Download Holocene land-ocean interaction and environmental change by Ian Shennan, Geological Society of London PDF
By Ian Shennan, Geological Society of London
Nearly all of study offered during this quantity arises from the Land-Ocean Evolution Perspecitve research (LOEPS), which was once one component to the Land-Ocean interplay examine (LOIS - funded through the normal setting study Council).The major objective of LOEPS was once to explain the evolution of coastal platforms from the Holocene to the current, in accordance with alterations in relative sea point and the effect of human activities.A key aspect within the good fortune of LOEPS has been the mixing and interplay among many of the parts of the learn programme. The papers released right here replicate this integration instead of summarizing the result of person examine tasks or the success of a unmarried LOEPS target. The contributions fall into 4 sections: ideas; Humber catchment; different parts in the studied area; neighborhood scale research. additionally to be had: The Geology of britain And Wales - ISBN 1862391998 weather swap and Groundwater - certain ebook No 288 - ISBN 9781862392359 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on this planet, and one of many biggest publishers within the Earth sciences.The Society publishes quite a lot of top quality peer-reviewed titles for lecturers and execs operating within the geosciences, and enjoys an enviable foreign recognition for the standard of its work.The many components during which we put up in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic stories and geochemistry-Remote sensing-History of geology-Regional geology courses
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Determination of organic carbon and 39 nitrogen in marine sediments using the Carlo Erba N A-1500 analyzer. Deep-Sea Research, 37, 157-165. Vos, P. C. & DE WOLF, H. 1993. Diatoms as a tool for reconstructing sedimentary environments in coastal wetlands; methodological aspects. Hydrobiologia, 269/270, 285-296. WALLER, M. P. 1998. An investigation into the palynological properties of fen peat through multiple pollen profiles from south-eastern ngland. Journal of Archaeological Science, 25, 631-642.
However, the SWLIs of samples from the lower clastic unit are exceptionally high: indeed the sample at 541 cm depth is above MHWST. This is caused by the low abundance of calcareous foraminifera within the clastic unit and hence, is dominated by agglutinated foraminifera (/. macrescens) with optima high in the tidal range. As a result, the change in SWLI across the regressive contact is negligible compared to the transgressive contact. 27m because all fossil samples possess good modern analogues.
Agglutinated Foraminifera as Indicators of Salt Marsh Development in Relation to Late Holocene Sea-level Rise. PhD thesis, Free University, Amsterdam. , FONTAINE, M. F. & JICKELLS, T. D. 1993. Isotopic and biochemical composition 38 J. RIDGWAY ET AL. of paniculate organic material in a shallow water estuary (Great Ouse, North Sea, England). Marine Chemistry, 43, 263-276. GAUNT, G. D. 1994. Geology of the Country around Goole, Doncaster and the Isle of Axholme. Memoirs of the British Geological Survey, Sheets 79 and 88 (England and Wales), Stationery Office, London.