Multi-proxy Analysis of the AD 1755 Lisbon Tsunami Deposits in El Palmar de Vejer, Spain
-
Frenken, Mike [1] ; Cämmerer, Christoph [1] ; Bellanova, Piero [1] ; Feist, Lisa [1] ; Chaumet, Max [1] ; Raith, Kira [2] ; Schulte, Philipp [1] ; Lehmkuhl, Frank [1] ; Schwarzbauer, Jan [1] ; Reicherter, Klaus [1]
-
[1] Rheinisch-Westfälische Technische Hochschule Aachen University
Rheinisch-Westfälische Technische Hochschule Aachen University
Städteregion Aachen, Alemania
-
[2] Oxford Brookes University
Oxford Brookes University
Oxford District, Reino Unido
-
- Localización: Historical Earthquakes,Tsunamis and Archaeology in the Iberian Peninsula / coord. por Manuel Álvarez Martí-Aguilar, Francisco Machuca Prieto, 2022, ISBN 978-981-19-1978-7, págs. 389-427
- Idioma: inglés
- Texto completo no disponible (Saber más ...)
-
Resumen
The study area, El Palmar de Vejer, located in the Gulf of Cadiz in southwestern Spain, was severely struck by the AD 1755 Lisbon tsunami. El Palmar de Vejer was chosen as the study area due to the topographical setting, characterized by the flat alluvial floodplain, which has good preconditions as a sedimentary archive for tsunami deposits in order togain a better understanding of the effects of the Lisbon tsunami based on previous studies and historical descriptions. The sedimentological and geochemical features indicate the processes of successive tsunami wash-overs and subsequent backwash and ponding conditions. An analysis of the major elements revealed a distinction between marine and terrestrial depositional environments. Using organic geochemistry, several different natural compounds were detected (e.g., n-alkanes and n-aldehydes), as well as some anthropogenic compounds (polycyclic aromatic hydrocarbons).The results suggest a differentiation between the AD 1755 tsunami deposit and the lagoonal background sediments, thus making it possible to identify tsunami processes. The results of this study analyzing the sedimentary archive provide strong evidence that a multi-proxy approach, with the inclusion of geochemical applications, can confidently detect tsunami deposits, distinguish them from the surrounding background sediments andsubsequently characterize their internal structure and composition.
