TITLE: Palmer LTER: Seasonal and geographic variability in the distribution of Antarctic krill, Euphausia superba, west of the Antarctic Peninsula AUTHOR CM Lascara, EE Hofmann, JM Klinck, RM Ross and LB Quetin PAGE: 161 of SCAR SIXTH BIOLOGY SYMPOSIUM, Antarctic Communities: Species, Structure and Survival ABSTRACT: Acoustic estimates of krill biomass in the waters west of the Antarctic Peninsula were collected during several multidisciplinary cruises to investigate patterns of geographic and seasonal krill distribution in relation to other habitat characteristics; in particular, the concentration and composition of food resources, ice history, large-scale flow regimes, and hydrographic and optical properties of the upper ocean. This study was conducted between November 1991 and September 1993 as part of the Palmer Long-Term Ecological Research (LTER) program and included sampling during all four seasons. Replicate acoustic tows were made over short distances (1-2 km) at stations within a large-scale grid west of the Antarctic Peninsula. The acoustically-derived distributions of krill biomass were analyzed to quantify patch characteristics and to compute the mean biomass (integrated from 10-200 m) at each station. For all cruises combined, over 80% of the 2440 swarms wer < 45 m in horizontal length, < 10 m in vertical thickness, and were positioned < 66 m from the surface. The cumulative frequency distributions of patch characteristics were similar between seasons with the exception that swarms were shallower in the summer and less dense during the winter. The percentage of acoustics events per cruise which were positive (at least one krill swarm) varied with season: 90% in spring and summer, 35% in fall, and 8% in the winter. There was a distinct difference between seasons in the station mean krill biomass (g m-2) which ranged from 0-95 in spring (n=15 stations), 0-460 in summer (n=39), 0-44 in fall (n=96), and 0-80 in winter (n=33). During spring mean krill biomass exceeded 50 g m-2 in three areas: coastal waters near Dallman Bay coincident with high phytoplankton concentrations, open waters within 20 km of the ice edge and an offshore station located over Circumpolar Deep Water. Krill were most abundant during the summer and biomass values exceeding 100 g m-2 were found at the inner stations along most transects, where the influence of ice melt on the hydrographic structure and water column stability was evident.