{"id":1901,"date":"2011-07-28T09:01:50","date_gmt":"2011-07-28T12:01:50","guid":{"rendered":"http:\/\/www.labec.com.br\/biodigital\/?page_id=1901"},"modified":"2011-07-28T09:01:50","modified_gmt":"2011-07-28T12:01:50","slug":"plataforma-continental-do-nordeste","status":"publish","type":"page","link":"http:\/\/www.labec.com.br\/biodigital\/ambientes\/plataforma-continental\/plataforma-continental-do-nordeste\/","title":{"rendered":"Plataforma Continental do Nordeste"},"content":{"rendered":"<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"font-size: small;\">A Plataforma Continental Nordestina,\u00a0 segundo o Projeto REVIZEE (1995), localiza-se entre o Delta do Rio Parna\u00edba (PI) e Salvador (BA). Ela \u00e9 caracteriza pela predomin\u00e2ncia de sedimentos biog\u00eanicos carbon\u00e1ticos e pela reduzida largura e profundidade, apresentando o talude mais abrupto do Atl\u00e2ntico.<\/p>\n<p>Conforme a defini\u00e7\u00e3o de COUTINHO, encontra-se dividida em:<\/span><\/span><\/p>\n<ul>\n<li>\n<div style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"font-size: small;\">Plataforma interna (at\u00e9 20m de profundidade): coberta por areia terr\u00edgena, com pouco cascalho e lama, e baixo teor em carbonato de c\u00e1lcio. Seu relevo \u00e9 suave, com poucas irregularidades.<\/span><\/span><\/div>\n<\/li>\n<li>\n<div style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"font-size: small;\">Plataforma m\u00e9dia (de 20 a 40 m de profundidade): coberta por sedimentos grosseiros de origem biog\u00eanica, com alto teor de carbonato de c\u00e1lcio. Seu relevo apresenta-se mais irregular.<\/span><\/span><\/div>\n<\/li>\n<li>\n<div style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"font-size: small;\">Plataforma externa (a partir de 40 m de profundidade): coberta com areias biodetr\u00edricas, cascalho, algas e lama, com alto teor de carbonato de c\u00e1lcio. Os sedimentos terr\u00edgenos s\u00e3o, predominantemente, rel\u00edquias, com algumas exce\u00e7\u00f5es nas desembocaduras dos rios, onde ocorre sedimenta\u00e7\u00e3o moderna.<\/span><\/span><\/div>\n<\/li>\n<\/ul>\n<p><span style=\"font-family: comic sans ms,sans-serif;\">\u00a0<\/span><\/p>\n<p><span style=\"font-family: comic sans ms,sans-serif;\">\u00a0<\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\"><strong>Refer\u00eancias Bibliogr\u00e1ficas:<\/strong><br \/>\nAGUIAR, J. E.; MARINS, R. V.; ALMEIDA, M. D. Compara\u00e7\u00e3o de metodologias de digest\u00e3o de sedimentos marinhos para caracteriza\u00e7\u00e3o da geoqu\u00edmica de metais-tra\u00e7o na Plataforma Continental Nordeste Oriental Brasileira. In: Geochimica Brasiliensis. Instituto de Ci\u00eancias do Mar-Labomar\/UFC, 2007.\u00a0 Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.biogeoquimicaufc.com.br\/publicacoes\/Artigos_Drude\/27_Geochimica_Brasiliensis.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.biogeoquimicaufc.com.br\/publicacoes\/Artigos_Drude\/27_Geochimica_Brasiliensis.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 20 jan. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">ARA\u00daJO, H. M. P.; RIBEIRO, V. A. Distribui\u00e7\u00e3o das esp\u00e9cies de Chaetognatha na Plataforma Continental de Sergipe e Alagoas. Braz. J. Aquat. Sci. Technol. 2005. Dispon\u00edvel em: &lt;www6.univali.br\/seer\/index.php\/bjast\/article\/download\/570\/482&gt;. Acesso em: 02 fev. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">BAPTISTA NETO, J. A. e SILVA, C. G. Morfologia do Fundo Oce\u00e2nico. In: BAPTISTA NETO, J. A.; PONZI, V. R. A.; SICHEL, S. E. (orgs.). Introdu\u00e7\u00e3o \u00e0 Geologia Marinha. Interci\u00eancia, Rio de Janeiro, 2004.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">BARRETO, A. V.; COELHO, P. A.; PORTO, M. R. Distribui\u00e7\u00e3o geogr\u00e1fica dos Brachyura (Crustacea, Decapoda) coletados na Plataforma Continental do Norte e Nordeste do Brasil. Rev. Bras. Zool., Curitiba, v. 10, n. 4, 1993. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.scielo.br\/scielo.php?pid=S0101-81751993000400010&amp;script=sci_arttext\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.scielo.br\/scielo.php?pid=S0101-81751993000400010&amp;script=sci_arttext<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 07 jan. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">CARVALHO, M. E. S. ; FONTES, A. L. . Caracteriza\u00e7\u00e3o geomorfol\u00f3gica da zona costeira do estado de Sergipe. In: SIMP\u00d3SIO NACIONAL DE GEOMORFOLOGIA, VI, 2006, GOI\u00c2NIA &#8211; GO. ANAIS\/RESUMOS. GOIANIA, 2006. v. 1. p. 154. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.labogef.iesa.ufg.br\/links\/sinageo\/index\/articles\/254.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.labogef.iesa.ufg.br\/links\/sinageo\/index\/articles\/254.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 28 dez. 2010.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">COUTINHO, P. N. Sedimenta\u00e7\u00e3o na Plataforma Continental de Alagoas-Sergipe. Arq. Ci\u00eancias do Mar, 21 (1\/2) p. 1-18. Dez. Fortaleza, Cear\u00e1, Brasil, 1981.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">CUNHA, S. B.; GUERRA, A. J. T. (Orgs.) Geomorfologia do Brasil. Rio de Janeiro: Bertrand Brasil, 2003.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">ESKINAZI-LE\u00c7A, E.; NEUMANN-LEIT\u00c3O, S.; COSTA, M. F.. (Orgs.) Oceanografia: um cen\u00e1rio tropical. Universidade Federal de Pernambuco. Centro de Tecnologia e Geoci\u00eancias. Departamento de Oceanografia. Recife: Baga\u00e7o, 2004.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">FONTES, A. L.; SANTOS, M. A.; LIMA, E. S.; CORREIA, A. L. F. Caracteriza\u00e7\u00e3o sedimentar e morfodin\u00e2mica do litoral Norte do estado de Sergipe &#8211; Contribui\u00e7\u00e3o ao ordenamento territorial. In: SIMP\u00d3SIO NACIONAL DE GEOMORFOLOGIA, VI, 2006, GOI\u00c2NIA &#8211; GO. ANAIS\/RESUMOS. GOIANIA, 2006. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.labogef.iesa.ufg.br\/links\/sinageo\/aut\/articles\/257.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.labogef.iesa.ufg.br\/links\/sinageo\/aut\/articles\/257.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 27 jan. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">GUIMAR\u00c3ES, C. R. P. Composi\u00e7\u00e3o e distribui\u00e7\u00e3o dos sedimentos superficiais e da fauna b\u00eantica na Plataforma Continental de Sergipe. Tese de Doutorado. P\u00f3s-Gradua\u00e7\u00e3o em Geologia: Geologia Marinha, Costeira e Sedimentar. Instituto de Geoci\u00eancias. Universidade Federal da Bahia. Salvador-BA, 2010.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">LACERDA, L. D.; MARINS, R. V. Geoqu\u00edmica de Sedimentos e Monitoramento de metais na plataforma continental nordeste oriental do Brasil. In: Geochemica Brasiliensis. Fortaleza, CE, 2006. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.institutomilenioestuarios.com.br\/pdfs\/Produtos\/005\/Produto_PDF_5.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.institutomilenioestuarios.com.br\/pdfs\/Produtos\/005\/Produto_PDF_5.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 10 jan 2009.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">MANSO, V. A. V.; CORR\u00caA, I. C. S.; GUERRA, N. C. Morfologia e Sedimentologia da Plataforma Continental Interna entre as Praias Porto de Galinhas e Campos &#8211; Litoral Sul de Pernambuco, Brasil. Instituto de Geoci\u00eancias, UFRGS. Porto Alegre\/RS, 2003. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.pesquisasemgeociencias.ufrgs.br\/3002\/02-3002.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.pesquisasemgeociencias.ufrgs.br\/3002\/02-3002.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 06 jan. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">PIRES, A. M. S. Structure and dynamics of benthic megafauna on the continental shelf offshore of Ubatuba, southeastern Brazil. Mar. Ecol. Prog. Ser., Vol. 86: 63-76. 1992. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.int-res.com\/articles\/meps\/86\/m086p063.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.int-res.com\/articles\/meps\/86\/m086p063.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 01 fev. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">SANTOS, M. A.; FONTES, A. L. Abordagem preliminar da morfodin\u00e2mica costeira, an\u00e1lise sedimentar e caracteriza\u00e7\u00e3o de uso do solo do Munic\u00edpio de Barra dos Coqueiros\/Sergipe. In: SIMP\u00d3SIO NACIONAL DE GEOMORFOLOGIA, VI, 2006, GOI\u00c2NIA &#8211; GO. ANAIS\/RESUMOS. GOIANIA, 2006. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.labogef.iesa.ufg.br\/links\/sinageo\/aut\/articles\/241.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.labogef.iesa.ufg.br\/links\/sinageo\/aut\/articles\/241.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 12 jan. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">SHEPARD, F. P, 1973. Submarine Geology. Harper and Row, New York. 3 rd ed., 517 pp.<br \/>\nVILELA, C. G. 2004. Foramin\u00edferos. In: CARVALHO, I.S. Paleontologia. Rio de Janeiro: Interci\u00eancia.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">SILVA, E. N. S. A Sedimenta\u00e7\u00e3o na Plataforma Continental do Munic\u00edpio de Conde (Litoral Norte da Bahia) desde o \u00faltimo m\u00e1ximo glacial: Integra\u00e7\u00e3o de dados sedimentol\u00f3gicos e geof\u00edsicos. Monografia (Gradua\u00e7\u00e3o em Geologia). Instituto de Geoci\u00eancias. Universidade Federal da Bahia. Salvador-BA, 2008. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.ici.ufba.br\/twiki\/pub\/IGeo\/GeolMono20081\/elisa_silva_2008.pdf\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.ici.ufba.br\/twiki\/pub\/IGeo\/GeolMono20081\/elisa_silva_2008.pdf<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 27 jan. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">SOUZA, J. M. de. Mar territorial, zona econ\u00f4mica exclusiva ou plataforma continental?. Rev. Bras. Geof.,\u00a0 S\u00e3o Paulo,\u00a0 v. 17,\u00a0 n. 1, Mar.\u00a0 1999.\u00a0\u00a0 Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.scielo.br\/scielo.php?script=sci_arttext&amp;pid=S0102-261X1999000100007&amp;lng=en&amp;nrm=iso\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.scielo.br\/scielo.php?script=sci_arttext&amp;pid=S0102-261X1999000100007&amp;lng=en&amp;nrm=iso<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 11\u00a0 jan.\u00a0 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">VITAL, H.; GOMES, M. P.; TABOSA, W. F.; FRAZ\u00c3O, E. P.; SANTOS, PL\u00c1CIDO J\u00daNIOR, C. L. A.; J. S. Characterization of the Brazilian Continental Shelf adjacent to Rio Grande do Norte state, NE, Brazil. Brazilian Journal of Oceanography, S\u00e3o Paulo, v. 58, 2010. Dispon\u00edvel em: &lt;<\/span><\/span><\/span><a href=\"http:\/\/www.scielo.br\/scielo.php?pid=S1679-87592010000500005&amp;script=sci_arttext\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">http:\/\/www.scielo.br\/scielo.php?pid=S1679-87592010000500005&amp;script=sci_arttext<\/span><\/span><\/span><\/a><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">&gt;. Acesso em: 01 fev. 2011.<\/span><\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"color: #999999;\"><span style=\"font-size: x-small;\">Cunha, E. M. S. Considera\u00e7\u00f5es Gerais Sobre A Zona Costeira.<\/span><\/span><\/span><\/p>\n<p><span style=\"font-family: comic sans ms,sans-serif;\">\u00a0<\/span><\/p>\n<p><span style=\"font-family: comic sans ms,sans-serif;\">\u00a0<\/span><\/p>\n<p style=\"text-align: center;\"><span style=\"font-family: comic sans ms,sans-serif;\"><span style=\"font-size: medium;\"><strong><a href=\"http:\/\/www.labec.com.br\/biodigital\/ambientes\/plataforma-continental\"><span style=\"color: #808000;\">VOLTAR<\/span><\/a><\/strong><\/span><\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>A Plataforma Continental Nordestina,\u00a0 segundo o Projeto REVIZEE (1995), localiza-se entre o Delta do Rio Parna\u00edba (PI) e Salvador (BA). Ela \u00e9 caracteriza pela predomin\u00e2ncia de sedimentos biog\u00eanicos carbon\u00e1ticos e pela reduzida largura e profundidade, apresentando o talude mais abrupto do Atl\u00e2ntico. Conforme a defini\u00e7\u00e3o de COUTINHO, encontra-se dividida em: Plataforma interna (at\u00e9 20m de [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":119,"menu_order":0,"comment_status":"open","ping_status":"open","template":"","meta":{"ngg_post_thumbnail":0},"_links":{"self":[{"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/pages\/1901"}],"collection":[{"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/comments?post=1901"}],"version-history":[{"count":2,"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/pages\/1901\/revisions"}],"predecessor-version":[{"id":1903,"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/pages\/1901\/revisions\/1903"}],"up":[{"embeddable":true,"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/pages\/119"}],"wp:attachment":[{"href":"http:\/\/www.labec.com.br\/biodigital\/wp-json\/wp\/v2\/media?parent=1901"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}