Aquaculture 261 (2006) 80 – 88 www.elsevier.com/locate/aqua-online Impact of high water carbon dioxide levels on Atlantic salmon smolts (Salmo salar L.): Effects on fish performance, vertebrae composition and structure Laura Gil Martens a,⁎, P. Eckhard Witten b , Sveinung Fivelstad c , Ann Huysseune d , Bjarte Sævareid a , Vibeke Vikeså a , Alex Obach a a c Nutreco Aquaculture Research Centre AS, Sjøhagen 3, P.O. Box 48, N-4001 Stavanger, Norway b AKVAFORSK (Institute of Aquaculture Research), N-6600 Sunndalsøra, Norway Laboratory of Environment, Bergen College of Engineering, Nygårdsgaten 112, P.O. Box 6030, N-5020 Bergen, Norway d Ghent University, Vakgroep Biologie, Ledeganckstraat 35,B-9000 Ghent, Belgium Received 8 July 2005; received in revised form 2 June 2006; accepted 8 June 2006 Abstract The role of high carbon dioxide (CO2) levels on fish performance, bone structure/composition and as a potential cause of spinal deformities was studied. Two groups of fish were exposed to a low (control) and a high level of CO2 for 135 days during the freshwater period. After smoltification, the fish were transferred to seawater and followed up for 517 days until they reached harvest weight (3.1 kg BW). Differences in body weight between the control and high CO2 groups were observed. At the end of the freshwater period, average weight in the group exposed to high CO2 levels was 20.9% lower than in the control group. Specific growth rates (SGR) from the start of the experiment (10 g BW) to smolt stage were 1.63 ± 0.04 and 1.36 ± 0.01 for the control group and the high CO2 group, respectively. Differences in body weight were maintained during the initial stages of the seawater period, but were not observed at harvest weight. Nephrocalcinosis was not observed in any of the experimental groups at the end of the freshwater period and no external signs of spinal deformities were observed either at smolt stage or at harvest weight. X-rays revealed mild abnormalities in some vertebrae bodies, which could not be related to any experimental group. Despite the lack of signs of pathological bone alterations, the histological examination suggested that the exposure to high CO2levels resulted in an increase in trabeculae volume and a higher rate of bone remodeling at the end of the freshwater period. Furthermore, fish exposed to a high CO2 level presented a higher bone ash content at the end of the freshwater period. These differences could not be observed at the end of the grow-out period. © 2006 Elsevier B.V. All rights reserved. Keywords: Atlantic salmon; Carbon dioxide; Growth; Minerals; Bone histology; Deformities 1. Introduction ⁎ Corresponding author. Tel.: +47 51657994. E-mail address: [email protected] (L. Gil Martens). 0044-8486/$ - see front matter © 2006 Elsevier B.V. All rights reserved. doi:10.1016/j.aquaculture.2006.06.031 In recent years, due to the fast growth of the industry, the need for higher numbers of smolts has resulted in a significant increase in fish densities in the tanks during L. Gil Martens et al. / Aquaculture 261 (2006) 80–88 the freshwater period. This has been achieved by the addition of oxygen (O2) to the water, and has resulted in a significant increase in the concentration of carbon dioxide (CO2) reaching levels up to 40 mg/l. CO2 in the water depends on water flow and CO2 excretion rate (Fivelstad et al., 2004a). High levels of CO2 in the water will reduce pH and increase the toxicity of aluminum causing hypertrophy and hyperplasia of the gill epithelium (Fivelstad et al., 2003). Effects of longterm CO2 exposure in rainbow trout (Eddy et al., 1977; Smart, 1979, 1981) and Atlantic salmon smolts (Fivelstad et al., 1999) in freshwater include reduced feed conversion ratio and reduced growth. When fish are exposed to high levels of CO2 for long periods, blood CO2 will increase (hypercapnia) and blood pH will decrease resulting in respiratory acidosis (Eddy et al., 1977; Ultsch, 1996). Fish compensate for acidosis by increasing the plasma bicarbonate levels and excreting phosphate via the kidney (Lloyd and Swift, 1967) and might also mobilise ions from the bones (Storset et al., 1997). Thus, the question remains whether these compensation mechanisms can induce bone demineralization and thereby cause spinal deformities. Exposing salmonids to high levels of CO2 is associated with nephrocalcinosis, a condition characterized by the presence of mineral deposits in the kidney tubules (Smart, 1981; Fivelstad et al., 1999). The most abundant minerals in these deposits are Ca, P and Mg (Smart, 1979). In the trial by Fivelstad et al. (1999), Atlantic salmon were exposed for 62 days to different concentrations of CO2, during the fresh water phase. The percentage of fish presenting nephrocalcinosis was significantly higher in the group exposed to 32 mg/l CO2 compared to the groups exposed to 7 and 19 mg/l CO 2 . Likewise, in the study by Smart (1979), significantly higher Ca and P concentrations were found in the kidney of fish exposed to high CO2 levels. Such a pathological accumulation of minerals in the kidney clearly reflects a disturbance in mineral homeostasis, which could also affect the bone. The purpose of the present study was to evaluate the impact of high CO2 levels in freshwater on growth performance, bone structure and development of spinal deformities in Atlantic salmon both during the freshwater period and at the end of the grow-out period in the sea. 81 high CO2 level) for 134 days during the freshwater period until they reached smolt stage. Fish were observed in seawater until an average weight of 3.1 kg was achieved. Growth performance was assessed at different intervals throughout the study in freshwater and at the end of the seawater period. Bone samples from the vertebral column were analyzed by radiology and histology and for mineral composition at the end of the freshwater phase only. 2.2. Rearing conditions Atlantic salmon with known history and the same genetic background were distributed in six indoor, experimental tanks (volume of 125 l) at Lerang Research Station (Stavanger, Norway), corresponding to 3 tanks per experimental treatment. Each tank contained 60 fish of an average weight of 10 g. The two experimental groups were exposed to the following CO2 conditions: • Control group (no CO2 addition): CO2 levels corresponded to the CO2 generated by the fish (max. 7 mg CO2/l). • High CO2 group: CO2 was added gradually according to fish size in order to mimic the conditions to which fish may be exposed to under commercial conditions. The targeted CO2 levels in the water were 10, 20 and 35 mg/l during periods 1, 2 and 3 respectively (Table 1). In the present experiment, carbon dioxide of a 99.9% purity was added to the water from a pressurized bottle in a mixing tank, then the water was distributed to the experimental tanks. The water flow was 8 l/min in all the experimental tanks. Seawater was added to the tanks in order to neutralize the acidity of the water. This is common practice in many Norwegian commercial hatcheries to reduce aluminum toxicity. Seawater addition increased with fish size in order to adjust salinities from 0.5‰ for 10 g fish to 5‰ for 30 g fish and larger. The light regime was in accordance to that used for O+ smolts production recommended by Handeland (1998). The fish were exposed to a 12 h light and 12 h darkness regime for 6 weeks, then continued with a 24 h light regime for 2. Material and methods Table 1 Schedule of the trial and targeted CO2 levels (mg/l) in the high CO2 group during the FW stage 2.1. Experimental design Period Day Duration (days) Targeted CO2 level (mg/l) 1 2 3 1–27 28–92 93–135 27 64 41 10 20 35 Atlantic salmon parrs (average weight of 10 g) were exposed to two water CO2 regimes (a standard and a 82 L. Gil Martens et al. / Aquaculture 261 (2006) 80–88 3 weeks until smolt stage. During the trial, the fish were fed commercial extruded diets manufactured by Skretting AS, Stavanger, Norway. The diets were Nutra™ and Nutra Parr™ for the freshwater period and Atlantic™ for the seawater period. Fish were fed twice a day to apparent satiation using automatic feeders. After smoltification, fish were transferred to larger tanks (circular 1m tanks), supplied with seawater. Forty-nine days after transfer, 30 fish per tank (90 per experimental group) were PIT tagged by implanting micro-transponders into the peritoneal cavity. The other 30 fish in each tank were discarded. Tagged fish were then transferred to a 5 × 5 m cage in the sea and followed up during the grow-out period in the sea (519 days) until they reached an average weight of 3.1 kg. the dorsal fin (comprising 8 vertebra) was preserved in 10% buffered formalin (formaldehyde solution at 37%) for histological examination. The following ten vertebrae were sampled for mineral analyses. 2.3. Water parameters 2.6. Histological procedures Water temperature was recorded daily. The average temperatures were 13.1 ± 1.7 °C and 9.2 ± 4.2 °C for the freshwater and seawater periods respectively. During the freshwater period, dissolved oxygen (Oxyguard Handy meter, Point Four Systems Inc., Richmond, BC, Canada) and water pH (pH meter WTW 340, Weilheim, Germany) were measured daily. Oxygen level was always higher than 8 mg/l at the outlet of the tank. Water samples were analyzed for CO2 on days 27, 92 and 134, which correspond to the end of the periods 1, 2, and 3 respectively, according to the method described by Fivelstad et al. (2003). Vertebrae were fixed in 10% neutral buffered paraformaldehyde for 24 h, rinsed in tap water for 24 h, and decalcified for 72 h in a 10% EDTA solution buffered with 0.1 M Tris base, pH 7.0. After decalcification, samples were stepwise dehydrated and embedded in Paraplast. Ten micrometer (μm) serial sections were prepared in the sagittal plane of the vertebrae, from the periphery to the middle plane of the spine. Sections were stained with Masson's trichrome as outlined in Witten and Hall (2002). From each individual four histological sections were examined to evaluate the bone microstructure and the bone cell morphology of osteoblasts, osteocytes and osteoclasts. Based on digitized microphotographs, the two-dimensional bone volume (area covered by bone) and the trabecular number were determined on vertebrae from five animals per group (10 animals in total) following the recommendations of American Society for Bone and Mineral Research (Parfitt et al., 1987). From each animal, four consecutive sections were analyzed. Sagittal sections were taken in a plane, half way between the outer rim and the midline of the vertebral body (Fig. 1a). The area covered by bone was determined by measuring the percentage of surface area occupied by mineralized and non-mineralized bone matrix bone in a square of 600 × 600 μm. Bone structures of the vertebral end plates were not measured. The area covered by bone was manually selected (Fig. 1b). The number of bone trabeculae within the 600 × 600 μm square was determined by regarding each unbranched leg of a bone trabecula as an entity (Fig. 1c). Using the same material as for determining the twodimensional bone volume, osteoclast activity was estimated based on the presence or absence of osteoclasts 2.4. Fish sampling All the fish in the two experimental groups were individually weighed at the start of the trial, at the end of periods 1, 2 and, 3 in freshwater, after 49 days in seawater, and at the end of the seawater phase. The specific growth rate (SGR) was calculated according to the formula: ! FinalW 1=Days SGR ¼ −1 d100 % InitialW where InitialW and FinalW are the initial and final fish weights for a given period and Days is the number of feeding days for the period. At the end of both the freshwater and the seawater period, all fish were examined for external signs of deformities. In addition, at the end of the freshwater period, five fish per tank were individually measured, weighed and X-rayed. Fish were examined for visible signs of nephrocalcinosis in the kidney. The spine below 2.5. Radiology X-rays from all sampled fish (15 per treatment) were taken using a portable Mini X-ray HF80+ machine (Mini X-ray Inc., Northbrock, USA) with Kodak Industrex M Film Ready Pack II (Kodak Industry, France) according to the protocol described by Witten and Hall (2002). Based on enlarged radiographs, vertebral columns of all sampled individuals were examined for signs of skeletal deformation. L. Gil Martens et al. / Aquaculture 261 (2006) 80–88 83 Fig. 1. Diagram showing the location of sections that were taken to determine the area covered by bone and to count the number of bone trabeculae. a: Scheme of a vertebral body. 1 = vertebral body end plate, 2 = bone spongiosa, 3 = parasagittal section plane, halfway between the centre and the outer rim of the vertebral body (black arrow). b: Scheme of a parasagittal section. The black square represents the plane that was chosen to determine the area covered by bone. c: An example of how bone trabeculae were counted within the selected area, here 1–5. (bone resorbing cells) or resorption lacunae, as traces of osteoclast activity. Each section was assigned to one of the following scores: 0 = no resorption, 1 = moderate resorption, 2 = abundant resorption. package, version 5.5.0). Results from the histological examinations were analyzed by non-parametric statistical tests (Kruskal–Wallis). The level of significance was chosen at p < 0.10. 2.7. Vertebrae mineral analyses 3. Results Pooled samples of vertebrae from five fish per tank were taken for mineral analysis. The soft tissue was removed from the spine and the bones were cleaned with demineralized water. Subsequently lipids were removed by rinsing the samples twice in a mixture of acetone and methanol (1:1, v/v). The samples were then dried for 24 h at 105 °C, ashed for 18 h at 550 °C and digested according to the AOAC method (AOAC, 1995). The phosphorous content of the ash was determined colorimetrically (Taussky and Shorr, 1953) whereas all other minerals were quantified by atomic absorption spectroscopy, ICP-AES (Kroglund and Finstad, 2003). 3.1. Water parameters 2.8. Aluminum in gills At the end of the freshwater period, the second gill arch the left side from six fish per CO2 level were dissected and frozen for determination of aluminum concentration. Aluminum was determined using ICP-AES (Kroglund and Finstad, 2003). The levels of aluminum in gills were 18.6± 5.0 and 8.7 ± 0.5 μg/g gill in the control and high CO2 groups respectively. 2.9. Statistics Growth parameters and bone mineral analyses for the two experimental groups were statistically evaluated according to a one-way ANOVA (Unistat® statistical CO2 levels and water pH were determined on days 27, 92 and 134, which correspond to the end of freshwater periods 1, 2, and 3, respectively. CO2 levels in the control group remained low throughout the study, varying from 5 to 7 mg CO2/l, as compared to increasing CO2 levels from period to period in the high CO2 group accomplished by manual addition of CO2 to the water (Fig. 2a). The pH measurements reflected the CO2 levels. In the control group, pH remained constant, averaging 6.6, whereas in the high CO2 group, pH decreased from 6.2 at the end of periods 1 and 2, to 5.8 at the end of period 3 (Fig. 2b). 3.2. Growth 3.2.1. Freshwater period Statistical differences in weight during the freshwater period were observed between the fish exposed to the high CO2 level and the control group (Table 2). The average weight of fish exposed to the high CO2 levels was significantly lower by 10.3%, 7.3% and 20.9% for periods 1, 2 and 3 respectively. Accordingly, the SGR was also significantly lower in the high CO2 group, except in period 2. For the whole freshwater period, the cumulative SGR in the group exposed to high CO2 levels was 16.5% lower than in the control group. No 84 L. Gil Martens et al. / Aquaculture 261 (2006) 80–88 3.2.2. Seawater period The differences in body weight observed at the end of the freshwater period persisted during the first 48 days after transfer to seawater with the SGR being significantly higher in the group exposed to high CO2 levels (Table 3). At the end of the seawater period, no significant differences between the high CO2 group and the control group were observed in terms of weight nor growth (Table 3). 3.3. External examination At the end of the freshwater phase, no external signs of deformities were observed. Condition factor was slightly lower in the high CO2 group (1.05 ± 0.04) compared to the control group (1.10 ± 0.04). No signs of visible nephrocalcinosis were observed in any of the groups. At the end of the grow-out period, all fish were examined externally. Again no visible signs of spinal deformities or vertebral abnormalities could be detected in any of the experimental groups. 3.4. Bone structure Fig. 2. (a) Water CO2 levels measured during the freshwater phase (mean ± S.D.; n = 3). (b) Variation in water pH during the freshwater phase (mean ± S.D.; n = 3). significant differences in mortality rate were found between the two experimental groups. At smolt stage the percentage of cumulative mortality was 6.62 ± 3.1 in the high CO2 group and 6.13 ± 1.5 in the control group. Table 2 Body weights (mean ± S.D.) and specific growth rate (SGR,%) in the two experimental groups for periods 1–3 and the cumulative data for the total freshwater phase Control group Period 1 (days 1–27) Initial weight (g) 9.2 ± 0.8 Final weight (g) 28.51 ± 0.8 SGR (%) 2.88 ± 0.3 Period 2 (day 28–92) Final weight (g) 55.91 ± 2.3 SGR (%) 1.58 ± 0.08 Period 3 (days 93–135) Final weight (g) 82.35 ± 7.3 SGR (%) 0.97 ± 0.1 Cumulative data (days 0– 135) SGR (%) 1.63 ± 0.04 Mortality (%) 6.13 ± 1.5 ns: not significant (p > 0.10). High CO2 group 10 mg/l CO2 10.4 ± 0.3 26.76 ± 0.7 1.99 ± 0.1 20 mg/l CO2 51.82 ± 0.1 1.63 ± 0.1 35 mg/l CO2 65.10 ± 2.2 0.63 ± 0.1 1.36 ± 0.01 6.62 ± 3.1 Statistics ns p < 0.10 p < 0.05 p < 0.10 ns p < 0.05 p < 0.05 p < 0.05 ns An evaluation of the bone structure was conducted based on radiographs and histological sections. The data obtained from the analysis of X-rays revealed no significant differences between fish from the two experimental groups (Fig. 3a–b). Vertebrae deformities, that had no visual effect on the fish external shape, were only observed in one individual out of fifteen individuals for each experimental group (Fig. 3c–d). Even though the X-rays did not reveal morphological differences between the two groups, the examination of histological serial sections suggests that the water CO2 level has an impact on the bone structure (Fig. 4a–c). Fish exposed to a high CO2 level displayed strong Table 3 Initial and final body weight (mean ± S.D.) and specific growth rate (SGR,%) in seawater Control group Period days 1–48 in seawater Initial weight (g) 82.3 ± 7.3 Final weight (g) 144. 8 ± 8.7 SGR (%) 1.28 ± 0.1 Period days 49–519 in seawater Final weight (g) 3215.6 ± 944.7 SGR (%) 0.86 ± 0.05 ns: not significant (p > 0.10). High CO2 group Statistics 65.1 ± 2.2 125.25 ± 5.3 1.41 ± 0.1 p < 0.05 p < 0.05 p < 0.10 3065.0 ± 1094.1 0.85 ± 0.07 ns ns L. Gil Martens et al. / Aquaculture 261 (2006) 80–88 85 Fig. 3. (a) Radiograph of the vertebral column from Atlantic salmon raised in 7 mg/l CO2 (smolt stage). Vertebral bodies are regular shaped with no observed significant variation. Magnification ×6, scale bar = 2 mm. (b) Radiograph of the vertebral column from Atlantic salmon raised in 35 mg/l CO2 (smolt stage). Vertebral bodies are regular shaped and no significant variations are observed. Magnification ×6, scale bar = 2 mm. (c) Radiograph of the vertebral column form Atlantic salmon raised under 7 mg/l CO2 (smolt stage), depicting an example of mild deformation of vertebral bodies consisting of slightly compressed vertebrae (white arrowheads) and enlarged intervertebral spaces (black arrowheads). The deformities observed did not affect the external shape of the fish. Magnification ×6, scale bar = 2 mm. (d) Radiograph of the vertebral column from Atlantic salmon raised under 35 mg/l CO2 (smolt stage), showing an example of mild vertebrae deformation consisting of one slightly compressed (white arrowhead) and two half sided deformed adjunct vertebral bodies (black arrowheads). A similar type of deformity (compression) was observed in the group of animals that were raised under non-elevated CO2 conditions (see panel c). Deformities had no visible consequences for the animals' external shape. Magnification ×6, scale bar = 2 mm. internal bone structures (bone trabeculae), reflected by the increased trabeculae volume (Table 4, Fig. 4b). The analysis of histological sections also suggests that increased CO2 levels result in a high rate of bone remodeling as indicated by the frequent occurrence of osteoclasts (bone resorbing cells) and signs of osteoclast activity (resorption lacunae), as shown in Fig. 4c. This suggestion is based on higher osteoclast index in the high CO2 group when compared to the control group (Table 4). 3.5. Mineral composition of the bone At the end of the freshwater phase, ash content was significantly higher (p < 0.05) in the high CO2 group than in the control group (Table 5). In general all the minerals analyzed were higher in this group compared to the control fish; however these differences were only significant for Ca, P, Cu, and Fe. A slight increase in the Ca:P ratio was also observed in fish exposed to high CO2 levels. 4. Discussion 4.1. Growth Fish exposed to high water CO2 level (10–35 mg/l CO2) during the freshwater period presented a significant lower growth and body weight compared to fish exposed to 7 mg/l CO2. A significant reduction in growth parameters (weight, condition factor) has been observed in earlier investigations (Smart, 1981; Fivelstad et al., 1998, 1999; Graff et al., 2002). Results from experiments performed with Atlantic salmon in freshwater (pH 6.5) indicated that safe levels of carbon dioxide range between 15 and 20 mg/l CO2 (Fivelstad et 86 L. Gil Martens et al. / Aquaculture 261 (2006) 80–88 Fig. 4. (a) Parasagittal section through a vertebral body from Atlantic salmon raised in 7 mg/l CO2 (smolt stage). Bone trabeculae are regularly formed and display no signs of structural changes that could indicate pathological alterations such as micro fractures or enhanced bone remodeling. Masson's trichrome staining, ×63, scale bar = 200 μm. (b) Parasagittal section through vertebral body from Atlantic salmon raised in 35 mg/l CO2 (smolt stage). Similar to the bone trabeculae shown in panel a. Trabeculae are regularly formed and display no sign of pathological alterations. In comparison to panel a the trabeculae are, however, wider and less numerous (see also Table 4). Parts of bone surface are eroded (black arrowheads) indicating abundant bone resorption. Masson's trichrome staining, ×63, scale bar = 200 μm. (c) Higher magnification of an area of intensive bone resorption at the bone trabeculae from a fish raised in 35 mg/l CO2 (smolt stage). Black arrowheads point to typical resorption lacunae, white arrowheads point to multinucleated osteoclasts. Masson's trichrome staining, ×160, scale bar = 80 μm. al., 1999, 2003). In the present experiment a 10% reduction in body weight was observed at 10 mg/l CO2. There is limited knowledge available concerning the effects of carbon dioxide on salmon growth (Fivelstad et al., 1998). One hypothesis is that the reduced growth during the freshwater period might be due to a lower food intake (Smart, 1981) and increased use of energy during stressful conditions (Wendelaar Bonga, 1997; Graff et al., 2002). In addition, it is also known that stress inhibits growth by affecting hormonal pathways, which regulates growth. These effects have been reported in relation to the growth hormone (Pickering, 1993), thyroidal hormones T3 and T4 (Brown et al., 1991) and insulin-like growth factor (IGF-1) levels (Plisetskaya and Duan, 1994). A second hypothesis is based on the aluminum toxicity on the gills. In the present study, water pH was not low enough to increase free aluminum levels (Fivelstad et al., 2004b), as shown by the low levels of aluminum in the gills of the fish from the two experimental groups. Unexpectedly the Table 4 Trabeculae number (mean ± S.D.), area covered by bone (mean ± S.D.) and osteoclast activity in smolts raised under two different CO2 regimes (n = 5) Group Trabeculae number Area covered by bone (%) Osteoclast activity (0–2) Control group High CO2 group 38.9 ± 12.81 35.4 ± 2.98 36.2 ± 2.83a 41.5 ± 3.60b 1.25 2.00 a,b Different superscripts indicate a statistical difference (p < 0.05). level of aluminum was higher in the control group than in the high CO2 group. In other studies, there was no effect of high carbon dioxide levels on fish performance in freshwater (Smart, 1979; Fivelstad et al., 2004b). The possibility that fish can develop a physiological tolerance towards certain chronic sub-lethal environmental stressors, like carbon dioxide, should be considered (Lloyd and Swift, 1967; Wedemeyer, 1980). Differences in body weight were maintained during the initial stages of the seawater period. SGR was significantly higher in the high CO2 group immediately after transfer likely due to compensatory growth or Table 5 Bone mineral composition at smolt stage (mean ± S.D., n = 3; pooled samples from 5 fish per tank) Ash (%) Ca (%) P (%) Ca:P Cu (mg/kg) Mg (%) Mn (mg/kg) K (%) Na (%) Fe (mg/kg) Zn (mg/kg) Al (mg/kg) Control group High CO2 group Statistics 32.1 ± 1.9 11.1 ± 0.8 6.2 ± 0.2 1.8 ± 0.1 4.2 ± 0.4 0.2 ± 0.0 23.3 ± 2.0 0.6 ± 0.0 0.2 ± 0.0 15.5 ± 3.5 409.2 ± 39.5 <0.2 34.2 ± 1.2 12.9 ± 1.4 6.9 ± 0.8 1.9 ± 0.0 5.0 ± 0.8 0.3 ± 0.1 24.3 ± 3.5 0.6 ± 0.1 0.2 ± 0.1 30.5 ± 17.1 400.8 ± 46.1 <0.2 p < 0.05 p < 0.10 p < 0.05 p < 0.10 p < 0.05 Ns Ns Ns Ns p < 0.10 Ns – ns: not significant (p > 0.10). L. Gil Martens et al. / Aquaculture 261 (2006) 80–88 because the fish were smaller than in the control group. This is in accordance with a study by Fivelstad et al. (1999) and Graff et al. (2002), where post-smolts seemed to completely recover from a weight gain depression caused by high dissolved CO2 levels in freshwater. However, no significant differences in weight and condition factor were observed between groups at the end of the seawater period. The duration of the present experiment was longer than previous CO2 experiments (Fivelstad et al., 1999, 2003). 4.2. Bone and spinal deformities Fish subjected to high water CO2 level displayed a significantly elevated bone ash and bone mineral content. The fish appeared externally normal and the condition factor was relatively similar in both groups. Furthermore, no external spinal deformities were observed in any of the two groups. The X-rays revealed mild abnormalities of vertebral bodies in two animals (out of 30), which could not be related to any experimental group. Severe deformities such as lordotic, kyphotic and skoliotic curvatures, compressed or fractured vertebral bodies and chordal tissue alterations (Vågsholm and Djupvik, 1998; Gavaia et al., 2002; Witten et al., 2005, Gil Martens et al., 2005) involving large parts of the spine, were not observed. The histological analysis of the spine indicated that fish exposed to high CO2 have an increased 2D bone volume (bone trabeculae) and a high rate of bone remodeling as indicated by increased bone deposition (osteoblast activity) and resorption (osteoclast activity). Since a CO2 related acidosis leads to the mobilisation of minerals from the skeleton and causes elevated renal mineral discharge (Storset et al., 1997; Weger et al., 1999), findings about a higher bone mineral content and a higher 2D bone volume in fish exposed to increased ambient CO2 levels are surprising. Indeed, also the observed stimulation of bone resorption should lead to a decrease of mineral content and volume in the bone. However, similar to mammals, resorption of the skeleton in salmonids and in related teleosts groups is coupled with bone formation (Witten et al., 2000, 2001; Witten and Hall, 2002). As observed in mammals (Manolagas, 2000), the stimulation of bone resorption can concurrently stimulate bone formation, enhance the total bone turnover and result in the increase of the bone volume. To satisfy extra mineral demands associated with the elevation of the bone metabolism, salmon and other teleosts can follow different pathways such as the increased intake of calcium via the gills, the mobilisation of minerals from other parts 87 of the skeleton, and the increased intestinal absorption of calcium and phosphate (Vielma and Lall, 1998; Persson et al., 2000; Witten and Hall, 2002). Since intestinal absorption is the main source for phosphate and because bone is mineralized by calcium phosphate (Vielma and Lall, 1998; Witten and Huysseune, in press), a CO2 triggered elevated bone turnover likely requires a sufficient nutritional phosphate supply in order to prevent under-mineralized and malformed bones (Baeverfjord et al., 1998; Helland et al., 2005). An additional argument to explain the findings that animals exposed to elevated ambient CO2 levels display a high bone mineral content relates to the fact that the fish of the experimental group display a reduced specific growth rate. Bone formation consists of two steps. The first step is the production of the non-mineralized bone matrix by bone osteoblasts and the second step is the slow mineralization of the bone matrix (Witten and Huysseune, in press). Fast bone growth, as it is generally the case under farming condition compared to the normal growth of wild animals, can thus lead to the production of large amounts of non-mineralized bone matrix, that only later (e.g. during the salmon sea life phase) mineralizes sufficiently (Witten and Hall, 2002; Fjelldal et al., 2004). In turn, the slower growth of animals in the experimental group could have allowed a more complete mineralization of the bone matrix and thus contributed to the elevated bone mineral content. 5. Conclusions In the present study levels of water carbon dioxide from 10 to 35 mg/l have been shown to be detrimental to Atlantic salmon growth in the freshwater period. Differences in weight were maintained during the initial stages of the seawater period but were not observed at harvest weight. No spinal deformities were observed throughout the study. 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