Palaeoenvironmental data from fluvial deposits associated to ancient fishing weirs in the Miño river, NW Iberia

  1. JORGE SANJURJO-SÁNCHEZ 1
  2. CARLOS ARCE CHAMORRO 2
  3. VÍCTOR BARRIENTOS 2
  4. ANA GOY-DIZ 3
  1. 1 Instituto Universitario de Geología “Isidro Parga Pondal”. Universidad de A Coruña
  2. 2 Instituto Universitario de Geología “Isidro Parga Pondal”. Universidade de A Coruña
  3. 3 Universidade de Santiago de Compostela.Facultade de Humanidades
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Revista:
Cadernos do Laboratorio Xeolóxico de Laxe: Revista de xeoloxía galega e do hercínico peninsular

ISSN: 0213-4497

Año de publicación: 2020

Número: 42

Páginas: 53-68

Tipo: Artículo

DOI: 10.17979/CADLAXE.2020.42.0.7284 DIALNET GOOGLE SCHOLAR lock_openAcceso abierto editor

Otras publicaciones en: Cadernos do Laboratorio Xeolóxico de Laxe: Revista de xeoloxía galega e do hercínico peninsular

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Resumen

Fluvial sediments provide environmental records of the Quaternary. In some cases, fluvial deposits are caused by anthropogenic processes that cause changes in the water regime of some river stretches. This is the case of dams. It has been reported that some dams or partial damming systems existed in the past, at least from some thousands of years ago. Such dams were used for fishing purposes and are referred as fishing weirs. In a recently published work it has been demonstrated that a fluvial thick deposit was caused by a damming system in a river of NW Iberia (River Miño, Pontevedra). Optically stimulated luminescence (OSL) provided the burial age of such fluvial deposit, showing a 1300-year-old fluvial record. The sedimentation rates of the record did not match with known climate fluctuations in the area. In this work, the sedimentation phases of such record are identified, and the detrital and organic matter content is studied to assess any change occurred in the environmental and fluvial conditions during the deposition period of the record that ranges from 814±134 to 1837±11 AD.

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Fuente de los datos: Dialnet