19th century environmental transformation of an industrialized estuary: the Avilés sedimentary record (Asturias, N Spain)

The Avilés estuary is one of the most important industrial ports in northern Spain, whose natural characteristics have been largely altered since the 1830s. Here, the environmental transformation of this estuary during the 19th century is explored using a multi-proxy approach including benthic foram...

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Detalles Bibliográficos
Autores: Gardoki Díaz, Jon, Cearreta Bilbao, Alejandro, García Artola, Ane, Irabien Gulias, María Jesús, Gómez Arozamena, José, Villasante Marcos, Víctor, Quijada, Emma
Tipo de recurso: artículo
Fecha de publicación:2022
País:España
Institución:Universidad del País Vasco
Repositorio:Addi. Archivo Digital para la Docencia y la Investigación
OAI Identifier:oai:addi.ehu.eus:10810/73035
Acceso en línea:http://hdl.handle.net/10810/73035
Access Level:acceso abierto
Palabra clave:foraminifera
sedimentology
geochemistry
reclamation
channeling.
Descripción
Sumario:The Avilés estuary is one of the most important industrial ports in northern Spain, whose natural characteristics have been largely altered since the 1830s. Here, the environmental transformation of this estuary during the 19th century is explored using a multi-proxy approach including benthic foraminiferal content, sedimentology (grain-size), trace metals and short-lived radionuclides (210Pb and 137Cs) analysed from a 50-cm-long sediment core and a surface sample collected from the middle part of the estuary in the Pedro Menéndez Channel. The obtained results provide evidence that indicate an evolution from a naturally-driven environment with high a marine influence towards a more restricted setting under brackish conditions. The observed environmental change is interpreted as being mostly derived from physical modifications linked to the marsh reclamation and channelling starting in 1833 and intensified since 1860. This study provides a preindustrial environmental reference framework for future studies in coastal areas of the NW Atlantic Iberian margin.