Diatoms and bacteria have cooccurred in common habitats for hundreds of millions of years,
thus fostering specific associations and interactions with global biogeochemical …

The accumulation of inorganic carbon from seawater by eukaryotic marine phytoplankton is
limited by the diffusion of carbon dioxide (CO2) in water and the dehydration kinetics of …

Humankind will need to remove hundreds of gigatons of carbon dioxide (CO2) from the
atmosphere by the end of the 21st century to keep global warming below 2° C within the …

Carbon dioxide is the most important greenhouse gas after water vapor in the atmosphere of
the earth. More than 98% of the carbon of the atmosphere-ocean system is stored in the …

The alkenone–p CO2 methodology has been used to reconstruct the partial pressure of
ancient atmospheric carbon dioxide (p CO2) for the past 45 million years of Earth's history …

The Dynamic Energy Budget theory unifies the commonalties between organisms, as
prescribed by the implications of energetics, and links different levels of biological …

The reliable and efficient production of microalgae in large-scale commercial culture,
whether in open ponds or in closed photobioreactors, requires a good understanding of the …

According to modelling studies, ocean alkalinity enhancement (OAE) is one of the proposed
carbon dioxide removal (CDR) approaches with large potential, and the beneficial side …

▪ Abstract Many microorganisms possess inducible mechanisms that concentrate CO2 at the
carboxylation site, compensating for the relatively low affinity of Rubisco for its substrate, and …

There is approximately 50 times more inorganic carbon in the global ocean than in the
atmosphere. On time scales of decades to millions of years, the interaction between these …