Ontology type: schema:ScholarlyArticle
2002-06
AUTHORSN.G. Cameron, Ø.A. Schnell, M.L. Rautio, A. Lami, D.M. Livingstone, P.G. Appleby, J.A. Dearing, N.L. Rose
ABSTRACTThe purpose of the palaeolimnological research project carried out at Øvre Neådalsvatn was to apply a number of physical and biological proxy-climate analyses to recent sediments and to compare the results of these analyses with instrumental records of climate. Using a radiometric chronology to match the sediment core with the calendar ages of the reconstructed instrumental record, and by time-averaging the instrumental record, the statistical significance of the relationships between each of the sediment-climate proxies and the reconstructed instrumental-climate measurements were evaluated. Acid deposition at Øvre Neådalsvatn has been low and its impact limited. Whilst there has been an overall rise in mean annual temperature of about 1 °C since 1900, the physical and biological sediment records studied appear to be insensitive to climate warming of this magnitude. On the one hand, this may be a result of the loss in temporal resolution caused by time-averaging the instrumental data; on the other hand, the lake may be insensitive to the impact of this climate change. More... »
PAGES79-93
http://scigraph.springernature.com/pub.10.1023/a:1020324019052
DOIhttp://dx.doi.org/10.1023/a:1020324019052
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