Coastal Plankton Assemblages in the Vicinity of Galindez Island and Neumayer Channel (Western Antarctic Peninsula) during the First Joint Turkish - Ukrainian Antarctic Research Expedition

• Published in: Turkish Journal of Fisheries and Aquatic Sciences
• Main Authors: Yilmaz, Izzet Noyan, Ergul, Halim Aytekin, Mavruk, Sinan, Tas, Seyfettin, Aker, Halim Vedat, Yildiz, Melek, Ozturk, Bayram
• Other Authors: Çukurova Üniversitesi
• Format: Article in Journal/Newspaper
• Language: English
• Published: CENTRAL FISHERIES RESEARCH INST 2018
• Subjects: Antarctica; Galindez Island; Vernadsky Research Base; phytoplankton; zooplankton; hydrography; Antarctic; Antarctic Peninsula; Austral; Galindez; Neumayer; Neumayer Channel; Ushuaia; Antarc*; Copepods
• Online Access: https://hdl.handle.net/20.500.12605/9401; https://doi.org/10.4194/1303-2712-v18_4_09

WOS: 000422953000009 Western Antarctic Peninsula is one of the fastest warming areas on Earth and coastal areas of the region are foremost affected. Here we present the state of coastal plankton assemblages of the Galindez Island and Neumayer Channel, Western Antarctic Peninsula in austral autumn (April 2016). Surface water temperatures were ranged between -0.12 degrees C and -0.97 degrees C and average chlorophyll-a concentrations were 0.65 mu g/l. A total of 50 phytoplankton and 24 zooplankton taxa (15 copepods and 9 meroplanktonic species) were identified during the sampling period. Diatom species (78%) predominated phytoplankton and the highest abundance was 820 cells l(-1), while the highest number of phytoplankton species was 42. Zooplankton was prevailed by the dominance of copepods, except contribution of meroplankton at the Neumayer channel. Highest zooplankton abundance was 101 ind.m(-3). The sampling season was the transition period from the productive spring-summer to dormant winter conditions, which explains the low abundances registered, however, on contrary to low cell abundances, diversity was high within plankton. Scientific Research Projects Coordination Unit of Istanbul UniversityIstanbul University [FOA-2016-20530]; Scientific Research Projects Coordination Unit of Kocaeli UniversityKocaeli University [KOU-BAPB-2016/026]; Scientific Research Projects Coordination Unit of Cukurova UniversityCukurova University [FBA-2016-6205]; first joint Turkish-Ukrainian Antarctic Research Expedition This work is supported by the Scientific Research Projects Coordination Unit of Istanbul University (FOA-2016-20530), Scientific Research Projects Coordination Unit of Kocaeli University (KOU-BAPB-2016/026), Scientific Research Projects Coordination Unit of Cukurova University (FBA-2016-6205) and the first joint Turkish-Ukrainian Antarctic Research Expedition. Authors thank the captain and crew of M/V Ushuaia, as well as the Turkish and Ukrainian authorities for their valuable help and support.