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  • 2020-2022  (2)
  • 1995-1999  (8)
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  • 1
    ISSN: 1573-0581
    Keywords: Deep-sea channel ; Mediterranean ; morphostructure ; Valencia Trough
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The 400 km long Valencia Channel occupies the axis of the Valencia Trough in the Northwestern Mediterranean. Four different types of seismic reflection profiles were used to analyze the morphology and structure of the Valencia Channel with regard to the role played by both margins, Balearic and Iberian, of the Valencia Trough. From a detailed morphoseismic analysis of the Valencia Channel, its upper, middle, and lower courses can be characterized as follows: (1) in the upper course, tributaries are short and only slightly incised, with recent mass-transport deposits occurring on the adjacent continental slopes; (2) in the middle course, the channel deepens, and tributary valleys merge into it; and (3) the lower course begins after a sudden change in the direction of the channel, has a meandering path, is flanked by levees, and is fed by some valleys. During the Pliocene and Quaternary, at least four erosional and filling phases are observed in seismic profiles of the lower course of the Valencia Channel. The varying intensity of mass-transport processes and associated retrogressive slumping, which are related with fluctuations in sediment supply and relative sea-level changes, have played a major role in the formation, maintenance and deepening of the Valencia Channel. In addition to these sedimentary processes, a basement tectonic control and some morphostructural features affect the direction of the Valencia Channel locally.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1573-0581
    Keywords: Back-arc basin ; incipient seafloor spreading ; rifting ; swath bathymetry ; morphostructure ; seismic reflection ; Bransfield Basin
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The Bransfield Basin is a narrow and elongated active rift basin located between the Antarctic Peninsula and the South Shetland Islands. The Bransfield Basin is composed of three small basins, and two of them, the Central and Eastern Bransfield Basins, were surveyed during a recent cruise (GEBRA 93). The full swath bathymetry coverage as well as the single-channel seismic reflection and magnetic profiles that have been acquired, help us to better understand the morphostructure and recent evolution of the Bransfield Basin. Six large volcanic edifices aligned with the basin axis stick out of the sedimented seafloor of the Central Bransfield Basin. In contrast, the Eastern Bransfield Basin is characterised by four deep troughs displaying a rhombic-shape, and small, scattered volcanic cones located in the southwestern half basin. Seamount volcanism plays an important role in the formation of new crust in the Bransfield Basin. The larger seamounts of the Central Bransfield Basin are located at the intersection of the two main orthogonal sets of faults (longitudinal ENE-WSW and transversal NNW-SSE). Morphological analysis of the seamounts indicates a multi-staged volcano-tectonic construction. The distribution and shape of these edifices suggests that both volcanism and extension are concentrated at the same preferential areas through time. This might be related to the fracturation style of the continental crust. The Central and Eastern Bransfield Basins are very different in morphostructure, volcanism, and sedimentary cover. The Central Bransfield Basin shows evidence of NW-SE extensional faulting and focused active MORB-volcanism interpreted as result of incipient seafloor spreading. The Eastern Bransfield Basin is still in a rifting stage, mainly dominated by a NW-SE extension and some left-lateral strike-slip component probably related to the South Scotia Ridge.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2021-03-08
    Description: The NEAM Tsunami Hazard Model 2018 (NEAMTHM18) is a probabilistic hazard model for tsunamis generated by earthquakes. It covers the coastlines of the North-eastern Atlantic, the Mediterranean, and connected seas (NEAM). NEAMTHM18 was designed as a three-phase project. The first two phases were dedicated to the model development and hazard calculations, following a formalized decision-making process based on a multiple-expert protocol. The third phase was dedicated to documentation and dissemination. The hazard assessment workflow was structured in Steps and Levels. There are four Steps: Step-1) probabilistic earthquake model; Step-2) tsunami generation and modeling in deep water; Step-3) shoaling and inundation; Step-4) hazard aggregation and uncertainty quantification. Each Step includes a different number of Levels. Level-0 always describes the input data; the other Levels describe the intermediate results needed to proceed from one Step to another. Alternative datasets and models were considered in the implementation. The epistemic hazard uncertainty was quantified through an ensemble modeling technique accounting for alternative models’ weights and yielding a distribution of hazard curves represented by the mean and various percentiles. Hazard curves were calculated at 2,343 Points of Interest (POI) distributed at an average spacing of ∼20 km. Precalculated probability maps for five maximum inundation heights (MIH) and hazard intensity maps for five average return periods (ARP) were produced from hazard curves. In the entire NEAM Region, MIHs of several meters are rare but not impossible. Considering a 2% probability of exceedance in 50 years (ARP≈2,475 years), the POIs with MIH 〉5 m are fewer than 1% and are all in the Mediterranean on Libya, Egypt, Cyprus, and Greece coasts. In the North-East Atlantic, POIs with MIH 〉3 m are on the coasts of Mauritania and Gulf of Cadiz. Overall, 30% of the POIs have MIH 〉1 m. NEAMTHM18 results and documentation are available through the TSUMAPS-NEAM project website (http://www.tsumaps-neam.eu/), featuring an interactive web mapper. Although the NEAMTHM18 cannot substitute in-depth analyses at local scales, it represents the first action to start local and more detailed hazard and risk assessments and contributes to designing evacuation maps for tsunami early warning.
    Description: The NEAMTHM18 was prepared in the framework of the European Project TSUMAPS-NEAM (http://www.tsumaps-neam.eu/) funded by the mechanism of the European Civil Protection and Humanitarian Aid Operations with grant no. ECHO/SUB/2015/718568/PREV26 (https://ec.europa.eu/echo/funding-evaluations/financing-civil-protection-europe/selected-projects/probabilistic-tsunami-hazard_en). The work by INGV authors also benefitted from funding by the INGV-DPC Agreement 2012-2021 (Annex B2).
    Description: Published
    Description: 616594
    Description: 6T. Studi di pericolosità sismica e da maremoto
    Description: 1SR TERREMOTI - Sorveglianza Sismica e Allerta Tsunami
    Description: 2SR TERREMOTI - Gestione delle emergenze sismiche e da maremoto
    Description: 3SR TERREMOTI - Attività dei Centri
    Description: 5SR TERREMOTI - Convenzioni derivanti dall'Accordo Quadro decennale INGV-DPC
    Description: 3IT. Calcolo scientifico
    Description: 4IT. Banche dati
    Description: JCR Journal
    Keywords: probabilistic tsunami hazard assessment ; earthquake-generated tsunami ; hazard uncertainty analysis ; ensemble modeling ; maximum inundation height ; NEAM ; 05.08. Risk ; 03.02. Hydrology ; 04.06. Seismology ; 04.07. Tectonophysics ; 05.01. Computational geophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2021-01-20
    Description: The seafloor covers some 70% of the Earth's surface and has been recognised as a major sink for marine litter. Still, litter on the seafloor is the least investigated fraction of marine litter, which is not surprising as most of it lies in the deep sea, i.e. the least explored ecosystem. Although marine litter is considered a major threat for the oceans, monitoring frameworks are still being set up. This paper reviews current knowledge and methods, identifies existing needs, and points to future developments that are required to address the estimation of seafloor macrolitter. It provides background knowledge and conveys the views and thoughts of scientific experts on seafloor marine litter offering a review of monitoring and ocean modelling techniques. Knowledge gaps that need to be tackled, data needs for modelling, and data comparability and harmonisation are also discussed. In addition, it shows how research on seafloor macrolitter can inform international protection and conservation frameworks to prioritise efforts and measures against marine litter and its deleterious impacts.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 5
    Publication Date: 2023-07-20
    Keywords: Aegeo_PUMP5; Aegeo_PUMP6; Aegeo_PUMP8; Alkenone, C37; Alkenone, C38; Alkenone, unsaturation index UK37; Calculated from UK'37 (Müller et al, 1998); Calculated from UK37 (Ternois et al, 1997); CTD; DEPTH, water; Event label; Methlyheptatriaconta-15E,22E-dien-2-one; Methlyheptatriaconta-15E,22E-trien-2-one; Octatriaconta-16E,23E-dien-2-one; Octatriaconta-16E,23E-dien-3-one; Octatriaconta-9E,16E,23E-trien-2-one; Octatriaconta-9E,16E,23E-trien-3-one; PUMP; Temperature, calculated; Temperature, water; Water pump
    Type: Dataset
    Format: text/tab-separated-values, 108 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Cacho, Isabel; Grimalt, Joan O; Pelejero, Carles; Canals, Miquel; Sierro, Francisco Javier; Flores, José-Abel; Shackleton, Nicholas J (1999): Dansgaard-Oeschger and Heinrich event imprints in the Alboran Sea paleotemperature record. Paleoceanography, 14(6), 698-705, https://doi.org/10.1029/1999PA900044
    Publication Date: 2023-07-20
    Description: Past sea surface temperature (SST) evolution in the Alboran Sea (western Mediterranean) during the last 50,000 years has been inferred from the study of C37 alkenones in International Marine Global Change Studies MD952043 core. This record has a time resolution of ~200 years allowing the study of millennial-scale and even shorter climatic changes. The observed SST curve displays characteristic sequences of extremely rapid warming and cooling events along the glacial period. Comparison of this Alboran record with delta18O from Greenland ice (Greenland Ice Sheet Project 2 core) shows a strong parallelism between these SST oscillations and the Dansgaard-Oeschger events. Five prominent cooling episodes standing out in the SST profile are accompanied by an anomalous high abundance of Neogloboquadrina pachyderma sinistral which is confined to the duration of these cold intervals. These features and the isotopic record reflect drastic changes in the surface hydrography of the Alboran Sea in association with Heinrich events Hl-5.
    Keywords: Alboran Sea; CALYPSO; Calypso Corer; IMAGES I; Marion Dufresne (1995); MD101; MD952043; MD95-2043
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Cacho, Isabel; Pelejero, Carles; Grimalt, Joan O; Calafat, Antonio M; Canals, Miquel (1999): C37 alkenone measurements of sea surface temperature in the Gulf of Lions (NW Mediterranean). Organic Geochemistry, 30(7), 557-566, https://doi.org/10.1016/S0146-6380(99)00038-8
    Publication Date: 2023-07-20
    Description: A study of the C37 alkenone compositions in suspended particulate matter in the northwestern Mediterranean Sea has shown a correspondence between Uk'37 and sea surface temperature that significantly deviates from the general equation regularly observed in most marine world areas (Müller et al., 1998, doi:10.1016/S0016-7037(98)00097-0). However, the temperatures measured in the core top sediments using the general equation are in agreement with the annual average water column temperatures between 0-40 m depth. These discrepancies suggest that despite the rather constant correlation between UK'37 and seawater temperature throughout the world oceans, specific calibrations should be developed for each new area of application of the C37 alkenones for paleotemperature determination.
    Keywords: Aegeo_5; Aegeo_6; Aegeo_8; Aegeo_9; Aegeo_PUMP5; Aegeo_PUMP6; Aegeo_PUMP8; Gulf of Lions; MUC; MultiCorer; PUMP; Water pump
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
    Publication Date: 2023-07-20
    Keywords: Age, 14C AMS; Age, calculated calendar years; Age, comment; Age, dated; Age, dated material; Age, dated standard deviation; Alboran Sea; Calendar age; CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES I; Isotopic event; Marion Dufresne (1995); MD101; MD952043; MD95-2043
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 9
    Publication Date: 2023-07-20
    Keywords: Aegeo_5; Aegeo_6; Aegeo_8; Aegeo_9; Alkenone, C37; Alkenone, C38; Alkenone, unsaturation index UK37; Calculated from UK'37 (Müller et al, 1998); Calculated from UK37 (Ternois et al, 1997); DEPTH, sediment/rock; Elevation of event; Event label; Gulf of Lions; Latitude of event; Longitude of event; Methlyheptatriaconta-15E,22E-dien-2-one; Methlyheptatriaconta-15E,22E-trien-2-one; MUC; MultiCorer; Octatriaconta-16E,23E-dien-2-one; Octatriaconta-16E,23E-dien-3-one; Octatriaconta-9E,16E,23E-trien-2-one; Octatriaconta-9E,16E,23E-trien-3-one; Temperature, calculated
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 10
    Publication Date: 2023-07-20
    Keywords: AGE; Alboran Sea; Calculated from UK'37 (Müller et al, 1998); CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES I; Marion Dufresne (1995); MD101; MD952043; MD95-2043; Sea surface temperature, annual mean
    Type: Dataset
    Format: text/tab-separated-values, 97 data points
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