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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 35 (1979), S. 65-74 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Fine grained (mud) deposits or coarse grained (sand) deposits, which occur in tidally dominated coastal environments (bays, tidal inlets and estuaries), are associated with topographical (small-scale) tidally induced eddies; these are considered to be caused by the phenomenon of flow separation, downstream from headlands and at abrupt coastal discontinuities. Extensive sand deposits, which have been described as bed-load convergence zones can, similarly, be associated with residual (large-scale) circulation eddies.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2023-05-12
    Description: The area under investigation is located within 22°45' to 23°45'E, and from 39°15' to 40°15'N. Sedimentological, bathymetric and shallow geophysical data were collected from here during the 7/78 cruise of R.R.S. "Shackleton". Twenty-seven sea-bed (surface) samples were collected, using a Day grab, from different environments; these were analysed for grain-size distribution, carbonate content, and clay mineralogy. On the basis of the bathymetric and shallow geophysical data, the area has been classified into five major physiographic environments, according to their bathymetry and topography: (1) shelf (Thermaicon Plateau); (2) slope; (3) marginal plateau; (4) the "canyon system" and valleys; and (5) (Sporades) basin. Based on the sedimentological analyses, the surface sediments have been classified into four major Provinces, as follows: (1) Province 1 - shelf muds; (2) Province 2 - muddy sands; (3) Province 3 - outer margin muds; and (4) Province 4 - outer shelf/shelf break. It is concluded that modern sedimentation in the N.W. Aegean Sea is dominated by the (terrigenous) river inputs and by the circulation of both high and low salinity masses.
    Keywords: Aegean Sea; Calcium carbonate; Calculated after FOLK; DEPTH, sediment/rock; Event label; Grab; GRAB; Grain size, mean; Grain size, pipette analysis; Grain size, sieving; Gravimetric analysis; Illite; Kaolinite+Chlorite; Latitude of event; Longitude of event; NA/78/1; NA/78/10; NA/78/19; NA/78/2; NA/78/28; NA/78/3; NA/78/32; NA/78/33; NA/78/34; NA/78/35; NA/78/36; NA/78/37; NA/78/38; NA/78/39; NA/78/4; NA/78/40; NA/78/41; NA/78/42; NA/78/44; NA/78/45; NA/78/46; NA/78/47; NA/78/5; NA/78/6; NA/78/7; NA/78/8; NA/78/9; Sand; Shackleton; Shackleton78/7; Silt; Size fraction 〈 0.002 mm, clay; Smectite; Thermaikos Gulf; X-ray diffraction, clay fraction
    Type: Dataset
    Format: text/tab-separated-values, 249 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Naeher, Sebastian; Geraga, Maria; Papatheodorou, George; Ferentinos, George; Kaberi, Helen; Schubert, Carsten J (2012): Environmental variations in a semi-enclosed embayment (Amvrakikos Gulf, Greece) - reconstructions based on benthic foraminifera abundance and lipid biomarker pattern. Biogeosciences, 9(12), 5081-5094, https://doi.org/10.5194/bg-9-5081-2012
    Publication Date: 2024-03-01
    Description: The evolution of environmental changes during the last decades and the impact on the living biomass in the western part of Amvrakikos Gulf was investigated using abundances and species distributions of benthic foraminifera and lipid biomarker concentrations. These proxies indicated that the gulf has markedly changed due to eutrophication. Eutrophication has led to a higher productivity, a higher bacterial biomass, shifts towards opportunistic and tolerant benthic foraminifera species (e.g. Bulimina elongata, Nonionella turgida, Textularia agglutinans, Ammonia tepida) and a lower benthic species density. Close to the Preveza Strait (connection between the gulf and the Ionian Sea), the benthic assemblages were more diversified under more oxygenated conditions. Sea grass meadows largely contributed to the organic matter at this sampling site. The occurrence of isorenieratane, chlorobactane and lycopane supported by oxygen monitoring data indicated that anoxic (and partly euxinic) conditions prevailed seasonally throughout the western part of the gulf with more severe oxygen depletion towards the east. Increased surface water temperatures have led to a higher stratification, which reduced oxygen resupply to bottom waters. Altogether, these developments led to mass mortality events and ecosystem decline in Amvrakikos Gulf.
    Keywords: HYPOX; In situ monitoring of oxygen depletion in hypoxic ecosystems of coastal and open seas and land-locked water bodies
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Ferentinos, George; Papatheodorou, George; Geraga, Maria; Iatrou, Margarita; Fakiris, Elias; Christodoulou, Dimitris; Dimitriou, Evagelos; Koutsikopoulos, Constantin (2010): Fjord water circulation patterns and dysoxic/anoxic conditions in a Mediterranean semi-enclosed embayment in the Amvrakikos Gulf, Greece. Estuarine, Coastal and Shelf Science, 88(4), 473-481, https://doi.org/10.1016/j.ecss.2010.05.006
    Publication Date: 2024-03-01
    Description: Oceanographic research in the Amvrakikos Gulf in Western Greece, a semi-enclosed embayment isolated from the Ionian Sea by a narrow, shallow sill, has shown that it is characterised by a fjord-like oceanographic regime. The Gulf is characterised by a well-stratified two layer structure in the water column made up of a surface layer and a bottom layer that are separated by a strong pycnocline. At the entrance over the sill, there is a brackish water outflow in the surface water and a saline water inflow in the near-bed region. This morphology and water circulation pattern makes the Amvrakikos Gulf the only Mediterranean Sea fjord. The investigations have also shown that the surface layer is well oxygenated, whereas in the pycnocline, the dissolved oxygen (DO) declines sharply and finally attains a value of zero, thus dividing the water column into oxic, dysoxic and anoxic environments. At the dysoxic/anoxic interface, at a depth of approximately 35 m, a sharp redox cline develops with Eh values between 0 and 120 mV occurring above and values between 0 and -250 mV occurring below, where oxic and anoxic biochemical processes prevail, respectively. On the seafloor underneath the anoxic waters, a black silt layer and a white mat cover resembling Beggiatoa-like cells are formed. The dysoxic/anoxic conditions appeared during the last 20 to 30 years and have been caused by the excessive use of fertilisers, the increase in animal stocks, intensive fish farming and domestic effluents. The inflicted dysoxia/anoxia has resulted in habitat loss on the seafloor over an area that makes up just over 50% of the total Gulf area and approximately 28% of the total water volume. Furthermore, anoxia is also considered to have been responsible for the sudden fish mortality which occurred in aquaculture rafts in the Gulf in February 2008. Therefore, anoxic conditions can be considered to be a potential hazard to the ecosystem and to the present thriving fishing and mariculture industry in the Gulf.
    Keywords: 09/08AMV02/CTD; 09/08AMV05/CTD; 09/08AMV06/CTD; 09/08AMV09/CTD; 09/08AMV13/CTD; 09/08AMV15/CTD; 09/08AMV17/CTD; 09/08AMV29/CTD; AMV09/08; AMV09/08_02; AMV09/08_05; AMV09/08_06; AMV09/08_09; AMV09/08_13; AMV09/08_15; AMV09/08_17; AMV09/08_29; Amvrakikos Gulf, Ionian Sea, Greece; Calculated; CTD; CTD/Rosette; CTD-RO; CTD with attached oxygen sensor; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Event label; HYPOX; In situ monitoring of oxygen depletion in hypoxic ecosystems of coastal and open seas and land-locked water bodies; Latitude of event; Longitude of event; Oxidation reduction (RedOx) potential; Oxygen; pH; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1638 data points
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  • 5
    Publication Date: 2024-03-01
    Keywords: AMV_core15; Amvr15; Amvrakikos Gulf, Ionian Sea, Greece; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic/Nitrogen, total ratio; Carbon/Nitrogen ratio; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; HYPOX; In situ monitoring of oxygen depletion in hypoxic ecosystems of coastal and open seas and land-locked water bodies; Kajak sediment core sampler; KC; Nitrogen, total; δ13C; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 162 data points
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  • 6
    Publication Date: 2024-03-01
    Keywords: AMV_core13; Amvr13; Amvrakikos Gulf, Ionian Sea, Greece; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic/Nitrogen, total ratio; Carbon/Nitrogen ratio; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; HYPOX; In situ monitoring of oxygen depletion in hypoxic ecosystems of coastal and open seas and land-locked water bodies; Kajak sediment core sampler; KC; Nitrogen, total; δ13C; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 138 data points
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  • 7
    Publication Date: 2024-03-01
    Keywords: AMV_core13; Amvr13; Amvrakikos Gulf, Ionian Sea, Greece; Chlorin index; Chlorins; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; HYPOX; In situ monitoring of oxygen depletion in hypoxic ecosystems of coastal and open seas and land-locked water bodies; Kajak sediment core sampler; KC; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 8
    Publication Date: 2024-03-01
    Keywords: AMV_core15; Amvr15; Amvrakikos Gulf, Ionian Sea, Greece; Chlorin index; Chlorins; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; HYPOX; In situ monitoring of oxygen depletion in hypoxic ecosystems of coastal and open seas and land-locked water bodies; Kajak sediment core sampler; KC; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
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  • 9
    Publication Date: 2015-01-24
    Description: Helike, the Achaean Dodecapolis capital, in the Corinth Gulf, Greece, was, according to historical sources, devastated and disappeared from sight during an earthquake followed by sea invasion on to land in 373/372 B.C. A marine remote sensing survey, which was carried out to examine a landslide following a 6.2 R earthquake in 1995, that affected the coastal and near-shore delta plain zone on which Helike stood, accompanied by onshore borehole data, enabled us to postulate the geological processes leading to the Helike catastrophe. Helike was initially leveled during a 6 to 6.7 R earthquake; it is postulated to have then submerged following a translational landslide caused by liquefaction. This Helike catastrophe model is consistent with historical sources and current views regarding the expected geological hazards magnitude in the Gulf.
    Electronic ISSN: 2072-4292
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by MDPI Publishing
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  • 10
    Publication Date: 2016-05-19
    Description: The Corinth Rift, central Greece, enables analysis of early rift development as it is young (〈5 Ma), highly active and its full history is recorded at high-resolution by sedimentary systems. A complete compilation of marine geophysical data, complemented by onshore data, is used to develop a high-resolution chronostratigraphy and detailed fault history for the offshore Corinth Rift, integrating interpretations and reconciling previous discrepancies. Rift migration and localization of deformation have been significant within the rift since inception. Over the last ca. 2 Myr the rift transitioned from a spatially complex rift to a uniform asymmetric rift, but this transition did not occur synchronously along-strike. Isochore maps at ca.100 kyr intervals illustrate a change in fault polarity within the short interval ca.620-340 ka, characterized by progressive transfer of activity from major S-dipping faults to N-dipping faults and southwards migration of discrete depocentres at ~30 m/kyr. Since ca.340 ka there has been localization and linkage of the dominant N-dipping border fault system along the southern rift margin, demonstrated by lateral growth of discrete depocentres at ~40 m/kyr. A single central depocentre formed by ca.130 ka, indicating full fault linkage. These results indicate that rift localization is progressive (not instantaneous) and can be synchronous once a rift border fault system is established. This study illustrates that development processes within young rifts occur at 100 kyr timescales, including rapid changes in rift symmetry, and growth and linkage of major rift faults.
    Print ISSN: 0278-7407
    Electronic ISSN: 1944-9194
    Topics: Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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