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Recent environmental change and human impact on Svalbard: the lake-sediment geochemical record

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dc.contributor.author Boyle, John F. eng
dc.contributor.author Rose, Neil L. eng
dc.contributor.author Appleby, P. G. eng
dc.contributor.author Birks, Harry John Betteley eng
dc.date.accessioned 2007-12-10T07:48:57Z
dc.date.available 2007-12-10T07:48:57Z
dc.date.issued 2004
dc.identifier.citation Journal of Paleolimnology 2004 31 (4): 515-530, en
dc.identifier.issn 1573-0417
dc.identifier.uri http://hdl.handle.net/1956/2484
dc.description This is the eighth in a series of nine papers published in this special issue dedicated to recent environmental change on Svalbard. H.J.B. Birks, Vivienne J. Jones, and Neil L. Rose were guest editors of this special issue. en
dc.description.abstract As part of a broader investigation into recent environmental change on Svalbard, the inorganic geochemical record of six lake-sediment cores was analysed. The major temporal trends in sediment elemental composition are driven by variations in two contrasting sediment components, both derived from catchment soils: (1) mineral matter, and (2) soil organic matter (SOM), enriched in Fe and Mn oxides and heavy metals. Two environmental impacts are recorded in most or all of the lake sediment sequences. An up-core increase in organic matter can be partly attributed to diagenetic effects, but also requires an enhanced supply of SOM relative to mineral matter. In addition, the central and southern sites all show a ca. 1970 event characterised by an enhanced mineral matter accumulation rate. This requires either an enhanced allochthonous supply or an enhanced mobilisation of littoral sediments. In either case a regional-scale driving force, such as a shift in climate, is required. At five of the lakes the sediment heavy metal concentration profiles can be explained entirely by natural factors. However, at Tenndammen (U), situated close to the Svalbard’s largest settlement at Longyearbyen, possible anthropogenic Pb enrichment is found. Comparison of observed and expected heavy metal profiles (based on Greenland ice-core data) shows that the lakes are generally too insensitive to have recorded a long-transported heavy metal pollution signal. en
dc.language.iso eng eng
dc.publisher Springer en
dc.subject Arctic eng
dc.subject Environmental change eng
dc.subject Geochemistry eng
dc.subject Heavy metals eng
dc.subject Palaeolimnology eng
dc.title Recent environmental change and human impact on Svalbard: the lake-sediment geochemical record en
dc.type Peer reviewed eng
dc.type Journal article eng
dc.subject.nsi VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480 nob
bora.peerreviewed Peer reviewed eng
bibo.doi http://dx.doi.org/10.1023/B:JOPL.0000022549.07298.6e eng
dc.identifier.doi http://dx.doi.org/10.1023/B:JOPL.0000022549.07298.6e


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