Foraminiferal biotopes and their distribution control in Ria de Aveiro (Portugal): a multiproxy approach |
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Authors: | Maria Virgínia Alves Martins Fabrizio Frontalini Lazaro L. M. Laut Frederico S. Silva João Moreno Silvia Sousa Noureddine Zaaboub Monia El Bour Fernando Rocha |
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Affiliation: | 1. Faculdade de Geologia, Departamento de Estratigrafia e Paleontologia, Universidade do Estado do Rio de Janeiro, Av. S?o Francisco Xavier, 524, sala 4037 F, Maracan?, 20550-013, Rio de Janeiro, RJ, Brasil 2. GeoBioTec, Dpto. Geociências, Universidade de Aveiro, Campus de Santiago, 3810-193, Aveiro, Portugal 3. CESAM, Dpto. Geociências, Universidade de Aveiro, Aveiro, Portugal 4. DiSTeVA, Facoltà di Scienze e Tecnologie, Università degli Studi di Urbino “Carlo Bo”, Urbino, Italy 5. Laboratório de Micropaleontologia – LabMicro, Universidade Federal do Estado do Rio de Janeiro – UNIRIO, Rio de Janeiro, Brasil 6. Laboratório de Palinofácies & Fácies Organicas – LAFO, Universidade Federal do Rio de Janeiro – UFRJ, Rio de Janeiro, Brasil 7. Faculdade de Ciências, Centro e Departamento de Geologia, Universidade de Lisboa, Campo Grande, 1749-016, Lisboa, Portugal 8. Instituo Oceanográfico, Universidade de S?o Paulo, S?o Paulo, Brasil 9. Institut des Sciences et Technologies de la Mer, Salammb?, Tunis, Tunisie
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Abstract: | Ria de Aveiro, which is located in the centre of Portugal (40° 38′ N, 8° 45′ W), is a well-mixed and complex coastal lagoon that is separated from the sea by a sandy barrier and connects with the Atlantic through an artificial inlet. Tidal currents are the main factor controlling the lagoon’s hydrodynamics and, to a great extent, the sedimentary dynamic. The inner lagoonal zones receive input from several rivers and experience the pressure caused by the accumulation of organic matter and pollutants (namely, trace metals) from diverse anthropic activities. This paper is the first piece of work aiming to recognize, characterize and explain the main benthic foraminiferal biotopes in Ria de Aveiro. To provide a broad overview of this kind of setting, our results are compared to those of previous published studies conducted in similar transitional environments. The research is based on an investigation of 225 sites spread throughout this ecosystem. Utilizing a statistical approach, this study analyses the details of dead benthic foraminiferal assemblages composed of 260 taxa, the texture and composition (mineralogical and geochemical) of the sediment and physicochemical data. On the basis of the results of R-mode and Q-mode cluster analyses, several different biotopes can be defined as marsh biotope/near-marsh biotope; marginal urban/marginal urban mixing biotope; inner-outer lagoon biotope or enclosed lagoon; outer lagoon biotope, mixed sub-biotope; and outer lagoon, marine sub-biotope. These biotopes are related to foraminifera assemblages and substrate type and are influenced by local currents, water depth, chemical and physicochemical conditions, river or oceanic proximity, and anthropogenic impact, as evidenced by the mapping of the six factor loadings of the principal component analysis conducted herein. Based on a similar methodology of analysis as that applied in previous studies in the Lagoon of Venice, comparable biotypes were identified in Lagoon of Aveiro. |
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