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- Bjorck, S, et al.
(författare)
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Synchronized terrestrial-atmospheric deglacial records around the North Atlantic
- 1996
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Ingår i: SCIENCE. - : AMER ASSOC ADVANCEMENT SCIENCE. - 0036-8075. ; 274:5290, s. 1155-1160
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Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
- On the basis of synchronization of three carbon-14 (C-14)-dated lacustrine sequences from Sweden With tree ring and ice core records, the absolute age of the Younger Dryas-Preboreal climatic shift was determined to be 11,450 to 11,390 +/- 80 years before
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3. |
- Goslar, T, et al.
(författare)
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Variations of atmospheric C-14 concentrations over the Allerod-Younger Dryas transition
- 1999
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Ingår i: CLIMATE DYNAMICS. - : SPRINGER VERLAG. - 0930-7575. ; 15:1, s. 29-42
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Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
- Highly variable atmospheric radiocarbon concentrations are a distinct feature during the last deglaciation. The synchronisation of two high-resolution AMS C-14-dated records, Lake Gosciaz, and a floating Late Weichselian glacial varve chronology at the Al
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- BJORCK, S, et al.
(författare)
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C-14 AMS MEASUREMENTS FROM THE LATE WEICHSELIAN PART OF THE SWEDISH TIME-SCALE
- 1995
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Ingår i: QUATERNARY INTERNATIONAL. - : PERGAMON-ELSEVIER SCIENCE LTD. ; 27, s. 11-18
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Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
- Accelerator mass spectrometry measurements on plant macrofossils from the older part of the Swedish Time Scale, a chronology spanning over the past 13,000 calendar years, indicate a good agreement between varve years and calibrated ages (tree-rings, U-Th)
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8. |
- Israelson, C, et al.
(författare)
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Direct U-Th dating of organic- and carbonate-rich lake sediments from southern Scandinavia
- 1997
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Ingår i: EARTH AND PLANETARY SCIENCE LETTERS. - : ELSEVIER SCIENCE BV. ; 153:3-4, s. 251-263
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Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
- U-Th ages of Holocene lacustrine sediments from southern Sweden have been determined to assess the reliability of this technique for dating climatic events from the last interglacial-glacial-interglacial cycle, and for calibration of the C-14 dating metho
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