Biodiversity of decapod crustaceans in the estuarine floodplain around the city of Belém (Pará) in Brazilian Amazonia

The present study focused on the decapod fauna of the fluvial-estuarine environment of the Guajará Bay, in the Brazilian state of Pará, where specimens were collected monthly from six sites, from May 2006 to April 2007. A total of 6,793 specimens were captured, belonging to 11 species of crab and sh...

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Bibliographic Details
Authors: CAVALCANTE, Danielle Viveiros, SILVA, Bianca Bentes da, MARTINELLI-LEMOS, Jussara Moretto
Format: article
Status:Published version
Publication Date:2012
Country:Brasil
Institution:Universidade Federal do Pará (UFPA)
Repository:Repositório Institucional da UFPA
Language:English
OAI Identifier:oai:repositorio.ufpa.br:2011/4416
Online Access:http://repositorio.ufpa.br/jspui/handle/2011/4416
Access Level:Open access
Keyword:Crustáceo
Decápode (Crustáceo)
Diversidade
Baía do Guajará - PA
Ilha de Mosqueiro - PA
Ilha de Arapiranga - PA
Icoaraci - PA
Ilha do Combu - PA
Estuários
Belém - PA
Pará - Estado
Amazônia brasileira
Description
Summary:The present study focused on the decapod fauna of the fluvial-estuarine environment of the Guajará Bay, in the Brazilian state of Pará, where specimens were collected monthly from six sites, from May 2006 to April 2007. A total of 6,793 specimens were captured, belonging to 11 species of crab and shrimp: eight palaemonids - Macrobrachium amazonicum (Heller, 1862), Macrobrachium surinamicum Holthuis, 1948, Macrobrachium carcinus (Linnaeus, 1758), Macrobrachium rosenbergii (De Man, 1879), Macrobrachium spp. 1-4 -, one portunid - Callinectes bocourti A. Milne-Edwards, 1879 -, and two trichodactylids - Sylviocarcinus devileii H. Milne-Edwards, 1853 and Sylviocarcinus pictus (Milne-Edwards, 1853). While no significant differences were found in the ecological indices of diversity with respect to season, site, or trap size, a tendency for increased abundance and species richness was found during the dry season (August-November), in particular at some sites, apparently reflecting the influence of the estuary's saline wedge.