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@Article{LimaJ˙niorCoheRossFran:2018:LaPlGl,
               author = "Lima J{\'u}nior, W. J. S. and Cohena, M. C. L. and Rossetti, 
                         Dilce de F{\'a}tima and Fran{\c{c}}a, M. C.",
          affiliation = "{Universidade Federal do Par{\'a} (UFPA)} and {Universidade 
                         Federal do Par{\'a} (UFPA)} and {Instituto Nacional de Pesquisas 
                         Espaciais (INPE)} and {Universidade Federal do Par{\'a} (UFPA)}",
                title = "Late pleistocene glacial forest elements of Brazilian Amazonia",
              journal = "Palaeogeography, Palaeoclimatology, Palaeoecology",
                 year = "2018",
               volume = "490",
                pages = "617--628",
                month = "jan.",
             keywords = "Alnus, Climate change, Last Glacial Maximum, Palynology.",
             abstract = "Pollen data recovered from the sedimentary record of western 
                         Amazonia is still inadequate to fully address climate changes over 
                         the Last Glaciation in this region. The present work focuses 
                         vegetation dynamics from an area of southwestern Amazonia during 
                         the past 42,000 cal yr B.P. based on the integration of previous 
                         and new pollen data. Sediment cores were sampled from two sites 
                         covered by tropical rainforest in fluvial terraces of the Madeira 
                         River, a major southern Amazonian tributary. The results indicated 
                         a significant proportion of cold-adapted Andean tree species, 
                         represented by Alnus (020%), Hedyosmum (115%), Podocarpus (05%), 
                         Illex (111%) and Weinmannia (01%) at least between > 43,16342,018 
                         cal yr B.P. and 10,39410,240 cal yr B.P. During the Holocene, only 
                         pollen representative of herbs and modern Amazonian vegetation 
                         persisted. The new pollen record confirmed previous documented 
                         results that vegetation communities presently restricted to Andean 
                         areas at altitudes higher than 20003000 m, occupied this region of 
                         the Amazonian lowlands close to the onset and probably also during 
                         the Last Glacial Maximum.",
                  doi = "10.1016/j.palaeo.2017.11.050",
                  url = "http://dx.doi.org/10.1016/j.palaeo.2017.11.050",
                 issn = "0031-0182",
             language = "en",
           targetfile = "lima_late.pdf",
        urlaccessdate = "29 nov. 2020"
}


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