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@Article{BusoJrPOGCVOTRLBSBFGS:2013:PaEvCo,
               author = "Buso Junior, Antonio Alvaro and Pessenda, Luiz Carlos Ruiz and 
                         Oliveira, Paulo Eduardo de and Giannini, Paulo C{\'e}sar Fonseca 
                         and Cohen, Marcelo Cancela Lisboa and Volkmer-Ribeiro, 
                         Cec{\'{\i}}lia and Oliveira, Sonia Maria Barros de and Teixeira 
                         Favaro, Deborah Ines and Rossetti, Dilce de Fatima and Lorente, 
                         Fl{\'a}vio Lima and Borotti Filho, Marcos Antonio and Schiavo, 
                         Jolimar Antonio and Bendassolli, Jos{\'e} Albertino and 
                         Fran{\c{c}}a, Marlon Carlos and Guimar{\~a}es, Jos{\'e} Tasso 
                         Felix and Siqueira, Geovane Souza",
          affiliation = "Center for Nuclear Energy in Agriculture (CENA/USP), Brazil and 
                         Center for Nuclear Energy in Agriculture (CENA/USP), Brazil and 
                         S{\~a}o Francisco University, Brazil and Instituto de 
                         Geoci{\^e}ncias da Universidade de S{\~a}o Paulo, Brazil and 
                         Federal University of Par{\'a}, Brazil and Funda{\c{c}}{\~a}o 
                         Zoobot{\^a}nica do Rio Grande do Sul, Brazil and Instituto de 
                         Geoci{\^e}ncias da Universidade de S{\~a}o Paulo, Brazil and 
                         Instituto de Pesquisas Energ{\'e}ticas e Nucleares, Brazil and 
                         {Instituto Nacional de Pesquisas Espaciais (INPE)} and Center for 
                         Nuclear Energy in Agriculture (CENA/USP), Brazil and Center for 
                         Nuclear Energy in Agriculture (CENA/USP), Brazil and Universidade 
                         Estadual de Mato Grosso do Sul, Brazil and Center for Nuclear 
                         Energy in Agriculture (CENA/USP), Brazil and Instituto de 
                         Geoci{\^e}ncias, Univ. Federal do Par{\'a} (UFPA), Brazil and 
                         Instituto de Geoci{\^e}ncias, Univ. Federal do Par{\'a} (UFPA), 
                         Brazil and Vale Nature Reserve, Brazil",
                title = "From an estuary to a freshwater lake: A paleo-estuary evolution in 
                         the context of holocene sea-level fluctuations, SE Brazil",
              journal = "Radiocarbon",
                 year = "2013",
               volume = "55",
               number = "2-3",
                pages = "1735--1746",
                 note = "{Proceedings of the 21st International Radiocarbon Conference}",
             keywords = "basin analysis, coastal zone, estuarine ecosystem, flooding, 
                         floodplain, Holocene, ocean basin, sea level change, valley, 
                         Brazil.",
             abstract = "A sediment core was studied to characterize the influences of 
                         Holocene sea-level variations in the Barra Seca River valley, in 
                         the Atlantic rainforest, Linhares, Esp{\'{\i}}rito Santo, 
                         southeastern Brazil. Biological proxies (pollen, spores, and 
                         sponge spicules), 14C dating, granulometry, 13C, 15N, C/N and 
                         major chemical elements revealed the establishment and the 
                         evolution of a paleo-estuary during the interval from ~7700-585 
                         cal BP. During the interval ~7700-7000 cal BP, the study site was 
                         occupied by a bay-head delta, the inner portion of the 
                         paleo-estuary, presenting the most dense mangrove coverage of the 
                         entire record. In the interval ~7000-3200 cal BP, the site was 
                         occupied by the central basin, possibly a consequence of the 
                         landward migration of the paleo-estuary. This interval presents 
                         reduced mangrove coverage, probably due to the permanent flooding 
                         of the valley. From ~3200 cal BP, the marine influence at the site 
                         decreased probably as result of the seaward migration of the coast 
                         line. From ~600 cal BP, the modern floodplain and freshwater lake 
                         were established. This interpretation is in agreement with the 
                         sea-level curves for the southeastern Brazilian coast, except for 
                         the fact that evidence of sea levels lower than the present at 
                         ~4000 and ~2500 cal BP as suggested by some authors were not 
                         found.",
                  doi = "10.2458/azu_js_rc.55.16210",
                  url = "http://dx.doi.org/10.2458/azu_js_rc.55.16210",
                 issn = "0033-8222",
                label = "scopus 2013-11",
             language = "en",
           targetfile = "16210-23017-3-PB.pdf",
        urlaccessdate = "20 jan. 2021"
}


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