Ea. Romankevich et Vi. Peresypkin, DISSOLVED AND SUSPENDED PARTICULATE ORGAN IC-MATTER IN ANTARCTIC WATERS OF THE ATLANTIC-OCEAN, Okeanologia, 33(6), 1993, pp. 863-870
On the basis of 332 analyses of dissolved (DOS) and particulate organi
c carbon (POC) taken from the surface to 4785 m depth at 10 stations o
f the Atlantic part of the Antarctic Ocean, the following regularities
were determined: low DOC concentrations, a sharp decrease in the uppe
r 40 - 120 m layer, small variability values in the Antarctic divergen
ce zone, the lack of correlation between DOC and phytoplankton primary
production. A decrease in depth of average POC concentrations with a
small gradient in the 0 - 200 m water layer, an increase of POC concen
trations in the pycnocline and during phytoplankton bloom were found.
The Antarctic Ocean is characterized, as a whole, by small POC concent
rations close to the average values for the World Ocean. Analysis of t
he measurements of variations of DOC and POC concentrations made on th
e ship's route in the surface layers of the Indian and the Atlantic oc
eans was considered.