Registro sedimentario en marmitas de erosión fluvial. Río Miño, Ourense

• Miguel Ángel Álvarez Vázquez ^[1] ; Alexandra María Ramírez Pérez ^[1] ; Elena de Uña Álvarez ^[1] ; Esther de Blas Varela ^[1] ; Ricardo Prego Reboredo ^[2]
  1. [1] Universidade de Vigo

     Universidade de Vigo

     Vigo, España

     
  2. [2] Instituto de Investigacións Mariñas

     Instituto de Investigacións Mariñas

     Vigo, España

     
• Localización: XV Reunión Nacional de Cuaternario Bizkaia Aretoa: Bilbao, 1-5 julio 2019. Libro de resúmenes, 2019, ISBN 978-84-17713-16-4, págs. 206-209
• Idioma: español
• Enlaces
  • Texto Completo Libro
• Resumen

  • The capacity of fluvial potholes to trap sediments led to the hypothesis that these deposits could serve as historical records. A sediment core, obtained from an erosion pothole, wasstudied. 11 samples (22 cm depth) were obtained. The 210Pb dating indicated that, in general, the pothole was gradually filled in the last 33-35 years. Using trace metals as indicators (Cu, Pb and V) it was possible to estimate their natural background (61±27 mgCu·kg-1, 72±45 mgPb·kg-1 and 19±4 mgV·kg-1). After calculating the normalized enrichment factor (NEF), the core showed indexes indicative of possible-moderate contamination for Cu and Pb (average contents 141±45 mgCu·kg-1 and 141±46 mgPb·kg-1), particularly in a layer (1993-2009) that seems to be a mixture of sediments of different ages, coinciding in time with humaninterventions in the local environment. Sediments trapped in potholes (as traps) showed potential to be used as historical records.