Benthic foraminiferal distribution on the southeastern Brazilian shelf and upper slope
Contribuinte(s) |
UNIVERSIDADE DE SÃO PAULO |
---|---|
Data(s) |
20/10/2012
20/10/2012
2011
|
Resumo |
Foraminiferal data were obtained from 66 samples of box cores on the southeastern Brazilian upper margin (between 23.8A degrees-25.9A degrees S and 42.8A degrees-46.13A degrees W) to evaluate the benthic foraminiferal fauna distribution and its relation to some selected abiotic parameters. We focused on areas with different primary production regimes on the southern Brazilian margin, which is generally considered as an oligotrophic region. The total density (D), richness (R), mean diversity (H) over bar`, average living depth (ALD(X) ) and percentages of specimens of different microhabitats (epifauna, shallow infauna, intermediate infauna and deep infauna) were analyzed. The dominant species identified were Uvigerina spp., Globocassidulina subglobosa, Bulimina marginata, Adercotryma wrighti, Islandiella norcrossi, Rhizammina spp. and Brizalina sp.. We also established a set of mathematical functions for analyzing the vertical foraminiferal distribution patterns, providing a quantitative tool that allows correlating the microfaunal density distributions with abiotic factors. In general, the cores that fit with pure exponential decaying functions were related to the oligotrophic conditions prevalent on the Brazilian margin and to the flow of the Brazilian Current (BC). Different foraminiferal responses were identified in cores located in higher productivity zones, such as the northern and the southern region of the study area, where high percentages of infauna were encountered in these cores, and the functions used to fit these profiles differ appreciably from a pure exponential function, as a response of the significant living fauna in deeper layers of the sediment. One of the main factors supporting the different foraminiferal assemblage responses may be related to the differences in primary productivity of the water column and, consequently, in the estimated carbon flux to the sea floor. Nevertheless, also bottom water velocities, substrate type and water depth need to be considered. Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP, Brazilian agency)[06/59947-3] Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP, Brazilian agency)[03/10740-0] |
Identificador |
MARINE BIOLOGY, v.158, n.1, p.159-179, 2011 0025-3162 http://producao.usp.br/handle/BDPI/32061 10.1007/s00227-010-1549-7 |
Idioma(s) |
eng |
Publicador |
SPRINGER |
Relação |
Marine Biology |
Direitos |
restrictedAccess Copyright SPRINGER |
Palavras-Chave | #DEEP-SEA #CONTINENTAL-MARGIN #ATLANTIC-OCEAN #MICROHABITAT PREFERENCES #ORGANIC-CARBON #OXYGEN-CONTENT #SAGAMI-BAY #CABO FRIO #ASSEMBLAGES #SEDIMENTS #Marine & Freshwater Biology |
Tipo |
article original article publishedVersion |