Macrobenthos from the Novaya Zemlya Trough, Kara Sea, supplement to: Galkin, Sergey V; Savilova, Tatyana A; Moskalev, Lev I; Kucheruk, Nikita V (2010): Macrobenthos of the Novaya Zemlya Trough. Translated from Okeanologiya, 2010, 50(6), 982-993, Oceanology, 50(6), 933-944

• Main Authors: Galkin, Sergey V, Savilova, Tatyana A, Moskalev, Lev I, Kucheruk, Nikita V
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2010
• Subjects: Multiple investigations; AMK54; Akademik Mstislav Keldysh; Archive of Ocean Data ARCOD; Kara Sea; Nikita; Novaya Zemlya Trough; Novaya Zemlya
• Online Access: https://dx.doi.org/10.1594/pangaea.769942; https://doi.pangaea.de/10.1594/PANGAEA.769942

During Cruise 54 of R/V Akademik Mstislav Keldysh macrobenthos of the Novaya Zemlya Trough was studied with use of a Sigsby trawl along a submeridional transect near 75°30'N at depth range from 68 to 362 m. In total 140 species of bottom animals were found. Relative role of taxons was assessed using three parameters: abundance, biomass, and energy flow. Similarity of the parameters was used for comparison of samples. New material greatly contributes to data on composition of fauna and structure of communities of the studied region. It was revealed that small scyphozoid polyps and sipunculoids play an important role in the trough's community. Presence of a community dominated by Ophiocten sericeum (with important role of small bivalves) was revealed for the first time not only at the eastern by also at the western slope of the Novaya Zemlya Trough. The sharpest changes in composition and structure of the bottom community were confined to a zone of transition from the trough floor to the slope. These changes are determined by specificity of the macrorelief (of the floor and slope), composition of ground (soft brown silts abound in rhizopods and dense gray silts with admixture of pebbles), and possibly by hydrodynamic processes near the bottom.