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Titlebook: Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas; Excavations at Holyw R. C. Preece,D.

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发表于 2025-3-21 17:24:35 | 显示全部楼层 |阅读模式
书目名称Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas
副标题Excavations at Holyw
编辑R. C. Preece,D. R. Bridgland
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图书封面Titlebook: Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas; Excavations at Holyw R. C. Preece,D.
描述Holywell Coombe, an embayment in the chalk scarp overlookingFolkestone, Kent, was designated a geological Site of SpecialScientific Interest in 1985 because it contains richly fossiliferousLate Quaternary sediments providing a unique archive of the last13,000 years. .The construction of the Channel Tunnel across the Holywell Coombe SSSIbrought about a major rescue excavation, funded by Eurotunnel, thatset an important precedent in Earth Science conservation. Thismultidisciplinary investigation has added enormously to ourunderstanding of the environment and natural history of theLate-glacial and Holocene. The climatic complexity of the Late-glacialis recorded in the nature of the sediments, the fossils recovered fromthem and the soils developed within them. .From the Neolithic, and especially during the Early Bronze Age, theslopes were destabilized as a result of forest clearance, leading tothe accumulation of hillwash. Archaeological excavations in thehillwash have revealed evidence of prehistoric occupation andagricultural activity in the coombe. .Eurotunnel also funded biological surveys of the local terrestrial andaquatic habitats. Combining these with the fossil evidence, it ha
出版日期Book 1998
关键词Geomorphology; Stratigraphy; agriculture; archaeology; biology; biostratigraphy; ecology; environment; envir
版次1
doihttps://doi.org/10.1007/978-94-011-4908-2
isbn_softcover978-94-010-6059-2
isbn_ebook978-94-011-4908-2
copyrightSpringer Science+Business Media Dordrecht 1998
The information of publication is updating

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Environmental Backgroundimmediately north of Folkestone contains a number of impressive coombe valleys (Fig. 2.1). Although the ecological work discussed in Part Seven was carried out over the whole of the Folkestone — Etchinghill SSSI (Fig. 2.2), the main focus of the geological and archaeological investigations reported
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Sedimentological investigationscal techniques (thin sections, particle size analyses, mineralogical analyses, % CaCO., % organic C) were employed in order to extract environmental evidence from these. Particle size and mineralogical analyses were also used to determine the sources of all the major sedimentary units.
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Radiocarbon Datingechniques all play a part and need to be evaluated carefully in the interpretation of the ages. The carbonaceous material on which the radiocarbon isotope concentration measurements are made is the final product of photosynthesis of contemporary atmospheric carbon dioxide preserved in the sedimentar
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Mollusca valuable technique for geologists and environmental archaeologists working in limestone regions (e.g. Evans, 1972). Two factors enable precise habitat reconstructions from the study of fossil land snails. First, in contrast to many paly-nomorphs, the vast majority of specimens can be identified to
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Insects has remained in a waterlogged condition since its original deposition. Since beetles are often closely tied to particular environmental niches, their fossils can provide a detailed picture of the available habitats close to the site at which they were found. For the most part, they do not seem to h
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