Food availability to an Adamussium bed during the austral summer 1993/1994(Terra Nova Bay, Ross Sea)

In the framework of the ROSSMIZE Project (Ross Sea Marginal Ice Zone Ecolog y) of the Italian Antarctic Research Programme (PNRA), the organic matter f lux through the water column and its role on benthic communities have been taken in particular account. During the austral Summer 1993-1994, from Dece mber 27, 1993 to February 11, 1994, a study on this flux in shallow waters was carried out, in a station close to Terra Nova Bay Italian base (Ross Se a), at 40 m depth. This site is characterized by the filter-feeding Adamuss ium colbecki, a scallop which reaches high values of density (60 ind/m(2)) and biomass (120 g DW/m(2)). At the beginning of the sampling period, a sed iment trap was positioned on the sea-bottom and samples were collected ever y 3-5 days, as well as temperature, salinity and fluorescence data from sea surface to bottom. Fluorescence profiles put in evidence a phytoplankton b loom occurring during the maximum water column stratification, in the last decade of January. Organic matter Bur through the water column showed rathe r constant values up to the 24th of January. Immediately after, a sudden in crease took place (24-29 January), reaching 13.55 g/m(2)/d for TSM, 0.24 g/ m(2)/d for lipids, 0.53 g/m(2)/d for proteins, 0.37 g/m(2)/d for carbohydra tes, 0.69 g/m(2)/d and 0.1 g/m(2)/d for POC and PON, respectively, 0.5 and 2.8 mg/m(2)/d for chlorophyll-a and phaeopigments, in correspondence to the fluorescence-peak occurring in the same period. A. large part of the total flux was represented by oval faecal pellets, as accounted by microscopical observations of sedimented material. Most of the pellets were 200-300 mu m long, filled mainly by diatom frustules.