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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Archaeological geology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (850 pages)
    Edition: 1st ed.
    ISBN: 9780128156872
    DDC: 551.4637072
    Language: English
    Note: Front Cover -- Geological Records of Tsunamis and Other Extreme Waves -- Geological Records of Tsunamis and Other Extreme Waves -- Copyright -- Contents -- Contributors -- About the Editors -- Preface -- 1 -Introduction -- 1 - Geological records of tsunamis and other extreme waves: concepts, applications and a short history of research -- Introduction -- Disciplinary background -- A short history of paleotsunami research -- Scope of the book -- Outline of the book -- Concluding remarks -- References -- 2 - Historical records: their importance in understanding and mitigating tsunamis -- Introduction -- Catalogues and databases -- Historical records: importance and limitation -- References -- 3 - Tsunami magnitude scales -- Introduction -- Tsunami magnitude scales: an overview -- Relation between tsunami magnitude and intensity -- Possibilities and limitations of tsunami magnitude scales -- Applicability of tsunami magnitude, Mt, to the case of October 25, 2018, earthquake -- Discussion and conclusions -- References -- 4 - Trigger mechanisms and hydrodynamics of tsunamis -- Trigger mechanisms -- Earthquakes -- Landslides -- Volcanism -- Impacts -- Complex trigger -- Hydrodynamics -- Propagation of tsunamis -- Wave deformation in shallow waters (shoaling) -- Inundation and runup -- Backwash -- References -- 5 - Tsunami databases -- Introduction -- Definition -- Database development -- Problems -- Challenges to creating a global tsunami database -- Paleotsunami data -- Structure -- Definition -- Validity -- Other attributes -- Opportunities -- References -- 6 - Onshore archives of tsunami deposits -- Introduction -- Onshore archives of tsunami deposits -- Low-lying coastal plains -- Marshes and estuaries -- Swales within beach-ridge plains -- Lagoons -- Coastal lakes -- Coastal sediment sections -- Beaches (back-beach environments) -- Caves. , Summary -- References -- 2 -Field methods -- 7 - Geophysical prospection and sedimentological characteristics of subaquatic tsunami deposits -- Introduction -- Why do we need research on offshore tsunami deposits? -- Methods to detect offshore tsunami deposits -- Sidescan sonar -- Multibeam echosounder -- Reflection seismic -- LiDAR measurements -- Sampling of offshore tsunami deposits -- Diagnostic criteria of offshore tsunami deposits -- Distribution of offshore tsunami deposits: case studies from different regions -- Conclusions -- References -- 8 - Ground-penetrating radar (GPR) in coastal hazard studies -- Introduction -- The GPR technique -- Theory of GPR and its application in coastal environments -- Data collection and processing -- Recent advancements -- Types of surveys -- Processing -- GPR use in studying past storms and tsunamis -- Erosional records -- Other research areas of methodology development -- Thin-bed studies -- Use of amplitude variation with offset (AVO) -- Multiconfiguration surveys -- Attribute analysis -- 3D modeling of GPR data -- Conclusions -- References -- 9 - Mapping of subaerial coarse clasts -- Introduction -- Aerial and satellite imagery -- Single-point to multi-point measurements -- Photogrammetry and Structure-from-Motion -- Laser scanning -- Point-cloud analysis -- Summary -- References -- 10 - Post-event field surveys -- Introduction and aims -- Overview of how to approach the development, deployment and activity of a post-event field survey -- Before the survey -- During the survey -- After the survey -- Summary reflections on the tasks/issues associated with organizing and undertaking a post-event field survey -- On the evolving "tool kit" of methods available to support post-event field surveys, including those from the broader geolo. , Reflections on the tensions and challenges a post-event field survey team leader might encounter -- Meeting my own and other's expectations -- Time -- Dealing with the unexpected -- Difficult emotions -- Conclusions -- References -- 3 -Fine-grained deposits -- 11 - The sedimentology and geometry of fine-grained tsunami deposits from onshore environments -- Introduction -- Methods -- Fine-grained onshore tsunami deposits -- Depositional features -- Horizontal trends -- Grain-size distribution -- Stratification -- Accumulation of components -- Vertical structures -- Asymmetrical structures that indicate flow direction -- Soft-sediment deformation -- Erosional features -- Discussion -- Conclusions -- References -- 12 - Foraminifera in tsunami deposits -- Characteristics of coastal foraminifera -- Field methods -- Modern foraminifera sampling -- Tsunami and paleotsunami foraminifera sampling -- Laboratory methods -- Sample preparation and foraminiferal analysis -- Foraminifera taxonomy -- Foraminifera test size -- Foraminifera taphonomy -- Statistical techniques -- Example application of foraminifera to tsunami studies -- Current challenges -- Summary of foraminifera use in tsunami research -- References -- 13 - Ostracoda in extreme-wave deposits -- Introduction -- Who are the Ostracoda? -- Taxonomy -- Distribution -- Preservation and taphonomy -- Methods -- Field-based methods -- Baseline ostracod fauna and ecologies -- Deposit sampling -- Lab-based methods -- Post-laboratory methods -- Distinguishing between overwash mechanisms -- Conclusions -- References -- 14 - Diatoms in tsunami deposits -- Introduction: physical and ecological characteristics of diatoms -- Diatoms in tsunami deposits -- Allochthonous diatoms in tsunami deposits, indicators for sediment provenance -- Diatoms as indicators of tsunami runup extent. , Sorting of diatom valves in tsunami deposits -- Preservation of diatom valves in tsunami deposits -- Comparison of diatoms in tsunami and storm-surge deposits -- Recommendations for investigating a candidate tsunami deposit -- Field work and data collection -- Laboratory processing and analyses -- Appendix 1: common diatoms reported in tsunami deposits -- Appendix 2: published criteria for identifying tsunami deposits using diatoms -- Appendix 3: diatom slide preparation and counting -- Appendix 4: assessment of diatom preservation -- References -- 15 - The application of molluscs for investigating tsunami deposits -- Introduction -- The use of molluscs in paleotsunami research -- Characteristics of mollusc species assemblages in tsunami deposits -- Paleo-current flow direction -- Infaunality as a proxy for erosion depth -- Shell size -- Taphonomic processes -- Shell material -- Taphonomic characteristics -- Differences between coastal and offshore settings -- Geochemical analysis -- Differentiating between tsunami and storm deposits -- Conclusions -- References -- 16 - Magnetic susceptibility and anisotropy of magnetic susceptibility: versatile tools to decipher hydrodynamic ch ... -- Introduction -- The principles of the anisotropy of magnetic susceptibility -- Magnetic susceptibility of tsunami deposits -- Anisotropy of magnetic susceptibility -- Methodology -- Sediment sampling in the field -- Caution and limits -- Sediment sampling in the laboratory -- Field experiments -- Laboratory measurements -- Contribution of MS/AMS to deciphering tsunami deposits -- Environmental magnetism of tsunami deposits -- Magnetic signatures of tsunami deposits -- Limitations and perspectives -- Contribution of AMS to reconstruct the hydrodynamic conditions for the 2004 Indian Ocean Tsunami flooding at Banda Aceh, Su ... -- Limitations of the method -- Conclusions. , References -- 17 - X-ray tomography applied to tsunami deposits -- Principles of X-ray tomography -- Application to tsunami deposits -- Sampling strategy -- Image analysis -- X-ray anatomy of tsunami deposits -- Internal structure of the deposit and bedforms -- Soft and fine-grained fraction: soil and mud -- Vertical trends of grain size -- Sedimentary fabric -- Distribution of heavy minerals -- Distribution of marine bioclasts -- Conclusions -- References -- 18 - Applications of geochemical proxies in paleotsunami research -- Introduction -- Methods -- Field sampling -- Analytical methods -- Examples and significance of geochemical proxies -- Onshore deposits -- Marine indicators (shell hash, marine carbonate, also seawater) -- Indicators of source material (proxy for mineral composition) -- Grain-size indicator (Zr/K, Rb and K, Si/(K+Ti)) -- Seawater influence and post-diagenetic formation of pyrite (TC, TS, Fe and S) -- Indicator of source material (terrestrial vs. marine/beach) and geochronological marker -- Stable isotopes and C/N -- Biomarkers/organic compounds -- DNA -- Offshore deposits -- Current challenges and potentialities -- Conclusions -- References -- 19 - Microtextures in tsunami deposits: a useful sediment fingerprinting tool -- Introduction -- Methodology -- Laboratory procedure -- Microtextural semi-quantitative classification -- Shape analysis -- Automated microtextural classification -- Case studies -- Boca do Rio (Portugal) -- Arauco and Mataquito (Chile) -- Conclusions -- References -- 20 - Paleogenetic approaches in tsunami deposit studies -- Background -- Pioneering metabarcoding applications in paleotsunami research -- Protocols for sampling and analysis -- Sediment sampling and storage -- Establishment of databases and significance of reference material -- DNA extraction procedures. , Polymerase chain reaction (PCR) and development of specific PCR primers.
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  • 2
    Keywords: Archaeological geology ; Tsunamis Research ; Tsunami ; Sediment ; Sedimentation ; Fazies ; Sedimentologie ; Angewandte Geophysik ; Sturmflut ; Tempestit ; Paläoseismologie ; Paläoseismizität ; Feinstratigraphie ; Biostratigraphie ; Tempestit ; Elektromagnetische Reflexionsmethode ; Fossil ; Geochronologie ; Lidar ; Seebeben ; Tempestit ; Stratigraphie
    Type of Medium: Book
    Pages: xxxi, 816 Seiten , Illustrationen, Diagramme, Karten , 24 cm
    ISBN: 9780128156865
    DDC: 551.4637072
    RVK:
    Language: English
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  • 3
    Keywords: Geschichte
    In: Geographische Rundschau 〈Braunschweig〉, Braunschweig : Westermann Bildungsmedien Verlag GmbH, 1949, 61(2009), 12, Seite 12-18, 0016-7460
    In: Geographische Rundschau 61.2009,12, 61(2009), 12, Seite 12-18
    In: volume:61
    In: year:2009
    In: number:12
    In: pages:12-18
    Type of Medium: Article
    ISSN: 0016-7460
    Language: German
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  • 4
    Publication Date: 2022-10-13
    Description: Abstract Sabkhas are key landforms along the southern coast of the Arabian Gulf and represent modern analogues for depositional and diagenetic processes controlling properties and quality of ancient hydrocarbon‐bearing carbonates. While previous investigations of coastal sabkhas in Qatar have mainly focused on dolomitization processes, presented here is one of the first studies reconstructing facies changes and coastal formation in great detail. In the sabkha of Al‐Kharayej (Gulf of Salwa), fifteen different facies types were distinguished based on twelve sediment cores, two trenches, as well as grain‐size distribution, X‐ray powder diffraction, thin section and microfossil analyses. Age estimates were based on seventy‐eight 14C‐AMS and optically stimulated luminescence data. The sabkha parasequence comprises pre‐transgressive dune sands, a thin, transgressive layer of reworked dune material, a mid‐energy open‐coast to open‐lagoon facies, a low‐energy lagoon facies, saline lake facies (salina: swallow‐tail gypsum and gypsum mush) and the supratidal sabkha characterized by diagenetic overprinting (buckled gypsum crusts and halite crust). Transgressive marine flooding created open‐coast to open‐lagoon sedimentation after ca 7000 cal yr bp, followed by initial spit formation at the northern sabkha end at the beginning of the relative sea‐level highstand (6000 cal yr bp). This main outer spit prograded southward and a more narrow, low‐energy spit, diverted landward, closing a small lagoon in the northern sabkha 4500 to 4000 cal yr bp. The falling relative sea‐level and longshore drift intensified the southward extension and widening of the main spit, and the main lagoon became more shallow. At 2000 to 1500 cal yr bp, the outer spit had almost closed the main lagoon, leading to salina and, finally, sabkha conditions. It is shown how specific local conditions (coastline orientation; wind, wave, tidal energy, longshore drift; depositional relief; sediment sources) created a spit‐controlled sabkha that is genetically distinct from the classical model of shore‐perpendicular accumulation of coarser sediment during high tides or storms.
    Description: Universität zu Köln
    Description: ExxonMobil Research Qatar
    Description: Ruprecht Karls Universitaet Heidelberg
    Keywords: ddc:552.5
    Language: English
    Type: doc-type:article
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Journal of molecular medicine 19 (1940), S. 1177-1180 
    ISSN: 1432-1440
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Zusammenfassung 1. Es werden die heutigen Erkenntnisse über den Chemismus des Blutfarbstoffabbaues zu Gallenfarbstoff an Hand des Schrifttums kurz dargestellt. 2. Eigene quantitative Untersuchungen über die gekuppelte Oxydation von Hämoglobin und Ascorbinsäure durch O2 ergaben folgende Ergebnisse: a) Die maximale Ausbeute an Biliverdin beträgt 10% des Porphyrinanteiles des Hämoglobins. b) Die Katalase hat einen hemmenden Einfluß auf die Bildung von Verdohämoglobin aus Hämoglobin. c) Die Anlagerung und Abspaltung von O2 hat keinen Einfluß auf den Hämoglobinabbau zu Gallenfarbstoff. 3. Die Bedeutung unserer Untersuchungen für die Frage der Blutmauserung wird erörtert. Es ist wahrscheinlich, daß bereits primär neben den Gallenfarbstoffen Biliverdin und Bilirubin andere Pyrrolverbindungen entstehen.
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2021-02-08
    Description: Marine conglomerates at high elevation on the flanks of ocean islands are usually interpreted as evidence of mega-tsunamis generated by volcano flank collapses, although their origin is sometimes debated (elevated littorals vs. tsunami). In this review, we introduce case studies of well-documented examples of tsunami conglomerates in Hawaii (Pacific Ocean), the Canary and Cape Verde Islands (Atlantic Ocean), and Mauritius Island (Indian Ocean). Other less-documented marine conglomerates are also presented as tsunami candidates. Then, we build a comprehensive picture of the general characteristics of these conglomerates and the different methods that can be applied to date them. Different perspectives of research are proposed, especially on the use of tsunami conglomerates as proxies for better constraining numerical models of ocean island flank collapses and associated tsunamis. We also discuss the possible links between volcano growth, flank instability, and climate.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2024-01-14
    Description: Severe storm flooding poses a major hazard to the coasts of north‐western Europe. However, the long‐term recurrence patterns of extreme coastal flooding and their governing factors are poorly understood. Therefore, high‐resolution sedimentary records of past North Atlantic storm flooding are required. This multi‐proxy study reconstructs storm‐induced overwash processes from coastal lake sediments on the Shetland Islands using grain‐size and geochemical data, and the re‐analysis of historical data. The chronostratigraphy is based on Bayesian age–depth modelling using accelerator mass spectrometry 14 C and 137 Cs data. A high XRF‐based Si/Ti ratio and the unimodal grain‐size distribution link the sand layers to the beach and thus storm‐induced overwash events. Periods with more frequent storm flooding occurred 980–1050, 1150–1300, 1450–1550, 1820–1900 and 1950–2000 ce, which is largely consistent with a positive North Atlantic Oscillation mode. The Little Ice Age (1400–1850 ce ) shows a gap of major sand layers suggesting a southward shift of storm tracks and a seasonal variance with more storm floods in spring and autumn. Warmer phases shifted winter storm tracks towards the north‐east Atlantic, indicating a possible trend for future storm‐track changes and increased storm flooding in the northern North Sea region.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2021-07-21
    Description: The Laacher See volcano (LSV) is located at the western margin of the Neuwied Basin, the central part of the Middle Rhine Basin of Germany. Its paroxysmal Plinian eruption c. 13 ka ago (Laacher See event; LSE) deposited a complex tephra sequence in the Neuwied Basin, whilst the distal ashes became one of the most important chronostratigraphic markers in Central Europe. However, some other impacts on landscape formation have thus far been largely neglected, such as buried gully structures in the proximity of the LSV. In this contribution, we map and discuss the spatial extent of these landforms at the site Lungenkärchen c. 4 km south of the LSV based on geophysical prospection as well as contrasting pedo‐sedimentary characteristics of the gully infill (particle‐size distribution, bulk‐sediment density, thin‐section analysis, saturated hydraulic conductivity) and the surrounding soils and tephra layers. These data are combined with a luminescence‐ and carbon‐14 (14C)‐based age model that relates them to the LSE. It is demonstrated how these gullies seem to have been formed and rapidly infilled by rainfall and surface discharge both during and subsequent to the eruptive phase, with modern analog processes documented for the 1980 Mount St Helens eruption (Washington State, USA). Given the density of the gullies at the site and their deviating pedo‐sedimentary properties compared to the surrounding soils, we propose a significant influence on agricultural production in the proximity of the LSV, which remains to be tested in future studies. Finally, in contrast, gullies of similar lateral and vertical dimensions identified in post‐LSE reworked loess and tephra deposits of the Wingertsbergwand (close to the main study site and proximal to the LSV) have shown to be unrelated to the LSE and can either be attributed to periglacial processes at the Younger Dryas‐Preboreal transition or to linear incision during the early Holocene.
    Description: Linear subsurface gullies were identified close to the Laacher See volcano in magnetometer and ground‐penetrating radar prospection. Optically stimulated luminescence data indicate they incised during or shortly after the Laacher See event 13 ka ago. Pedo‐sedimentary characteristics of the gully infill differs from the surrounding regosols and brown earths, possibly influencing regional agricultural land use. image
    Description: University of Cologne http://dx.doi.org/10.13039/501100008001
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: 551 ; 554.3 ; Eifel ; ground‐penetrating radar (GPR) ; gully erosion ; Laacher See event (LSE) ; luminescence dating ; magnetometer prospection ; micromorphology ; tephra ; Wingertsbergwand
    Type: article
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  • 9
    Publication Date: 2022-04-01
    Description: In light of global warming and rising relative sea level (RSL), detailed reconstructions of RSL histories and their controlling processes are essential in order to manage coastal‐protection challenges. This study contributes to unravelling Holocene RSL change on the East Frisian North Sea coast in high resolution and with a new approach for the German Bight. For the first time, a transfer function (vertical error: 29.7 cm ≙ ~11% of the mean tidal range) for RSL change based on a combined training set of benthic foraminifers and ostracods from the back‐barrier tidal basin of Spiekeroog is applied to the Holocene record of the back‐barrier tidal basin of Norderney. The resulting RSL curve for the Norderney tidal basin is corrected for decompaction and shows a deceleration in RSL rise between 6000 and 5000 cal bp. The smallest possible error envelope (~1 m) results from the good suitability of salt‐marsh layers between 5000 and 4000 cal bp. The RSL curve provides an approach towards the closure of the common data gap of peat‐based curves for the southern North Sea related to a lack of basal peats in the youngest age range, and verifies regional differences in glacial isostatic adjustment.
    Description: Volkswagen Foundation http://dx.doi.org/10.13039/501100001663
    Description: Niedersächsisches Ministerium für Wissenschaft und Kultur http://dx.doi.org/10.13039/501100010570
    Keywords: ddc:551.468
    Language: English
    Type: doc-type:article
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