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• W2053102815 abstract "Research Article| January 01, 2005 FORAMINIFERAL ZONATIONS AS BASE LINES FOR QUATERNARY SEA-LEVEL FLUCTUATIONS IN SOUTH-SOUTHEAST BRAZILIAN MANGROVES AND MARSHES Cãtia F. Barbosa; Cãtia F. Barbosa 1Departamento de Oceanografia/Universidade Federal de Per-nambuco, Av. Arquitetura s/n, 50740-550, Recife, PE, Brazil. E-mail: catia@geoq.uff.br *Present Address: Departamento de Geoquímica/Universidade Federal Fluminense, Outeiro de São João Batista, s/no. 5o, Centro, Niterói, R.J. 24020-007, Rio de Janeiro. Search for other works by this author on: GSW Google Scholar David B. Scott; David B. Scott 2Centre for Marine Geology, Dalhousie University, Halifax, Nova Scotia B3H3J5 Canada. Search for other works by this author on: GSW Google Scholar José C. S. Seoane; José C. S. Seoane 3Departamento de Geologia/Universidade Federal do Rio de Janeiro/IGEO/CCMN, Cep: 21949-900, Rio de Janeiro, RJ, Brazil. Search for other works by this author on: GSW Google Scholar Bruno J. Turcq Bruno J. Turcq 4Centre IRD, d’Ile de France—32, avenue Henri Varagnat, 93143 Bondy cedex, France. *Present Address: Departamento de Geoquímica/Universidade Federal Fluminense, Outeiro de São João Batista, s/no. 5o, Centro, Niterói, R.J. 24020-007, Rio de Janeiro. Search for other works by this author on: GSW Google Scholar Author and Article Information Cãtia F. Barbosa *Present Address: Departamento de Geoquímica/Universidade Federal Fluminense, Outeiro de São João Batista, s/no. 5o, Centro, Niterói, R.J. 24020-007, Rio de Janeiro. 1Departamento de Oceanografia/Universidade Federal de Per-nambuco, Av. Arquitetura s/n, 50740-550, Recife, PE, Brazil. E-mail: catia@geoq.uff.br David B. Scott 2Centre for Marine Geology, Dalhousie University, Halifax, Nova Scotia B3H3J5 Canada. José C. S. Seoane 3Departamento de Geologia/Universidade Federal do Rio de Janeiro/IGEO/CCMN, Cep: 21949-900, Rio de Janeiro, RJ, Brazil. Bruno J. Turcq *Present Address: Departamento de Geoquímica/Universidade Federal Fluminense, Outeiro de São João Batista, s/no. 5o, Centro, Niterói, R.J. 24020-007, Rio de Janeiro. 4Centre IRD, d’Ile de France—32, avenue Henri Varagnat, 93143 Bondy cedex, France. Publisher: Cushman Foundation for Foraminiferal Research Received: 21 Oct 2002 Accepted: 11 Apr 2004 First Online: 03 Mar 2017 Online ISSN: 1943-264X Print ISSN: 0096-1191 © 2005 Journal of Foraminiferal Research Journal of Foraminiferal Research (2005) 35 (1): 22–43. https://doi.org/10.2113/35.1.22 Article history Received: 21 Oct 2002 Accepted: 11 Apr 2004 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Cãtia F. Barbosa, David B. Scott, José C. S. Seoane, Bruno J. Turcq; FORAMINIFERAL ZONATIONS AS BASE LINES FOR QUATERNARY SEA-LEVEL FLUCTUATIONS IN SOUTH-SOUTHEAST BRAZILIAN MANGROVES AND MARSHES. Journal of Foraminiferal Research 2005;; 35 (1): 22–43. doi: https://doi.org/10.2113/35.1.22 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Foraminiferal Research Search Advanced Search Abstract Small vertical variations in occurrences of mangrove foraminifera and arcellaceans (thecamoebians) provide a zonation scheme that is applicable to the study of short-term sea-level change. Sampling along transects was carried out at three sites in southern Brazil and four sites along the Rio de Janeiro lagoon system. The Saí-Guaçú fluvial-estuarine point bar that divides the states of Santa Catarina and Paraná, and the Capinzal and Veiga islands at the ancient flood tidal delta of the Guaratuba Bay, were sampled during two summers for a total of 42 samples. In the state of Rio de Janeiro, the seaward borders of the Urussanga, Boqueirão and Fora lagoons, which comprise the incipient brackish mangroves of the Saquarema Lagoon system, were sampled in both summer and winter for a total of 17 samples. Three samples were collected during the summer at the freshwater marsh of Jacarepiá Lake. These coastal sedimentary environments differ in latitude, climate, physio-chemical conditions, vegetation, and sediment type. Altitude, rate of sediment transport and salinity influence the distribution of three faunal zones: higher, middle, and lower. Statistics on the dead foraminiferal distribution and ecological indications given by live occurrences showed that Haplophragmoides sp. is the dominant species at the uppermost stations (higher high water—HHW, with a 6-cm vertical range) in both Guaratuba and Rio de Janeiro transects, whereas Trochammina inflata dominates the southernmost Saí-Guaçú site. The Haplophragmoides-Trochammina association was also the most consistent in both dead and live HHW assemblages. Trochammina inflata and two forms of T. macrescens were found to be salinity-sensitive HHW assemblages, as were Polysaccammina hyperhalina and Miliammina fusca in the Guaratuba intertidal zone. In Saquarema, the intertidal zone is marked by T. macrescens, and Centropyxis aculeata predominates in Jacarepiá. The subtidal zone in Paraná contains Arenoparrella mexicana, Tiphotrocha comprimata, Trochammina macrescens f. macrescens, and Difflugia oblonga, whereas in Rio de Janeiro, T. macrescens f. polystoma predominates.Similar HHW assemblages are also observed in Oregon, British Columbia, Maritime Canada, and New England. Thus, the assemblages found in Brazil are potentially applicable to the study of sea-level variation as recorded in Quaternary deposits, like their counterparts in temperate marshes. These transects are the first well-constrained vertical transects of mangrove faunas in South America. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2053102815 title "FORAMINIFERAL ZONATIONS AS BASE LINES FOR QUATERNARY SEA-LEVEL FLUCTUATIONS IN SOUTH-SOUTHEAST BRAZILIAN MANGROVES AND MARSHES" @default.
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