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Sea-level constitutes a critical planetary boundary for geological processes and human life. Sea-level fluctuations during major greenhouse phases are still enigmatic and strongly discussed in terms of changing climate systems. The geological record of the Cretaceous greenhouse period provides a deep-time view on greenhouse-phase Earthsystem processes that facilitates a much better understanding of the causes and consequences of global, geologically short-term, sea-level changes. In particualr, Cretaceous hothouse periods can serve as a laboratory to better understand a near-future greenhouse Earth. This volume presents high-resolution sea-level records from globally distributed sedimentary archives of the Cretaceous involving a large group of scientists from the International Geoscience Programme IGCP 609. Marine to non-marine sedimentary successions were analysed for revised age constraints, the correlation of global palaeoclimate shifts and sea-level changes, tested for climate-driven cyclicities, and correlated within a high-resolution stratigraphic framework of the Geological Timescale. For hothouse periods, the hypothesis of significant global groundwater-related sea-level change, i.e. aquifer-eustasy as a major process, is reviewed and substantiated.
This volume combines original data from the offshore and onshore Levant in various fields like sedimentology, palaeontology, geochemistry, structural geology and geophysics. This multidisciplinary approach provides an overview of the development of the Levant Basin and allows discussion of the later geological history and deformation processes of the Levant provinces
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
This volume also discusses the computer modelling of carbonate cycles and sequence analysis. This will prove an invaluable text for senior undergraduate and postgraduate students in the earth sciences in general and will also be of value to the professional researcher. Carbonate platforms contains contributions from an international authorship and the volume has been edited by one of the most respected names in the earth sciences. Areas covered include; early rifting deposition; examples from carbonate sequences of Sardinia (Cambrian) and Tuscany (Triassic-Jurassic), Italy; geometry and evolution of platform-margin bioclastic shoals, late Dinantian (Mississippian), Derbyshire, UK; cyclic sedimentation in cabonate and mixed carbonate/clastic environments; four simulation programs for a desktop computer; middle Triassic carbonate ramp systems in the Catalan Basis, N.E. Spain; facies, cycles, depositional sequencies and controls; stages in the evolution of late Triassic and Jurassic platform carbonates; western margin of the Subalpine basin, Ardech, France. The formation and drowning of isolated carbonate platforms; tectonic and ecologic control of the Northern Apennines; controls on Upper Jurassic carbonate build up development in the Lusitanian Basin, Portugal; Hauterivian to Lower Aptian carbonate shelf sedimentation and sequence stratigraphy in the Jura and northern Subalpine chains (southeastern France and Swiss Jura); basement structural controls on Mesozoic carbonate facies in northeastern Mexico; the Aptian-Albian carbonate episode of the Basque-Cantabrian Basis (Northern Spain); general characteristics, controls and evolution; response of the Arabian carbonate platform margin slope to orogenic closing of an ocean basin, Cretaceous, Oman.
Taking a new global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys s.l. and Eurasian plates over the last 600 Ma of Earth's history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have attracted international research interest in the geology of the Iberian Peninsula. This volume presents the most comprehensive, and updated description of the Alpine cycle in Iberia. This volume focuses in the different geological events during the Alpine orogeny as well as the lithological succession . This book is of interest not only for scientists of Portugal and Spain but also for geoscientists searching for analogies for oil and gas as well as tourists visiting the main mountain ridges of Iberia such as the Pyrenees.