Since the mid-1980s, our understanding of nutrient limitation of oceanic primary production
has radically changed. Mesoscale iron addition experiments (FeAXs) have unequivocally …

Polar organisms have adapted their seasonal cycles to the dynamic interface between ice
and water. This interface ranges from the micrometre-sized brine channels within sea ice to …

Aquatic Photosynthesis is a comprehensive guide to understanding the evolution and
ecology of photosynthesis in aquatic environments. This second edition, thoroughly revised …

Ocean Biogeochemical Dynamics provides a broad theoretical framework upon which
graduate students and upper-level undergraduates can formulate an understanding of the …

The rise of angiosperms during the Cretaceous period is often portrayed as coincident with a
dramatic drop in the diversity and abundance of many seed-free vascular plant lineages …

Estimates of primary production in the Southern Ocean are difficult to obtain but are
essential if we are to understand its role in the global carbon cycle. Here we present a 9 …

The availability of iron limits primary productivity and the associated uptake of carbon over
large areas of the ocean. Iron thus plays an important role in the carbon cycle, and changes …

Despite the growing number of in situ iron fertilization experiments, the efficiency of such
fertilization to sequester atmospheric CO2 remains largely unknown. For the first time, a …

Comparison of eight iron experiments shows that maximum Chl a, the maximum DIC
removal, and the overall DIC/Fe efficiency all scale inversely with depth of the wind mixed …

The availability of iron is known to exert a controlling influence on biological productivity in
surface waters over large areas of the ocean and may have been an important factor in the …