Austral fall-winter transition of mesozooplankton assemblages and krill aggregations in an embayment west of the Antarctic Peninsula

• Published in: Marine Ecology Progress Series
• Main Authors: ESPINASSE, Boris, ZHOU, Meng, ZHU, Yiwu, HAZEN, Elliott L., FRIEDLAENDER, Ari S., NOWACEK, Douglas P., CHU, Dezhang, CARLOTTI, Francois
• Format: Other/Unknown Material
• Language: English
• Published: Inter Research 2012
• Subjects: Antarctic Peninsula; Chlorophyll; Zooplankton; Krill; Food web; Austral fall; Sciences du Vivant [q-bio]/Ecologie; Environnement/Ecosystèmes; Sciences de l'environnement/Biodiversité et Ecologie; Antarctic; Austral; Inner Bay; The Antarctic; Wilhelmina; Wilhelmina Bay; Antarc*; Antarctic Krill; Euphausia superba; Humpback Whale; Megaptera novaeangliae
• Online Access: https://oskar-bordeaux.fr/handle/20.500.12278/28299; https://doi.org/10.3354/meps09626

To assess krill aggregations and humpback whale Megaptera novaeangliae foraging behavior, spatial and temporal relationships between Antarctic krill Euphausia superba and zooplankton taxonomic groups were studied during an interdisciplinary cruise conducted in May and June 2009 within Wilhelmina Bay on the western side of the Antarctic Peninsula. A vesselmounted acoustic Doppler current profiler (ADCP) and a calibrated EK-60 echo sounder were used to assess circulation patterns and krill distributions in the bay, and a multiple opening and closing net (with 333 μm mesh) and environmental sensing system (MOCNESS) was used to collect live samples of mesozooplankton and krill for taxonomic composition analysis. The results from this field study complement a previous one that examined an anticyclonic bay-scale circulation of Antarctic krill. This super-aggregation of krill covered ~100 km2, had a concentration of 1000s of individuals m-2 and was associated with more than 306 humpback whales present in Wilhelmina Bay. Our results from the mesozooplankton study revealed that krill continuously conducted diel vertical migrations and formed aggregations in the inner bay, while the chlorophyll concentration at the surface decreased from 2.2 to 0.6 g C m−2 due to the decrease of daylight, and zooplankton concentrations increased from 0.5 to 1.5 g C m−2 probably from advective influx. Most zooplankton were distributed below 200 m while krill fed in the upper 150 m. The spatial and temporal correlations between krill and small- to medium-sized mesozooplankton imply that krill may become omnivorous when there is a lack of phytoplankton in the late austral fall. Though both phytoplankton and zooplankton biomasses contributed only small fractions of the daily ration needed for krill metabolism in Wilhelmina Bay, it is not clear what caused krill to aggregate on such a large scale, as this led to high mortality as a result of starvation and predation by whales and other top predators.