SwePub
Sök i LIBRIS databas

  Extended search

onr:"swepub:oai:DiVA.org:su-29432"
 

Search: onr:"swepub:oai:DiVA.org:su-29432" > Diatom oxygen isoto...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Diatom oxygen isotopes in pro-galcial lake sediments from northern Sweden: A 5000 year record of atmospheric circulation.

Rosqvist, G. (author)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Jonsson, C. (author)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Yam, R. (author)
show more...
Karlén, W. (author)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Shemesh, A. (author)
show less...
 (creator_code:org_t)
Elsevier BV, 2004
2004
English.
In: Quaternary Science Reviews. - : Elsevier BV. - 0277-3791 .- 1873-457X. ; 23:7-8, s. 851-859
  • Journal article (peer-reviewed)
Abstract Subject headings
Close  
  • We use a pro-glacial oxygen isotope record of diatom silica (δ18Odiatom) and a sedimentary proxy for glacier flutuations to determine centennial-millennial scale climate change during the last 5000 yeras in northern Sweden. We show that the lake water isotopic composition åredominantly reflects the isotopic composition of the precipitation. Superimposed on a general depletion trend of 3.5‰ over the past 5000 years we found that the isotopic composition of precipitation became depleted (> 1‰ excursions) during four occasions centered at 4400, 3000, 2000 and, after 1200 cal yr BP. Climate simultaneously sustained a positive glacier mass balance, taht caused the catchment glacier to advance. A peristan cgange in the atmopheric circulation pattern could potentially have caused the registered chnages in the δ18Odiatom because different air masses hold characteristics δ18O signatures of their precipitation. The glacier mass balance primarily responds to the influence of summer temperature on ablation. We suggest that the most likely cause for the recorded chnages in both these proxies is a steadily increasing but fluctuating dominance of colder and δ18O depleted air masses from the north/northeast during the past 5000 years. Theδ18Odiatom depletion and glacier events all occur at times of relative ice-rafted-debris maxima in the North Atlanic, consistent with cold conditions and changes in surface wind directions. Our results confirm that changes towards a predominace of north/northeasterly winds occured at these time intervals.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

Keyword

pro-glacial
lake sediment
diatom silica
oxygen isotopes
Physical geography
Naturgeografi

Publication and Content Type

ref (subject category)
art (subject category)

Find in a library

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Find more in SwePub

By the author/editor
Rosqvist, G.
Jonsson, C.
Yam, R.
Karlén, W.
Shemesh, A.
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Physical Geograp ...
Articles in the publication
Quaternary Scien ...
By the university
Stockholm University

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view