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Spatial and seasonal dynamics of elemental composition and mineralogy of intertidal and subtidal sediments in the Lima estuary (NW Portugal)

  • E. FernandesEmail author
  • N. Vitorino
  • M. J. Ribeiro
  • C. Teixeira
  • A. A. Bordalo
Original Paper
  • 69 Downloads

Abstract

In estuaries, the mineral distribution in the top sediment layer results from the combined effect of fluvial and coastal inputs and may present seasonal patterns owing to forcing, e.g., floods, storms, waves, and tides. Our main goal was to study the estuarine sedimentological components, including textural and geochemical parameters, in order to characterize the seasonal and spatial dynamics of subtidal and intertidal sediments in a highly energetic temperate estuary (River Lima, NW Portugal). Subtidal sediments were usually anoxic within the middle estuary and presented higher amounts of clay and silt than intertidal sediments. Oxygen, silicon, carbon, aluminum, and potassium were the most abundant elements. The amount of silicon and carbon was related to the clay and silt content of the sediments. The mineralogical composition of sediments reflected the lithology of the watershed, with the most representative minerals being quartz, microcline (k-alkaloid feldspar), and albite (plagioclase), in line with the results obtained in the elementary characterization. The lower stretches were particularly rich in iron silicates and anatase. No clear seasonal variation was found for sediment elemental and mineralogical compositions. Factor analysis explained 80% of the elemental origin, being 33% related to terrigenous origin, 24% to marine sediments, and 15% to anthropogenic inputs.

Keywords

Elemental composition Mineralogy Intertidal and subtidal sediments Seasons Lima estuary 

Notes

Acknowledgments

This work was partially funded by the Strategic Funding UID/Multi/04423/2019 through national funds provided by the Portuguese Science Foundation (FCT) and European Regional Development Fund (ERDF), in the framework of the program PT2020. C. Teixeira also acknowledges FCT for a post-doctoral grant (ref. SFRH/BPD/110730/2015) through POCH, co-founded by MCTES and the European Social Fund. The authors acknowledge all colleagues involved in sample collection. The SEM and XRD facilities were funded by FEDER Funds through QREN—Aviso SAIECT-IEC/2/2010, Operação NORTE-07-0162-FEDER-000050.

Supplementary material

12517_2019_4569_MOESM1_ESM.docx (1.3 mb)
ESM 1 (DOCX 1.26 mb)

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Copyright information

© Saudi Society for Geosciences 2019

Authors and Affiliations

  1. 1.Laboratory of Hydrobiology and Ecology, Institute of Biomedical Sciences (ICBAS)University of PortoPortoPortugal
  2. 2.School of Technology and ManagementPolytechnic Institute of Viana do Castelo (ESTG-IPVC)Viana do CasteloPortugal
  3. 3.Universidade de Aveiro (UA)AveiroPortugal
  4. 4.UIDM (Unidade de Investigação & Desenvolvimento em Materiais)—School of Technology and ManagementPolytechnic Institute of Viana do Castelo (ESTG-IPVC)Viana do CasteloPortugal
  5. 5.Centre of Marine and Environmental Research (CIIMAR)MatosinhosPortugal

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