Holocene offshore tsunami archive-Tsunami deposits on the Algarve shelf (Portugal)

被引:9
|
作者
Feist, Lisa [1 ]
Costa, Pedro J. M. [2 ,3 ]
Bellanova, Piero [1 ]
Bosnic, Ivana [2 ]
Santisteban, Juan I. [4 ]
Andradeb, Cesar [2 ]
Brueckner, Helmut [5 ]
Duarte, Joao F. [6 ]
Kuhlmann, Jannis [7 ]
Schwarzbauer, Jan [8 ]
Voett, Andreas [9 ]
Reicherter, Klaus [1 ]
机构
[1] Rhein Westfal TH Aachen, Inst Neotecton & Nat Hazards, Aachen, Germany
[2] Univ Lisbon, Fac Ciencias, Inst D Luiz, Lisbon, Portugal
[3] Univ Coimbra, Fac Sci & Technol, Dept Earth Sci, Coimbra, Portugal
[4] Univ Complutense Madrid, Fac Geol Sci, Dept Geodynam Stratig & Paleontol, Madrid, Spain
[5] Univ Cologne, Inst Geog, Dept Geosci, Cologne, Germany
[6] Inst Hidrog, Div Geol Marinha, Lisbon, Portugal
[7] Univ Bremen, Res Fac, Ctr Marine Environm Sci, MARUM, Bremen, Germany
[8] Rhein Westfal TH Aachen, Inst Geol & Geochem Petr & Coal, Lab Organ Geochem Anal, Aachen, Germany
[9] Johannes Gutenberg Univ Mainz, Inst Geog, Nat Hazard Res & Geoarchaeol Grp, Mainz, Germany
关键词
Tsunami backwash; Offshore tsunami deposits; Continental shelf; 1755 CE Lisbon tsunami; INNER CONTINENTAL-SHELF; LAST GLACIAL MAXIMUM; PALEOENVIRONMENTAL CHANGES; SEDIMENT CORES; EVENT LAYERS; SENDAI BAY; VS; STORM; SEA-LEVEL; KHAO LAK; COAST;
D O I
10.1016/j.sedgeo.2023.106369
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The well-known 1755 CE Lisbon tsunami caused widespread destruction along the Iberian and northern Moroccan coastlines. Being affected by the powerful 1755 CE Lisbon tsunami, the southwestern Algarve shelf provides environ-ments for detecting offshore tsunami imprints. Our multidisciplinary investigations (hydroacoustics, sedimentology, geochemistry, radiocarbon dating) of the Holocene sediments have revealed tsunami deposits linked to this tsunami and a ca. 3600 cal yr BP event. The latter event is until now unidentified in Portugal. Both event deposits contrast with the background shelf sedimentation by their coarser grain size, element composition, internal structure, and erosive base, making them discernible in the sub-bottom data and cores. Especially the ca. 3600 cal yr BP deposit is excep-tionally well-preserved at one of the coring sites. The clear differentiation into several sections enables further in-sights into offshore tsunami transport and depositional processes. This study demonstrates that the record and preservation of tsunami deposits were possible on the Algarve shelf in specific locations sheltered from possible al-terations. Our findings extend the tsunami catalogs of Portugal with a previously unknown tsunami dated to ca. 3600 cal yr BP.(c) 2023 Elsevier B.V. All rights reserved.
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页数:20
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