@Article{LorentePOBRGCOMFFBM:2018:11ReDe,
               author = "Lorente, Fl{\'a}vio Lima and Pessenda, Luiz Carlos Ruiz and 
                         Oboh-Ikuenobe, Francisca and Buso Junior, Antonio Alvaro and 
                         Rossetti, Dilce de F{\'a}tima and Giannini, Paulo C{\'e}sar 
                         Fonseca and Cohen, Marcelo Cancela Lisboa and Oliveira, Paulo 
                         Eduardo de and Mayle, Francis Edward and Francisquini, Mariah Izar 
                         and Fran{\c{c}}a, Marlon Carlos and Bendassolli, Jos{\'e} 
                         Albertino and Macario, Kita",
          affiliation = "{Centro de Energia Nuclear em Agricultura (CENA)} and {Centro de 
                         Energia Nuclear em Agricultura (CENA)} and {Missouri University of 
                         Science and Technology} and {Centro de Energia Nuclear em 
                         Agricultura (CENA)} and {Instituto Nacional de Pesquisas Espaciais 
                         (INPE)} and {Universidade de S{\~a}o Paulo (USP)} and 
                         {Universidade Federal do Par{\'a} (UFPA)} and {Universidade de 
                         S{\~a}o Paulo (USP)} and {University of Reading} and {Centro de 
                         Energia Nuclear em Agricultura (CENA)} and {Instituto Federal do 
                         Par{\'a} (IFPA)} and {Centro de Energia Nuclear em Agricultura 
                         (CENA)} and {Universidade Federal Fluminense (UFF)}",
                title = "An 11,000-year record of depositional environmental change based 
                         upon particulate organic matter and stable isotopes (C and N) in a 
                         lake sediment in southeastern Brazil",
              journal = "Journal of South American Earth Sciences",
                 year = "2018",
               volume = "84",
                pages = "373--384",
                month = "July",
             keywords = "Holocene, Organic matter, Stable isotopes, Paleoenvironment, 
                         Palynofacies.",
             abstract = "The aim of this paper is to reconstruct an 11,000-year history of 
                         depositional environmental change in southeastern Brazil, based 
                         upon the integration of particulate organic matter and stable 
                         isotope (C and N) data from a 136-cm sediment core from Lake Canto 
                         Grande. These proxies are used to explore the evolution of 
                         terrestrial and marine influence on the lake. Isotopic 
                         (\δ13C: \−27.87 to \−31.9; \δ15N: 
                         \−0.074.9) and elemental (total organic carbon - TOC: 
                         0.58%37.19%; total nitrogen - TN: 0.08%1.73%; C/N: 0.3 to 54.7) 
                         values recorded in Lake Canto Grande suggest that the sedimentary 
                         organic matter was derived from mostly C3 land plants and 
                         freshwater phytoplankton. Particulate organic matter and cluster 
                         analyses distinguished four associations characterized by the 
                         predominance of amorphous organic matter, followed by phytoclasts 
                         and palynomorphs. These results indicate two different phases of 
                         lake evolution. The first phase (136 - 65 cm; \∼10,943 cal 
                         yr. B.P. to \∼8529 cal yr. B.P.) is recorded by sand layers 
                         interbedded with mud, which contain amorphous organic matter (AOM, 
                         4559%) and phytoclasts (opaques - OP: 618%; non-opaques NOP: 
                         1723%) which indicate a floodplain area. The second phase (650 cm; 
                         \∼8529 cal yr. B.P. to \∼662 cal yr. B.P.) comprises 
                         mud, AOM (6886%) and palynomorphs (PAL, 816%) related to lake 
                         establishment comparable to modern conditions. Thus, 
                         characterizing particulate organic matter, in combination with 
                         stable isotopes, proved to be invaluable proxies for lacustrine 
                         paleoenvironmental change through the Holocene.",
                  doi = "10.1016/j.jsames.2018.04.006",
                  url = "http://dx.doi.org/10.1016/j.jsames.2018.04.006",
                 issn = "0895-9811",
             language = "en",
           targetfile = "lorente_11.pdf",
        urlaccessdate = "27 abr. 2024"
}