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  • PANGAEA  (107)
  • Berlin : Cornelsen
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  • 1
    Keywords: Schulbuch ; Meer ; Meereskunde
    Type of Medium: Book
    Pages: 64 S , zahlr. Ill., graph. Darst., Kt.
    Edition: 1. Aufl.
    ISBN: 9783060108282 , 9783060108251
    Series Statement: Naturwissenschaften : [Biologie, Chemie, Physik] [Schülerbd.]
    RVK:
    Language: German
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  • 2
    Publication Date: 2024-07-19
    Description: Our knowledge of venting at intraplate seamounts is limited. Almost nothing is known about past hydrothermal activity at seamounts, because indicators are soon blanketed by sediment. This study provides evidence for temporary hydrothermal circulation at Henry Seamount, a re-activated Cretaceous volcano near El Hierro island, close to the current locus of the Canary Island hotspot. In the summit area at around 3000-3200 m water depth, we found areas with dense coverage by shell fragments from vesicomyid clams, a few living chemosymbiotic bivalves, and evidence for sites of weak fluid venting. Our observations suggest pulses of hydrothermal activity since some thousands or tens of thousands years, which is now waning. We also recovered glassy heterolithologic tephra and dispersed basaltic rock fragments from the summit area. Their freshness suggests eruption during the Pleistocene to Holocene, implying minor rejuvenated volcanism at Henry Seamount probably related to the nearby Canary hotspot. Heat flow values determined on the surrounding seafloor (49 ± 7 mW/m2) are close to the expected background for conductively cooled 155 Ma old crust; the proximity to the hotspot did not result in elevated basal heat flow. A weak increase in heat flow towards the southwestern seamount flank likely reflects recent local fluid circulation. We propose that hydrothermal circulation at Henry Seamount was, and still is, driven by heat pulses from weak rejuvenated volcanic activity. Our results suggest that even single eruptions at submarine intraplate volcanoes may give rise to ephemeral hydrothermal systems and generate potentially habitable environments.
    Keywords: Atlantic; Canary Islands; Center for Marine Environmental Sciences; heatflow; hydrothermal activity; MARUM; Seamount; vesicomyid clams
    Type: dataset publication series
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2024-07-19
    Description: This dataset includes seismic reflection data, sediment core line scanner images, and logging data from the region of the Tuaheni Landslide Complex, east of New Zealand's North Island on the Hikurangi margin. The seismic reflection data were collected in 2014 aboard RV Tangaroa (TAN1404) using GEOMAR's P-Cable system. The line scanner images and logging data were generated from sediment core recovered using gravity cores and MeBo200 drilling during Voyage SO247 aboard RV Sonne. The datasets have been used in a core-log-seismic integration study of the Tuaheni Landslide Complex.
    Keywords: linescanner images; MeBo200; Multi-sensor core logger; New Zealand; P-Cable; SCHLIP3D; seismic reflection; Tuaheni Landslide Complex; Understanding slow-slipping submarine landslides: 3D seismic investigations of the Tuaheni landslide complex
    Type: dataset bundled publication
    Format: application/zip, 10 datasets
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  • 4
    Publication Date: 2024-07-19
    Description: Lake Ladoga in northwestern Russia is Europe's largest lake. The postglacial history of the Ladoga basin is for the first time documented continuously with high temporal resolution in the upper 13.3 m of a sediment core (Co1309) from the northwestern part of the lake. We applied a multiproxy approach including (bio‐)geochemical and granulometric analyses. The dataset comprises grain-size data (clay, silt, sand), biogeochemical data (total organic carbon (TOC), total sulphur (TS)), water content and XFR data (Fe, P, Ti, K, Zr, Ti/Al, Rb/Sr, Zr/Rb) of the composit profile of sediment core Co1309 as presented in Gromig et al. 2019.
    Keywords: AWI_Envi; Geochemistry; Lake Ladoga; lake sediments; PLOT-Project; Polar Terrestrial Environmental Systems @ AWI; Sediment core
    Type: dataset bundled publication
    Format: application/zip, 3 datasets
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  • 5
    Publication Date: 2024-07-19
    Description: The bulk of multibeam bathymetric data were acquired during RV Maria S. Merian cruises MSM11/2 (Bickert et al., 2009), MSM82/2 (Krastel et al., 2019a) and MSM87 (Krastel et al., 2019b) with hull-mounted Kongsberg Simrad systems EM120 (MSM11/2) and EM122 (MSM82/2 and MSM87). The nominal sonar frequency is 12 kHz. The angular coverage is up to 150°, and each angular beam accuracy was 2° by 2°. Kongsberg Seapath system provides the combined motion, position and time data, which are transmitted to the Processing Unit (PU) of the multibeam echosounder to achieve real-time motion compensation in pitch, roll and yaw. All raw data were processed with MB-System software (Caress and Chayes, 2017: https://www.mbari.org/products/research-software/mb-system/). Sound velocities were measured with a Conductivity, Temperature, Depth (CTD) probe during MSM 82/2 and an expendable sound velocimeter during MSM87. The multibeam data in cruise MSM82/2 were collected from the 11th to 13th of May in 2019 in the headwall area of the Sahara Slide Complex. Only two sound velocities were measured on the 11th and 12th of May, and we applied the measured sound velocities to data from these two days. In the mean time, the measured sound velocity on 12th of May was also applied to data collected on 13th of May. For MSM11/2, sound velocities were adjusted using the mbvelocity tool implemented in the MB-System software. The multibeam bathymetric data were gridded by using the splines with tension algorithm to a final grid with 150 m cell spacing in lateral direction. Echosounder data were acquired during several cruises with RV Maria S. Merian (MSM11/2, MSM82/2, MSM87). The high-resolution parametric ATLAS Parasound System DS3 (Atlas Hydrographic®) is a hull-mounted parametric echo sounder; the secondary low frequency (SLF) was set to 4 kHz through our cruises. The opening angle of the system is 4.5°. The system allows imaging of the uppermost 50-100 m of sediment at a sub-meter vertical resolution. The echogram sections were filtered with a wide band pass filter to improve the signal-to-noise ratio. The data were analyzed and interpreted in IHS Kingdom®. Gravity cores were acquired with a 5 m-long standard gravity corer during RV Maria S. Merian Cruise MSM82/2 (cores MSM82/2-34, MSM82/2-35 and MSM82/2-36). They were studied by color analysis, photography and sedimentological description. Accelerated Mass Spectrometry 14C-age dating of the planktonic foraminifera Globigerinoides ruber (Bonfardeci et al., 2018) was performed at the Leibniz Laboratory for Radiometric Dating and Stable Isotope Research at Kiel University. The Calib 704 and the Marine 13 calibration curve were applied to calibrate 14C age to calendar years (Reimer et al., 2013); the reservoir age was set to ±500 years (Mangerud and Gulliksen, 1975).
    Keywords: echosounder; Gravity core; Multibeam
    Type: dataset bundled publication
    Format: application/zip, 6 datasets
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  • 6
    Publication Date: 2024-07-19
    Description: On November 18, 1929, a M7.2 earthquake occurred beneath the Laurentian Channel off the coast of Newfoundland. Nearly simultaneously, 12 undersea trans-Atlantic communication cables were severed and within two hours, a devastating tsunami struck the south coast of Newfoundland, claiming 28 lives. Only in 1952, it was understood that a slump-generated turbidity current caused the sequential severance of the cables and likely generated the tsunami. The 1929 Grand Banks events were pivotal, as they led to the first unequivocal recognition of a turbidity current and landslide-triggered tsunami. The landslide site was visited numerous times as underwater survey technologies evolved. No major head scarp related to the event is recognized. The landslide appears to have affected shallow sediments (top 5-100 m) and was laterally extensive. In order to test the hypothesis that a distributed, laterally extensive, shallow submarine mass failure event caused the tsunami, we collected ~ 1500 km of seismic lines in combination with a dense net of hydroacoustic data. A total of ~130 m of gravity cores were recovered at 30 stations. Giant box cores were taken at 15 stations. Three CPT (free-fall cone penetrating testing) transects were collected across landslide scarps. The data in the failure area show abundant small scarps and several young landslide deposits. The existing bathymetric data were slightly expanded to the shelf break but no obvious major scarp was discovered. The combined interpretation of existing and new data will allow estimating the volume of the failed material, which is an important input parameter for tsunami modelling. Another important aspect will be to assess the activity of listric faults in the failure area with special emphasis on their role for the failure dynamics and the triggering of the tsunami. The deposits of the related turbidity current were investigated in a complex channel area downslope of the failure area. Several coring transects will allow to reconstruct the flow lines of the 1929 turbidity current from bypass- dominated to depositional areas. Very coarse gravel was sampled up to 150 m above the canyon thalweg. First estimates suggest high concentrations of sediments in the flow, which was able to run out over 1000s of kilometers. The collected raw data of the surface and shallow subsurface is attached here. A detailed description of the dataset und utilised methods and the overview of track lines can be found in the official cruise report (Krastel et al. 2016, doi:10.2312/cr_msm47).
    Keywords: Bathymetry; landslide; multi beam echo sounder; Sediment cores; Seismic
    Type: dataset publication series
    Format: application/zip, 7 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Berndt, Christian; Feseker, Tomas; Treude, Tina; Krastel, Sebastian; Liebetrau, Volker; Niemann, Helge; Bertics, Victoria J; Dumke, Ines; Dünnbier, Karolin; Ferre, Benedicte; Graves, Carolyn; Gross, Felix; Hissmann, Karen; Hühnerbach, Veit; Krause, Stefan; Lieser, Kathrin; Schauer, Jürgen; Steinle, Lea (2014): Temporal constraints on hydrate-controlled methane seepage off Svalbard. Published Online January 2 2014, Science, https://doi.org/10.1126/science.1246298
    Publication Date: 2024-07-19
    Description: Methane hydrate is an ice-like substance that is stable at high-pressure and low temperature in continental margin sediments. Since the discovery of a large number of gas flares at the landward termination of the gas hydrate stability zone off Svalbard, there has been concern that warming bottom waters have started to dissociate large amounts of gas hydrate and that the resulting methane release may possibly accelerate global warming. Here, we can corroborate that hydrates play a role in the observed seepage of gas, but we present evidence that seepage off Svalbard has been ongoing for at least three thousand years and that seasonal fluctuations of 1-2°C in the bottom-water temperature cause periodic gas hydrate formation and dissociation, which focus seepage at the observed sites.
    Keywords: Center for Marine Environmental Sciences; GEOMAR; Helmholtz Centre for Ocean Research Kiel; MARUM
    Type: dataset publication series
    Format: application/zip, 29 datasets
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  • 8
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    PANGAEA
    In:  Supplement to: Steinle, Lea; Graves, Carolyn; Treude, Tina; Ferre, Benedicte; Biastoch, Arne; Bussmann, Ingeborg; Berndt, Christian; Krastel, Sebastian; James, Rachael H; Behrens, Erik; Böning, Claus W; Greinert, Jens; Sapart, Célia-Julia; Scheinert, Markus; Sommer, Stefan; Lehmann, Moritz F; Niemann, Helge (2015): Water column methanotrophy controlled by a rapid oceanographic switch. Nature Geoscience, 8(5), 378–382, https://doi.org/10.1038/ngeo2420
    Publication Date: 2024-07-19
    Description: Large amounts of the greenhouse gas methane are released from the seabed to the water column where it may be consumed by aerobic methanotrophic bacteria. This microbial filter is consequently the last marine sink for methane before its liberation to the atmosphere. The size and activity of methanotrophic communities, which determine the capacity of the water column methane filter, are thought to be mainly controlled by nutrient and redox dynamics, but little is known about the effects of ocean currents. Here, we report measurements of methanotrophic activity and biomass (CARD-FISH) at methane seeps west of Svalbard, and related them to physical water mass properties (CTD) and modelled current dynamics. We show that cold bottom water containing a large number of aerobic methanotrophs was rapidly displaced by warmer water with a considerably smaller methanotrophic community. This water mass exchange, caused by short-term variations of the West Spitsbergen Current, constitutes a rapid oceanographic switch severely reducing methanotrophic activity in the water column. Strong and fluctuating currents are widespread oceanographic features common at many methane seep systems and are thus likely to globally affect methane oxidation in the ocean water column.
    Type: dataset publication series
    Format: application/zip, 4 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Riedinger, Natascha; Brunner, Benjamin; Krastel, Sebastian; Arnold, Gail Lee; Wehrmann, Laura Mariana; Formolo, Michael J; Beck, Antje; Bates, Steven M; Henkel, Susann; Kasten, Sabine; Lyons, Timothy W (2017): Sulfur cycling in an iron oxide-dominated, dynamic marine depositional system: The Argentine continental margin. Frontiers in Earth Science, 5, https://doi.org/10.3389/feart.2017.00033
    Publication Date: 2024-07-19
    Description: The interplay between sediment deposition patterns, organic matter type and the quantity and quality of reactive mineral phases determines the accumulation, speciation and isotope composition of pore water and solid phase sulfur constituents in marine sediments. Here, we present the sulfur geochemistry of siliciclastic sediments from two sites along the Argentine continental slope--a system characterized by dynamic deposition and reworking, which result in non-steady state conditions. The two investigated sites have different depositional histories but have in common that reactive iron phases are abundant and that organic matter is refractory--conditions that result in low organoclastic sulfate reduction rates. Deposition of reworked, isotopically light pyrite and sulfurized organic matter appear to be important contributors to the sulfur inventory, with only minor addition of pyrite from organoclastic sulfate reduction above the sulfate-methane transition (SMT). Pore-water sulfide is limited to a narrow zone at the SMT. The core of that zone is dominated by pyrite accumulation. Iron monosulfide and elemental sulfur accumulate above and below this zone. Iron monosulfide precipitation is driven by the reaction of low amounts of hydrogen sulfide with ferrous iron and is in competition with the oxidation of sulfide by iron (oxyhydr)oxides to form elemental sulfur. The intervals marked by precipitation of intermediate sulfur phases at the margin of the zone with free sulfide are bordered by two distinct peaks in total organic sulfur. Organic matter sulfurization appears to precede pyrite formation in the iron-dominated margins of the sulfide zone, potentially linked to the presence of polysulfides formed by reaction between dissolved sulfide and elemental sulfur. Thus, SMTs can be hotspots for organic matter sulfurization in sulfide-limited, reactive iron-rich marine sedimentary systems. Furthermore, existence of elemental sulfur and iron monosulfide phases meters below the SMT demonstrates that in sulfide-limited systems metastable sulfur constituents are not readily converted to pyrite but can be buried to deeper sediment depths. Our data show that in non-steady state systems, redox zones do not occur in sequence but can reappear or proceed in inverse sequence throughout the sediment column, causing similar mineral alteration processes to occur at the same time at different sediment depths.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: dataset publication series
    Format: application/zip, 12 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Henkel, Susann; Strasser, Michael; Schwenk, Tilmann; Hanebuth, Till J J; Hüsener, Johannes; Arnold, Gail Lee; Winkelmann, Daniel; Formolo, Michael J; Tomasini, Juan; Krastel, Sebastian; Kasten, Sabine (2011): An interdisciplinary investigation of a recent submarine mass transport deposit at the continental margin off Uruguay. Geochemistry, Geophysics, Geosystems, 12, Q08009, https://doi.org/10.1029/2011GC003669
    Publication Date: 2024-07-19
    Description: Assessing frequency and extent of mass movement at continental margins is crucial to evaluate risks for offshore constructions and coastal areas. A multidisciplinary approach including geophysical, sedimentological, geotechnical, and geochemical methods was applied to investigate multistage mass transport deposits (MTDs) off Uruguay, on top of which no surficial hemipelagic drape was detected based on echosounder data. Nonsteady state pore water conditions are evidenced by a distinct gradient change in the sulfate (SO4**2-) profile at 2.8 m depth. A sharp sedimentological contact at 2.43 m coincides with an abrupt downward increase in shear strength from approx. 10 to 〉20 kPa. This boundary is interpreted as a paleosurface (and top of an older MTD) that has recently been covered by a sediment package during a younger landslide event. This youngest MTD supposedly originated from an upslope position and carried its initial pore water signature downward. The kink in the SO4**2- profile approx. 35 cm below the sedimentological and geotechnical contact indicates that bioirrigation affected the paleosurface before deposition of the youngest MTD. Based on modeling of the diffusive re-equilibration of SO4**2- the age of the most recent MTD is estimated to be 〈30 years. The mass movement was possibly related to an earthquake in 1988 (approx. 70 km southwest of the core location). Probabilistic slope stability back analysis of general landslide structures in the study area reveals that slope failure initiation requires additional ground accelerations. Therefore, we consider the earthquake as a reasonable trigger if additional weakening processes (e.g., erosion by previous retrogressive failure events or excess pore pressures) preconditioned the slope for failure. Our study reveals the necessity of multidisciplinary approaches to accurately recognize and date recent slope failures in complex settings such as the investigated area.
    Keywords: 352; 353; 359; 362; 483; GC; GeoB13803-2; GeoB13804-1; GeoB13804-2; GeoB13808-1; GeoB13854-1; Gravity corer; M78/3A; M78/3B; Meteor (1986); MUC; MultiCorer
    Type: dataset publication series
    Format: application/zip, 8 datasets
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