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  • 2015-2019  (42)
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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (78 Seiten = 7 MB) , Illustrationen, Graphen, Karten
    Language: English
    Note: Zusammenfassung in deutscher und englischer Sprache
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  • 2
    Keywords: Hochschulschrift
    Type of Medium: Book
    Pages: 75 Seiten
    Language: English
    Note: Kiel, Univ., Masterarbeit, 2019
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  • 3
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource ( 82Seiten = 8MB)
    Language: English
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  • 4
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    PANGAEA
    In:  Supplement to: Hensen, Christian; Scholz, Florian; Nuzzo, Marianne; Valadares, Vasco; Gràcia, Eulàlia; Terrinha, Pedro; Liebetrau, Volker; Kaul, Norbert; Silva, Sonia; Martinez-Loriente, Sara; Bartolome, Rafael; Piñero, Elena; Magalhães, Vitor H; Schmidt, Mark; Weise, Stephan M; Cunha, Marina Ribeiro; Hilário, Ana; Perea, Hector; Rovelli, Lorenzo; Lackschewitz, Klas Sven (2015): Strike-slip faults mediate the rise of crustal-derived fluids and mud volcanism in the deep sea. Geology, 43(4), 339-342, https://doi.org/10.1130/G36359.1
    Publication Date: 2023-09-01
    Description: We report on newly discovered mud volcanoes located at about 4500 m water depth 90 km west of the deformation front of the accretionary wedge of the Gulf of Cadiz, and thus outside of their typical geotectonic environment. Seismic data suggest that fluid flow is mediated by a 〉400-km-long strike-slip fault marking the transcurrent plate boundary between Africa and Eurasia. Geochemical data (Cl, B, Sr, 87Sr/86Sr, Delta18O, DeltaD) reveal that fluids originate in oceanic crust older than 140 Ma. On their rise to the surface, these fluids receive strong geochemical signals from recrystallization of Upper Jurassic carbonates and clay-mineral dehydration in younger terrigeneous units. At present, reports of mud volcanoes in similar deep-sea settings are rare, but given that the large area of transform-type plate boundaries has been barely investigated, such pathways of fluid discharge may provide an important, yet unappreciated link between the deeply buried oceanic crust and the deep ocean.
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Scholz, Florian; Schmidt, Mark; Hensen, Christian; Eroglu, Sümeyya; Geilert, Sonja; Gutjahr, Marcus; Liebetrau, Volker (2019): Shelf-to-basin iron shuttle in the Guaymas Basin, Gulf of California. Geochimica et Cosmochimica Acta, 261, 76-92, https://doi.org/10.1016/j.gca.2019.07.006
    Publication Date: 2023-09-01
    Description: Enrichments of highly reactive iron (Fe) (sum of Fe (oxyhydr)oxide, carbonate and sulfide minerals) in marine sediments and sedimentary rocks are commonly interpreted as an indication of anoxic conditions in the bottom water at the time of deposition. The model system for this proxy rationale is the semi-restricted Black Sea, where sediments underneath the anoxic and sulfidic (i.e., euxinic) deep-water are enriched in reactive Fe, which was mobilized from the surrounding shelf areas. To test whether such a shelf-to-basin Fe shuttle can operate in semi-restricted basins without euxinic deep water, we investigated sedimentary Fe speciation and Fe isotope compositions in sediments of the Guaymas Basin, Gulf of California.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Völker, David; Scholz, Florian; Geersen, Jacob (2011): Analysis of submarine landsliding in the rupture area of the 27 February 2010 Maule earthquake, Central Chile. Marine Geology, 288(1-4), 79-89, https://doi.org/10.1016/j.margeo.2011.08.003
    Publication Date: 2023-10-28
    Description: The comparison of bathymetric datasets compiled before and after the Mw = 8.8 Maule Earthquake of the 27 February 2010 offshore Central Chile proves that no new submarine landslides on a size scale detectable with hull-mounted bathymetric echosounders (features of a horizontal size of 〉 1 km) formed as a direct consequence of the ground shaking. Gravity coring around a pre-existing slide feature offshore Concepción (BioBio Slide), however, documents that (1) a number of events occurred as retrogressive failures of the BioBio Slide wall, the youngest of which is 700?1000 years old, and that (2) a very recent small scale slide structure resulted from non-destructive imbricate stacking of a thin sediment layer. Pore water geochemical data show that this event post-dates the Maule Earthquake, suggesting that it was triggered by one of the numerous aftershocks. The absence of larger failures and the presence of a small slide let us propose that in contrast to apparent logic, frequent violent earthquakes at convergent margins do not necessarily pose a particular tsunami risk by landslides. The frequent shaking might even limit the slide volume and therefore their tsunami hazard, as instead of rare and large slides, frequent smaller slides are induced.
    Keywords: SFB574; Volatiles and Fluids in Subduction Zones
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Scholz, Florian; Löscher, Carolin R; Fiskal, Annika; Sommer, Stefan; Hensen, Christian; Lomnitz, Ulrike; Wuttig, Kathrin; Göttlicher, Jörg; Kossel, Elke; Steininger, F F; Canfield, Donald E (2016): Nitrate-dependent iron oxidation limits iron transport in anoxic ocean regions. Earth and Planetary Science Letters, 454, 272-281, https://doi.org/10.1016/j.epsl.2016.09.025
    Publication Date: 2023-10-28
    Description: Iron is an essential element for life on Earth and limits primary production in large parts of the ocean. Oxygen-free continental margin sediments represent an important source of bioavailable iron to the ocean, yet little of the iron released from the seabed reaches the productive sea surface. Even in the anoxic water of oxygen minimum zones, where iron solubility should be enhanced, most of the iron is rapidly re-precipitated. To constrain the mechanism(s) of iron removal in anoxic ocean regions we explored the sediment and water in the oxygen minimum zone off Peru. During our sampling campaign the water column featured two distinct redox boundaries separating oxic from nitrate-reducing (i.e., nitrogenous) water and nitrogenous from weakly sulfidic water. The sulfidic water mass in contact with the shelf sediment contained elevated iron concentrations 〉300 nM. At the boundary between sulfidic and nitrogenous conditions, iron concentrations dropped sharply to 〈20 nM coincident with a maximum in particulate iron concentration. Within the iron gradient, we found an increased expression of the key functional marker gene for nitrate reduction (narG). Part of this upregulation was related to the activity of known iron-oxidizing bacteria. Collectively, our data suggest that iron oxidation and removal is induced by nitrate-reducing microbes, either enzymatically through anaerobic iron oxidation or by providing nitrite for an abiotic reaction. Given the important role that iron plays in nitrogen fixation, photosynthesis and respiration, nitrate-dependent iron oxidation likely represents a key-link between the marine biogeochemical cycles of nitrogen, oxygen and carbon.
    Keywords: Aluminium, particulate; Climate - Biogeochemistry Interactions in the Tropical Ocean; Date/Time of event; DEPTH, water; Event label; GOFLO; Go-Flo bottles; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron, dissolved; Iron, particulate; Iron/Aluminium ratio; Latitude of event; Longitude of event; M92; M92_0031-1; M92_0060-1; M92_0072-1; M92_0102-1; M92_0112-1; M92_0126-1; M92_0135-1; M92_0278-1; Meteor (1986); Sample code/label; SFB754
    Type: Dataset
    Format: text/tab-separated-values, 250 data points
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  • 8
    Publication Date: 2023-10-28
    Keywords: Angle; Area; Chile; Chile_slope_track; DEPTH, water; Height; HEIGHT above ground; LATITUDE; Length; Location; LONGITUDE; Name; Reference/source; SBM; SFB574; Swath bathymetry mapping; Volatiles and Fluids in Subduction Zones; Width
    Type: Dataset
    Format: text/tab-separated-values, 1072 data points
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  • 9
    Publication Date: 2023-10-28
    Keywords: Chile; Chile_slope_track; Frequency-size distribution; Name; SBM; SFB574; Swath bathymetry mapping; Volatiles and Fluids in Subduction Zones
    Type: Dataset
    Format: text/tab-separated-values, 1830 data points
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  • 10
    Publication Date: 2023-10-28
    Keywords: Aluminium; Carbon, organic, total; Climate - Biogeochemistry Interactions in the Tropical Ocean; DEPTH, sediment/rock; Iron; Molybdenum; Nitrogen, total; SFB754; SN4; Tarfaya SN°4; Vanadium; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 761 data points
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