ArticleBiogeochemistry2017
Stability of dissolved and soluble Fe(II) in shelf sediment pore waters and release to an oxic water column.
Article in Biogeochemistry, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 10 papers.
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Who cites it
10 citing papers in PubMed.
- Contrasting microbial iron metabolism in sediments from oxic and hypoxic estuaries.Frontiers in microbiology · 2026Article
- Non-Nitrogen-Fixers or Nitrogen-Fixers? Factors Distinguishing the Dominance of Chroococcal and Diazotrophic Cyanobacterial Species.International journal of environmental research and public health · 2022Article
- Constraints on the Cycling of Iron Isotopes From a Global Ocean Model.Global biogeochemical cycles · 2021Article
- Iron colloids dominate sedimentary supply to the ocean interior.Proceedings of the National Academy of Sciences of the United States of America · 2021Article
- The eastern extent of seasonal iron limitation in the high latitude North Atlantic Ocean.Scientific reports · 2019Article
- A mesocosm study of oxygen and trace metal dynamics in sediment microniches of reactive organic material.Scientific reports · 2017Article
- Comparing benthic biogeochemistry at a sandy and a muddy site in the Celtic Sea using a model and observations.Biogeochemistry · 2017Article
- Benthic pH gradients across a range of shelf sea sediment types linked to sediment characteristics and seasonal variability.Biogeochemistry · 2017Article
- An approach for the identification of exemplar sites for scaling up targeted field observations of benthic biogeochemistry in heterogeneous environments.Biogeochemistry · 2017Article
- Oxygen dynamics in shelf seas sediments incorporating seasonal variability.Biogeochemistry · 2017Article
Corrections and comments
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Authors and funding
13 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Shelf sediments underlying temperate and oxic waters of the Celtic Sea (NW European Shelf) were found to have shallow oxygen penetrations depths from late spring to late summer (2.2-5.8 mm below seafloor) with the shallowest during/after the spring-bloom (mid-April to mid-May) when the organic carbon content was highest. Sediment porewater dissolved iron (dFe, <0.15 µm) mainly (>85%) consisted of Fe(II) and gradually increased from 0.4 to 15 μM at the sediment surface to ~100-170 µM at about 6 cm depth. During the late spring this Fe(II) was found to be mainly present as soluble Fe(II) (>85% sFe, <0.02 µm). Sub-surface dFe(II) maxima were enriched in light isotopes (δ
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