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  • 2020-2023  (2)
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  • 1
    Publication Date: 2022-07-15
    Description: Summary Cruise MSM96 sailed to assess small-and large-scale geochemical and seafloor substrate heterogeneity across the NE Atlantic basin. Weemployed a hierarchical surveying strategy at three spatial scales: local, regional, and basin,to investigatetrace metaland Rare Earth Element and Yttrium concentrationsand patterns. At each of the survey sitesPorcupine Abyssal Plain and Iberian Abyssal Plain, we sampledcovering three data resolution scales: centimeter (TV-MUC), meter (OFOS), and kilometer scale (MBES). Our objective was to quantify the impact of topography on the geochemistry within and between regions and to establish the link –across resolution scales –between geochemistry, imagery,and bathymetrytofacilitate spatial extrapolation of seafloor geochemical dataand substrate characteristics to kilometer-scale.We studied three topography types: valleys, plains,and hills. Theirlocation was objectively chosen bya geomorphons terrain classification.By studying heterogeneity on the local and regional scales, we focused on topographic heterogeneity because spatial heterogeneity with respect to particle and organic matter flux from the sea surface can be expected to be minimal.As a basis, solid-phase and pore-watersamples were taken for on-shore lab analyses of porosity, major elements,total organic carbon, nitrate, anddissolved Mn and Fe.This basic data helps to assess REY controls in the solid phase and pore water. All geochemical parameters together will be used to assess local-to basin-scale heterogeneity and how it is linked to topography.In the future, this should be extended to also incorporate, e.g., oceanography, minerology, microbiology, and eventually link all these parameters across scales.
    Type: Report , NonPeerReviewed , info:eu-repo/semantics/book
    Format: text
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  • 2
    Publication Date: 2022-01-06
    Description: Deep sea mining for poly-metallic nodules impacts the environment in many ways. A key potential hazard is the creation of a sediment plume from resuspending sediment during seabed mining. The resuspended matter disperses with currents but eventually resettles on the seabed. Resettling causes a blanketing of the seafloor environment, potentially causing harm to in-, epi- and hyperbenthic communities with possible cascading effects into food webs of deep sea habitats. Mapping the extent of such blanketing is thus an important factor in quantifying potential impacts of deep-sea mining.One technology that can assess seabed blanketing is optical imaging with cameras at square-kilometre scale. To efficiently analyse the resulting Terabytes of image data with minimized bias, automated image analysis is required. Moreover, effective quantitative monitoring of the blanketing requires ground truthing of the image data. Here, we present results from a camera-based monitoring of a deep-sea mining simulation combined with automated image analysis using the CoMoNoD method and low-cost seabed sediment traps for quantification of the blanketing thickness. We found that the impacted area was about 50 percent larger than previously determined by manual image annotation.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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