JOURNAL OF PLANKTON RESEARCH j VOLUME 26 j NUMBER 1 j PAGES 99–105 j 2004 SHORT COMMUNICATION Lagrangian description of zooplankton swimming trajectories MARCO UTTIERI*, MARIA GRAZIA MAZZOCCHI, AI NIHONGI1, MAURIZIO RIBERA D’ALCALÀ, J. RUDI STRICKLER1 AND ENRICO ZAMBIANCHI2 1 LABORATORY OF BIOLOGICAL OCEANOGRAPHY, STAZIONE ZOOLOGICA ‘ANTON DOHRN’, VILLA COMUNALE, 80121 NAPOLI, ITALY, GREAT LAKES WATER INSTITUTE, UNIVERSITY OF WISCONSIN MILWAUKEE, WI 53204, USA AND 2INSTITUTE OF METEOROLOGY AND OCEANOGRAPHY, UNIVERSITY OF NAPLES ‘PARTHENOPE’, VIA DE GASPERI, 80121 NAPOLI, ITALY *CORRESPONDING AUTHOR: [email protected] Three-dimensional swimming, in 20 trajectories of Daphnia pulex, was characterized in terms of its kinematic properties. Results show that the random component was stronger than the deterministic component at time scales >1–2 s. Such random movements may have evolved to outwit potential predators and prey. Zooplankton swimming behaviour corresponds to a trade-off between searching for prey or mates and avoiding predators. Motion can be considered a basic adaptive trait and therefore a relevant source of information on the biological and behavioural responses of animals to variable environmental conditions. Moreover, it is a key aspect for understanding aspects of autoecology (Strickler, 1977), including niche separation between species (Strickler, 1985). Zooplankton trajectories have been quantitatively analysed using parameters such as the net-to-gross displacement ratio (Buskey, 1984) or the realized encounter volume (Bundy et al., 1993); their fractal (Coughlin et al., 1992) or multifractal (Schmitt and Seuront, 2001) characteristics have also been considered. These parameters describe the morphological complexity of swimming tracks, without considering other aspects of the motion such as the kinematic properties. Additional tools are necessary to parameterize the paths exhaustively. In the present paper, we decompose the swimming motion of 20 individuals of the freshwater cladoceran Daphnia pulex into two superimposed fractions: a relatively larger scale one and a smaller scale component of irregularly fluctuating character. For the latter, we propose a characterization following a Lagrangian approach. In Lagrangian analysis, each particle is followed in space and time (Pickard and Emery, 1982; Emery and Thomson, 1998) and its trajectory is reconstructed and characterized. The trajectories were characterized in terms of their kinematic properties by means of: (i) the velocity autocovariance (Kundu, 1990); (ii) the spectral analysis (Press et al., 1989; Kundu, 1990; Emery and Thomson, 1998); and (iii) the reconstruction of the kinetic energies associated with the motion (Patterson, 1985). The Lagrangian approach allows us to classify and compare trajectories effectively, thus improving our knowledge about the complex behaviour of zooplanktonic organisms. This approach has been tested on three-dimensional trajectories described by D. pulex exposed to two different light conditions. Forty-four D. pulex adults were sorted from a batch culture (started from some females kindly provided by Dr S. I. Dodson, University of Wisconsin, Madison, WI, USA) and transferred into a vessel (30 30 15 cm) filled with 11 L of artesian water (temperature 20 1 C), without food to avoid any prey influence. The vessel was covered to prevent any turbulent mixing. Animal trajectories were recorded for 2 h, with filming equipment and techniques as described in detail by Strickler (Strickler, 1998). Swimming behaviour of D. pulex was analysed under two different light conditions: a red laser (He–Ne laser, wavelength l = 632 nm) as ‘background light’, and a blue laser (Ar laser, l = 514.5 doi: 10.1093/plankt/fbg116, available online at www.plankt.oupjournals.org Journal of Plankton Research Vol. 26 No. 1, Ó Oxford University Press 2004; all rights reserved JOURNAL OF PLANKTON RESEARCH j VOLUME 26 j NUMBER 1 j PAGES 99–105 j 2004 Fig. 1. Four examples of swimming trajectories of D. pulex. It is evident that, in the presence of the blue laser light (BL condition), the trajectories are more convoluted than in the RL condition. The trajectories are scaled in a reference frame that represents the volume of observation. nm), which is reported to attract D. pulex, Cyclops scrutifer and Chydorus sphaericus (Strickler, 1998) (Figure 1). Through the entire filming, the area was always illuminated by the red laser. During the first 60 min, the room lights were on (RL condition), then during the following 45 min the blue laser was added to the red one and the room lights were off (BL condition). For the next 5 min, the blue laser was off and then it was switched on again; room lights were still off. Prior to filming, the animals were allowed to acclimatize to the light condition for 10 min. Here we report the analysis of the 20 longest clips recorded, each one lasting nearly 90 s (10 clips in RL condition, 10 clips in BL). Shorter clips, besides not being comparable with the 90 s ones, would not yield as reliable statistics. For each clip, the three-dimensional coordinates of the displacement were obtained using an Amiga-running tracking software (Strickler, 1998). All clips were digitized with the sampling frequency ( fs) at 6 Hz. Since the maximum appendage beat rate of D. pulex is 7 Hz (Porter et al., 1982), this value of fs allowed us to reconstruct the trajectories without redundant information on the movement of the appendages. The data so obtained were neither smoothed nor fitted. 100 M. UTTIERI ETAL. j ZOOPLANKTON SWIMMING TRAJECTORIES The swimming trajectories performed by D. pulex were quite complex (Figure 1). The scales involved in the motion spanned between some centimetres (i.e. the length spanned by the trajectory as a whole) and 1–2 mm (i.e. the typical scale of the organism displacement). These two scales were clearly separated. The larger one was characterized by repeated, even though non-periodic, abrupt changes or even complete reversals of direction, showing strong differences between RL and BL conditions (Figure 2). We evaluated the autocovariance of the fluctuating part of the three components of the velocity, in order to determine the degree of randomness of the swimming tracks, where we define a random, or stochastic, variable as an irregularly fluctuating one (Gardiner, 1990; Gnedenko, 1997). Velocities were computed using a central difference method. The autocorrelation of the i-th component of the velocity at an arbitrary time t with itself at a later time t + t can be expressed as (Bendat and Piersol, 1966): Rii ðtÞ ¼ ui ðtÞui ðt þ tÞ ð1Þ Dividing the equation by u2i (mean square velocity), we obtain the autocovariance (Kundu, 1990): r ii ðtÞ Rii ðtÞ u2i in terms of their peak frequency composition (Emery and Thomson, 1998). The power spectral density function represents the way the energy associated with the process is distributed over the spectrum of frequencies (Kundu, 1990; Legendre and Legendre, 1998). In both RL and BL, the autocovariance of the three velocity components dropped sharply to zero (deltashaped pattern) indicating very short correlation of velocities (Figure 3). Accordingly, the values of the integral time scale T were very small (Table I). The spectral analysis showed that the motion could be considered as the superposition of a large number of frequencies. The PSD plots displayed a flat spectrum without any pronounced peak (Figure 4), showing that there was no preferential frequency in the motion, either during RL or during BL. Moreover, the PSD plots were characteristic of white noise (no defined slope) confirming the absence of any apparent memory in the velocity. The distinction between different kinetic energies associated with the motion allows the characterization of the strictly kinematic properties of the organisms’ motion itself. Based on the kinematic or Reynolds decomposition, we can assume that the velocity of an organism is the sum of a larger-scale mean field and of a smaller-scale one, fluctuating around zero (Pond and Pickard, 1983; Mann and Lazier, 1996): u ¼ u þ u0 ð2Þ which is as a normalized measure of the correlation of the velocity with itself at subsequent times. For short memory velocities, rii(t) is significantly different from zero only at short time lags. At distant times randomness implies little self-correlation (Bendat and Piersol, 1966), therefore, for t > 0, rii (t) will rapidly decrease and asymptotically approach zero as t increases. The problem of the presence of small-scale coherent motions detectable only in the off-diagonal elements of the autocovariance matrix [rij (t) with i 6¼ j] was recently discussed in the Lagrangian oceanographic context (Reynolds, 2002). None of our trajectories presented any such occurrence. The parameter T, the integral time scale, given by (Kundu, 1990): 1 ð T ¼ r ii ðtÞdt ð3Þ 0 measures the ‘memory’ of the process, being an estimate of how long the velocity at a certain time influences the later motion. Further information can be drawn from the Fourier transform of the velocity autocorrelation [power spectral density (PSD), in the following], which describes the data ð4Þ where the underlines represent vector quantities. The total kinetic energy (TKE) per unit mass is: TKE ¼ u2 2 ð5Þ whereas the kinetic energies associated with the mean (MKE) and stochastic (eddy) (EKE) fields are, respectively: u2 ð6Þ MKE ¼ 2 u0 2 EKE ¼ ð7Þ 2 It is worth noticing that the above energies are kinematic properties associated with the organisms’ motion, and do not reflect any metabolic process. In particular, we evaluated the EKE/TKE ratio over the three orthogonal planes (XY, XZ and YZ) by combining the three velocity components (Patterson, 1985); for example, the three kinetic energies associated with motion on the XY plane are given, respectively, by: 101 TKE ¼ u2 þ v2 2 ð8Þ JOURNAL OF PLANKTON RESEARCH j VOLUME (a) 26 j NUMBER 1 j PAGES 99–105 j 2004 (b) Fig. 2. Histograms of the frequency of the reversals of the three velocity components in (a) RL and (b) BL conditions, evaluated after low-pass filtering the velocity data by means of a 25-element running average. 102 M. UTTIERI ETAL. j ZOOPLANKTON SWIMMING TRAJECTORIES Fig. 3. Autocorrelation of one velocity component of a freely swimming D. pulex. Fig. 4. Power spectral density plot calculated on one velocity component of a D. pulex. Frequencies are in Hz, whereas the power spectral density is in mm2 s2/s. Table I: Mean values ( standard deviation) of the integral time scale T (in seconds) along the three directions (X, Y, Z ) for 20 swimming paths in D. pulex in two different light conditions The mean flow evaluated in order to derive the fluctuating part is the result of averaging the velocities in quasi-cubic subregions (‘bins’) into which the domain spanned by the organisms was divided. Particular attention was paid to the width of the bins (bs ) used; this issue is subject to debate within the oceanographic community [e.g. (Poulain and Niiler, 1989)]. Narrow bins allow the small-scale variability of the process to be accounted for, but wide ones, containing more data-points, yield more reliable statistics (Patterson, 1985). Moreover, a crucial point for the operational usefulness of the kinematic decomposition is the presence of a scale separation between the mean and the residual portions, i.e. bs has to be much larger than the typical length scale of the displacement fluctuations. For these reasons, for each trajectory the evaluation of the different EKE/TKE ratios was reiterated over a range of bs (from 2 to 7 cm). Not only did these values respect the scaleseparation, but also they were large enough so that a minimum of 15 points was present in every bin, thus making the averaging statistically more consistent. The characterization by means of the kinetic energies confirmed the relevant random component in the paths. The role of the kinetic energy associated with the fluctuating portion in the total energetic budget was evident from the values of the EKE/TKE ratios. In both RL and BL they were %0.94 over the three planes considered (Table II), i.e. >90% of the total energetic budget was due to the random component. In addition, the values of the EKE/TKE ratios were comparable for each of the three planes, so that the movement could be assumed to be energetically isotropic independent of the light condition. Integral time scale Mean values SD (s) (n = 10) RL T(X) 1.19 0.41 T(Y) 1.07 0.19 T(Z) 1.18 0.32 BL T(X) 1.34 0.22 T(Y) 1.53 0.32 T(Z) 1.18 0.17 RL, blue laser off; BL, blue laser on. u2 þ v2 2 ð9Þ u02 þ v02 2 ð10Þ MKE ¼ EKE ¼ The EKE/TKE ratio determines the relative importance of the fluctuating component of the velocity in the overall motion, and we therefore used it as an estimate of the irregularity of the motion. Values close to 1 would be typical of random motions, for which most of the total kinetic energy budget is represented by the fluctuating part. 103 JOURNAL OF PLANKTON RESEARCH j VOLUME Mean values SD (n = 10) RL XY 0.94 0.03 XZ 0.94 0.02 YZ 0.95 0.02 0.94 0.02 XZ 0.94 0.03 YZ 0.95 0.02 NUMBER 1 j PAGES 99–105 j 2004 ACKNOWLEDGEMENTS BL XY j random when clues are absent (as in our experimental conditions) and that only once they detect a signal (either mechanical or chemical) does their motion become more coherent and deterministic, reflecting a change in the kinematic properties of the trajectories. Additional tests using experimental conditions resembling those experienced by the animals in nature will be carried out, integrating all the above analysis, so as better to compare the different responses. Table II: Mean values ( standard deviation) of EKE/TKE ratio (non-dimensional), measured over three planes (XY, XZ and YZ ) in the swimming trajectories performed by D. pulex in two different light conditions EKE/TKE 26 EKE, eddy kinetic energy; TKE, total kinetic energy; RL, blue laser off; BL, blue laser on. Based on our results, some conclusions can be drawn. The autocovariance and the spectral analysis characterized the organism’s motion, allowing us to evaluate the degree of randomness of the tracks and the role of the different frequencies involved in the motion. Our results showed that the swimming velocities of D. pulex were not self-correlated even at short times and resembled a random process. This suggests that after few time steps the motion was independent of the previous dynamics and could be in this sense assumed to be stochastic (in the sense described above). It has indeed been shown by the presence of white energy spectra that no dominant frequency occurred in the motion: all the frequencies sum up and the motion of the animal generates a complex hydromechanic signal. The kinetic energies associated with the trajectories confirmed the strong random character of the motion, in agreement with what is suggested by the velocity autocovariance and by the spectral analysis. We suggest that D. pulex adopts such complex swimming behaviour to outwit the sensory perception of potential prey and predators, which could lack cues by which to determine the source of the signal. This hypothesis is in agreement with the ‘fluid-dynamical camouflage’ proposed by Hwang and Strickler (Hwang and Strickler, 2001). The analysis of the kinematics of the swimming tracks may be needed to understand the behaviour of zooplanktonic organisms. Based on our application, some general behavioural hypotheses can be formed. 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