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First record of cysts in the tidal tardigrade Echiniscoides sigismundi
Helgoland Marine Research volume 68, pages 531–537 (2014)
Tardigrades are microscopic metazoans that withstand environmental extremes by entering dormant states, such as cryptobiosis (latent life). In addition, they may also form cysts. Here, we present the first report of cyst formation in a marine heterotardigrade, i.e., Echiniscoides sigismundi, which constitutes a cryptic species complex present worldwide in tidal zones. The cysts were initially discovered during experimental series constructed to investigate osmotic stress tolerance. The animals, which eventually formed cysts, showed signs of an imminent molt at the beginning of experimentation. We use the term “cyst” for stages, where a total of three or more cuticles have been synthesized. Our observations show that encystment in E. sigismundi involves synthesizing of at least two new cuticle layers. Legs with discharged claws are present in connection with the first outer cuticle, as well as the second cuticular layer. In the most developed cyst, a third cuticle lacking claws seems to surround the animal, which is delineated by a fourth cuticle. Many features are shared with the well-studied cysts of eutardigrades. The cysts of E. sigismundi, however, lack pigmentation and have an extra set of claws, and the animal inside retains buccopharyngeal sclerified parts, until discharging the third cuticle. The finding of cysts in a marine heterotardigrade is novel and confirms that encystment also occurs within this major evolutionary lineage.
Tardigrades are microscopic metazoans that colonize ecosystems worldwide and show great tolerance of environmental stress (e.g., Goldstein and Blaxter 2002; Nelson 2002; Møbjerg et al. 2011). Three major evolutionary lineages are currently recognized: (1) eutardigrades and (2) mesotardigrades, which are predominantly semiterrestrial/limnic, and (3) heterotardigrades that split into the semiterrestrial/tidal echiniscoideans and the marine arthrotardigrades. Tardigrades endure extremes, such as desiccation and freezing by entering dormant states, which include quiescence (cryptobiosis) and diapause (e.g., encystment). Noticeably, tardigrades comprise one of few phyla that exhibit both types of dormancy (Guidetti et al. 2008). Little attention has been dedicated to encystment, and the phenomenon has mainly been described from a few limnic and semiterrestrial species belonging to Eutardigrada (see, e.g., Weglarska 1957; Ramazzotti and Maucci 1983; Westh and Kristensen 1992; Guidetti et al. 2006). An aberrant cyst is found in the marine eutardigrade Halobiotus crispae Kristensen, 1982 as part of a seasonal change in morphology and physiology—i.e., cyclomorphosis (Kristensen 1982; Møbjerg et al. 2007; Halberg et al. 2009; Guidetti et al. 2011; Halberg et al. 2013a). In addition, within the heterotardigrades, cyst formation has been reported from moss-dwelling species of the genus Echiniscus C.A.S. Schultze, 1840 (Murray 1907; Ramazzotti and Maucci 1983). Importantly, cyst formation in tardigrades is mostly an optional response to environmental changes; however, when occurring during cyclomorphosis, it seems to be an obligate and integrated part of the seasonal change (Kristensen 1982; Møbjerg et al. 2007). In H. crispae, cyclomorphosis is apparently directed by changes in temperature (Halberg et al. 2013a).
Tardigrades belong to Ecdysozoa—a large clade of protostomes that shed their exoskeleton during growth (Aguinaldo et al. 1997). Based on investigations in eutardigrades, cyst formation shares many characteristics with the normal molting process, beginning with the discharge of buccopharyngeal sclerified parts and closing of the mouth (simplex stage), followed by synthesis of a new cuticle (Kristensen 1982; Walz 1982; Guidetti et al. 2008). However, instead of discharging the old cuticle (exuvium), as in a molt, a tardigrade in the process of encystment may secrete up to three new cuticles and keep the old ones as protective coats. The final cyst is generally oval shaped, with mouth and cloaca closed by cuticular invaginations and/or thickenings (Bertolani et al. 2004; Guidetti et al. 2006). From outside to inside, the cuticle layers forming eutardigrade cysts have been referred to as (1) old cuticle (exuvium), (2) sarcophagus cuticle and (3) mummy cuticle (Hansen and Katholm 2002; Guidetti et al. 2006). Interestingly, eutardigrades, e.g., species within the genus Bertolanius Özdikmen, 2008, may produce more than one type of cyst according to season (Westh and Kristensen 1992; Guidetti et al. 2006). The outermost cuticle of eutardigrade cysts becomes sclerotized and opaque during the encystment process (Guidetti et al. 2011), with pigmentation varying both among and within species. Cysts of Bertolanius volubilis (Durante Pasa and Maucci, 1975) are generally white–opaque, orange–yellow, red–purple or brown, while Dactylobiotus parthenogeneticus Bertolani, 1982 cysts typically display a brown–black coloration (Weglarska 1957; Guidetti et al. 2006).
Here, we present evidence of cyst formation in Echiniscoides sigismundi (M. Schultze, 1865), thereby consolidating that encystment also occurs within the major evolutionary lineage comprising the heterotardigrades.
Methods and materials
The genus Echiniscoides Plate, 1888 comprises cryptic species complexes with huge genetic variation (Faurby et al. 2011, 2012). In the present study, we describe cyst formation in Echiniscoides sigismundi sampled at two localities: Roscoff, France in July 2012 (48°43′30″N, 03°59′35″W) and Lynæs, Denmark in 2012 and 2013 (55°56′42″N, 11°51′15″E). We use the term “cyst” for stages of the encystment process where three or more cuticles have been synthesized. Echiniscoides sigismundi from the two localities seems to undergo similar cyst formation.
Echiniscoides sigismundi on barnacles was collected from rocks in the tidal zone. Soft tissue was removed from barnacle shells in the laboratory, and the shells were subsequently washed and sieved through a 62-µm mesh, thereby filtering bacteria, microalgae, ciliates and fine detritus from the material. The shells containing numerous tardigrades were transferred to seawater from the locality and kept at approximately 4 °C (Lynæs) and 17 °C (Roscoff). Temperature and salinity was 17 °C and 35 ‰ at the time of sampling at Roscoff, and in the range 0.5–15 °C and 16–20 ‰ at the time of sampling at Lynæs.
The cysts were initially discovered following exposures to various salinities during experiments constructed to investigate osmotic stress tolerance (Table 1). During these experiments, single specimens were transferred to glass slides at given time points and thus followed over time at high magnification. A Leica DM1000 microscope equipped with a digital camera (InfinityX, Deltapix, Denmark) was used for the investigation. Specifically, single tardigrades were monitored and photographed in seawater from their locality (t = 0 h; 35 ‰ Roscoff, 16 ‰ Lynæs), three times during a subsequent 48-h exposure to a given test salinity (t = 2 h, t = 24 h and t = 48 h), and up to three times following retransfer to normal seawater (t = 50 h, t = 72 h and t = 96 h). A total of four cysts, two from Roscoff (specimens R1 and R2) and two from Lynæs (specimens L1 and L2) were found during these experiments (Fig. 1). Specimens R1 and L1 were exposed to hypotonic solutions (3.5 and 1.6 ‰) during the 48-h period in test salinities, while R2 and L2 were exposed to a hypertonic solution (70 ‰) during this time interval. The cysts of R1 and R2 are preserved as permanent mounts in glycerol on glass slides.
Several additional cysts were subsequently discovered in the Lynæs material kept at 4 °C, two of which are documented here (L3 and L4). L3 had been kept for approximately 1 week in a watch glass together with numerous other specimens, organic material from barnacles and small algae. A considerable amount of microbial growth as well as free-moving ciliates were present at the time of discovery (Fig. 2a–c). The other specimen (L4) had been kept for approximately 1 day in a watch glass, then exposed to distilled water for an hour, dehydrated on a filter for 48 h and subsequently rehydrated with 18 ‰ seawater. The cyst was discovered 48 h after rehydration (Fig. 2d, e).
In the following, we describe in detail the four specimens, which formed cysts in connection with osmotic stress experiments. Figure 3 illustrates cyst formation in Echiniscoides sigismundi based on the observation of these specimens.
At the onset of the experiments, (t = 0 h) newly synthesized claws, and a clear double cuticle, could be seen in R1 and R2. In L2, an extra cuticle was visible at the onset of experimentation (t = 0 h), while new claws were visible in L1 two hours after exposure to the hypotonic solution (t = 2 h). Clear cyst formation, in which at least two cuticle coats surrounded the animal, was visible in R1 and R2, 72 h after experimental start (Fig. 1c, d), while cyst formation in L1 and L2 appeared at t = 96 h and t = 50 h, respectively (Fig. 1a, b). At these time points, the animals had contracted into a “tun”-like state, positioned in the posterior/central (R2 and R1) to central (L2) part of the cyst (Fig. 1b–d). The tardigrade in L1 was, however, not fully contracted (Fig. 1a, t = 96 h), and we interpreted the cyst of L1 as being the least developed of the observed cysts.
At t = 96 h, the tardigrade in L1 had an abnormally formed pharyngeal bulb, indicating a recent discharge of sclerified parts, with new cuticular parts of the bulb not yet fully reconstructed (Fig. 1a). At this time point, L1 had an outer cuticular coat with a newly synthesized cuticle beneath it. This second cuticle was in the process of being discharged, and a third cuticle lined the animal. Cysts L2 (Fig. 1b) and R2 (Fig. 1c) had three cuticle layers at t = 72 h. If the terminology used for eutardigrades (Guidetti et al. 2006) is applied, the two newly synthesized layers would correspond to, respectively, the sarcophagus and the animal body cuticle, which are both surrounded by the old outer cuticle. R1 seemed to have four cuticle layers at t = 72 h; three layers of protective coats and a fourth cuticle lining the animal (Fig. 1d). Old claws were found discharged with the exuvium in all cysts. Legs formed by the second cuticle were clearly visible in L2, R2 and R1 and, noticeably, contained an additional set of claws. These claws had been discharged from the animals together with the second cuticle layer. Thickenings on the discharged cuticles clearly marked the region of the anus in L2 (Fig. 1b, t = 72). The animals inside L2 and R2 had a cuticle-lined pharyngeal bulb with readily visible placoids and stylets. In R1, a structure recognized as the cuticular lining of the pharyngeal bulb with placoids was visible in the anterior region of the cyst within the second cuticle (Fig. 1d, t = 72). We did not find evidence of discharged sclerified elements within the other E. sigismundi cysts.
During our observations, the animals within the cysts were moving, however, with reduced activity compared with experimental onset. Reduced activity was a general feature of the tardigrades following experimentation with osmotic stress and no food access. No color changes were observed, apart from the emptying of some gut content (bright yellow) into the discharged second cuticle in L2 (Fig. 1b, t = 50 h).
The two additional cysts, L3 and L4, had two outer cuticle layers (both with claws), in addition to the animal cuticle (Fig. 2). Moreover, both cysts had a well-developed buccopharyngeal apparatus with clearly visible stylets, buccal tube and placoids. None of the animals left their cysts while being observed.
Echiniscoides sigismundi is a common marine heterotardigrade, which inhabits barnacles, algae and lichens in tidal zones worldwide. Consequently, this species may experience large fluctuations in temperature and osmotic pressure, especially during low tides. The marine family Echiniscoididae, comprising Echiniscoides and another genus (Anisonyches Pollock, 1975), is phylogenetically basal in the clade Echiniscoidea, which also includes a large and diverse group of terrestrial tardigrades (Jørgensen et al. 2010, 2011). Echiniscoides sigismundi may thus provide an evolutionary link between sea and land. Terrestrial Echiniscus cysts have previously been observed (Murray 1907; Ramazzotti and Maucci 1983), and our observations on Echiniscoides sigismundi thus confirm that cyst formation occurs in echiniscoidean heterotardigrades. A similar pattern of encystment suggests that the differences observed among E. sigismundi cysts represent successive stages of encystment, rather than different cyst types, as known from, e.g., Bertolanius (see Westh and Kristensen 1992; Guidetti et al. 2006).
We show that Echiniscoides sigismundi is capable of producing cysts that in some aspects resemble cysts of limno-terrestrial eutardigrades. In the latter, the progression of encystment is generally associated with less activity and ultimately immobility of the tardigrade (Guidetti et al. 2006). Interestingly, however, cysts of the marine Halobiotus crispae (pseudosimplex 1 stage) remain mobile (Kristensen 1982). During our observations of encystment in E. sigismundi, the cysts were clearly immobile; however, the animals inside the cysts were moving. Markedly, the animal inside the most developed cyst, R1, was also moving. Despite this activity, it is likely that metabolism takes place at a slower rate than in active animals, as generally holds for diapausing animals (Guidetti et al. 2006).
Noticeably, Echiniscoides sigismundi cysts have a set of discharged claws in connection with both the first (outer) and the second cuticles (Fig. 2c). This has not been described for any eutardigrade species. In limnic eutardigrades, e.g., Dactylobiotus parthenogeneticus, the outermost cuticle has legs with distal positioned claws, the second (sarcophagus) cuticle has legs but no claws, while the third (mummy) cuticle lacks both legs and claws (Guidetti et al. 2006). “Type 2” cysts of the moss-dwelling Bertolanius volubilis have legs in the mummy cuticle, and both cysts (“type 1” and “type 2”) in Bertolanius nebulosus (Dastych, 1983) lack the sarcophagus cuticle. Cyst morphology thus differs greatly among eutardigrades and a consensus eutardigrade cyst cannot be ascribed. Another example of cyst variation, observed among eutardigrades, is seen in D. parthenogeneticus, as this species often slugs off its old outer cuticle, leaving the hardened and pigmented sarcophagus cuticle as a protective barrier to the external environment (Guidetti et al. 2006).
Encysted Echiniscoides sigismundi seem to retain buccopharyngeal sclerified parts until shedding the third cuticle. In cysts of Dactylobiotus parthenogeneticus, stylets and structures associated with them (sheath and supports) are absent, while they are present, but greatly modified, in the cyst of B. volubilis (Guidetti et al. 2006). Eutardigrade cysts are generally characterized by opaque pigmentation (Guidetti et al. 2008), whereas encystment in E. sigismundi apparently does not involve color change. This difference in pigmentation could correlate with habitat, as limno-terrestrial tardigrades are likely exposed to higher levels of UV radiation.
True limnic eutardigrades, e.g., Dactylobiotus parthenogeneticus, as well as the marine Halobiotus crispae, form cysts but do not enter cryptobiosis, while Echiniscoides sigismundi as well as the semiterrestrial species are cryptobionts (Bertolani et al. 2004; Guidetti et al. 2006; Møbjerg et al. 2011). Cryptobiosis provides the ultimate means of resistance to environmental extremes and generally involves anatomical changes (Halberg et al. 2013b). Encysted tardigrades undergo major structural changes, and with reduced metabolism, the encysted state can also withstand adverse factors including desiccation and freezing (Weglarska 1957; Guidetti et al. 2011; Møbjerg et al. 2011).
Encystment is thought to be under endogenous control and may be initiated by changes in environmental factors such as temperature, pH, oxygen tension and food availability (Bertolani et al. 2004; Guidetti et al. 2008). In the present study, five of the Echiniscoides sigismundi cysts were formed following osmotic stress treatments, suggesting that both hypo- and hypertonic stress represents adverse conditions that ultimately may stimulate cyst formation. A continuous internal osmotic imbalance thus seems to be yet another significant diapause inducing stimulus.
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The current study was funded by the Carlsberg Foundation. Station Biologique de Roscoff (France) is warmly thanked for logistic support.
Communicated by H.-D. Franke.
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Clausen, L.K.B., Andersen, K.N., Hygum, T.L. et al. First record of cysts in the tidal tardigrade Echiniscoides sigismundi . Helgol Mar Res 68, 531–537 (2014). https://doi.org/10.1007/s10152-014-0409-0
- Extreme environments
- Osmotic stress