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IAS Special Publication 35, Fluvial Sedimentology VII, comprises ofa series of peer-reviewed papers that were initially presented atthe 7th International Conference on Fluvial Sedimentology, held inLincoln, Nebraska on August 6-10, 2001. The 29 papers in this volume reflect the topical and geographicdiversity of exciting research conducted by fluvialsedimentologists at the beginning of the 21st century. Themesrepresented in this volume include (a) flow, sediment transport,and bedform dynamics, (b) characteristics of modern fluviallandforms, environments and systems, (c) physical analogue andnumerical modeling of fluvial systems, (d) the responses ofQuaternary fluvial systems to climate change, active tectonics,and/or sea-level change, and (e) characteristics of pre-Quaternaryfluvial deposits and evolution of pre-Quaternary fluvial systems.
This book gives a new global perspective on the Phanerozoic timescale, by bringing together extensive Australian and overseas research on biostratigraphy, geochronology, and magnetostratigraphy. For the first time, correlations are established between Australian and European biozonal schemes for the entire Phanerozoic, by integrating local and international biozones, isotopic ages, and magnetic polarity intervals. Tie points are based on tightly constrained isotopic and biostrastigraphic ages, and this is the first compilation for the whole of the Phanerozoic to apply results from the latest isotopic dating techniques, including the high resolution ion microprobe (SHRIMP) and variants of the (superscript 40)Ar/(superscript 39)Ar method. These have radically rescaled some parts of the geological column. An Australian Phanerozoic Timescale gives the essential framework for resource exploration, geologic modelling, and reconstruction of past environments and land-sea configurations during the last 545 million years of earth history.
The seventh International Palynological Congress was held in Brisbane, Australia, from 29th August to 3rd September, 1988. Both the Congress and the papers compiled here show palynology to be a discipline striking in its breadth, characterised by a diversity of content, methodology and application. The breadth spans important applications in medicine, in evolutionary biology and taxonomy, in ecology, in stratigraphy and sedimentology, in oil exploration and recovery, in paleoclimatology and even in the highly practical forensic science. Within the fields themselves there is clearly an increasing depth of understanding as well as breadth of compass.
"A locality index to the reports of the Geological survey of N. S. Wales from 1875 to 1892 inclusive, by W. S. Dun": v. 3, p. 154-194.
High-latitude settings are sensitive to climatically driven palaeoenvironmental change and the resultant biotic response. Climate change through the peak interval of Cretaceous warmth, Late Cretaceous cooling, onset and expansion of the Antarctic ice sheet, and subsequently the variability of Neogene glaciation, are all recorded within the sedimentary and volcanic successions exposed within the James Ross Basin, Antarctica. This site provides the longest onshore record of Cretaceous-Tertiary sedimentary and volcanic rocks in Antarctica and is a key reference section for Cretaceous-Tertiary global change. The sedimentary succession is richly fossiliferous, yielding diverse invertebrate, vertebrate and plant fossil assemblages, allowing the reconstruction of both terrestrial and marine systems. The papers within this volume provide an overview of recent advances in the understanding of palaeoenvironmental change spanning the mid-Cretaceous to the Neogene of the James Ross Basin and related biotic change, and will be of interest to many working on Cretaceous and Tertiary palaeoenvironmental change.