Sedimentary and mineral dust sources of dissolved iron to the World Ocean

coupled to a low resolution 3-D GCM ocean including an ocean carbon cycle; a state of the art vegetation model (Sim-CYCLE); and a database of daily temperature, pre- cipitation,

microstructure anaIysis were etched with use or FcCI3 for chromium cast iron and casl stccl padding wcld and Nital for nodular cast imn.. Hopper with

The present symposium is largely devoted to human iron metabolism: the body's requirements for iron, its absorption from food, the turnover of iron compounds and

Here, we investigate the potential evolution of marine N 2 O emissions in the 21st century in response to anthropogenic climate change using the global ocean biogeochemical

Pollard et al., 2009; Zhou et al., 2010, 2013) iron-fertilization experiments in the South- ern Ocean demonstrated the role of iron in enhancing the phytoplankton biomass and

tion and tower aeration. The research contains two parts: 1) a particle fingerprint of the treatment, resulting in a quantification of particles breaking through the rapid

bhlh100/bhlh101 is Hypersensitive to Iron Deficiency To evaluate the potential role of the two iron-starvation induced bHLH transcription factors bHLH100 and bHLH101 in

(2006) observed that 80–90% of the dissolved iron is present under colloidal fraction in the surface waters and 70% in the deep waters in the Atlantic Ocean. A few duplicates of