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Biological Uptake, Water Mass Mixing and Scavenging Limit the Transport of Manganese-Rich Waters From the East Antarctic Shelf. Global Biogeochemical Cycles, 2023 (Ref: 17119)
Category 1: Peer-reviewed literature

Manganese (Mn) is an essential element involved in photosynthesis, yet its concentrations in Southern Ocean open waters are very low, arising from biological uptake and limited external inputs. At southern latitudes…

Circumpolar Deep Water and Shelf Sediments Support Late Summer Microbial Iron Remineralization Global Biochemical Cycles, 2021 (Ref: 16549)
Category 1: Peer-reviewed literature

Despite widespread iron (Fe) limitation in the Southern Ocean, intense phytoplankton blooms are observed around productive coastal regions such as the Mertz Polynya (off George V Land and Adelie Land, East Antarctica; 140–155°E). Sources of Fe across coastal East Antarctica vary…

Identifying potential sources of iron-binding ligands in coastal Antarctic environments and the wider Southern Ocean Frontiers of Marine Science, 2022 (Ref: 16599)
Category 1: Peer-reviewed literature

The availability of iron (Fe) to marine microbial communities is enhanced through complexation by ligands. In Fe limited environments, measuring the distribution and identifying the likely sources of ligands is therefore central to understanding the drivers of marine productivity.

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