The ocean is warming, losing oxygen and being acidified, primarily as a result of
anthropogenic carbon emissions. With ocean warming, acidification and deoxygenation …

Organic matter (OM) plays a significant role in the formation of oxygen minimum zones
(OMZs) and associated biogeochemical cycling. OM supply processes to the OMZ include …

Marine particles of different nature are found throughout the global Ocean. The term" marine
particles" describes detritus aggregates, fecal pellets, but also bacterio-, phyto-, zooplankton …

Gelatinous zooplankton can be present in high biomass and taxonomic diversity in
planktonic oceanic food webs, yet the trophic structuring and importance of this “jelly web” …

Oceanic eddies are recognized as pivotal components in marine ecosystems, believed to
concentrate a wide range of marine life spanning from phytoplankton to top predators …

Subsurface eddies are known features of ocean circulation, but the sparsity of observations
prevents an assessment of their importance for biogeochemistry. Here we use a global …

Mesoscale eddies are energetically dominant and pervasive over most of the world's
oceans. Among them, many are subsurface intensified with strongest signals in the ocean …

The patterns of species diversity of plankton functional groups (PFGs) remain poorly
understood although they matter greatly for marine ecosystem functioning. Here, we use an …

The temporal evolution of the physical and biogeochemical structure of an oxygen-depleted
anticyclonic modewater eddy is investigated over a 2-month period using high-resolution …

Subsurface-intensified anticyclones are ubiquitous in the ocean, yet their impact on the large-
scale transport of heat, salt and chemical tracers is poorly understood. These submesoscale …