Life under ice in the perennial ice‐covered Lake Glubokoe in Summer ( East Antarctica)

• Published in: Lakes & Reservoirs: Research & Management
• Main Authors: Sharov, Andrey N., Berezina, Nadezhda A., Tolstikov, Aleksey V.
• Other Authors: State Topic of the Zoological Institute RAS, Russian Foundation for Basic Researches
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2015
• Subjects: Austral; East Antarctica; Thala Hills; Antarc*; Antarctica; Enderby Land
• Online Access: http://dx.doi.org/10.1111/lre.12093; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Flre.12093; https://onlinelibrary.wiley.com/doi/pdf/10.1111/lre.12093; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/lre.12093

Abstract This study focuses on hydrological and biotic variables in Lake Glubokoe, which is located in Thala Hills of Enderby Land (East Antarctica). Water and sediment samples and physical measurements were collected once a week in the austral summer (19 December 2010 – 6 February 2011). This lake exhibits perennial ice cover that reached a thickness of 2.5–2.7 m during the study period. A very low concentration of planktonic chlorophyll‐ a (0.06–0.45 μg L −1 ) was measured in the lake, indicating its ultra‐oligotrophic status. The water was poorly populated by algae and metazoans, especially in upper waters below ice cover to a depth of 2 m. Small planktonic organisms (2–5 μm) were observed throughout the study period, but larger organisms (>8 μm) such as the cyanobacteria Planktolyngbya limnetica occurred only during the warmest period (January). Only few individuals of metazoans (rotifers) were found in planktonic samples. Due to deep light penetration (10–15% of incoming active solar radiation reached the depth of 30 m), thick cyanobacterial mats (30 cm) cover all the bottom surface (grey silts) in the lake. Abundant benthic biota associated with these mats was found (up to 1000 ind. m −2 ). Among the benthic metazoans, bdelloid rotifers and tardigrades were the dominating taxa. The results of this study suggest a typical ecological feature of most subglacial lakes in East Antarctica is that metazoans are very poor in the pelagic zone, preferring instead to occupy an area near the lake bottom because of a favourable constant temperature of 4 °C, good level of dissolved oxygen and available food resources as the bacterial detritus.