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Marine Biology

, Volume 158, Issue 1, pp 159–179 | Cite as

Benthic foraminiferal distribution on the southeastern Brazilian shelf and upper slope

  • Leticia BuroneEmail author
  • Silvia Helena de Mello e Sousa
  • Michel Michaelovitch de Mahiques
  • Paulo Valente
  • Aurea Ciotti
  • Cíntia Yamashita
Original Paper

Abstract

Foraminiferal data were obtained from 66 samples of box cores on the southeastern Brazilian upper margin (between 23.8°–25.9°S and 42.8°–46.13°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 (\( \overline{{H^{\prime } }} \)), 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.

Keywords

Foraminifera Benthic Foraminifera Rose Bengal Foraminiferal Assemblage Brazilian Current 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

This work was supported by Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP, Brazilian agency) via a post-doctoral fellowship (Proc. No. 06/59947-3) provided to L.B and via grant No. 03/10740-0. We are grateful to Joachim Schönfeld for the helpful comments and suggestions. The authors also wish to thank Mr. Daniel P. Alves and Mr. Edilson Faria for their help in the laboratory with the sedimentological analyses. We also thank Mrs. Fabiana Barbosa for the calculation of the primary productivity values.

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© Springer-Verlag 2010

Authors and Affiliations

  • Leticia Burone
    • 1
    • 4
    Email author
  • Silvia Helena de Mello e Sousa
    • 1
  • Michel Michaelovitch de Mahiques
    • 1
  • Paulo Valente
    • 2
  • Aurea Ciotti
    • 3
  • Cíntia Yamashita
    • 1
  1. 1.Instituto OceanográficoUniversidade de São PauloSão PauloBrazil
  2. 2.Instituto de Física, Facultad de IngenieríaMontevideoUruguay
  3. 3.UNESP Campus do Litoral PaulistaSão VicenteBrazil
  4. 4.Facultad de Ciencias, Sección OceanologíaMontevideoUruguay

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