Dissolved organic matter (DOM) is the strongest light-absorbing component of seawater,
especially in coastal regions, and therefore it plays a dominant role in marine photochemical …

Solar UV radiation, climate and other drivers of global change are undergoing significant
changes and models forecast that these changes will continue for the remainder of this …

Although methanogenesis is considered a strictly anaerobic process, oxygen‐replete
surface open‐ocean waters are usually supersaturated with methane (CH4), a phenomenon …

The ocean is a source of atmospheric carbon monoxide (CO), a key component for the
oxidizing capacity of the atmosphere. It constitutes a minor source at the global scale, but …

Carbonyls have previously been dismissed as significant precursors for carbon monoxide
(CO) photoproduction from natural chromophoric dissolved organic matter (CDOM). Here …

Dimethyl sulfide (DMS) plays an important role in the atmosphere by influencing the
formation of aerosols and cloud condensation nuclei. In contrast, the role of methanethiol …

Marine phytoplankton contribute about one half of global primary production and play a key
role in global biogeochemical cycles. High cell densities in extensive phytoplankton blooms …

Absorption spectra of chromophoric dissolved organic matter (CDOM) and particles were
obtained in May 2007 in the St. Lawrence estuary (SLE, Canada), the northwestern Gulf of …

Biological processes on glacier surfaces affect glacier reflectance, influence surface energy
budget and glacier response to climate warming, and determine glacier carbon exchange …

During the ARK XXV 1+ 2 expedition in the Arctic Ocean carried out in June–July 2010
aboard the R/V Polarstern, we measured carbon monoxide (CO), non-methane …