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  • CI1; CI1_trap; CI2; CI2_trap; CI3; CI3_trap; CI4; CI4_trap; ESTOC; European Station for Time-Series in the Ocean Canary Islands; Silicon Cycling in the World Ocean; SINOPS; Trap; TRAP  (1)
  • Calcium carbonate, flux; Calculated; Calculated, see reference(s); Canary Islands Azores Gibraltar Observations; CANIGO; Carbon, organic, particulate, flux; DATE/TIME; Date/time end; DEPTH, water; Duration, number of days; ESTOC; European Station for Time-Series in the Ocean Canary Islands; LP1; LP1_trap; Mass spectrometer Finnigan Delta Plus; Nitrogen, organic, particulate, flux per day; Sample code/label; Total mass, flux per day; Trap; TRAP; δ15N, gas  (1)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Neuer, Susanne; Ratmeyer, Volker; Davenport, Robert; Fischer, Gerhard; Wefer, Gerold (1997): Deep water particle flux in the Canary Island region: seasonal trends in relation to long-term satellite derived pigment data and lateral sources. Deep Sea Research Part I: Oceanographic Research Papers, 44(8), 1451-1466, https://doi.org/10.1016/S0967-0637(97)00034-4
    Publication Date: 2023-05-12
    Description: We present a 3 year record of deep water particle flux at the recently initiated ESTOC (European Station for Time-series in the Ocean, Canary Islands) located in the eastern subtropical North Atlantic gyre. Particle flux was highly seasonal, with flux maxima occurring in late winter-early spring. A comparison with historic CZCS (Coastal Zone Colour Scanner) data shows that these flux maxima occurred about 1 month after maximum chlorophyll was observed in surface waters in a presumed primary source region 100 km * 100 km northeast of the trap location. The main components of the particles collected with the traps were mineral particles and carbonate, both correlating strongly with organic matter sedimentation. Mineral particles in the sinking matter are indicative of the high aeolian input from the African desert regions. Comparing particle fluxes at 1 km and 3 km depth, we find that particle sedimentation increased substantially with depth. Yearly organic carbon sedimentation was 0.6 g m**-2 at 1 km depth compared with 0.8 g m**-2 at 3 km. We hypothesize that higher phytoplankton biomass observed further north could be a source of laterally advecting particles that interact with fast sinking particles originating from the primary source region. This hypothesis is also supported by the differences in size distribution of lithogenic matter found at the two trap depths.
    Keywords: CI1; CI1_trap; CI2; CI2_trap; CI3; CI3_trap; CI4; CI4_trap; ESTOC; European Station for Time-Series in the Ocean Canary Islands; Silicon Cycling in the World Ocean; SINOPS; Trap; TRAP
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-02-12
    Keywords: Calcium carbonate, flux; Calculated; Calculated, see reference(s); Canary Islands Azores Gibraltar Observations; CANIGO; Carbon, organic, particulate, flux; DATE/TIME; Date/time end; DEPTH, water; Duration, number of days; ESTOC; European Station for Time-Series in the Ocean Canary Islands; LP1; LP1_trap; Mass spectrometer Finnigan Delta Plus; Nitrogen, organic, particulate, flux per day; Sample code/label; Total mass, flux per day; Trap; TRAP; δ15N, gas
    Type: Dataset
    Format: text/tab-separated-values, 284 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
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