In this review article, plankton community structure observations are analyzed both for
artificial iron fertilization experiments and also for experiments dedicated to the study of …

Diatoms are a major group of phytoplankton that account for approximately 40% of the
ocean carbon fixation and the vast majority of biogenic silica production through the …

Potential for, and limits to, adaptation to environmental changes are critical for resilience and
risk mitigation. The Mediterranean basin is a mosaic of biodiversity‐rich ecosystems long …

Benthic iron fluxes from sites along the Oregon–California continental shelf determined
using in situ benthic chambers, range from less than 10μmolm− 2d− 1 to values in excess …

Global climate change is predicted to have large effects on the ocean that could cause shifts
in current algal community structure, major nutrient cycles, and carbon export. The Bering …

We conducted a factorial shipboard continuous culture experiment to examine the
interactive effects of altered iron, irradiance and CO2 on the summer phytoplankton …

Though it is clear that plankton in oceanic regions access iron bound to strong organic
ligands, the mechanism mediating the release of iron from these complexes remains …

Zinc (Zn) serves as a cofactor in several extracellular phosphatases, which allow
microorganisms to acquire phosphorus from organic P compounds. In oligotrophic ocean …

The biogeochemical cycle of zinc (Zn) in the South Atlantic, at 40° S, was investigated as
part of the UK GEOTRACES program. To date there is little understanding of the supply of …

The biogeochemical cycling of zinc (Zn) is intimately coupled with organic carbon in the
ocean. Based on an extensive new sedimentary Zn isotope record across Earth's history, we …