Iron (Fe) is the fourth most abundant element on earth and represents an essential nutrient
for life. As a fundamental mineral element for cell growth and development, iron is available …

Diatoms and bacteria have coexisted and coevolved for more than 200 million years, and
their interactions have driven the processes of underlying major biogeochemical cycles …

Iron is one of the most abundant elements on Earth, and it is essential for life. Despite the
abundance of iron, its chemistry leads to very limited bioavailability, which has resulted in …

Specific bacterial species induce algal blooms by producing growth-promoting substances,
such as siderophores, under iron-limited conditions. However, the molecular mechanisms …

The simultaneous limitation of productivity by two or more nutrients, commonly referred to as
nutrient co-limitation, affects microbial communities throughout the marine environment and …

In the field of bone substitution, calcium carbonate cements have been proposed as
bioactive mineral cements complementary to calcium phosphate cements for applications …

Iron (Fe) is a growth-limiting micronutrient for phytoplankton in major areas of oceans and
deposited wind-blown desert dust is a primary Fe source to these regions. Simulated …

The oceanic acidification and coastal hypoxia have potential to enhance biological uptake of
dissolved iron (Fe) by phytoplankton. In this study, the Fe uptake rate (FeUR) in Daya Bay …

Both bioavailable iron (Fe) and water stability have been proposed to regulate primary
production in large parts of the Southern Ocean. Freshwater is not only an important factor …

Coastal upwelling currents such as the California Current System (CCS) comprise some of
the most productive biological systems on the planet. Diatoms dominate these upwelling …