@article{1195,
  keywords = {Ecology, Forestry, Geochronology, Plants (botany), Sedimentology, stratigraphy, vegetation, 14C dating, Alps, Europe, Historic timberline, Holocene thermal maximums, Holocenes, Palaeoecology, Paleoclimatology, vegetation dynamics, climate change, altitude, carbon isotope, climate conditions, coniferous forest, deglaciation, ecotone, glacier advance, historical record, Holocene, human activity, Hypsithermal, Middle Ages, paleoclimate, paleoecology, radiocarbon dating, stratigraphy, treeline, vegetation dynamics, vegetation history, Alps, Italy, Italy, Rutor Glacier, Valle d Aosta, Pinus cembra},
  author = {F. Badino and C. Ravazzi and F. Vallè and R. Pini and A. Aceti and M. Brunetti and E. Champvillair and V. Maggi and F. Maspero and R. Perego and G. Orombelli},
  title = {8800 years of high-altitude vegetation and climate history at the Rutor Glacier forefield, Italian Alps. Evidence of middle Holocene timberline rise and glacier contraction},
  year = {2018},
  journal = {Quaternary Science Reviews},
  url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85041821782&doi=10.1016%2fj.quascirev.2018.01.022&partnerID=40&md5=d01d7aa277f03ded376844b9aaaabe2b},
  doi = {10.1016/j.quascirev.2018.01.022},
}