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  • 1
    Keywords: Hochschulschrift ; Island ; Hydrothermale Lagerstätte
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (239 Seiten) , Illustrationen, Karten
    DDC: 550
    Language: English
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  • 2
    Publication Date: 2024-02-02
    Description: Multibeam bathymetry raw data was recorded in the North Atlantic Ocean during cruise MSM75 that took place between 2018-06-29 and 2018-08-08. The data was collected using the ship's own Kongsberg EM 122. Sound velocity profiles (SVP) were applied on the data for calibration. SVP data are part of this dataset publication. This data is part of the DAM (German Marine Research Alliance) underway research data project.
    Keywords: DAM_Underway; DAM Underway Research Data; Data file recording distance; Data file recording duration; DATE/TIME; Event label; File content; File format; File name; File size; Kongsberg EM122 Multibeam Echo Sounder; LATITUDE; LONGITUDE; Maria S. Merian; MSM75; MSM75_0_Underway-1; MSM75_1-1; MSM75_20-1; MSM75_218-1; MSM75_74-1; Multibeam Echosounder; Ship speed; Sound velocity profiler; Start of data file recording, date/time; Start of data file recording, latitude; Start of data file recording, longitude; Stop of data file recording, date/time; Stop of data file recording, latitude; Stop of data file recording, longitude; SVP; Swath bathymetry; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 768 data points
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  • 3
    Publication Date: 2024-04-20
    Description: Multibeam bathymetry raw data was recorded in the North Atlantic during cruise MSM75 that took place between 2018-06-29 and 2018-08-08. The data was collected using the ship's own Kongsberg EM 712. This data is part of the DAM (German Marine Research Alliance) underway research data project. Underway data is collected continuously on German research vessels and can include data from transits or from the entire cruise. Underway data is shared in line with the FAIR principles.
    Keywords: Binary Object; Binary Object (File Size); Binary Object (Media Type); DAM_Underway; DAM Underway Research Data; Data file recording distance; Data file recording duration; DATE/TIME; EM712; EM712 multibeam echosounder; File content; LATITUDE; LONGITUDE; Maria S. Merian; MSM75; MSM75_0_Underway-3; Multibeam Echosounder; Ship speed; Start of data file recording, date/time; Start of data file recording, latitude; Start of data file recording, longitude; Stop of data file recording, date/time; Stop of data file recording, latitude; Stop of data file recording, longitude; Swath bathymetry
    Type: Dataset
    Format: text/tab-separated-values, 5984 data points
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  • 4
    Publication Date: 2021-10-06
    Description: During RV MS Merian expedition MSM75, an international, multidisciplinary team explored the Reykjanes Ridge from June to August 2018. The first area of study, Steinahóll (150–350 m depth), was chosen based on previous seismic data indicating hydrothermal activity. The sampling strategy included ship- and AUV-mounted multibeam surveys, Remotely Operated Vehicle (ROV), Epibenthic Sledge (EBS), and van Veen grab (vV) deployments. Upon returning to Steinahóll during the final days of MSM75, hydrothermal vent sites were discovered using the ROV Phoca (Kiel, GEOMAR). Here we describe and name three new, distinct hydrothermal vent site vulnerable marine ecosystems (VMEs); Hafgufa, Stökkull, Lyngbakr. The hydrothermal vent sites consisted of multiple anhydrite chimneys with large quantities of bacterial mats visible. The largest of the three sites (Hafgufa) was mapped, and reconstructed in 3D. In total 23,310 individual biological specimens were sampled comprising 41 higher taxa. Unique fauna located in the hydrothermally venting areas included two putative new species of harpacticoid copepod (Tisbe sp. nov. and Amphiascus sp. nov.), as well as the sponge Lycopodina cupressiformis (Carter, 1874). Capitellidae Grube, 1862 and Dorvilleidae Chamberlin, 1919 families dominated hydrothermally influenced samples for polychaetes. Around the hydrothermally influenced sites we observed a notable lack of megafauna, with only a few species being present. While we observed hydrothermal associations, the overall species composition is very similar to that seen at other shallow water vent sites in the north of Iceland, such as the Mohns Ridge vent fields, particularly with peracarid crustaceans. We therefore conclude the community overall reflects the usual “background” fauna of Iceland rather than consisting of “vent endemic” communities as is observed in deeper vent systems, with a few opportunistic species capable of utilizing this specialist environment.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 5
    Publication Date: 2022-06-28
    Description: Hotspot-influenced spreading axes are characterized by a shallow axis, thickened crust, and possibly by higher-than-normal eruption frequency, all signs of an excess of magma and heat being supplied to such ridges by the hotspot. Despite this, these ridges are also characterized by an apparently lower-than-average incidence of high-temperature hydrothermal venting, raising questions about their thermal budget. The type example for hotspot-ridge interaction is the Reykjanes Ridge south of Iceland, which shows abnormally shallow bathymetry between the Reykjanes Peninsula at ca. 63°N and the Charlie Gibbs Fracture Zone at 53°N.The seafloor surrounding the present spreading axis is also characterized by V-shaped bathymetric ridges, thoughtto be produced by regions of excess melting migrating along the axis through time. Cruise MSM75aimed to produce geological maps of four key areas along the ridge -one with thickened crust where a V-shaped ridge intersects the present-day axis, one with thickened crust but no on-axis V-shaped ridge anomaly, a third with more normal crustal thickness and an axial valley and a fourth at the only known, but up to present unsampled, Reykjanes hydrothermal site Steinaholl. This geological mapping is to be usedto investigate questions of variations in eruption size or frequency away from Iceland, the interplay between magmatism and tectonism, the axial volcanology of V-shaped ridges and how thick crust is cooled in the apparent paucity of high-temperature vent fields.
    Type: Report , NonPeerReviewed
    Format: text
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  • 6
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    Elsevier
    In:  Journal of Volcanology and Geothermal Research, 348 . pp. 62-81.
    Publication Date: 2020-02-06
    Description: Highlights • Formation of Axial Volcanic Ridges is more complex than previous models suggest. • Faults on the Reykjanes Ridge strike orthogonal to spreading direction. • Seamounts and fault densities reflect volcanic robustness of Axial Volcanic Ridges. • Steinahóll Vent Field occupies shallow eruptive fissure located between two faults. Abstract Current estimates indicate that the number of high-temperature vents (one of the primary pathways for the heat extraction from the Earth's mantle) – at least 1 per 100 km of axial length – scales with spreading rate and should scale with crustal thickness. But up to present, shallow ridge axes underlain by thick crust show anomalously low incidences of high-temperature activity. Here we compare the Reykjanes Ridge, an abnormally shallow ridge with thick crust and only one high-temperature vent known over 900 km axial length, to the adjacent subaerial Reykjanes Peninsula (RP), which is characterized by high-temperature geothermal sites confined to four volcanic systems transected by fissure swarms with young (Holocene) volcanic activity, multiple faults, cracks and fissures, and continuous seismic activity. New high-resolution bathymetry (gridded at 60 m) of the Reykjanes Ridge between 62°30′N and 63°30′N shows seven Axial Volcanic Ridges (AVR) that, based on their morphology, geometry and tectonic regime, are analogues for the volcanic systems and fissure swarms on land. We investigate in detail the volcano-tectonic features of all mapped AVRs and show that they do not fit with the previously suggested 4-stage evolution model for AVR construction. Instead, we suggest that AVR morphology reflects the robust or weak melt supply to the system and two (or more) eruption mechanisms may co-exist on one AVR (in contrast to 4-stage evolution model). Our interpretations indicate that, unlike on the Reykjanes Peninsula, faults on and around AVRs do not cluster in orientation domains but all are subparallel to the overall strike of AVRs (orthogonal to spreading direction). High abundance of seamounts shows that the region centered at 62°47′N and 25°04′W (between AVR-5 and -6) is volcanically robust while the highest fault density implies that AVR-1 and southern part of AVR-6 rather undergo period of melt starvation. Based on our observations and interpretations we expect all of the AVRs on Reykjanes Ridge to be hydrothermally active but morphological and hydrographic settings of this ridge may cause hydrothermal plumes to be quickly dispersed and diluted due to exposure to strong bottom currents. Therefore, combined CTD and autonomous vehicles surveys are probably the most efficient methods for hydrothermal exploration along the Reykjanes Ridge.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 7
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    Elsevier
    In:  Journal of Volcanology and Geothermal Research, 316 . pp. 22-33.
    Publication Date: 2019-09-24
    Description: Highlights • Hydrothermalism in off-axis Tertiary Iceland crust is low-temperature (〈 100 °C). • Hydrothermalism is dike-controlled, unlike the fault-hosted venting in on-axis areas. • Inactive off-axis faults seal quickly due to fluids reacting with fine-grained gouge. • Cracks in country rock next to the dikes form major vertical off-axis permeability. • We predict locations of venting in off-axis regions (〉 2 Ma) of the Reykjanes Ridge. Abstract Hydrothermal activity along the Mid-Atlantic Ridge is predominantly high-temperature venting controlled by volcano-tectonic processes confined to the ridge axis and neotectonic zone, which extends ~ 20 km on each side of the axis (e.g. TAG or Logatchev 1). These vents cannot, however, account for all the heat which needs to be removed to cool the plate and a significant amount of heat is probably removed in the off-axis regions as well. These regions have previously not been systematically surveyed for hydrothermal activity due to a lack of predictive models for its nature, location or controlling structures. Here we use hot springs in the Tertiary Westfjords of Iceland as onshore analogs for hydrothermal activity along the off-axis Mid-Atlantic Ridge to better understand tectonic and volcanological controls on their occurrence, as well as the processes which support hydrothermal circulation. Our results show that even crust ≥ 10 Ma has abundant low-temperature hydrothermal activity. We show that 66% of hot springs investigated, and 100% of those for which a detailed geological setting could be determined, are associated with basaltic dikes cross-cutting the sub-horizontal lava sequence. This is in strong contrast to on-axis springs, which are known (both from underwater and on land) to be predominantly associated with faults. Absence of earthquakes in Westfjords suggests that the faults there are no longer active and possibly sealed by secondary minerals, suppressing fluid circulation. In such a situation, the jointed and fractures dike margins may provide the major pathways for fluid circulation. Extrapolating this idea to the off–axis regions of the Reykjanes Ridge, we suggest, based on bathymetric maps, potential sites for future exploration for off-axis hydrothermal systems.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2020-06-02
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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  • 9
    Publication Date: 2016-03-21
    Description: More than 25% of heat-loss from the Earth's interior occurs via hydrothermal cooling of newly-formed oceanic lithosphere at mid-ocean ridges. In the process, elements (including economically-relevant base and precious metals) are re-distributed and concentrated in seafloor massive sulphide (SMS) deposits. A recent estimate1 suggested that the amount of metal being deposited at the presently-active ridges is not economically significant (with a total copper+zinc inventory equal to only one year of global copper+zinc consumption), but also highlighted the unknown potential of older seafloor, for which no viable exploration models existed. Here we present the results of hydrothermal exploration along 3000 km of the Mid-Atlantic Ridge (representing almost 5% of the total length (64.000km) of the global mid-ocean ridge system and over 8% of the economically more interesting slow-spreading (〈40mm/yr) ridges). We find significant correlations between axial morphology as determined by ship-mounted multibeam and the presence of high-temperature hydrothermal venting determined from water column studies. Using these relationships we can, for the first time, predict the location of extinct hydrothermal deposits within the plate interior solely based on ship-based multibeam surveys.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
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    In:  [Poster] In: Sustainable Ocean Development Symposium, 28.-30.09.2015, New York City, USA .
    Publication Date: 2016-12-06
    Description: Hydrothermal activity along Mid–Ocean Ridges is dominated by high–temperature venting mostly confined to ridge axis and neotectonic zone extending ~15km on each side of the axis. However, extensive exploration and discoveries of new hydrothermal fields in off–axis regions (e.g. Lost City, MAR) show that hydrothermal activity may be dominated by off–axis venting. Hence, little is known about controls and nature of such systems, for example, weather low–temperature “diffuse” venting dominates? Such systems may transport even 90% of hydrothermal heat to the oceans. This makes them a great potential source of renewable energy. However, we need to know where to look for them on the seafloor? On Iceland 95% of hydrothermalism takes place through low-temperature venting, therefore as subaerial part of the Mid-Atlantic Ridge, Iceland can help us better understand underwater hydrothermalism. Unfortunately, the technology to detect these systems is rudimentary. Therefore we need to develop an inexpensive and precise method for detecting low-temperature venting that will have very little impact on environment but will help us accurately assess potential of these systems. Observations of Icelandic systems helped me to develop predictive model for locating low-temperature venting on the Reykjanes Ridge (south of Iceland) based on existing bathymetry maps. This method could potentially be applied to other mid-ocean ridges worldwide. Seafloor of Reykjanes Ridge is easy to reach due to shallow depth. With high resolution maps we can focus investigations to pre-targeted areas of interest. Biological observations can significantly improve this method since detecting signals created by low-temperature fluids is very difficult with only geological, acoustic and optic measurements. Visual observations of bacteria mats or mussels (e.g. Bathymodiolus) can help directly locating sites where fluids escape from the crust.
    Type: Conference or Workshop Item , NonPeerReviewed
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