The CO2 uptake by the Southern Ocean (< 35° S) varies substantially on all timescales and
is a major determinant of the variations of the global ocean carbon sink. Particularly strong …

Global climate and the atmospheric partial pressure of carbon dioxide () are correlated over
recent glacial cycles, with lower during ice ages, but the causes of the changes are …

This chapter addresses the biogeochemical cycles of carbon dioxide (CO2), methane (CH4),
and nitrous oxide (N2O). The three greenhouse gases have increased in the atmosphere …

The Southern Ocean plays a critical role in regulating global climate as a major sink for
atmospheric carbon dioxide (CO2), and in global ocean biogeochemistry by supplying …

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 …

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 …

Diatoms are a type of microalgae with diverse capabilities which make them useful for
multiple applications. The abundance of diatoms in water bodies facilitates the removal of …

Dust has the potential to modify global climate by influencing the radiative balance of the
atmosphere and by supplying iron and other essential limiting micronutrients to the ocean …

The silicon isotope composition of biogenic silica (δ 30 Si BSi) in the ocean is a function of
the δ 30 Si of the available dissolved Si (DSi; H 2 SiO 4), the degree of utilisation of the …