The need for more effective environmental monitoring of the open and coastal ocean has
recently led to notable advances in satellite ocean color technology and algorithm research …

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 …

The addition of iron to high-nutrient, low-chlorophyll regions induces phytoplankton blooms
that take up carbon,,. Carbon export from the surface layer and, in particular, the ability of the …

We report results collected year‐round since 1998 in northern Marguerite Bay, just inside
the Antarctic Circle. The magnitude of the spring phytoplankton bloom is much reduced …

Most of our knowledge about deep-sea habitats is limited to bathyal (200–3000 m) and
abyssal depths (3000–6000 m), while relatively little is known about the hadal zone (6000 …

The annual phytoplankton bloom occurring north of the Crozet Plateau provides a rare
opportunity to examine the hypothesis that natural iron fertilization can alleviate high-nutrient …

Most of the Southern Ocean is a high‐nutrient, low‐chlorophyll (HNLC) area. There are
exceptions to this situation downstream of some of the islands, where iron from the islands …

This special issue describes the findings of the first planned natural iron fertilisation
experiment in the Southern Ocean, the CROZet natural iron bloom and EXport experiment …

The production of organic carbon in the ocean's surface and its subsequent downward
export transfers carbon dioxide to the deep ocean. This CO2 drawdown is countered by the …

Elevated levels of productivity in the wake of Southern Ocean island systems are common
despite the fact that they are encircled by high-nutrient low-chlorophyll (HNLC) waters. In the …