An observation of two oceanic salp swarms in the Tasman Sea: Thetys vagina and Cyclosalpa affinis
© Henschke et al. 2016
Received: 6 April 2016
Accepted: 12 April 2016
Published: 1 June 2016
Large oceanic salps are rarely encountered. The highest recorded biomasses of the salps Thetys vagina (852 g WW m−3) and Cyclosalpa affinis (1149 g WW m−3) were observed in the Tasman Sea during January 2009.
Due to their fast sinking rates the carcasses and faecal pellets of these and other large salps play a significant role in carbon transport to the seafloor. We calculated that faecal pellets from these swarms could have contributed up to 67 % of the mean organic daily carbon flux in the area. This suggests that the flux of carbon from salp swarms are not accurately captured in current estimates.
This study contributes information on salp abundance and biomass to a relatively understudied field, improving estimates for biogeochemical cycles.
The role of gelatinous zooplankton, such as salps, pyrosomes and cnidarians, in ocean food webs and biogeochemical cycling has garnered increased attention in recent years (Lebrato et al., 2011; Henschke et al., 2013; Lebrato et al., 2013; Smith et al. 2014). Salps (Phylum: Thaliacea, Order Salpidae) in particular, are significant contributors to oceanic carbon flux. They have the highest per-individual filtration rates of all marine zooplankton filter feeders (Alldredge and Madin, 1982) consuming particles across three orders of magnitude (1 μm up to 1 mm in size; Vargas and Madin, 2004; Sutherland et al., 2010) using a fine mucous net that is continuously secreted and fed toward the oesophagus. This efficient feeding mechanism and their alternating sexual and asexual life-cycle results in fast individual (up to 21 % in length h−1; Heron, 1972a) and population (up to 2.5 d−1; Heron, 1972b; Henschke et al., 2015) growth rates. As a result, salps form large swarms that often reach abundances greater than 1000 individuals m−3 (~6 kg WW m−3; Henschke et al., 2014) and persist for up to 6 months (Smith et al. 2014). When salps occur in high abundances, their fast-sinking faecal pellets (Bruland and Silver, 1981) and carcasses (Henschke et al., 2013) can increase the carbon flux in an area up to ten-fold the daily average (Fischer et al., 1988) for a sustained period of time (Smith et al. 2014).
Due to their regular occurrence (Henschke et al., 2014) and coastal dominance (Henschke et al 2011), smaller salps such as Thalia democratica are studied with greater frequency. Although these smaller salps contribute significantly to biogeochemical cycling with fast growth rates (Heron, 1972a) and faecal pellets, carcasses of these smaller salps rarely sink as they are neutrally buoyant (Tsukamoto et al., 2009). The carcasses of larger salps however, sink rapidly and have the potential to reach the sea floor in less than 2 days (Henschke et al., 2013; Lebrato et al., 2013). Due to the combined input from both faecal pellets and carcasses, swarms of larger salps are thought to play a greater role in carbon export (Smith et al. 2014). Of significance however, is that very little is known about the distribution and abundance of larger salps as they are oceanic and rarely encountered. The aim of this study is to document swarm observations from the Tasman Sea of two large salps: Thetys vagina and Cyclosalpa affinis and compare these biomasses to previous observations.
Thetys vagina is often observed opportunistically as a single individual and little is known about their ecology (Nakamura and Yount, 1958; McAlice, 1986; Sims, 1996; Stone and Steinberg, 2014). Large biomasses (900 t WW km−3) of T. vagina have been observed in the Japan Sea (Iguchi and Kidokoro, 2006) and Tasman Sea (Thompson, 1948; Henschke et al., 2013). Although T. vagina has been found across a wide temperature (7–20 °C) and salinity (33.9–35.6) range (Thompson, 1948; Iguchi and Kidokoro, 2006; Henschke et al., 2013), there appears to be no seasonality to T. vagina swarms (Henschke et al 2013). In the Japan Sea and Tasman Sea, higher T. vagina biomass occurred in areas of higher chlorophyll a (Iguchi and Kidokoro, 2006; Henschke et al., 2013). As seamounts have been found to promote localised upwelling (Boehlert and Genin, 1987; Suthers, 1996), this is one factor that may have encouraged the T. vagina population to aggregate around Gascoyne Seamount in this report.
Although the ecology of Cyclosalpa affinis is well studied (e.g. Madin, 1974; Madin et al., 1981; Vargas and Madin, 2004), their distribution is not well known. Unlike T. vagina, the relationship between upwelling events and C. affinis populations is unknown. Long-term studies have found that C. affinis generally occurs in low numbers (<30 g WW m−3) and has been characterised as a cool-phase species, occurring after intrusions of cooler high latitude water (Lavaniegos and Ohman, 2003). However, C. affinis has also been found in the subtropical Tasman Sea (32.8°S and 32.57°S) and the warmer parts of the Indian, Pacific and Atlantic oceans (Thompson, 1948) suggesting that its temperature tolerance may be quite broad.
At each sampling station a Seabird SBE911-plus Conductivity–Temperature–Depth (CTD) recorder equipped with an AquaTracker Mk3 fluorometer (Chelsea, UK) was used to record salinity, temperature, and fluorescence, respectively. Salps were sampled at the surface with a neuston net (0.75 m × 0.75 m, 500 μm mesh; n = 2) and from 0 to 40 m using a rectangular mid-water trawl (RMT; 1 m × 1 m, 1 mm mesh, double-oblique tows; n = 1). The neuston net was towed for 5 min, and the RMT for 30 min, both at 1.5 m s−1. All tows were undertaken at night (2100–0200 h). Immediately after sampling, zooplankton were preserved in 5 % formaldehye solution. Salps were identified to species and total length and wet weight was measured for each individual. Due to salps being damaged in the RMT net, total length of salps from the RMT samples could not be measured. Carbon calculations were based on carbon-length relationships previously established for T. vagina (Henschke et al., 2013) and C. affinis (Madin et al., 1981). Pearson correlations were undertaken to determine if there were any relationships between salp biomass and location to the seamount.
Results and discussion
The Gascoyne Seamount transect extended for 38 km crossing west-east over the seamount. At the time of sampling, sea surface temperature at Gascoyne Seamount was ~22 °C compared to Challenger Plateau which was cooler (~19 °C) and had higher chlorophyll a concentrations (Fig. 1). Thetys vagina was present at all Gascoyne Seamount stations (n = 5) but absent at Challenger Plateau (n = 1) where only Cyclosalpa affinis occured. Biomass of T. vagina did not significantly differ with distance to the seamount (Pearson correlation, R = -0.36, p = 0.55).
Biomass and abundance
Cyclosalpa affinis was only observed at the Challenger Plateau, with a surface biomass of 1148.6 g WW m−3 (4.3 mg C m−3) and oblique biomass of 2251.4 g WW m−3 (8.3 mg C m−3; Fig. 2h). Compared to Gascoyne seamount, the water was cooler and less saline at the Challenger Plateau with a 100 m depth-integrated temperature of 15 °C compared to 19 °C (Fig. 2e,f). The fluorescence at Challenger Plateau was higher in the surface waters, but showed a similar sub-surface maximum at 60 m to Gascoyne Seamount (Fig. 2c,g). C. affinis is not believed to undergo diel-vertical migration (Madin et al., 1996) and to date this is the largest observed biomass of C. affinis population.
C. affinis aggregates ranged from 9 to 77 mm in length (mean = 37 mm, n = 36; Fig. 3b). Unlike T. vagina, there appears to be two distinct aggregate size classes in the C. affinis population with respective modes of 14 (n = 4) and 66 mm (n = 3). Only 3 solitaries were measured and lengths ranged from 56 to 96 mm (mean = 74 mm) with no developing buds observed. C. affinis aggregates reach a maximum size of 80 mm (Thompson, 1948), suggesting that the swarm has been developing for a while, and a cohort of solitary buds may have already been released from the larger aggregates.
Potential carbon input
Salps are significant contributors to oceanic carbon flux (Henschke et al., 2013; Smith et al. 2014). The defecation rate of Cyclosalpa affinis has been calculated at 9.9 μg C mg body C h−1, and although no defecation rate has been calculated for Thetys vagina, we can assume an average defecation rate of 11.8 μg C mg body C h−1 based on a range of salp species (Madin and Deibel, 1998). Therefore, using the mean surface salp biomass from this study (and assuming a 1:1 conversion for m3:m2), T. vagina faecal pellets would have contributed ~2 mg C m−2 d−1 at Gascoyne Seamount, and C. affinis would have contributed ~1 mg faecal carbon m−2 d−1 at the Challenger Plateau. These carbon flux values are likely to be an underestimation, as we have not considered population growth and the carbon input from carcasses. Considering the mean organic carbon flux in the area has been calculated as 4.5 mg C m−2 d−1 (Kawahata and Ohta, 2000), it is likely that the contribution from salp swarms is not accurately captured in current estimates.
This study confirms recent literature that has identified that swarms of large salps frequently occur in the Tasman Sea (Henschke et al., 2013), and this is likely the case in oceans around the world. Large salps have recently been found to be nutritionally important for several marine organisms and salp faecal pellets and carcasses play a large role in carbon export (Henschke et al., 2013). As salp remains are rarely found in sediment traps (Rowe and Staresinic, 1979), this suggests the biogeochemical carbon budgets of the area are significantly underestimated. To incorporate salps into ecosystem models, it is important to understand which environmental factors promote high abundances of large salps in order to have accurate representations of their abundance and distribution. Their ephemeral nature will continue to make sampling of large oceanic salps difficult, but improved reporting of all encountered salp blooms will allow their contribution to global biogeochemical cycles to be better estimated.
This work as funded by a UNSW Evolution and Ecology Research Centre Skills Transfer Award. The authors thank the captain and crew of the RV Southern Surveyor T01/2009. This is manuscript 180 from the Sydney Institute of Marine Science.
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