceous, Austria: stratigraphy, sedimentology, and models of development. Palaeogeography, Palaeoclimatology, Palaeoecology, 148,249-284. SEILACHER, A.