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

Sökning: WFRF:(Lemdahl G) > (1995-1999)

  • Resultat 1-10 av 12
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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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2.
  • 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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3.
  • 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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4.
  • 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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5.
  • Coope, G.R., et al. (författare)
  • Regional differences in the Lateglacial climate of northern Europe based on coleopteran analysis.
  • 1995
  • Ingår i: Journal of Quaternary Science. - : Wiley. - 0267-8179 .- 1099-1417. ; 10:4, s. 391-395
  • Tidskriftsartikel (refereegranskat)abstract
    • The termination of the Last Glaciation, the Lateglacial period, was characterised by highly unstable climates which, in northern Europe, oscillated between warm temperate and arctic conditions. Different indicators of past climate have provided contrasting views an the timing and intensity of these climatic changes. Here we present preliminary reconstructions of the thermal climate interpreted from subfossil coleopteran assemblages from Britain, Norway, Sweden and Poland, in which regional differences can be ascribed to the varying influence of, (a) the North Atlantic surface water temperatures, (b) the proximity of the Fennoscandian ice sheet and (c) the ice free continent. Quantification of the thermal climate enables these local differences to be resolved.
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6.
  • Coope, G.R., et al. (författare)
  • Temperature gradients in northern Europe during the last glacial-Holocene transition (14-9 14C kyr BP) interpreted from coleopteran assemblages.
  • 1998
  • Ingår i: Journal of Quaternary Science. - 0267-8179 .- 1099-1417. ; 13:5, s. 419-433
  • Tidskriftsartikel (refereegranskat)abstract
    • Late-glacial and early Holocene climatic conditions have been reconstructed for northern Europe using the mutual climatic range (MCR) palaeoclimate method based on fossil coleopteran assemblages. Altogether, beetle faunas from 77 sites have been analysed ranging from Ireland in the west to Poland and Finland in the east, and MCR estimates calculated. The results are plotted on 16 maps, each representative of a selected time-slice covering the period from 14.5 C-14 kyr BP to 9.0 C-14 kyr BP. Eight of the maps show the MCR estimates of T-max (mean temperature of the warmest month) derived from each site for which data are available, while the remainder show estimated T-max isotherms interpolated from these values. It can be demonstrated that at times the thermal climate was fairly uniform throughout the study area, whereas at others temperature gradients were much steeper than they are in the region today. There also appears to be a distinct contrast between cold periods, when contours trended NW-SE, and warmer periods, when contours trend W-E or even NE-SW. The pattern of climatic changes that emerges is shown to be very different from the traditional view that has been used up to now as a template for classifying Late-glacial climatic events on a wide, even global, scale. The suddenness and intensity of changes in the thermal climate may have been partially responsible for an apparent lack of equilibrium between the flora and fauna of the time and the physical environment in which they lived.
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8.
  • Hellqvist, M, et al. (författare)
  • Insect assemblages and local environment in the mediaeval town of Uppsala, Sweden
  • 1996
  • Ingår i: JOURNAL OF ARCHAEOLOGICAL SCIENCE. - : ACADEMIC PRESS LTD. - 0305-4403. ; 23:6, s. 873-881
  • Tidskriftsartikel (refereegranskat)abstract
    • Insect remains from a mediaeval settlement in the town of Uppsala, S. Sweden, were analysed. Eighty-one insect taxa were identified from samples dating from the 12th to the 15th century. The insect assemblages are totally dominated by beetles. Only a few
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  • Resultat 1-10 av 12

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