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  • 2015-2019  (6)
  • 2019  (1)
  • 2017  (2)
  • 2016  (3)
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  • 2015-2019  (6)
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  • 2019  (1)
  • 2017  (2)
  • 2016  (3)
  • 2018  (5)
  • 1
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    PANGAEA
    In:  IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University
    Publication Date: 2024-06-26
    Keywords: AEROS; Aerosol sampler; Aluminium, soluble; Aluminium, standard deviation; Aluminium, total; Ammonium; Ammonium, standard deviation; Calcium; Calcium, standard deviation; Chloride, standard deviation; Chloride in air; Date/time end; Date/time start; Event label; Iron, soluble; Iron, standard deviation; Iron, total; LATITUDE; Latitude 2; LONGITUDE; Longitude 2; Magnesium; Magnesium, standard deviation; Manganese, soluble; Manganese, standard deviation; Manganese, total; Nitrate; Nitrate, standard deviation; Nitrogen, total dissolved; Nitrogen, total dissolved, standard deviation; POS348; POS348_TM01; POS348_TM02; POS348_TM03; POS348_TM04; POS348_TM05; POS348_TM06; POS348_TM07; POS348_TM08; POS348_TM09; POS348_TM10; POS348_TM11; Poseidon; Potassium; Potassium, standard deviation; Sample volume; Sodium; Sodium, standard deviation; SOPRAN; Sulfate; Sulfate, standard deviation; Surface Ocean Processes in the Anthropocene; Titanium, soluble; Titanium, standard deviation; Zinc, soluble; Zinc, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 420 data points
    Location Call Number Limitation Availability
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  • 2
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    Unknown
    PANGAEA
    In:  IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University
    Publication Date: 2024-06-26
    Keywords: 23-10; AEROS; Aerosol sampler; Aluminium, soluble; Aluminium, standard deviation; Bromide; Bromide, standard deviation; Cadmium, soluble; Cadmium, standard deviation; Calcium; Calcium, standard deviation; Chloride, standard deviation; Chloride in air; Cobalt, soluble; Cobalt, standard deviation; Copper, soluble; Copper, standard deviation; Date/time end; Date/time start; Event label; Iron, soluble; Iron, standard deviation; LATITUDE; Latitude 2; Lead, soluble; Lead, standard deviation; LONGITUDE; Longitude 2; Magnesium; Magnesium, standard deviation; Manganese, soluble; Manganese, standard deviation; Nickel, soluble; Nickel, standard deviation; Nitrate; Nitrate, standard deviation; Oxalate; Oxalate, standard deviation; POS399/2; POS399/2_TM01; POS399/2_TM02; POS399/2_TM03; POS399/2_TM04; POS399/2_TM05; POS399/2_TM06; POS399/2_TM07; POS399/2_TM08; POS399/2_TM09; POS399/2_TM10; POS399/2_TM11; POS399/2_TM12; POS399/3; POS399/3_TM13; POS399/3_TM14; POS399/3_TM15; POS399/3_TM16; Poseidon; Potassium; Potassium, standard deviation; Quality code; Sample volume; Sodium; Sodium, standard deviation; SOPRAN; Sulfate; Sulfate, standard deviation; Surface Ocean Processes in the Anthropocene; Thorium, soluble; Thorium, standard deviation; Titanium, soluble; Titanium, standard deviation; Vanadium, soluble; Vanadium, standard deviation; Zinc, soluble; Zinc, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 768 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2021-04-23
    Description: Anthropogenic emissions completely overwhelmed natural marine lead (Pb) sources during the past century, predominantly due to leaded petrol usage. Here, based on Pb isotope measurements, we reassess the importance of natural and anthropogenic Pb sources to the tropical North Atlantic following the nearly complete global cessation of leaded petrol use. Significant proportions of up to 30–50% of natural Pb, derived from mineral dust, are observed in Atlantic surface waters, reflecting the success of the global effort to reduce anthropogenic Pb emissions. The observation of mineral dust derived Pb in surface waters is governed by the elevated atmospheric mineral dust concentration of the North African dust plume and the dominance of dry deposition for the atmospheric aerosol flux to surface waters. Given these specific regional conditions, emissions from anthropogenic activities will remain the dominant global marine Pb source, even in the absence of leaded petrol combustion.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2021-04-23
    Description: The supply and bioavailability of iron (Fe) controls primary productivity and N2-fixation in large parts of the global ocean. An important, yet poorly quantified, source to the ocean is particulate Fe (pFe). Here we present the first combined dataset of particulate, labile-particulate (L-pFe) and dissolved Fe (dFe) from the (sub)-tropical North Atlantic. We show a strong relationship between L-pFe and dFe, indicating a dynamic equilibrium between these two phases whereby particles ‘buffer’ dFe and maintain the elevated concentrations observed. Moreover, L-pFe can increase the overall ‘available’ (L-pFe + dFe) Fe pool by up to 55%. The lateral shelf flux of this available Fe was similar in magnitude to observed soluble aerosol-Fe deposition, a comparison that has not been previously considered. These findings demonstrate that L-pFe is integral to Fe cycling and hence plays a role in regulating carbon cycling, warranting its’ inclusion in Fe budgets and biogeochemical models.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2021-04-23
    Description: Stable isotope compositions can potentially be used to trace atmospheric Cd inputs to the surface ocean and anthropogenic Cd emissions to the atmosphere. Both of these applications may provide valuable insights into the effects of anthropogenic activities on the cycling of Cd in the environment. However, a lack of constraints for the Cd isotope compositions of atmospheric aerosols is currently hindering such studies. Here, we present stable Cd isotope data for aerosols collected over the Tropical Atlantic Ocean. The samples feature variable proportions of mineral dust-derived and anthropogenic Cd, yet exhibit similar isotope compositions, thus negating the distinction of these Cd sources using isotopic signatures in this region. Isotopic variability between these two atmospheric Cd sources may be identified in other areas, and thus warrants further investigation. Regardless, these data provide important initial constraints on the isotope composition of atmospheric Cd inputs to the ocean.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2022-01-31
    Description: The marine iodine cycle has significant impacts on air quality and atmospheric chemistry. Specifically, the reaction of iodide with ozone in the top few micrometres of the surface ocean is an important sink for tropospheric ozone (a pollutant gas) and the dominant source of reactive iodine to the atmosphere. Sea surface iodide parameterisations are now being implemented in air quality models, but these are currently a major source of uncertainty. Relatively little observational data is available to estimate the global surface iodide concentrations, and this data has not hitherto been openly available in a collated, digital form. Here we present all available sea surface (〈20 m depth) iodide observations. The dataset includes values digitised from published manuscripts, published and unpublished data supplied directly by the originators, and data obtained from repositories. It contains 1342 data points, and spans latitudes from 70°S to 68°N, representing all major basins. The data may be used to model sea surface iodide concentrations or as a reference for future observations.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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