Articles | Volume 7, issue 8
https://doi.org/10.5194/bg-7-2489-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/bg-7-2489-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
23 Aug 2010
Fractionation of iron species and iron isotopes in the Baltic Sea euphotic zone
J. Gelting
Division of Applied Geology, Luleå University of Technology, Sweden
E. Breitbarth
Division of Applied Geology, Luleå University of Technology, Sweden
Department of Chemistry, University of Gothenburg, Gothenburg, Sweden
Department of Chemistry, University of Otago, Dunedin, New Zealand
B. Stolpe
Department of Chemistry, University of Gothenburg, Gothenburg, Sweden
Department of Marine Science, University of Southern Mississippi, Hattiesburg, USA
M. Hassellöv
Department of Chemistry, University of Gothenburg, Gothenburg, Sweden
J. Ingri
Division of Applied Geology, Luleå University of Technology, Sweden
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- 铁对海洋沉积有机碳保存的影响及其碳汇意义 利. 胡 et al. 10.1360/SSTe-2023-0014
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- Efficient protection of the Baltic Sea needs a revision of phosphorus metric A. Iho et al. 10.1007/s13280-023-01851-2
- Iron‐Mediated Organic Matter Preservation in the Mississippi River‐Influenced Shelf Sediments N. Ghaisas et al. 10.1029/2020JG006089
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- Extreme iron isotope fractionation between colloids and particles of boreal and temperate organic-rich waters S. Ilina et al. 10.1016/j.gca.2012.10.023
- Dissolved Organic Nitrogen Inputs from Wastewater Treatment Plant Effluents Increase Responses of Planktonic Metabolic Rates to Warming R. Vaquer-Sunyer et al. 10.1021/acs.est.5b00674
- Distribution and lability of dissolved iron in surface waters of marginal seas in southeastern Asia K. Jiann & L. Wen 10.1016/j.ecss.2012.01.006
- Organic carbon remobilized from thawing permafrost is resequestered by reactive iron on the Eurasian Arctic Shelf J. Salvadó et al. 10.1002/2015GL066058
- Copper and nickel in ultrafiltered brackish water: Labile or non-labile? H. Österlund et al. 10.1016/j.marchem.2012.02.002
- Iron isotope heterogeneity in pyrite fillings of Holocene worm burrows J. Virtasalo et al. 10.1130/G33556.1
- Trace metals and nutrients in Baltic Sea cyanobacteria: Internal and external fractions and potential use in nitrogen fixation J. Walve et al. 10.1016/j.marchem.2013.11.002
- Sphagnum-dominated bog systems are highly effective yet variable sources of bio-available iron to marine waters R. Krachler et al. 10.1016/j.scitotenv.2016.03.012
- Organic Carbon Concentration in the Northern Coastal Baltic Sea between 1975 and 2011 V. Fleming-Lehtinen et al. 10.1007/s12237-014-9829-y
- Flow field-flow fractionation for the analysis and characterization of natural colloids and manufactured nanoparticles in environmental systems: A critical review M. Baalousha et al. 10.1016/j.chroma.2011.04.063
- Iron distribution and speciation in oxic and anoxic waters of the Baltic Sea C. Pohl & E. Fernández-Otero 10.1016/j.marchem.2012.09.001
- Isotope fractionation between dissolved and suspended particulate Fe in the oxic and anoxic water column of the Baltic Sea M. Staubwasser et al. 10.5194/bg-10-233-2013
- Organic iron complexes enhance iron transport capacity along estuarine salinity gradients of Baltic estuaries S. Herzog et al. 10.5194/bg-17-331-2020
- The effect of iron on the preservation of organic carbon in marine sediments and its implications for carbon sequestration L. Hu et al. 10.1007/s11430-023-1139-9
- The isotopic signature and distribution of particulate iron in the North Atlantic Ocean B. Revels et al. 10.1016/j.dsr2.2014.12.004
- New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments J. Faust et al. 10.1088/1748-9326/aca780
- Distribution and bioavailability of mercury in the surface sediments of the Baltic Sea U. Kwasigroch et al. 10.1007/s11356-021-13023-4
- 铁对海洋沉积有机碳保存的影响及其碳汇意义 利. 胡 et al. 10.1360/SSTe-2023-0014
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