Despite the huge extent of the ocean's surface, until now relatively little attention has been
paid to the sea surface microlayer (SML) as the ultimate interface where heat, momentum …

Ocean current is one of the major drivers of water mass, energy, and biogeochemical cycles
in the global ocean–atmosphere boundary layer and also a key variable in the formation of …

A carbon budget for the northwest European continental shelf seas (NWES) was
synthesized using available estimates for coastal, pelagic and benthic carbon stocks and …

Long-term secular variation in the isotopic composition of seawater fixed nitrogen (N) is
poorly known. Here, we document variation in the N-isotopic composition of marine …

Highlights•Climate change will enhance methane emission from wetlands.•Effects of climate
change on methane emission from soils are contradictory.•Effect of nitrogen on methane …

Coastal seas may account for more than 75% of global oceanic methane emissions. There,
methane is mainly produced microbially in anoxic sediments from which it can escape to the …

The impact of anthropogenic ocean acidification (OA) on marine ecosystems is a vital
concern facing marine scientists and managers of ocean resources. Euthecosomatous …

The air–sea exchange and oceanic cycling of greenhouse gases (GHG), including carbon
dioxide (CO2), nitrous oxide (N2O), methane (CH4), carbon monoxide (CO), and nitrogen …

Oxygen-deficient zones (ODZs) are major sites of net natural nitrous oxide (N 2 O)
production and emissions. In order to understand changes in the magnitude of N 2 O …

Global atmospheric methane concentrations have continued to rise in recent years, having
already more than doubled since the Industrial Revolution. Further environmental change …