- Original Article
A functional and morphological approach to evaluate the vertical migration of estuarine intertidal nematodes during a tidal cycle
Helgoland Marine Research volume 67, pages 83–96 (2013)
We tested herein the hypothesis that exposure time significantly contributes to the vertical distribution profile of nematodes during a tidal cycle as a function of distinct feeding and locomotion behaviors, conditioned by body morphology. We showed that the vertical distribution profile of the slender with filiform tail, numerically dominant Terschellingia longicaudata is in fact significantly correlated with sediment changes induced by tidal variation. Conversely, none of the other nematode species showed unequivocal evidence of vertical migration. Horizontal spatial heterogeneity also influenced the vertical distribution of nematode associations, probably as a response to varying temperature and desiccation levels at the sediment surface. The resulting vertical profiles for individual or species groups are a trade-off among locomotory and feeding strategies and concordant morphological adaptations.
Regardless of their predominantly benthic life, meiofaunal animals can be moved or resuspended by water currents due to their small size and preference for the surface sediment layers (Boeckner et al. 2009). However, free-living nematode species can present variable vertical distribution patterns (Maria et al. 2012). The vertical distribution of species belonging to the genus Sabatieria, for example, might be more related to the availability of preferred food than with the environmental variations arising from the redox discontinuity layer (Steyaert et al. 2001, 2003). Differing vertical distribution patterns suggest that functional groups or individual nematode species can display distinct migration behaviors as an adaptive strategy to the environmental dynamism, especially in intertidal areas (Steyaert et al. 2001). In particular, variations in the water content are known to affect the locomotion behavior of more “active” nematodes, such as Enoploides longispiculosus, which actively captures its food (Steyaert et al. 2001; Gallucci et al. 2005). Thus, biological interactions may play an important role in the vertical spatial segregation of nematode associations. Nematode prey can change their vertical distribution or migrate as a response to predation pressure by top-down control of predaceous nematodes (Maria et al. 2012). In addition, engineering processes caused by other benthic organisms can influence nematode vertical distribution patterns. Bioturbation, bioirrigation, and predation may differently alter vertical distribution of nematode associations (Braeckman et al. 2011a, b).
The ability of nematodes for vertical migration in the sediment depends on their locomotion and feeding strategies. Nematode locomotion behavior is described as undulating, with the length and frequency of body waves varying as a function of viscosity (Gray and Lissmann 1964; Wallace 1968). Tail shape (Thistle and Sherman 1985; Thistle et al. 1995), size and shape of the body (Soetaert et al. 2002; Vanaverbeke et al. 2004; Schratzberger et al. 2007), and presence of caudal glands (Gingold et al. 2011) may be related to the ability to move and eventually explain differences in distribution patterns. Nematode feeding strategies are also rather variable, and their locomotion behavior may be conditioned by the “mobility” of the food itself, as diatoms and other microorganisms, mainly in the case of nematodes classified as epistrate feeders. Diatoms, euglenophytes, and cyanobacteria are able to migrate vertically in the sediment in synchrony with periods of greater or lesser light and tidal exposure (Saburova and Polikarpov 2003; Mitbavkar and Anil 2004). Nematodes are able to follow microphytobenthic migration toward the surface during the low tide (Boaden and Platt 1971).
Although the vertical migration of meiofauna has been widely discussed in the literature (Boaden and Platt 1971; Palmer and Molloy 1986; Fegley 1987), few studies have assessed interspecific differences (Steyaert et al. 2001; Maria et al. 2012) or used statistically significant spatial replication. We describe herein the vertical distribution patterns of nematodes during a tidal cycle in a subtropical intertidal flat. We tested the hypothesis that exposure time during a tidal cycle significantly contributes to the vertical distribution profile of nematodes as a function of distinct feeding and locomotion behaviors, conditioned by body morphology.
Materials and methods
The experiment was performed in an intertidal flat on Papagaios Island in the euhaline sector of Paranaguá Bay, in southern Brazil (Fig. 1). Local flats are formed by well-sorted fine sand with low organic matter levels (Noernberg et al. 2006) and are often covered with seaweeds such as Ulva and Enteromorpha (Ulvaceae, Chlorophyta) or diatom biofilms (Lana 2003). Tides are semidiurnal mixed, with a maximum range of around 2 meters. Tidal currents are unidirectional in the rising tides with an average speed of 9 cm s−1 (Thomas and Lana 2011). The average salinity is over 30 (Lana et al. 2001). Dynamics of local flats is strongly influenced by the tidal currents, which overcome the effect of the adjacent river flows.
The study was performed during a spring tide, when the tidal flat is exposed nearly twice as long than during the neap tides. Sampling was done every 2 h for 6 h (sampling times T1, T2, T3, and T4), which corresponded to the maximum time of tidal exposure. T1 was performed at the end of the ebb tide, when the tidal flat was still submerged (at 8:30 hours, with 30 cm water cover). The subsequent samplings (T2 and T3) were performed when the flat was fully emerged. T4 was performed during the flood tide, with the flat already submerged (at 14:30 hours, with 50 cm water cover).
Three sites of 1 m2 were established 50 m apart from each other, in order to ensure proper experimental replication. Each experimental site was subdivided in square areas of 10 cm2, which were randomly sampled in each sampling time.
Samples were taken with a PVC corer of 2.5 cm in diameter and 5 cm in length, sectioned in ten 0.5 cm strata. In each experimental site and each sampling time, four samples of sediment were taken for meiofaunal analyses (fixed in 4 % formaldehyde), and three for chlorophyll and phaeopigment analyses (stored in a cooler and subsequently frozen at −18 °C). Water content was measured from samples taken at each site. Sediment temperature was measured in situ at each site using a precision digital thermometer with the sensor inserted into each of the strata. Three additional samples, one in each experimental site, were taken for sediment texture analysis.
Biological samples were initially washed through a sieve with a mesh of 63 μm for the removal of formaldehyde. After the washing, the organisms were separated based on their differential densities (Somerfield and Warwick 1996) using a flotation method based on a colloidal silica solution (Ludox TM 50) adjusted to a specific gravity of 1.15 g cm−3.
All nematodes from each stratum were counted under a stereomicroscope. Permanent slides were mounted for 120 organisms. The nematodes were identified using the identification keys from Platt and Warwick (1983, 1988), Warwick et al. (1998) and taxonomic literature.
The pigments were extracted from the sediment samples with 10 ml of 100 % acetone (Strickland and Parsons 1972). The chlorophyll-a and phaeopigment concentrations were estimated using the Lorenzen equation (Lorenzen 1967). The water content was obtained by the difference between the wet weight of an aliquot of 3 g of sediment and the dry weight after drying in an oven at 60 °C for 12 h. Total organic matter content (TOM) was determined by oxidation with hydrogen peroxide H2O2, and the carbonates were removed by acidification with 0.1 N HCl. Grain-size distribution of the sandy fraction was analyzed using dry sieve technique (% sand = fraction >62 μm) and the fine particle fraction (silt + clay, with particles smaller than 62 μm) followed the pipetting method proposed by Carver (1971). Sediment statistical parameters were calculated using the SysGran software (Camargo 2006). Redox potential discontinuity depth (RPD in cm) was visually estimated as the depth at which sediment color was turned from brown to black.
A tri-factorial permutational multivariate analysis of variance PERMANOVA (Anderson 2001, 2005), based on the Euclidean distance matrices, was used for significance testing of the differences between the physicochemical sediment variables over time. Sampling times and strata were treated as fixed factors, the sites as the random factor, and the water content, temperature, and concentrations of chlorophyll-a and phaeopigments as the dependent variables. The homogeneity of dispersions was tested with PERMDISP, using distances among centroids calculated both within Sites(Ti) averaged depths and within Ti × St averaged sites groups. Data from the chlorophyll-a and phaeopigment concentrations were transformed into log values (x + 1) to meet the assumptions of homogeneity of variances.
Nonparametric multivariate methods from the PRIMER v6 software (Clarke and Gorley 2006) were used to correlate species vertical distribution to biological traits presumed to be relevant to locomotion behavior. Times and strata were defined as the fixed factors and the densities of nematodes species as the dependent variables. Bray–Curtis similarity matrices were based on non-transformed abundance and relative frequency data. Nematode species or taxa were classified in 14 categories according to the morphology of the mouth, tail, body shape, body length, and life history strategy (Schratzberger et al. 2007). Buccal morphology was used to recognize the four trophic categories defined by Wieser (1953) as selective deposit feeders (1A), non-selective deposit feeders (1B), epistrate feeders (2A), and omnivorous predators (2B). The morphology of the tail comprises other four categories defined as short/rounded, filiform/elongated, conical, and clavate (Thistle and Sherman 1985; Thistle et al. 1995). Lastly, four categories were recognized based on the body length (<1 mm, 1–2 mm, 2–4 mm, and >4 mm) and two categories based on the body shape (stout with the length/width ratio <18, and slender with the length/width ratio >18) following Soetaert et al. (2002) and Schratzberger et al. (2007).
Temporal variations of associations during the study were visualized through non-metric multidimensional scaling (nMDS) plots. A tri-factorial PERMANOVA, based on the non-transformed Bray–Curtis dissimilarity matrices, was used to significance testing of the differences between the groups, and homogeneity of dispersions was tested with PERMDISP.
The species choice for univariate analysis followed two criteria: (a) the four numerically dominants in the four trophic groups, namely T. longicaudata, S. parasitifera, S. pulchra, and Viscosia glabra and (b) one species with a different vertical distribution profile in each trophic group, namely Daptonema setosum, M. chandlleri, Gomphionema sp., and Euristomina sp. No selective deposit feeders other than T. longicaudata were included on account of their low numbers.
Once the species that contributed the most to the observed differences were identified, a tri-factorial PERMANOVAs was conducted, the sampling times and the strata were used as the fixed factors, the sites as the random factor, and the densities of nematode species as the dependent variable. The homogeneity of variances was examined by PERMDISP. All fauna data were transformed to the fourth root to meet the assumptions.
The PERMANOVAs were based on the mixed linear model below:
where μ = global average; Tii = time factor, fixed with 4 levels; Stj = stratum factor, fixed with 10 levels; Si(Ti)k(i) = site factor, random with 3 levels, nested in time; Ti × Stij = interaction of the factors time and stratum; St × Si(Ti)jk(i) = interaction of stratum and site nested in time; eijkl = error or residue. In case of significant Ti × St interactions, pairwise tests of Ti within Ti × St were performed to investigate which strata differed in time.
Lastly, a canonical correspondence analysis (CCA) was conducted to correlate the variation patterns of the more representative species with the physicochemical variables. The environmental variables were standardized, and the fauna data were log-transformed. The Monte Carlo permutation test was performed to select the environmental variables that significantly explain the variability in the abundance of nematode species (∞ = 0.05). A second Monte Carlo permutation test was performed to evaluate the significance of the canonical axes. The CCA and the Monte Carlo permutation tests were carried out in the CANOCO software for Windows (Ter Braak and Smilauer 1998).
Environmental characteristics of the intertidal flat
The Papagaios tidal flat is composed primarily of poorly sorted, very fine to fine sand (Table 1). During the sampling period, the intertidal flat was covered with the green alga Ulva flexuosa and presented high densities of the bivalve Anomalocardia brasiliana. Redox potential discontinuity depth, varying between 1 and 1.5 cm of depth, was considered as the limit of the sediment surficial layer.
Temperature differed significantly among strata over sites nested in sampling times (St × Si(Ti), pseudo-F = 7.487, P(perm) = 0.001) (Table 2).
The temperature profile increased in all analyzed strata over the tidal exposure time. On T1 and T2, highest temperatures were observed in the deeper sediment layers (between 4.0 and 5.0 cm depth). An inverse trend was observed on T3, when the highest recorded temperatures occurred in the surface layers (between 0 and 1.0 cm depth). On T4, the temperature profile of the submerged flat was again similar to T1 and T2 (Fig. 2). The water content differed significantly among strata (pseudo-F = 7.470, P(perm) = 0.001) and among sites nested in sampling times (pseudo-F = 2.437, P(perm) = 0.012), but not in the tested interaction terms (Table 2). The water content was always higher in superficial sediment layer throughout the experiment (0–0.5 cm depth) although there was a relative increase in the deeper layers (between 2.5 and 3.5 cm depth) on T2. The water content profile on T3 resumed to what was observed before (Fig. 2).
Chlorophyll-a concentration differed significantly among strata over the sampling times (pseudo-F = 1.626, P(perm) = 0.050). Pairwise comparisons showed that on T1, when the tidal flat was submersed, chlorophyll-a concentration was significantly higher in 0–0.5 and 0.5–1.0 cm depths, compared with subsequent depths, than in other sampling times. On T2, at 1.0–1.5 and 1.5–2.0 cm depths, when the tidal flat was exposed, chlorophyll-a concentration was similar to T1 and significantly higher than in T3 and T4 (Fig. 3).
Phaeopigments concentration differed significantly among strata (pseudo-F = 8.369, P(perm) = 0.001) and among sites nested in sampling times (pseudo-F = 2.279, P(perm) = 0.021), but not in the tested interaction terms (Table 2). During the ebb tide (T1), when tidal flat was still submersed, phaeopigments concentration was lower in 0- to 0.5- and 0.5- to 1.0-cm strata in comparison with the other sampling times, when the highest concentrations were always recorded in the surface sediment layers (Fig. 3).
Variation patterns in the vertical distribution of nematode associations
The average number of nematodes per site with all layers integrated (5 cm depth) was 3229 ± 1256 ind. 10 cm−2. The total number of identified nematode taxa was 54 with an average per site of 29 ± 3 ind. 10 cm−2. Terschellingia longicaudata, Spirinia parasitifera, Sabatieria pulchra, Metachromadora chandlleri, Pseudochromadora incubans, and Gomphionema sp. accounted for 75.1 % at site 1, 77 % at site 2 and 80.4 % at site 3 of the relative abundance of nematode association (Table 3).
The structure of nematode associations and biological traits matrix differed significantly among strata over sites nested in sampling times St × Si(Ti) (pseudo-F = 1.187, P(perm) = 0.011 and pseudo-F = 1.275, P(perm) = 0.001, respectively). Therefore, separate nMDS was performed to each site (Fig. 4). SIMPER analysis showed that eight species, T. longicaudata, S. parasitifera, S. pulchra, M. chandlleri, P. incubans, Gomphionema sp., Chromadorina germanica, and Anoplostoma viviparum, accounted together for more than 75 % of dissimilarity among the sampling times across all analyzed strata. Biological traits that most contributed to dissimilarities (>75 % of cumulative percentage) among sampling times across all strata were selective deposit (1A) and epistrate (2A) feeding types, filiform and conical tail shapes, intermediate size classes of adult individuals (1–2 mm and 2–4 mm) and slender and stout body shapes.
We can recognize two different vertical distribution profiles. The first distribution profile was shown by the numerically dominant T. longicaudata that is a selective deposit feeder (1A) and has filiform tail, slender body, and size varying between 1 and 2 mm. The second profile was displayed mainly by S.parasitifera, M. chandlleri, P. incubans, and Gomphionema sp that are epistrate feeders (2A), with conical tails, stout, and slender bodies and size varying between 1 and 2 mm and 2–4 mm (Table 3).
Variation patterns in the vertical distribution of individual species
Only the densities of the numerically dominant Terschellingia longicaudata differed significantly among strata over the sampling times (pseudo-F = 1.439, P(perm) = 0.026). The pairwise test performed on the interaction term of the sampling times and strata (Ti × St) showed that the average densities were significantly higher in 0–0.5 cm depth at T1 than at the other sampling times. At T4, densities were significantly smaller in the depth of 0.5–1.0 cm and significantly higher in 1.5–2.0 cm depth compared to the other sampling times (Fig. 5).
With the exception of S. pulchra, the densities of analyzed species differed significantly among strata and among sites nested in sampling times Si(Ti) but not between the interaction term St × Si(Ti). Thus, vertical distribution patterns were consistent and did not vary among sites (Table 2).
Spirinia parasitifera, Metachromadora chandlleri, and Gomphionema sp. are epistrate feeders (2A) with conical tail, but differ in body size and body shape. S. parasitifera has a longer body size (between 2-4 mm), and M. chandlleri has a stouter body shape. In addition, the three species presented distinct vertical distribution patterns. While the maximum densities of S. parasitifera were recorded in the subsurface layers of the sediment between 0.5 and 1.5 cm (Fig. 5), maximum densities of M. chandlleri were recorded in the surface layers, between 0 and 1.0 cm depth. Gomphionema sp. occurred preferentially in the deeper layers between 1.5 and 3.5 cm (Fig. 6).
Viscosia glabra and Eurystomina sp. are predators (2B) and have slender body shape; however, they differ in characteristics such as the tail shape and body size (filiform and conical, 1–2 and 2–4 mm, respectively). Both species displayed near-surface distributions, although V. glabra has a wider vertical distribution profile with maximum densities between 0 and 1.5 cm depth. Eurystomina sp. preferentially occurred in the surface layer between 0 and 0.5 cm (Fig. 7).
Sabatieria pulchra and Daptonema setosum are non-selective deposit feeders (1B), with a clavate tail, slender body shape, and body size between 1 and 2 mm. The maximum densities of D. setosum were recorded in the surface layers of the sediment, between 0 and 1.0 cm. On the other hand, the vertical distribution profile of S. pulchra differed significantly among sites nested in sampling times St × Si(Ti) (pseudo-F = 1.202, P(perm) = 0.049). Large density variations were recorded among experimental sites (Fig. 8).
Correlation between the species and the environmental variables
The canonical correspondence analysis showed that the species V. glabra and D. setosum, represented in the positive part of axes 1 and 2, and M. chandlleri, represented in the positive part of axis 1 and close to the origin of axis 2, are associated with high concentrations of chlorophyll-a and phaeopigments, low levels of sediment water content, and low temperatures. Eurystomina sp., represented in the positive part of axis 1 and negative part of axis 2, is associated with high levels of sediment water content and low temperatures. S. parasitifera and S. pulchra, represented in the negative part of axis 1 and in the positive part of axis 2, are associated with high temperatures, low concentrations of chlorophyll-a and phaeopigments, and low levels of sediment water content. T. longicaudata, represented in the negative part of axis 1 and close to the origin of axis 2, and Gomphionema sp., represented in the negative part of axes 1 and 2, are both associated with low concentrations of chlorophyll-a and phaeopigments, low levels of sediment water content, and low temperatures (Fig. 9).
The environmental variables included in the model, with the exception of temperature, explain the significant variability in the densities (P < 0.05) of the nematode species (Table 4). The first two axes of the CCA explain 97 % of the relationships between the fauna and the environmental variables. The Monte Carlo permutation test indicated that the explanation of the axes is significant (P = 0.005).
Our study showed that only the vertical distribution profile of the numerically dominant T. longicaudata was unequivocally altered by varying exposure during a tidal cycle. The hypothesis that exposure time during a tidal cycle significantly contributes to the vertical distribution profile of nematodes as a function of distinct feeding and locomotion behaviors, conditioned by body morphology was thus only partially supported.
Two distinct behaviors were displayed by two different species groups. The first pattern was displayed by active species with filiform tail, slender body shape, and body size between 1 and 2 mm, which performed vertical migration. Tail shape, size, and shape of the body are well recognized as relevant to explain the ability of locomotion in nematodes (Thistle and Sherman 1985; Soetaert et al. 2002; Schratzberger et al. 2007). Species belonging to this group also share thin cuticles. Boaden and Platt (1971) suggested that the species with thinner cuticles are less tolerant to episodic desiccation and tend to migrate to deeper sediment layers. Their migration behavior can be affected by changes in the temperature profiles, more variable mainly in the surface sediment layers, between 0 and 1.5 cm. This was mainly due to the direct impact of the solar radiation and the changes in the local albedo as a tidal exposure function.
The second group, dominant between 0 and 0.5 cm depth, was composed by epistrate feeders (2A), with conical tail, slender body shape, and body size between 1 and 2 mm. These species did not display vertical migration though they share some traits with the first group, such as size and body shape, which facilitate locomotion in the interstitial spaces. Their feeding behavior can explain their greater concentration or restriction to the surface strata. Boaden and Platt (1971) and Steyaert et al. (2001) suggested that the vertical distribution of epistrate-feeder nematodes could be related to the movement of the microphytobenthos, which is able to migrate vertically into the sediment in synchrony with periods of greater or lesser tidal and light exposure. However, the epistrate-feeder species did not show any clear trends of vertical migration during the tidal cycle, despite their locomotory abilities. This pattern is in accordance with the behavior of microphytobenthic preys, which remained in the surface layers. Rather than to vertical migration, the differences in concentrations of cloroplastic pigments among sampling times were due to high small-scale variability possibly caused by feeding and bioturbation by the bivalve Anomalocardia brasiliana. Despite significant variations in pigments content in experiments with the bivalve Alba alba, bioturbation activity is probably limited to feeding and sediment reworking and does not consist of deep organic matter burial (Braeckman et al. 2011a, b).
The numerically dominant species, T. longicaudata, migrated to deeper layers of the sediment during emersion periods. The intensification of this migration behavior at T4, just after the flood tide, stresses the importance of the tidal currents and their erosive potential on changing nematode vertical distribution patterns, as suggested by Boaden and Platt (1971), Fegley (1987), Steyaert et al. (2001), Gallucci and Netto (2004). This species displays the feeding strategies and body characteristics that favor an active migrating behavior. Soetaert et al. (2002) correlated smaller body size and filiform shape with greater mobility described. Vertical segregation of nematode predators and preys may also be a function of predation pressure and top-down control on nematode associations (Maria et al. 2012). The search for different food items can be an additional motivation for migration. Moens et al. (1999) reported that selective deposit feeder nematodes are extreme specialists and respond differently to the quality and quantity of food.
Spirinia parasitifera and Metachromadora chandlleri did not display vertical movements, but showed a zonation pattern, concentrating in more surficial layers, probably due to their reduced locomotion abilities because of their body length (in the case of S. parasitifera) or body shape (in the case of M. chandleri). These conditions were seen as adaptations against predation (Soetaert et al. 2002). In addition, their tolerance to temperature variations and their food preferences may be related to this behavior. On the other hand, Gomphionema sp concentrated in the deeper layers of the sediment probably due to a lesser tolerance to sediment variations and a better locomotion capacity.
Viscosia glabra and Eurystomina sp. are omnivores/predators (2B) and share a slender body shape, although they differ in the size and shape of the tail (1–2 and 2–4 mm, conical and filiform, respectively). No evidence of vertical movement behavior was observed for these two species, but V. glabra displayed a wider vertical distribution profile. V. glabra is more able to move through more compacted sediments because it is smaller than Eurystomina sp., besides possessing a filiform tail and slender body. Spending less energy in foraging during the emersion periods and preying upon smaller preys can be advantageous. Eurystomina sp. are larger animals, and their motility is facilitated by higher water content in the surface layer. Prey capturing rates have been shown to be positively correlated with the sediment water content (Gallucci et al. 2005). Water content was more stable in the surface layers, probably because of the low permeability of fine sediments and the roughness of the sediment surface, which led to the formation of puddles over the entire tidal flat area.
Although S. pulchra presented a wider vertical distribution than D. setosum, both are non-selective deposit feeders (1B) and share clavate tail shape, body size between 1 and 2 mm, and slender body shape. The wider range of vertical distribution can be competitive advantageous for S. pulchra that is well-known resistant to anoxic and sulphydric conditions and is able to exploit the available food resources at deeper sediment layers (Steyaert et al. 2003, 2005). On the other hand, the vertical distribution of D. setosum did not vary significantly among sites. The species always remained in the surface layers of the sediment. This behavior may be related to a feeding preference for diatoms (Steyaert et al. 2001; Moens et al. 2005), an increased tolerance to changes in sediment characteristics, resulting from a well-developed cuticle (Boaden and Platt 1971), and the adaptive response to the action of currents in events of submersion. This species possesses caudal glands that help in both the movement and adhesion to the substrate.
Although the spatial variability of the meiofauna is relatively well documented on small scales (Pinckney and Sandulli 1990; Azovsky et al. 2004; Somerfield et al. 2007), studies on the vertical migration of marine nematodes with a statistically relevant spatial replication have not been previously performed. By incorporating meiofaunal spatial variability in our model for testing a working hypothesis, it was possible to recognize whether the processes of nematode migration occurred recurrently in the tidal flat as a whole or whether these processes were punctual or random. A clear trend of migration to deeper sediment layers during emersion periods was displayed only by the numerically dominant T. longicaudata. The vertical distribution profiles of the nematode association as a whole were not homogeneous among the sampling sites due to spatial variations in population densities. These short-scale variations in horizontal distribution may reflect distinct aggregation and dispersal patterns among the species (Somerfield et al. 2007). Distribution patterns can be modified by the erosive potential of the waves and tide currents (Gallucci and Netto 2004), chemical changes caused by the death and decomposition of organisms (Ólafsson 1992), bioturbation and bioirrigation engineering (Pinto et al. 2006; Braeckman et al. 2011a, b), competition with the macrofauna for food (Ólafsson 2005), preferential selection of food (Gallucci et al. 2005; dos Santos et al. 2008; Franco et al. 2008), and the differing locomotion ability of the species (Gingold et al. 2011).
Despite its potential ecological relevance, the analysis of vertical migration of marine nematodes at the functional groups level can mask the variation patterns of individual species. Our results showed that the vertical distribution profile of a slender with filiform tail, numerically dominant free-living nematode is in fact significantly correlated with sediment changes induced by tidal variation. Conversely, body morphology and feeding strategies may restrict the locomotion of most of the other associated nematode species. We provide strong evidence for morphological and functional differentiation in free-living nematode species across a vertical sediment profile in a subtropical tidal flat subject to significant variation in sediment parameters during a tidal cycle. The resulting vertical profiles for individual or species groups are a trade-off among locomotory and feeding strategies and concordant morphological adaptations.
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We thank three anonymous reviewers for their helpful comments and suggestions. Our thanks also to Nice Shindo for the English translation and helpful comments, to our colleagues and friends Sergio Antonio Netto (Laboratório de Ciências Marinhas, Universidade do Sul de Santa Catarina), Mauricio Garcia de Camargo, Leonardo Sandrini-Neto, Maikon Di Domenico and Verônica Maria de Oliveira (Centro de Estudos do Mar, Universidade Federal do Paraná) for their generous help and advice. Ana Carolina dos Passos, Augusto Luiz Ferreira-Jr., Renato Luiz Bot Neto, Barbara Maichak de Carvalho, Raissa Nogueira, and Diógenes Magno Laube were most helpful during field sampling and sample processing. This study was supported by the Brazilian National Council for Technological and Scientific Development (CNPq), which provided fellowships and grants for the authors.
Communicated by Heinz-Dieter Franke.
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Brustolin, M.C., Thomas, M.C. & Lana, P.C. A functional and morphological approach to evaluate the vertical migration of estuarine intertidal nematodes during a tidal cycle. Helgol Mar Res 67, 83–96 (2013). https://doi.org/10.1007/s10152-012-0306-3
- Spatial structure
- Locomotion behavior
- Feeding strategies
- Functional diversity
- Tidal flat