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Träfflista för sökning "WFRF:(Possnert G.) srt2:(1995-1999)"

Sökning: WFRF:(Possnert G.) > (1995-1999)

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1.
  • Birks, HH, et al. (författare)
  • The Krakenes late-glacial palaeoenvironmental project
  • 1996
  • Ingår i: JOURNAL OF PALEOLIMNOLOGY. - : KLUWER ACADEMIC PUBL. ; 15:3
  • Annan publikation (övrigt vetenskapligt/konstnärligt)abstract
    • Krakenes is the site of a small lake on the west coast of Norway that contains a long sequence of late-glacial sediments. The Younger Dryas is well represented, as a cirque glacier developed in the catchment at this time. This site offers unique opportuni
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3.
  • Bjorck, S, et al. (författare)
  • Synchronized terrestrial-atmospheric deglacial records around the North Atlantic
  • 1996
  • Ingår i: SCIENCE. - : AMER ASSOC ADVANCEMENT SCIENCE. - 0036-8075. ; 274:5290, s. 1155-1160
  • 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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4.
  • Eriksson, JA, et al. (författare)
  • An improved method for preparing a pollen concentrate suitable for C-14-dating
  • 1996
  • Ingår i: GRANA. - : SCANDINAVIAN UNIVERSITY PRESS. - 0017-3134. ; 35:1, s. 47-50
  • Tidskriftsartikel (refereegranskat)abstract
    • An improved procedure for preparing a pollen concentrate from clayey sediments is presented. Two new steps have been added compared with earlier procedures. Firstly an initial dispersion which enhances the pollen yield from a sample so that a smaller amou
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5.
  • Wohlfarth, B, et al. (författare)
  • Pitfalls in the AMS radiocarbon-dating of terrestrial macrofossils
  • 1998
  • Ingår i: JOURNAL OF QUATERNARY SCIENCE. - : JOHN WILEY & SONS LTD. - 0267-8179. ; 13:2, s. 137-145
  • Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
    • The AMS C-14 technique has the advantage that small samples of Late Quaternary age can be dated with high accuracy, and that errors due to reservoir effects can be avoided if specifically determined terrestrial micro- and macrofossils are measured. Howeve
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8.
  • Aldahan, AA, et al. (författare)
  • Be-10 records from sediments of the Arctic Ocean covering the past 350 ka
  • 1997
  • Ingår i: MARINE GEOLOGY. - : ELSEVIER SCIENCE BV. - 0025-3227. ; 144:1-3, s. 147-162
  • Tidskriftsartikel (refereegranskat)abstract
    • Records of Be-10, Be-9, mineralogy and grain size were obtained from two cores collected by the Polarstern Expedition 1991 in the southern Nansen Basin (Core 2213-6) and the Yermak Plateau (Core 2208-2). The accumulation of sediments examined started from
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11.
  • Aldahan, A, et al. (författare)
  • Sixty year Be-10 record from Greenland and Antarctica
  • 1998
  • Ingår i: PROCEEDINGS OF THE INDIAN ACADEMY OF SCIENCES-EARTH AND PLANETARY SCIENCES. - : INDIAN ACADEMY SCIENCES. - 0253-4126. ; 107:2, s. 139-147
  • Tidskriftsartikel (refereegranskat)abstract
    • We report in this study the distribution of Be-10 in the top 40 m of the Renland ice core (East Greenland) and in a 30 m long core from DML (Dronning Maud Land, Antarctica) for the period 1931-1988. The two sites show differences in Be-10 content, the Ant
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13.
  • Birks, H.H., et al. (författare)
  • The Kråkenes Late-glacial Palaeoenvironmental Project.
  • 1996
  • Ingår i: Journal of Paleolimnology. - 0921-2728 .- 1573-0417. ; 15:3, s. 281-286
  • Tidskriftsartikel (refereegranskat)abstract
    • Krakenes is the site of a small lake on the west coast of Norway that contains a long sequence of late-glacial sediments. The Younger Dryas is well represented, as a cirque glacier developed in the catchment at this time. This site offers unique opportunities to reconstruct late-glacial environments from independent sources of evidence; physical evidence (glacial geomorphology, sedimentology, palaeomagnetism, radiocarbon dating), and biological evidence from the remains of animals and plants derived from both the terrestrial and aquatic ecosystems. This report describes the background to the site, and the international multidisciplinary project to reconstruct late-glacial and early Holocene environmental and climatic changes at Krakenes.
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14.
  • Birks, HH, et al. (författare)
  • New radiocarbon dates for the Vedde ash and the Saksunarvatn ash from western Norway
  • 1996
  • Ingår i: QUATERNARY RESEARCH. - : ACADEMIC PRESS INC JNL-COMP SUBSCRIPTIONS. ; 45:2, s. 119-127
  • Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
    • The Vedde Ash Bed (mid-Younger Dryas) and the Saksunarvatn Ash (early Holocene) are important regional stratigraphic event markers in the North Atlantic, the Norwegian Sea, and the adjacent land area, It is thus essential to date them as precisely as poss
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15.
  • BJORCK, S, et al. (författare)
  • C-14 AMS MEASUREMENTS FROM THE LATE WEICHSELIAN PART OF THE SWEDISH TIME-SCALE
  • 1995
  • Ingår i: QUATERNARY INTERNATIONAL. - : PERGAMON-ELSEVIER SCIENCE LTD. ; 27, s. 11-18
  • 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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16.
  • Björck, S., et al. (författare)
  • Synchronized terrestrial-atmospheric deglacial records around the North Atlantic.
  • 1996
  • Ingår i: Science. - : American Association for the Advancement of Science (AAAS). - 0036-8075 .- 1095-9203. ; 274:5290, s. 1155-1160
  • Tidskriftsartikel (refereegranskat)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 the present. A 150-year-long cooling in the early Preboreal, associated with rising Delta(14)C values, is evident in all records and indicates an ocean ventilation change. This cooling is similar to earlier deglacial coolings, and box-model calculations suggest that they all may have been the result of increased freshwater forcing that inhibited the strength of the North Atlantic heat conveyor, although the Younger Dryas may have begun as an anomalous meltwater event.
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17.
  • Buraglio, N, et al. (författare)
  • Distribution and inventory of I-129 in the central Arctic Ocean
  • 1999
  • Ingår i: GEOPHYSICAL RESEARCH LETTERS. - : AMER GEOPHYSICAL UNION. - 0094-8276. ; 26:8, s. 1011-1014
  • Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
    • The concentration of I-129 was measured in water samples from three depth profiles collected in the central Arctic Ocean during 1996. The results indicate >7x10(8) atoms/liter in the cold, low salinity, 100-m-deep surface layer, and 0.06x10(8) atoms/liter
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18.
  • Goslar, T, et al. (författare)
  • Variations of atmospheric C-14 concentrations over the Allerod-Younger Dryas transition
  • 1999
  • Ingår i: CLIMATE DYNAMICS. - : SPRINGER VERLAG. - 0930-7575. ; 15:1, s. 29-42
  • 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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19.
  • Greenwood, AD, et al. (författare)
  • Nuclear DNA sequences from late Pleistocene megafauna
  • 1999
  • Ingår i: MOLECULAR BIOLOGY AND EVOLUTION. - : SOC MOLECULAR BIOLOGY EVOLUTION. - 0737-4038. ; 16:11, s. 1466-1473
  • Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
    • We report the retrieval and characterization of multi- and single-copy nuclear DNA sequences from Alaskan and Siberian mammoths (Mammuthus primigenius). In addition, a nuclear copy of a mitochondrial gene was recovered. Furthermore, a 13,000-year-old grou
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20.
  • Gulliksen, S, et al. (författare)
  • A calendar age estimate of the Younger Dryas-Holocene boundary at Krakenes, western Norway
  • 1998
  • Ingår i: HOLOCENE. - : ARNOLD, HODDER HEADLINE PLC. - 0959-6836. ; 8:3, s. 249-259
  • Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
    • The Younger Dryas/Holocene transition (YD/H) in the sediments of Krakenes Lake, western Norway, is well marked both lithologically and palaeobiologically at 756.5 cm in the investigated core. A series of 70 AMS radiocarbon dates on terrestrial plant macro
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21.
  • Hammarlund, Dan, et al. (författare)
  • Multi-component carbon isotope evidence of early Holocene environmental change and carbon-flow pathways from a hard-water lake in northern Sweden
  • 1997
  • Ingår i: Journal of Paleolimnology. - 0921-2728. ; 18:3, s. 219-233
  • Tidskriftsartikel (refereegranskat)abstract
    • A 9000-year carbonate-rich sediment sequence from a small hard-water lake in northernmost Sweden was studied by means of multi-component stable carbon isotope analysis. Radiocarbon dating of different sediment fractions provides chronologic control and reveals a rather constant hard-water effect through time, suggesting lake has remained hydrologically open throughout the Holocene. Successive depletion of C-13 in fine-grained calcite and carbonate shells during the early Holocene correlate with a change in catchment vegetation from pioneer herb communities to boreal forest. The vegetational change and associated soil development likely gave rise to an increased supply of C-13-depleted carbon dioxide in groundwater recharging the lake. This process is therefore believed to be the main cause of decreasing values of delta(13)C in dissolved inorganic carbon of the lake and thereby in limnic carbonates. Strongly C-13-depleted sedimentary organic matter may be related to enhanced kinetic fractionation during photosynthetic assimilation by means of proton pumping in Characean algae. This interpretation is supported by a substantial offset between delta(13)C of DIC as recorded by mollusc shells and delta(13)C Of fine-grained calcite.
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23.
  • Israelson, C, et al. (författare)
  • Direct U-Th dating of organic- and carbonate-rich lake sediments from southern Scandinavia
  • 1997
  • Ingår i: EARTH AND PLANETARY SCIENCE LETTERS. - : ELSEVIER SCIENCE BV. ; 153:3-4, s. 251-263
  • 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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24.
  • Jungner, H, et al. (författare)
  • Use of bomb-produced C-14 to evaluate the amount of CO2 emanating from two peat bogs in Finland
  • 1995
  • Ingår i: RADIOCARBON. - : UNIV ARIZONA DEPT GEOSCIENCES. ; 37:2, s. 567-573
  • Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
    • We used moss increment counting to obtain well-defined samples of the topmost peat layers of two Sphagnum fuscum hummocks. The two ombrotrophic bogs, Lakkasuo in central Finland and Korvinsuo in eastern Finland, are of different ages, covering 3 and 9 ka,
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  • Resultat 1-25 av 36

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