Biogeosciences, 14, 5705–5725, 2017 https://doi.org/10.5194/bg-14-5705-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 4.0 License. Hydrothermal activity lowers trophic diversity in Antarctic hydrothermal sediments James B. Bell1,2,3, William D. K. Reid4, David A. Pearce5, Adrian G. Glover2, Christopher J. Sweeting4, Jason Newton6, and Clare Woulds1 1School of Geography & Water at Leeds, University of Leeds, LS2 9JT, UK 2Life Sciences Dept., Natural History Museum, Cromwell Rd, London SW7 5BD, UK 3Centre for Environment, Fisheries and Aquaculture Science, Lowestoft NR34 0HT, UK 4Marine Sciences-School of Natural and Environmental Sciences, Ridley Building, Newcastle University, NE1 7RU, UK 5Applied Sciences, Northumbria University, Newcastle NE1 8ST, UK 6NERC Life Sciences Mass Spectrometry Facility, SUERC, East Kilbride G75 0QF, UK Correspondence: Clare Woulds (
[email protected]) Received: 5 July 2017 – Discussion started: 1 August 2017 Revised: 25 October 2017 – Accepted: 6 November 2017 – Published: 20 December 2017 Abstract. Hydrothermal sediments are those in which hy- 1 Introduction drothermal fluid is discharged through sediments and are one of the least studied deep-sea ecosystems. We present a com- Hydrothermal sediments (also called sediment-hosted or sed- bination of microbial and biochemical data to assess tropho- imented hydrothermal vents), the product of subsurface mix- dynamics between and within hydrothermal and background ing between hydrothermal fluid and ambient seawater within areas of the Bransfield Strait (1050–1647 m of depth). Mi- the sediment, are physically more similar to background crobial composition, biomass, and fatty acid signatures var- deep-sea habitats than to high-temperature hard substratum ied widely between and within hydrothermally active and vents (Bemis et al., 2012; Bernardino et al., 2012).