Abstract
Faunal assemblages at hydrothermal vents associated with island-arc volcanism are less well known than those at vents on mid-ocean ridges and back-arc spreading centres. This study characterizes chemosynthetic biotopes at active hydrothermal vents discovered at the Kemp Caldera in the South Sandwich Arc. The caldera hosts sulfur and anhydrite vent chimneys in 1375–1487 m depth, which emit sulfide-rich fluids with temperatures up to 212°C, and the microbial community of water samples in the buoyant plume rising from the vents was dominated by sulfur-oxidizing Gammaproteobacteria. A total of 12 macro- and megafaunal taxa depending on hydrothermal activity were collected in these biotopes, of which seven species were known from the East Scotia Ridge (ESR) vents and three species from vents outside the Southern Ocean. Faunal assemblages were dominated by large vesicomyid clams, actinostolid anemones, Sericosura sea spiders and lepetodrilid and cocculinid limpets, but several taxa abundant at nearby ESR hydrothermal vents were rare such as the stalked barnacle Neolepas scotiaensis. Multivariate analysis of fauna at Kemp Caldera and vents in neighbouring areas indicated that the Kemp Caldera is most similar to vent fields in the previously established Southern Ocean vent biogeographic province, showing that the species composition at island-arc hydrothermal vents can be distinct from nearby seafloor-spreading systems. δ13C and δ15N isotope values of megafaunal species analysed from the Kemp Caldera were similar to those of the same or related species at other vent fields, but none of the fauna sampled at Kemp Caldera had δ13C values, indicating nutritional dependence on Epsilonproteobacteria, unlike fauna at other island-arc hydrothermal vents.
Highlights
The presence of active volcanoes on the Antarctic continent and several islands in the Southern Ocean was recorded by early polar explorers, such as Sir James Clark Ross who observed an eruption of Mount Erebus in 1841 [1]
Hot vents and cold seeps have been discovered in the Bransfield Strait in 990–1500 m depth [12,13,14,15,16,17], in the Larsen B ice shelf area, eastern Antarctic Peninsula, in 215–850 m water depth [18,19,20], and on the shelf of South Georgia in 250–350 m water depth [21,22], but the fauna associated with these locations mostly comprise elements of typical Antarctic and Southern Ocean shelf fauna, with two exceptions associated with chemosynthetic environments including the siboglinid polychaete Sclerolinum contortum at Hook Ridge, Bransfield Strait [23] and a large vesicomyid clam at Larsen B [22,24,25,26]
The vent biotopes and assemblages at the Kemp Caldera differed from those of the E2 and E9 vent fields on the nearby East Scotia Ridge (ESR): seven species were shared between the Kemp Caldera and the ESR vent fields, the stalked barnacle N. scotiaensis and sea star P. tyleri were rare at Kemp, and several species that are abundant at ESR vents were not observed at Kemp Caldera, including the yeti crab K. tyleri and the gastropods G. chessoia, Bruceiella indurata [85] and Provanna cooki [86]
Summary
The presence of active volcanoes on the Antarctic continent and several islands in the Southern Ocean was recorded by early polar explorers, such as Sir James Clark Ross who observed an eruption of Mount Erebus in 1841 [1]. These clearly visible volcanoes have been the subject of geological and biological research for a long time Hydrothermal vent fields with abundant novel fauna have been discovered on the back-arc spreading centre of the East Scotia Ridge (ESR) in 2400–2600 m depth, and on the Australian Antarctic Ridge (AAR) in 1800–1900 m depth [27,28]. The AAR sites have not been visited and imaged by remotely operated vehicles (ROVs), but specimens of associated vent fauna Kiwa araonae and Paulasterias tyleri have been collected, indicating the presence of faunal assemblages supported by chemosynthesis [28,41]
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