[ 35 ] also described a decreasing trend in phytoplankton biomass (from 2.9 to 0.2 μg L −1 ) in summer 2012 from the BC towards oceanic waters, following the increasing salinity and decreasing trends in particulate organic carbon (POC) and nitrogen (PON), and dissolved organic matter (DOM) [ 35 , 70 ].
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Microbial plankton configuration in the epipelagic realm from the Beagle Channel to the Burdwood Bank, a Marine Protected Area in Sub-Antarctic waters.
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