Seasonal variation of diel vertical migration of zooplankton from ADCP backscatter time series data in the Lazarev Sea, Antarctica

• Published in: Deep Sea Research Part I: Oceanographic Research Papers
• Main Authors: Cisewski, Boris, Strass, Volker, Rhein, M., Krägefsky, Sören
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2010
• Subjects: Austral; Greenwich; Lazarev; Lazarev Sea; Antarc*; Antarctica; Sea ice
• Online Access: https://epic.awi.de/id/eprint/19768/; https://epic.awi.de/id/eprint/19768/1/Cis2008b.pdf; https://doi.org/10.1016/j.dsr.2009.10.005; https://hdl.handle.net/10013/epic.33898; https://hdl.handle.net/10013/epic.33898.d001

Ten-month time series of mean volume backscattering strength (MVBS) and vertical velocity obtained from three moored acoustic Doppler current profilers (ADCPs) deployed from February until December 2005 at 64°S, 66.5°S and 69°S along the Greenwich Meridian were used to analyse the diel vertical zooplankton migration (DVM) and its seasonality and regional variability in the Lazarev Sea. The estimated MVBS exhibited distinct patterns of DVM at all three mooring sites. Between February and October, the timing of the DVM and the residence time of the zooplankton at depth were clearly governed by the day-night rhythm. Mean daily cycles of the ADCP-derived vertical velocity were calculated for successive months and showed maximum ascent and descent velocities of 16 and -15 mm s-1. However, a change of the MVBS pattern occurred in late spring/early austral summer (October/November), when the zooplankton communities ceased their synchronous vertical migration at all three mooring sites. Elevated MVBS values then were concentrated in the uppermost layers (<50 meters) at 66.5°S. This period coincided with the decay of the sea ice coverage at 64°S and 66.5°S between early November and mid-December. Elevated chlorophyll concentrations, which were measured at the end of the deployment, extended from 67°S to 65°S and indicated a phytoplankton bloom in the upper 50 meters. Thus, we propose that the increased food supply associated with an ice edge bloom caused the zooplankton communities to cease their DVM in favour of feeding.