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"The Ordovician period is a significant chapter in Earth's history that included the great Mid-Ordovician biodiversification event, the Hirnantian glaciation, and long-term greenhouse conditions. Ordovician rocks are widespread on most continents and the recent finalization of a modern chronostratigraphic classification of the Ordovician system now facilitates high-resolution correlations that allow for integrated multidisciplinary research. The diverse papers comprising this volume address orogenesis, paleogeography, climate modeling, sedimentation, biodiversity, and isotopic excursions; together they promote an integrated view of the Ordovician earth system."--Publisher's description.
This special publication Perspectives in Carbonate Geologyis a collection of papers most of which were presented at asymposium to honor the 80th birthday of Bob Ginsburg at the meetingof Geological Society of America in Salt Lake City in 2005. Themajority of the papers in this publication are connected with thestudy of modern carbonate sediments. Bob Ginsburg pioneered theconcept of comparative sedimentology - that is using the modern tocompare to and relate to and understand the ancient. These studiesare concerned with Bob's areas of passion: coral reefs andsea-level; submarine cementation and formation of beach rock;surface sediments on Great Bahama Bank and other platforms; originof ooids; coastal sediments; formation of stromatolites; impact ofstorms on sediments; and the formation of dolomite. The remainderof the papers apply the study of modern environments andsedimentary processes to ancient sediments. Recent other publications of the International Association ofSedimentologists SPECIAL PUBLICATIONS 40 Analogue and Numerical Modelling of Sedimentary Systems From Understanding to Prediction Edited by P. de Boer, G. Postma, K. van der Zwan, P. Burgess and P.Kukla 2008, 336 pages, 172 illustrations 39 Glacial Sedimentary Processes and Products Edited by M.J. Hambrey, P. Christoffersen, N.F. Glasser and B.Hubbard 2007, 416 pages, 181 illustrations 38 Sedimentary Processes, Environments and Basins A Tribute to Peter Friend Edited by G. Nichols, E. Williams and C. Paola 2007, 648 pages, 329 illustrations 37 Continental Margin Sedimentation From Sediment Transport to Sequence Stratigraphy Edited by C.A. Nittrouer, J.A. Austin, M.E. Field, J.H.Kravitz, J.P.M. Syvitski and P.L. Wiberg 2007, 549 pages, 178 illustrations 36 Braided Rivers Process, Deposits, Ecology and Management Edited by G.H. Sambrook Smith, J.L. Best, C.S. Bristow and G.E.Petts 2006, 390 pages, 197 illustrations 35 Fluvial Sedimentology VII Edited by M.D. Blum, S.B. Marriott and S.F. Leclair 2005, 589 pages, 319 illustrations REPRINT SERIES 4 Sandstone Diagenesis: Recent and Ancient Edited by S.D. Burley and R.H. Worden 2003, 648 pages, 223 illustrations Please see inside the book for the full list of IASpublications Cover design by Code 5 Design For information, news, and content about Wiley-Blackwell booksand journals in Earth Sciences please visit www.earthpages.com
Continental margins and their fossilized analogues are important repositories of natural resources. With better processing techniques and increased availability of high-resolution seismic and potential field data, imaging of present-day continental margins and their embedded sedimentary basins has reached unprecedented levels of refinement and definition, as illustrated by examples described in this volume. This, in turn, has led to greatly improved geological, geodynamic and numerical models for the crustal and mantle processes involved in continental margin formation from the initial stages of rifting through continental rupture and break-up to development of a new ocean basin. Further informing these models, and contributing to a better understanding of the features imaged in the seismic and potential field data, are observations made on fossilized fragments of exhumed subcontinental mantle lithosphere and ocean–continent transition zones preserved in ophiolites and orogenic belts of both Palaeozoic and Mesozoic age from several different continents, including Europe, South Asia and Australasia.