Abstract
A general overview and background of a two-ship study to examine biogeochemical fluxes in the marginal ice-zone of the Bellingshausen Sea (65-70°S; 80-87°W), SE Pacific sector of the Southern Ocean is presented. The major feature studied was an intense band of chlorophyll that was found geographically close to a receding ice-edge. However, the bloom appeared not to be a result of a shallow mixed layer caused by ice-melt stabilisation, but rather associated with an oceanic front that coincided with the ice-edge. Details of the hydrographic conditions existing along the 85°W meridian from the ice-edge to open water to the north, and detailed surveys of surface hydrographic conditions are presented.
| Original language | English |
|---|---|
| Pages (from-to) | 907-932 |
| Number of pages | 26 |
| Journal | Deep-Sea Research Part II |
| Volume | 42 |
| Issue number | 4-5 |
| DOIs | |
| Publication status | Published - 1995 |
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SDG 14 Life Below Water
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