Density and distribution of megafauna at the Håkon Mosby mud volcano (the Barents Sea) based on image analysis

• Published in: Biogeosciences
• Main Authors: E. Rybakova (Goroslavskaya), S. Galkin, M. Bergmann, T. Soltwedel, A. Gebruk
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2013
• Subjects: Ecology; QH540-549.5; Life; QH501-531; Geology; QE1-996.5; Barents Sea; Bear Island
• Online Access: https://doi.org/10.5194/bg-10-3359-2013; https://doaj.org/article/1d6bc3e1be914ea3aa87d6bbde718ead

During a survey of the Håkon Mosby mud volcano (HMMV), located on the Bear Island fan in the southwest Barents Sea at ∼1250 m water depth, different habitats inside the volcano caldera and outside it were photographed using a towed camera platform, an Ocean Floor Observation System (OFOS). Three transects were performed across the caldera and one outside, in the background area, each transect was ∼2 km in length. We compared the density, taxa richness and diversity of nonsymbiotrophic megafauna in areas inside the volcano caldera with different bacterial mat and pogonophoran tubeworm cover. Significant variations in megafaunal composition, density and distribution were found between considered areas. Total megafaunal density was highest in areas of dense pogonophoran populations (mean 52.9 ind. m −2 ) followed by areas of plain light-coloured sediment that were devoid of bacterial mats and tube worms (mean 37.7 ind. m −2 ). The lowest densities were recorded in areas of dense bacterial mats (mean ≤1.4 ind. m −2 ). Five taxa contributed to most of the observed variation: the ophiuroid Ophiocten gracilis , lysianassid amphipods, the pycnogonid Nymphon macronix , the caprellid Metacaprella horrida and the fish Lycodes squamiventer . In agreement with previous studies, three zones within the HMMV caldera were distinguished, based on different habitats and megafaunal composition: "bacterial mats", "pogonophoran fields" and "plain light-coloured sediments". The zones were arranged almost concentrically around the central part of the caldera that was devoid of visible megafauna. The total number of taxa showed little variation inside (24 spp.) and outside the caldera (26 spp.). The density, diversity and composition of megafauna varied substantially between plain light-coloured sediment areas inside the caldera and the HMMV background. Megafaunal density was lower in the background (mean 25.3 ind. m −2 ) compared to areas of plain light-coloured sediments inside the caldera. So the effect of the mud-volcano environment ...