1. Introduction
Mediterranean rivers are characterized by frequent hydrological disturbances, including seasonally predictable drought events, exposing biota to harsh environmental conditions [
1]. An extensive period of low summer flows naturally leads to an increase in temperature and primary production, and subsequently to a reduction of oxygen levels [
2]. Mediterranean fish populations are adapted to naturally occurring seasonal oxygen fluctuations [
1]. However, human activities, such as water abstraction, the discharge of organic wastes, and the diffusion of agricultural fertilizers into aquatic systems, are common problems in Mediterranean rivers, causing further diminishment of oxygen levels of already stressed freshwater systems and possibly leading to hypoxic conditions [
3,
4] that affect fish and subsequently the entire aquatic community [
3,
4,
5,
6].
Hypoxic conditions can cause behavioral and physiological stress in fish [
7], which can entail many ecological consequences, including impaired reproduction, feeding, and predator avoidance [
8,
9]. Regarding swimming activity, fish experience a trade-off between activity increase as they try to find more oxygenated water and activity decrease due to lower oxygen availability [
10]. When exposed to hypoxia, fish groups may reduce their school density and size as they tend to increase their horizontal spacing to one another in a tentative manner to counteract the limiting effect of oxygen depletion on schools [
5]. However, this may cause disadvantages, such as lower coordination or higher energetic costs of locomotion [
11]. Both activity changes, individual fish movements and shoaling cohesion, are, however, species-dependent and are influenced by the degree of hypoxia [
5,
9]. Too low oxygen saturation will at some point be lethal for fish, whereby the lethal concentration also differs between species [
12].
The Mediterranean region has been identified as one of the most prominent hot spots of climate change [
13]. According to future predictions of climate change for Southern Europe, precipitation will decrease by up to 20% [
14], which will also entail significant changes in seasonal runoff asymmetry [
15]. Hence, exacerbated and extended summer low flow conditions, in combination with existing human pressures, will likely increase the frequency and duration of hypoxic events in rivers [
1,
15,
16]. To protect and manage rivers, it is vital to understand the impact of deoxygenation on individual fish movements, schooling behavior, and the implications thereof for fish populations, which are a pivotal component of aquatic ecosystems.
To our knowledge, no study has assessed the effects of oxygen depletion on the movements of Mediterranean freshwater fish. Therefore, this work analyzed the impact of three different dissolved oxygen levels on the behavior of a common fish species of the Iberian Peninsula, the Iberian barbel, Luciobarbus bocagei. We hypothesized that increasing levels of oxygen depletion would (1) reduce fish movement and (2) decrease the cohesion of fish shoals.
2. Materials and Methods
We conducted flume experiments in a section (2.0 × 1.0 m) of an artificial channel, set at a slope of 3% and a discharge of 28 L∙s
−1, resulting in a water depth of 0.7 m. We caught 75 wild adult Iberian barbel,
Luciobarbus bocagei (150–250 mm total length), via electrofishing in the Lizandro River, Portugal (33 m a.s.l.), and brought them to the lab facilities (92 m a.s.l.), where they were held in three 800 L tanks (25 fish per tank) in a controlled environment for 48 h before experimentation. After the trials, fish were returned alive to the river. Further details on fish sampling, holding, and the testing facility are given in Branco et al. [
17,
18] and Santos et al. [
19].
In each experiment, we monitored the movement of a shoal of five fish [
20] under three levels of dissolved oxygen (DO) conditions: (1) a control level (normoxic condition with DO saturations >80% [
21]), (2) a mild depletion level of 48.4% DO saturation (4.4 ± 0.2 mg∙L
−1), and (3) a high depletion level of 16.5% DO saturation (1.4 ± 0.1 mg∙L
−1) (
Table 1). These levels allowed for testing along a decreasing gradient, whereby the latter represents a level of extreme oxygen depletion that may induce stress or even death in fish [
6,
22]. We reduced oxygen values by adding sodium sulfite (Na
2SO
3). This compound is a recognized oxygen scavenger [
23] that has been used to create oxygen-deficient conditions in fish research [
18,
24], as well as in aquatic research more generally [
25,
26]. Each experiment lasted for eight minutes (six min acclimation [
27] plus two min video-tracking) and was replicated five times, whereby a new subset of fish was used for each trial, giving a total of 75 tested fish.
The experiments were conducted in strict accordance with ethical provisions on the welfare of experimental animals enforced by the European Union and were coordinated by J.M. Santos, who holds FELASA level C certification (
www.felasa.eu) to direct animal experiments. Fish sampling permits were obtained from the Institute for Nature Conservation and Forests (ICNF). Fish experiments and maintenance in the laboratory and experimental facility were authorized by the Department for Health and Animal Protection (Direcção de Serviços de Saúde e Protecção Animal; permit issued on 6 October 2011) in accordance with the recommendations of the “protection of animal use for experimental and scientific work”.
We recorded fish movements with a GoPro Hero 3 Black edition camera mounted above the channel. The camera was set to record at 1280 × 720 pixels. We processed the videos with GoPro Studio to exclude the fisheye effect and then analyzed them at 10 frames per second, resulting in 1200 data points per single fish (
Table 1) with the software Tracker (
http://physlets.org/tracker/), whereby we calibrated the measurement settings of each video with the size of the channel’s bottom tiles (20 × 20 cm).
We calculated kinematics indicators, i.e., mean swimming velocity (cm∙s
−1), acceleration (cm∙s
−2), and distance traveled (cm) for every single fish to investigate spontaneous locomotion activity changes between DO treatments [
27]. To test for differences in shoaling cohesion between treatments, we measured the horizontal (XY) inter-individual distance between all fish within a shoal, based on center of mass [
27,
28], whereby we used the average of the minimum, mean, and maximum values as a proxy for the shoal cohesion. In all analyses, we first tested for overall statistical significance between the treatment levels. If this was detected, it was followed by pair-wise post-hoc tests. For most of the tests, data did not fulfill all assumptions required for parametric tests. Therefore, omnibus tests were conducted with the non-parametric Kruskal-Wallis H test, followed by Dunn’s pairwise tests (adjusted using the Bonferroni correction) (α = 0.05) using SPSS 24. The dataset to this article can be found online in the
Supplementary Material Section (Datasheet S1).