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Cryptotephra sedimentation processes within two lacustrine sequences from west central Sweden

Davies, SM (author)
Elmquist, M (author)
Stockholms universitet,Institutionen för tillämpad miljövetenskap (ITM)
Bergman, J (author)
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Wohlfarth, B (author)
Stockholms universitet,Institutionen för geologi och geokemi
Hammarlund, Dan (author)
Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science
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 (creator_code:org_t)
2016-07-27
2007
English.
In: The Holocene. - : SAGE Publications. - 0959-6836 .- 1477-0911. ; 17:3, s. 319-330
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Distal tephra horizons, particularly within lacustrine sequences, are increasingly being used as time-synchronous marker horizons within palaeoclimatic and palaeoenvironmental investigations. As sedimentary features marking the presence of these so-called cryptotephras are absent to the naked eye, it is of some importance that the stratigraphic position representing primary airfall, and likewise the timing Of the volcanic event, is accurately and consistently recorded amongst these deposits. Often tephra shards from a cryptotephra deposit can be found spanning several centimetres of sediments within lacustrine and peat sequences. Very few studies, however, have looked in detail at the sedimentation and vertical distribution of cryptotephra deposits within such sequences and, more importantly, the criteria for defining the correct stratigraphic position of the volcanic event. Two sediment cores from Lake Spaime and Lake Getvaltjarnen, west central Sweden are employed to investigate in detail the vertical distribution of the tephra shards derived from the AD 1875 eruption of the Askja volcano in Iceland. Detailed geochemical analysis of shards from both records indicate that products of the Askja eruption are present for at least 120 years and thus emphasize the importance of carefully identifying the correct horizon that marks the timing of the volcanic event rather than shards resulting from a period of reworking or downward migration. Both sites yield contrasting shard concentration profiles and thus raise a number of questions regarding the influence of site-specific processes on cryptotephra sedimentation, particularly the role of snow-beds acting as tephra traps, the possibility of reworking, and downward migration of shards in soft sediment. A second tephra is also identified at Lake Getvaltjarnen and is believed to originate from the AD 1477 Veidivotn eruption and represents the first occurrence of this tephra outside of Iceland.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Keyword

Askja AD 1875 tephra
historical volcanic eruptions
cryptotephra sedimentation processes
lacustrine deposits
Iceland
Sweden
Environmental science

Publication and Content Type

art (subject category)
ref (subject category)

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By the author/editor
Davies, SM
Elmquist, M
Bergman, J
Wohlfarth, B
Hammarlund, Dan
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Geology
Articles in the publication
The Holocene
By the university
Lund University
Stockholm University

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