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

爆裂

書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas影響因子(影響力)




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas影響因子(影響力)學科排名




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas網(wǎng)絡(luò)公開度




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas網(wǎng)絡(luò)公開度學科排名




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas被引頻次




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas被引頻次學科排名




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas年度引用




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas年度引用學科排名




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas讀者反饋




書目名稱Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-eas讀者反饋學科排名

織物

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

稱贊

epidermis

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.

情感

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

receptors

具體

assail

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

奴才

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

alliance