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Sökning: WFRF:(Aunina Liene)

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1.
  • Jiroušek, Martin, et al. (författare)
  • Classification of European bog vegetation of the Oxycocco‐Sphagnetea class
  • 2022
  • Ingår i: Applied Vegetation Science. - : Wiley. - 1402-2001 .- 1654-109X. ; 25:1, s. 1-19
  • Tidskriftsartikel (refereegranskat)abstract
    • Aims: Classification of  European bog   vegetation (Oxycocco- Sphagnetea class);    iden  -tification of  diagnostic species for   the   class    and   vegetation subgroups (orders and alliances); development of  an  expert     system for   automatic classification of  vegetation plots; and production of distribution maps of the Oxycocco- Sphagnetea class and its alliances.Location: Europe.Methods: A  data   set   of  vegetation- plot   records was   compiled to  include various bog types    over    most    of  the   European continent. An   unsupervised classification (beta- flexible linkage    method, Sørensen distance measure) and  detrended correspondenceanalysis (DCA)    ordination were    applied. Formal definitions of  syntaxa based    on  spe -cies  presence  and  covers,  and  respecting  the  results  of  the  unsupervised  classifica-tion, were developed and included in a classification expert system.Results: The Oxycocco- Sphagnetea class,    its  two   orders (Sphagno- Ericetalia  tetralicisand Sphagnetalia medii)  and   seven    compositionally distinct alliances were    formally de -fined.    In  addition to  the   syntaxa included in  EuroVegChecklist, three    new    alliances were distinguished: Rubo chamaemori- Dicranion elongati (subarctic polygon and   palsa mires);    Erico mackaianae- Sphagnion papillosi (blanket bogs   of  the  northwestern IberianPeninsula); and  Sphagno  baltici- Trichophorion  cespitosi (boreal bog   lawns). The   latter alliance is newly described in this article.Conclusions: This   first   pan-   European formalized classification of  European bog   veg -etation partially followed the   system presented in  EuroVegChecklist, but   suggested three  additional  alliances.  One  covers  palsa  and  polygon  mires,  one  covers  Iberian  bogs    with    endemics and   one   fills   the   syntaxonomical gap   for   lawn    microhabitats in boreal    bogs.    A  classification expert     system has   been   developed, which    allows    assign   -ment of vegetation plots to the types described.
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2.
  • Sim, Thomas G., et al. (författare)
  • Regional variability in peatland burning at mid-to high-latitudes during the Holocene
  • 2023
  • Ingår i: Quaternary Science Reviews. - : Elsevier. - 0277-3791 .- 1873-457X. ; 305
  • Tidskriftsartikel (refereegranskat)abstract
    • Northern peatlands store globally-important amounts of carbon in the form of partly decomposed plant detritus. Drying associated with climate and land-use change may lead to increased fire frequency and severity in peatlands and the rapid loss of carbon to the atmosphere. However, our understanding of the patterns and drivers of peatland burning on an appropriate decadal to millennial timescale relies heavily on individual site-based reconstructions. For the first time, we synthesise peatland macrocharcoal re-cords from across North America, Europe, and Patagonia to reveal regional variation in peatland burning during the Holocene. We used an existing database of proximal sedimentary charcoal to represent regional burning trends in the wider landscape for each region. Long-term trends in peatland burning appear to be largely climate driven, with human activities likely having an increasing influence in the late Holocene. Warmer conditions during the Holocene Thermal Maximum (similar to 9e6 cal. ka BP) were associated with greater peatland burning in North America's Atlantic coast, southern Scandinavia and the Baltics, and Patagonia. Since the Little Ice Age, peatland burning has declined across North America and in some areas of Europe. This decline is mirrored by a decrease in wider landscape burning in some, but not all sub-regions, linked to fire-suppression policies, and landscape fragmentation caused by agricultural expansion. Peatlands demonstrate lower susceptibility to burning than the wider landscape in several instances, probably because of autogenic processes that maintain high levels of near-surface wetness even during drought. Nonetheless, widespread drying and degradation of peatlands, particularly in Europe, has likely increased their vulnerability to burning in recent centuries. Consequently, peatland restoration efforts are important to mitigate the risk of peatland fire under a changing climate. Finally, we make recommendations for future research to improve our understanding of the controls on peatland fires.(c) 2023 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
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