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Iron and light limitation of phytoplankton growth off East Antarctica Journal of Marine Systems, 2022 (Ref: 16547)
Category 1: Peer-reviewed literature

Phytoplankton production controls the transfer of carbon dioxide from the atmosphere into the ocean through the biological carbon pump, facilitating the sequestration of carbon dioxide and thus, contributing to the regulation of global climate. In the Southern Ocean…

Effects of ocean alkalinity enhancement on plankton in the Equatorial Pacific Communications Earth and Environment, 2025 (Ref: 17329)
Category 1: Peer-reviewed literature

Ocean alkalinity enhancement is a potential strategy for gigatonne-scale atmospheric carbon dioxide removal. It uses alkaline substances to convert seawater carbon dioxide into (bi)carbonate, enabling uptake of additional carbon dioxide from the atmosphere.

Microbial competition for iron determines its availability to the ferrous wheel The ISME Journal, 2025 (Ref: 17280)
Category 1: Peer-reviewed literature

Iron plays a pivotal role in regulating ocean primary productivity. Iron is supplied from diverse sources such as the atmosphere and the geosphere, and hence iron biogeochemical research has focused on identifying and quantifying such sources of "new" iron. However…

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…

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