Microbial plankton respiration is the key determinant in the balance between the storage of
organic carbon in the oceans or its conversion to carbon dioxide with accompanying …

The climate in the Arctic is changing faster than anywhere else on earth. Poorly understood
feedback processes relating to Arctic clouds and aerosol–cloud interactions contribute to a …

Although plastic is ubiquitous in marine systems, our current knowledge of transport
mechanisms is limited. Much of the plastic entering the ocean sinks; this is intuitively obvious …

Predicting the magnitude of herbicide impacts on marine primary productivity remains
challenging because the extent of worldwide herbicide pollution in coastal waters and the …

Marine heatwaves are increasing in frequency and intensity as climate change progresses,
especially in the highly productive Arctic regions. Although their effects on primary producers …

The Arctic is warming faster than anywhere else on Earth, prompting glacial melt, permafrost
thaw, and sea ice decline. These severe consequences induce feedbacks that contribute to …

Microplastics (MPs) overlap in size with phytoplankton and can be ingested by zooplankton,
transferring them to higher trophic levels. Copepods are the most abundant metazoans …

Arsenic (As) uptake by plants is largely influenced by the presence of microbial consortia
and their interactions with As. In the coastal region of Bengal deltaic plain of Eastern India …

Dissolved organic matter (DOM) plays important roles in the aquatic biogeochemical cycle
and the global carbon cycle. However, it is highly spatially and temporally varied due to …

Dissolved organic matter (DOM) changes in quantity and quality over time and space,
especially in highly dynamic coastal estuaries. Bacterioplankton usually display seasonal …