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  • 1
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    Geological Society London
    In:  In: Subaqueous Mass Movements and Their Consequences: Assessing Geohazards, Environmental Implications and Economic Significance of Subaqueous Landslides. , ed. by Lintern, D. G. Special Publications Geological Society London, 477 . Geological Society London, London, pp. 479-495.
    Publication Date: 2020-01-10
    Description: The southern Tuaheni Landslide Complex (TLC) at the Hikurangi subduction margin displays distinctive morphological features along its distribution over the Tuaheni slope offshore Gisborne, New Zealand. We here present first analyses of a gravity core transect that systematically samples surficial sediments from the source area to the toe of this landslide complex, thus providing important new insight into shallow lithological variation in the slide complex. Geophysical and geochemical core logs and core descriptions form the basis for a characterization of representative sediment successions that are indicative of the respective slope segment of recovery. Our results show that the lithology of surficial sediments varies significantly along the length of the landslide complex. Depending on the slope segment observed, this variation includes post-Last Glacial Maximum (LGM) outer-shelf sediments, and hemipelagic drape and near-surface reworked debris avalanche deposits, as well as multiple intercalated thinner turbidites and tephra layers at the distal end of the profile. Lithological downslope variability suggests ongoing mass transport events through the late Holocene that were likely to have been limited to small mud-turbidite flows. Integration with acoustic sub-bottom imagery reveals the presence of multiple stacked mass-transport deposits at depth, contrasting with previous interpretations of a single parent failure.
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 2
    Publication Date: 2023-03-08
    Description: Bottom trawling represents the most widespread anthropogenic physical disturbance to shelf sea sediments. While trawling-induced mortality in benthic fauna has been extensively investigated, its impacts on ecosystem functioning and carbon cycling at regional scales remain unclear. Using the North Sea as an example, we address these issues by synthesizing a high-resolution dataset of bottom trawling impact on sediments, feeding this dataset into a 3-dimensional physical–biogeochemical model to estimate trawling-induced changes in biomass, bioturbation and sedimentary organic carbon, and assessing model results with field samples. Results suggest a trawling-induced net reduction in macrobenthic biomass by 10-27%. Trawling-induced resuspension and reduction of bioturbation jointly and accumulatively reduce the regional sedimentary organic carbon sequestration capacity by 21-67%, equivalent to 0.58-1.84 Mt CO2 yr-1. Our study emphasizes the need for proper management of trawling on muddy seabeds, if the natural capacity of shelf seas for carbon sequestration should be conserved and restored.
    Type: Article , NonPeerReviewed
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  • 3
    Publication Date: 2024-02-07
    Description: We have successfully constructed and tested a new, portable, Hybrid Lister‐Outrigger (HyLO) probe designed to measure geothermal gradients in submarine environments. The lightweight, low‐cost probe is 1‐3 m long, contains 4‐12 semiconductor temperature sensors that have a temperature resolution of 0.002 oC, a sample rate of 〈2 seconds, and a maximum working depth of ~2100 meters below sea level (mbsl). Probe endurance is continuous via ship‐power to water depths of ~700 mbsl, or up to ~1 week on batteries in depths 〉500 mbsl. Data are saved on solid‐state disks, transferred directly to the ship during deployment via a data cable, or transmitted via Bluetooth when the probe is at the sea surface. The probe contains an accelerometer to measure tilt, and internal pressure, temperature, and humidity gauges. Key advantages of this probe include (1) near‐real time temperature measurements and data transfer; (2) a low‐cost, transportable, and lightweight design; (3) easy and rapid two‐point attachment to a gravity corer, (4) short (3‐5 minute) thermal response times; (5) high temporal/spatial resolution and (6) longer deployment endurance compared to traditional methods. We successfully tested the probe both in lakes and during sea trials in May 2019 offshore Montserrat during the R/V Meteor Cruise 154/2. Probe‐measured thermal gradients were consistent with seafloor ocean‐drilling temperature measurements. Ongoing probe improvements include the addition of real‐time bottom‐camera feeds and long‐term (6‐12 month) deployment for monitoring. Key Points - We have designed, developed, and tested a low‐cost, portable hybrid Lister‐type probe to measure shallow thermal gradients - The probe consists of lightweight, quickly interchangeable/expendable components deployable to 2100 meters depth - The probe provides high vertical and temporal temperature resolution and rapid data transmission, reducing down‐time
    Type: Article , PeerReviewed
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    Format: other
    Format: other
    Format: other
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  • 4
    Publication Date: 2018-04-03
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 5
    Publication Date: 2017-04-24
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 6
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    PANGAEA
    In:  Supplement to: Kuhlmann, Jannis; Asioli, Alessandra; Strasser, Michael; Trincardi, Fabio; Huhn, Katrin (2014): Integrated Stratigraphic and Morphological Investigation of the Twin Slide Complex Offshore Southern Sicily. In: Krastel, Sebastian; Behrmann, Jan-Hinrich; Völker, David; Stipp, Michael; Berndt, Christian; Urgeles, Roger; Chaytor, Jason; Huhn, Katrin; Strasser, Michael; Harbitz, Carl Bonnevie (eds.), Submarine Mass Movements and Their Consequences, Advances in Natural and Technological Hazards Research, 37, Springer International Publishing, Cham, 583-594, https://doi.org/10.1007/978-3-319-00972-8_52
    Publication Date: 2023-03-03
    Description: The Holocene Twin Slides form the most recent of recurrent mass wasting events along the NE portion of Gela Basin within the Sicily Channel, central Mediterranean Sea. Here, we present new evidence on the morphological evolution and stratigraphic context of this coeval slide complex based on deepdrilled sediment sequences providing a 〉100 ka paleo-oceanographic record. Both Northern (NTS) and Southern Twin Slide (STS) involve two failure stages, a debris avalanche and a translational slide, but are strongly affected by distinct preconditioning factors linked to the older and buried Father Slide. Core-acoustic correlations suggest that sliding occurred along sub-horizontal weak layers reflecting abrupt physical changes in lithology or mechanical properties. Our results show further that headwall failure predominantly took place along sub-vertical normal faults, partly through reactivation of buried Father Slide headscarps.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Kuhlmann, Jannis; Asioli, Alessandra; Trincardi, Fabio; Klügel, Andreas; Huhn, Katrin (2015): Sedimentary response to Milankovitch-type climatic oscillations and formation of sediment undulations: evidence from a shallow-shelf setting at Gela Basin on the Sicilian continental margin. Quaternary Science Reviews, 108, 76-94, https://doi.org/10.1016/j.quascirev.2014.10.030
    Publication Date: 2023-03-03
    Description: A multi-proxy chronological framework along with sequence-stratigraphic interpretations unveils composite Milankovitch cyclicity in the sedimentary records of the Last GlacialeInterglacial cycle at NE Gela Basin on the Sicilian continental margin. Chronostratigraphic data (including foraminifera-based eco-biostratigraphy and d18O records, tephrochronological markers and 14C AMS radiometric datings) was derived from the shallow-shelf drill sites GeoB14403 (54.6 m recovery) and GeoB14414 (27.5 m), collected with both gravity and drilled MeBo cores in 193 m and 146 m water depth, respectively. The recovered intervals record Marine Isotope Stages and Substages (MIS) from MIS 5 to MIS 1, thus comprising major stratigraphic parts of the progradational deposits that form the last 100-ka depositional sequence. Calibration of shelf sedimentary units with borehole stratigraphies indicates the impact of higher-frequency (20-ka) sea level cycles punctuating this 100-ka cycle. This becomes most evident in the alternation of thick interstadial highstand (HST) wedges and thinner glacial forced-regression (FSST) units mirroring seaward shifts in coastal progradation. Albeit their relatively short-lived depositional phase, these subordinate HST units form the bulk of the 100-ka depositional sequence. Two mechanisms are proposed that likely account for enhanced sediment accumulation ratios (SAR) of up to 200 cm/ka during these intervals: (1) intensified activity of deep and intermediate Levantine Intermediate Water (LIW) associated to the drowning of Mediterranean shelves, and (2) amplified sediment flux along the flooded shelf in response to hyperpycnal plumes that generate through extreme precipitation events during overall arid conditions. Equally, the latter mechanism is thought to be at the origin of undulated features resolved in the acoustic records of MIS 5 Interstadials, which bear a striking resemblance to modern equivalents forming on late-Holocene prodeltas of other Mediterranean shallow-shelf settings.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 8
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    PANGAEA
    In:  Supplement to: Kuhlmann, Jannis; Huhn, Katrin; Ikari, Matt J (2016): Do embedded volcanoclastic layers serve as potential glide planes? - An integrated analysis from the Gela Basin offshore southern Sicily. In: Lamarche et al. (eds.) Submarine Mass Movements and Their Consequences. Springer, Heidelberg, 41, 273-280, https://doi.org/10.1007/978-3-319-20979-1_27
    Publication Date: 2023-03-03
    Description: To gain information on the role of marine tephra Y-7 in the framework of slope stability and failure initiation, high resolution data on radiodensity and mesoporosity was extracted from a 20 cm CT scan of whole-round section GeoB14403 5P-2. Additionally, three drained direct-shear experiments were performed on samples of this section representing the sedimentary transition from overlying homogeneous background sedimentation of silty clay to the volcanoclastic layer.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Kuhlmann, Jannis; Asioli, Alessandra; Trincardi, Fabio; Klügel, Andreas; Huhn, Katrin (2017): Landslide Frequency and Failure Mechanisms at NE Gela Basin (Strait of Sicily). Journal of Geophysical Research-Earth Surface, 122(11), 2223-2243, https://doi.org/10.1002/2017JF004251
    Publication Date: 2023-03-03
    Description: This study uses an integrated chronological framework from two MeBo boreholes and complementary ultra-high-resolution acoustic profiling in order to assess (1) the frequency of submarine landsliding at the continental margin of NE Gela Basin and (2) the associated mechanisms of failure. Accurate age control was achieved through absolute radiocarbon dating and indirect dating relying on isotope stratigraphic and micropaleontological reconstructions. A total of nine major slope failure events have been recognized that occurred within the last 87 kyr (~10 kyr return frequency), though there is evidence for additional syn-depositional, small-scaled transport processes of lower volume. The majority of recognized events occurred during conditions of sea level fall and lowstand. Preferential failure involves translational movement of mudflows along sub-horizontal key surfaces that are induced by sedimentological changes relating to pre-failure stratal architecture. Along with sequence-stratigraphic boundaries reflecting paleoenvironmental fluctuations, intercalated volcanoclastic layers are shown to be key to the basal confinement and lateral movement of these events. Another major predisposing factor in this area is given by rapid loading of fine-grained homogenous strata and successive generation of excess pore pressure, as expressed by several fluid escape structures. Recurrent failure, however, requires repeated generation of favorable conditions and seismic activity, though low in this area if compared to many other Mediterranean settings, is shown to represent a legitimate trigger mechanism.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 8 datasets
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  • 10
    Publication Date: 2023-03-03
    Description: The southern Tuaheni Landslide Complex (TLC) at the Hikurangi subduction margin displays distinctive morphological features along its distribution over the Tuaheni slope offshore Gisborne, New Zealand. The datasets provide geophysical (MSCL) and geochemical (XRF) core logs from a gravity core transect that systematically samples surficial sediments from the source area to the toe of this landslide complex.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 8 datasets
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