To study sinking particle sources and dynamics, sediment traps were deployed at three sites in the Amundsen Sea for 1 year from February–March 2012 and at one site from February 2016 to February 2018. Unexpectedly, large benthic invertebrates were found in three sediment traps deployed 130–567 m above the sea floor. The organisms included long and slender worms, a sea urchin, and juvenile scallops of varying sizes. This is the first reported collection of these benthic invertebrates in sediment traps. The collection of these organisms, predominantly during the austral winter, and their intact bodies suggests they were trapped in anchor ice, incorporated into the overlying sea ice, and subsequently transported by ice rafting. The observations imply that anchor ice forms episodically in the Amundsen Sea and has biological impacts on benthic ecosystems. An alternative hypothesis that these organisms spend their juvenile period underneath the sea ice and subsequently sink to the seafloor is also suggested.
The majority of the Amundsen Shelf in the Antarctic is perennially covered with sea ice, except for the two seasonal polynyas. The Amundsen Sea Polynya in the western Amundsen Sea is the most productive polynya around Antarctica (Arrigo and van Dijken, 2003). Intensive flux of particulate organic carbon to the seafloor occurs in the austral summer, while the sea interior is in starvation in the other seasons (Ducklow et al., 2015; Kim et al., 2015, 2019). Biogeochemical processes related to biological pump in the Amundsen Sea have been investigated by recent field campaigns (Arrigo and Alderkamp, 2012; Yager et al., 2012; Meredith et al., 2016; Lee et al., 2017).
Locations of sediment traps deployed in the Amundsen Sea. The satellite image showing the sea ice distribution was taken on 15 February 2012. The satellite image was obtained from rapid response imagery from the Land, Atmosphere Near real-time Capability for EOS (LANCE) system, operated by the NASA's GSFC Earth Science Data and Information System (ESDIS). Areas marked from east to west: Thwaites Ice Shelf (TIS), Thwaites Glacier Tongue (TGT), Thwaites Iceberg Tongue (TIBT), Thwaites Fast-ice Tongue (TFT), Crosson Ice Shelf (CIS), Dotson Ice Shelf (DIS), and eastern Getz Ice Shelf (E-GIS).
Sediment traps were deployed in the Amundsen Sea to study sinking material flux and composition. Sampling occurred from February and March 2012 for 1 year at three locations along the paleoglacier-carved Dotson Trough and from February 2016 to February 2018 in a trap deployed in front of the eastern Getz Ice Shelf, near Duncan Peninsula. Unexpectedly, at three locations macrobenthic organisms were found in the sampling cups, including long and slender worms, a sea urchin, and juvenile scallops of varying sizes. This is the first reported collection of these benthic invertebrates in sediment traps.
This paper reports on details of the benthic invertebrates collected, in addition to sinking particle flux data. The distinct environmental conditions and characteristics of the polar seas relative to temperate and tropical oceans probably explain the unusual occurrence of benthic invertebrates in sediment traps. For example, starvation in the winter due to a reduced supply of organic matter from the overlying water column may stimulate the relocation of benthos. The undersurface of the sea ice may provide a habitat for juvenile benthos before they settle to the seafloor. Anchor ice, which forms at the seafloor in supercooled water, can lift benthos to the overlying sea ice for further transport by ice rafting (Dayton et al., 1969). Studies in the Arctic have shown the incorporation of sediment particles and benthic organisms into sea ice and their subsequent transport (e.g., Nürnberg et al., 1994). Potential transport mechanisms for the collected benthos are considered, and the implications of the surprising observations are discussed.
Time-series sediment traps (McLane PARFLUX Mark 78G; conical type, 80 cm
aperture diameter, height/diameter ratio
Station K4 (73.89
Sequential trap schedules and organisms collected at Stations K1, K3, and K4 in the Amundsen Sea. Quantity, lengths, and thicknesses of worm specimens collected in the sediment traps are shown. Total particle and POC fluxes are also presented for Station K4.
(1) The length in cm and thickness in mm of the 24 specimens collected in cup no. 6 were (31.5, 4.1), (16.5, 3.5), (19.5, 4.4), (24.5, 3.0), (27.7, 3.8), (31.5, 2.4), (17.5, 2.4), (11.0, 2.2), (9.0, 2.3), (6.0, 2.5), (2.0, 5.1), (3.5, 4.9), (7.9, 3.8), (4.0, 3.5), (1.5, 4.4), (4.8, 3.8), (8.2, 4.6), (2.0, 3.0),(10.0, 4.4), (9.0, 3.9), (5.3, 4.3), (3.5, 3.3), (20.4, 2.9), (3.0, 2.0).(2) The length in cm and thickness in mm of the 5 specimens in cup no. 7 were (22.7, 3.4), (53.5, 4.1), (11.8, 4.0), (11.4, 2.2), (7.7, 2.1).(3) The length in cm and thickness in mm of the 5 specimens in cup no. 5 were (4.0, 2.9), (12.0, 1.9).(4) The length in cm and thickness in mm of the 7 specimens in cup no. 15 were (2.0, 1.6), (5.0, 1.5), (8.0, 2.9), (7.0, 1.5), (3.0, 2.6), (12.0, 0.2), (80, 2.7).(5) The height and width in cm of the 11 scallops collected in cup nos. 16 and 17 were (1.3, 1.3), (1.2, 0.9), (1.3, 1.1), (1.5, 1.4), (1.5, 1.4), (1.6, 1.5), (1.7, 1.6), (1.9, 1.7), (1.9, 1.6), (2.0, 2.0), (2.8, 2.5). The diameter of the sea urchin was approximately 0.5 cm, excluding the spine.
Worm specimens were removed by hand from samples on return to the laboratory and were stored in a 10 % formalin solution. The specimen numbers were determined following visual assessment of whether each specimen was an entire body or a body part. The length and thickness of specimens were measured using a ruler and a Vernier caliper, respectively. At Station K4, juvenile scallops and a sea urchin were collected in addition to worms. The length of each of these organisms was measured using a ruler.
Five worm specimens were freeze dried, weighed, and finely ground using a
mortar and pestle. The total carbon content of the ground samples
(
Sea ice concentration data were obtained from the European Centre for
Medium-Range Weather Forecasts (ECMWF) ERA-Interim reanalysis
(
Station K4 is located within the seasonal Amundsen Sea Polynya, and the sea
ice concentration there decreases to zero in summer (Fig. 2). Ice-free
conditions lasted for
Long and slender worms were found in the sediment traps at Stations K1 and K3 during the 2012–2013 deployments. No worms were found in the traps at
Station K2. The worm specimens were either entire bodies or body parts. The
specimens were all similar in appearance (Fig. 3). All had a rubbery
texture and were easily torn apart when gently stretched. The bodies were
round and slender and had a body thickness
In total, 33 specimens (including 18 incomplete bodies) were collected at
Station K3 in six sampling bottles from April to August and in mid-December
2012 (Fig. 2, Table 1) and 24 specimens (10 complete and 14 incomplete
bodies) were collected in July. Two specimens were collected at Station K1
in two sampling bottles in June 2012 and in early March 2013 (Fig. 2). The
lengths of the specimens collected at Stations K1 and K3 varied from 2 to 69 cm (average:
The average total carbon and nitrogen contents of five randomly selected worm
samples were 44.0 %
At Station K4 during the 2016–2018 deployment, 11 juvenile scallops and 1 juvenile sea urchin were found, in addition to 12 worm specimens (including 7 incomplete bodies). Worm specimens were found in five samples collected in March–September 2016 and June–July 2017 (Fig. 2, Table 1). These worms were similar in shape to those collected at Stations K1 and K3 (Fig. 3). A single scallop was collected in August–September 2017 and 10 were collected in October–November 2017. The scallops were all juveniles and varied in size from 1.2 to 2.8 cm. The baffle of the sediment trap (approximately 2.5 cm diameter) would have blocked any larger creatures from falling into the trap. One juvenile sea urchin was also collected in October–November 2017. No specimens were collected under sea-ice-free conditions.
It is puzzling that large benthic invertebrates lacking swimming capability
were collected in sediment traps deployed 130–567 m above the sea floor.
The worms had no parapodia or appendages for swimming. It is unlikely that
these organisms crawled up the mooring lines to the traps, and human
activities were not responsible because the region is not accessible during
winter, when most of the specimens were collected. According to the pressure
registered to the current meters, ADCPs (acoustic doppler current
profilers) and Microcats (Seabird, SBE-37SMP) moored with the sediment
traps did not show any sign for considerable tilting of the mooring lines to
facilitate better access for the benthos (Kim et al., 2016). Several
mechanisms may explain the transport of the collected organisms. Strong
currents, especially near Station K3, may have been responsible for swiping
and transporting these organisms to the trap sites. Stations K3 and K4 were
within
A likely explanation is that the organisms were transported by and released from sea ice. Two mechanisms could entrain benthic organisms in the sea ice: anchor ice formation and adfreezing of land fast ice. Ice foot formation, fast ice, and subsequent scouring are causes of disturbance of the benthic environment in the Antarctic (Barnes, 1999; Gutt, 2001; Barnes et al., 2011), and benthic organisms can be incorporated into the ice during these processes. For example, adfreezing by bottom fast ice can incorporate benthic organisms in addition to coarse sediment grains (Pfirman et al., 1990; Nürnberg et al., 1994). Several observations indicate that bottom fast-ice formation is not a likely mechanism in this case. Firstly, the collected specimens were intact and well preserved, with no evidence of mechanical abrasion (Reimnitz et al., 1992); breaking of bottom fast ice would have destroyed these soft-bodied benthic organisms. Secondly, no coarse particles (grain size larger than sand) were collected in the sediment traps at the same time; small granules and rock fragments were collected only in one sample at Station K4 in April and May 2016. Thirdly, the organisms were collected mostly in winter; bottom fast ice at the shoreline would remain attached to the land during winter and would thus only release entrained particles near the shore (Reimnitz et al., 1992). In contrast, anchor ice formation could have gently entrained these delicate organisms. Anchor ice forms in supercooled water (Dayton et al., 1969). Any anchor ice that formed on the bodies of benthic organisms would be buoyant and thus able to lift them to the overlying sea ice canopy, in which they could become incorporated (Dayton et al., 1969; Heine et al., 1991). Organisms would be released when the attached anchor ice melted by the heat provided by the underlying water.
Another hypothesis is that the benthic animals actually spend their juvenile period in a habitat underneath the sea ice and fall down to the seafloor. This idea was suggested by a reviewer, Paul Dayton, and we agree that this could be a possibility. This hypothesis is based on his visual inspections in numerous dives at McMurdo Sound that no baby nemerteans were observed and tiny sea urchins and scallops were rare. The undersurface of the sea ice can harbor a thick layer of frazil ice platelets formed by supercooled water and cavities and tunnels formed by brine flow. Diatoms and other algae growing in and/or underneath the sea ice would supply food for juvenile sea urchins and pectins. Also amphipods and small invertebrates would provide food for juvenile nemertean recruits. These organisms may passively sink to the seafloor upon melting of the platelets or actively abandon the sea ice habitat due to depletion of algal food in the winter. This kind of habitat with large populations of these animals has not been observed yet and needs to be verified.
When ice grows on objects at the seafloor in supercooled water it is called anchor ice (Denny et al., 2011). Anchor ice can grow on epibenthic animals as nucleation sites. Studies of anchor ice formation have focused mainly on sediment entrainment into sea ice in the Arctic (Pfirman et al., 1990; Reimnitz et al., 1992; Nürnberg et al., 1994), where this mechanism is considered to be the most important process for entrainment of sediment into sea ice and subsequent sediment transport (Nürnberg et al., 1994). Arctic sea ice transports well-preserved benthic organisms, including mollusks and sea urchins, in addition to sediments (Reimnitz et al., 1992). Studies of anchor ice in the Antarctic have focused mostly on biological effects (Barnes, 1999).
Anchor ice has been reported in McMurdo Sound in the Ross Sea (Dayton et
al., 1969; Robinson et al., 2014), Potter Cove in the South Shetland islands
(Barrera-Oro and Casaux, 1990), Ellis Fjord, and a few other locations
(Kirkwood and Burton, 1988 and references therein). Supercooling has not
been reported in the Amundsen Sea because no hydrographic data near the
coast are available for seasons other than summer. Observations in summer on
the Amundsen Shelf have shown that winter water (water that mimics the
properties of water formed in winter) was at near freezing temperature
(potential temperature
Another mechanism for anchor ice formation is the so-called “ice pump”, which occurs underneath ice shelves (Mager et al., 2013). Lenard et al. (2014) investigated the potential for anchor ice formation in coastal Antarctic waters, focusing particularly on the ice pump mechanism. They estimated that a wide area of McMurdo Sound is suitable for anchor ice formation. The Amundsen Sea includes several ice shelves. According to a modeling study by Assmann et al. (2005), temperatures below surface freezing were simulated close to the Abbot and Getz Ice Shelves.
The observations show that transport and release of benthic invertebrates occurs episodically with potentially high interannual variability. No invertebrates were collected in sediment traps in the preceding year at either Station K1 or the central polynya (Ducklow et al., 2015; Kim et al., 2015). This phenomenon is episodic, probably because particular conditions must occur for anchor ice to form if anchor ice is indeed the mechanism responsible (Kempema et al., 1989; Reimnitz et al., 1992). An implication for coastal benthic ecosystems is that anchor ice formation around Antarctica may be more prevalent than previously thought; the occurrence of many ice shelves and polynyas implies this possibility (Leonard et al., 2014; Mager et al., 2015).
Uplift of benthic organisms to the sea surface by anchor ice has been considered to be important for the Arctic food web (Reimnitz et al., 1992). The role of anchor ice in the transport of benthic organisms off the coast has not been investigated in the Antarctic. Organic carbon supplied by worms accounted for up to 5-fold the POC flux derived from primary production in the overlying water column. This supply of organisms occurred during winter, when little primary production occurs; hence, this flux may provide energy for overwintering organisms. Transport by anchor ice and sea ice rafting may be a means of dispersal for benthic invertebrates (Picken, 1980), provided that the organisms are able to survive this process. In this context, there is no evidence as to whether the organism entered the sediment traps alive or dead.
More studies are needed to clarify the spatial distribution of anchor ice formation. Lenard et al. (2014) noted that detailed information on ice shelf drafts, ground lines, and edges is needed to enable prediction of anchor ice formation, and observations of anchor ice are needed for validation of model outputs. Studies of these aspects of anchor ice formation in the Amundsen Sea would be a useful future study. In parallel, the impact of anchor ice on Antarctic biology, including as a disturbance to benthic ecosystems; a dispersal mechanism for benthic invertebrates; and as a supply of energy, nutrients, and detrital material to the deeper benthic ecosystems, also need to be investigated.
Any data not listed in Table 1 are available upon request to the corresponding author.
EJY, HJK, and DK collected samples and produced sinking particle data. TWK and HSL contributed physical oceanography data. SL organized the research of the Amundsen Sea. MK produced data of C and N contents of the worm specimens. MK and JH wrote the manuscript. All authors discussed the results and commented on the manuscript.
The authors declare that they have no conflict of interest.
Junsung Noh is thanked for carbon and nitrogen analyses of the worm
specimens; Karen M. Assmann, Okhwan Yu, Dong-Hoon Im, Seung Hee Kim, and
Eunah Han for helpful discussion; and the captain and crew of the IBRV
This research has been supported by the Korea Institute of Ocean Science and Technology (grant no. PN67330), the Korea Polar Research Institute (grant no. PE18060), and the National Research Foundation of Korea (global PhD fellowship no. 2015032018).
This paper was edited by Minhan Dai and reviewed by Tiantian Tang, Weilei Wang, and one anonymous referee.