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First published online December 14, 2006
Journal of Experimental Biology 210, 149-165 (2007)
Published by The Company of Biologists 2007
doi: 10.1242/jeb.02628
Changes in mitochondrial oxidative capacities during thermal acclimation of rainbow trout Oncorhynchus mykiss: roles of membrane proteins, phospholipids and their fatty acid compositions
1 Unité mixte CNRS 6521, Université de Bretagne Occidentale,
C.S. 93837, 29238 Brest cedex 3, France
2 Département de Biologie, Université Laval, Québec,
G1K 7P4, Canada
* Author for correspondence (e-mail: Edouard.Kraffe{at}univ-brest.fr)
Accepted 1 November 2006
| Summary |
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Key words: mitochondria, thermal acclimation, oxidative muscle, cytochrome c oxidase, ADP affinity, thermal compensation, phospholipids, plasmalogens, fatty acids, rainbow trout, Oncorhynchus mykiss
| Introduction |
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Lipids that constitute mitochondrial membranes should be regarded as
structural partners of membrane proteins and as potential modulators of
mitochondrial processes (Daum,
1985
). Proper functioning of biomembranes becomes difficult below
the transition temperature at which the liquid crystalline structure of the
acyl core changes into a gel-like structure. Ectothermal organsims are thought
to adapt their membranes to temperature decreases by increasing the acyl chain
unsaturation of phospholipids to maintain membrane fluidity. This homeoviscous
adaptation (HVA) also includes shifts in the proportions of phospholipid
classes (phosphatidylethanolamine (PE) relative to phosphatidylcholine (PC)
and cholesterol content (Hazel and
Williams, 1990
; Hazel,
1995
; Crockett and Hazel,
1995
). Modification of the capacity for oxidative phosphorylation
during thermal acclimation is claimed to be due, at least in part, to HVA
(Van Der Thillart and Modderkolk,
1978
; Wodtke,
1981a
; Wodtke,
1981b
; Itoi et al.,
2003a
; Guderley,
2004
). On the other hand, requirements for specific phospholipids
in the vicinity of electron transport chain components
(Hoch, 1992
) suggest that
changes in the FA composition of specific phospholipids may be central in the
modulation of catalytic activity during thermal acclimation. Thus, due to the
complexity of membrane lipid constituents (sterol, 8 main phospholipid classes
and subclasses, and more than 50 fatty acids) and the elaborately subvided
submembrane domains, specific effects may be obscured when examining the acyl
composition of total phospholipids.
Particularly in the protein-dense mitochondrial membranes
(Hazel and Williams, 1990
),
only a small number of lipid molecules is thought to separate membrane
proteins or protein aggregates. In mammalian systems, mitochondrial membrane
proteins can show specific requirements for phospholipid head group
arrangements and FA in their proximity
(Clandinin et al., 1985
).
Thus, even minor phospholipid classes can have an important functional impact
on membrane-bound enzymes. Cardiolipin (CL), in particular, is specifically
located in the inner mitochondrial membrane, and is a key factor in the
control of CCO, F0F1-ATPase and ANT
(Schlame et al., 2000
).
Localised changes of specific membrane phospholipids, like CL, may be critical
in establishing the activities of membrane proteins and provide a powerful
means of adjusting activity without requiring protein synthesis or
modification of existing proteins during thermal acclimation. Thus, a detailed
characterisation of membrane lipids is a prerequisite to understanding how
heterogeneous mixtures of phospholipids interact with membrane proteins to
alter biological functions. Although thermal acclimation leads to well
characterised changes in the abundance of muscle mitochondria and
mitochondrial oxidative capacities in temperate zone fishes
(Guderley, 2004
), changes of
capacity of protein and phospholipid components have typically been studied
separately. A few exceptions are provided by the classic studies
(Hazel, 1972a
;
Hazel, 1972b
;
Van den Thillart and Modderkolk,
1978
; Wodtke,
1981a
; Wodtke,
1981b
), in which changes in overall phospholipid composition
brought about by cold acclimation were linked with changes in the activity of
succinate dehydrogenase, State 3 respiration and CCO.
Little is known about the time course of thermal acclimation. Modifications
in membrane structure during the time course of thermal acclimation of rainbow
trout follow a defined sequence, as shown by the restructuring of phospholipid
composition and molecular species in kidney plasma membrane
(Hazel and Landrey, 1988a
;
Hazel and Landrey, 1988b
).
After 8 h of cold acclimation (20°C to 5°C), the PC/PE ratio
decreases. The proportions of saturated and monounsaturated FA change after
16-48·h and long-chain polyunsaturated FA only increase after 10-21
days of cold acclimation. Such a sequence of compositional changes in membrane
phospholipids was suggested to explain the non-linear time course of
mitochondrial oxidative capacity during warm and cold acclimation of rainbow
trout (Bouchard and Guderley,
2003
), but no study has established such a relationship.
The present study aims to evaluate at the same time, detailed modifications of phospholipid composition, levels of membrane proteins and functional capacities of red muscle mitochondria during warm acclimation (5°C to 15°C) of rainbow trout Oncorhynchus mykiss. After characterising 5°C-acclimated trout, we studied trout shortly (3 days) after transfer to 15°C and after 8 weeks acclimation to 15°C. By examining mitochondrial substrate oxidation at 5°C and 15°C, the concentrations and activities of mitochondrial components, as well as the phospholipid composition of mitochondrial membranes we sought to identify potential mechanisms by which oxidative capacities change. We measured (1) the levels of adenine nucleotide translocase (ANT), (2) the concentrations of cytochromes a, b, c and c1, (3) the apparent ADP affinity and (4) the activity of CCO. The content of cytochromes a, b and c1 reflect the numbers of respiratory chain complexes: cytochrome b is present in Complexes II and III, c1 occurs in Complex III, and cytochrome a is part of Complex IV. To evaluate the implication of the lipid environment in the time course of changes in mitochondrial oxidative capacities, we determined the proportions of each mitochondrial phospholipid class and subclass as well as their specific FA compositions and the sterol levels at each sampling time.
| Materials and methods |
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Twelve fish were used to assess the oxidative capacities of these winter-acclimatised trout that had been held at 5°C for a week before beginning the study (cold acclimated). Then, water temperature was gradually raised to 15°C over 3 days, and eight specimens were studied during the subsequent 3 days (short-term warm exposed). Finally, 8 weeks after the beginning of the thermal change, when we assumed acclimation was complete (warm acclimated), 12 trout were used to assess final oxidative capacities.
Isolation of mitochondria
The fish were killed by a blow on the head, and the superficial lateral red
muscle was immediately removed and minced. All the manipulations were carried
out on ice except the centrifugations, which were performed at 4°C.
Mitochondria were isolated and assayed
(Guderley et al., 1997
). To
optimise the purity of mitochondrial pellets, additional steps were done
during the differential centrifugation protocol. Briefly, after centrifuging
the homogenate at 900 g for 10 min, the superficial lipid
layer was removed. The remaining supernatant was recentrifuged at 900
g for 10 min. The supernatant obtained was considered free of
unbroken cells or cell debris and was centrifuged at 9000 g.
The resulting pellet was rinsed once to remove MgCl2 by
resuspension in isolation buffer free of MgCl2 and recentrifuged at
9000 g. The mitochondrial pellet was resuspended in a volume
of reaction buffer corresponding to one-tenth of the mass of muscle used.
Measurement of mitochondrial respiration
Oxygen consumption was measured in the reaction buffer at 5°C and
15°C. For each assay, malate was added to a final concentration of 0.37
mmol l-1 to spark the Krebs cycle, and pyruvate was added to a
final concentration of 3.45 mmol l-1. The maximal rate of oxidative
phosphorylation (State 3) was obtained by the addition of ADP to a final
concentration of 0.92 mmol l-1. State 4 rates were measured after
depletion of ADP, once oxygen uptake rates had stabilized. The ADP/O ratio was
measured (Chance and Williams,
1956
).
ADP affinity determinations
The apparent affinity of mitochondria for ADP (Km) was
determined polarographically as described
(Guderley and St Pierre,
1999
). This approach used the hexokinase reaction to maintain
constant ADP levels so that oxidation rates could be obtained at low ADP
levels. The assay medium was supplemented with glucose, MgCl2 and
hexokinase (yeast; Boehringer Mannheim Biochemicals, Montreal, Quebec, Canada)
at final concentrations of 38 mmol l-1 glucose, 19 mmol
l-1 MgCl2 and 3 units l-1 hexokinase.
Hexokinase exerts no control over mitochondrial respiration when the ratio of
mg mitochondrial protein to units of hexokinase is less than 3
(Jacobus et al., 1982
). In our
study, these ratios were consistently less than 0.6. Similar ranges of excess
hexokinase were present for the mitochondria from cold and warm acclimated
trout as well as for short-term warm exposed animals. Pyruvate was the carbon
substrate (3.45 mmol l-1), with malate present at 0.37 mmol
l-1. Saturation curves for mitochondria were determined by
sequential additions of ADP starting with the lowest concentration
(approximately 3x10-3 mmol l-1 total ADP),
followed by gradual additions of ADP to attain saturating concentrations.
Oxygen uptake rates were determined for at least 90 s at each ADP
concentration. Experiments were carried out at 5°C and 15°C. We
standardised the quantity of mitochondrial protein at
0.15 mg
mitochondrial protein ml-1 assay medium to facilitate comparison
between the sampling periods. The apparent Km for ADP
(Km, app) and Vmax (maximal velocity)
were calculated using the Marquardt iterative search algorithm to fit the
Michaelis-Menten equation using Nonlinear Regression analysis (StatGraphics
Plus 5.1). The ADP solutions were calibrated spectrophotometrically using the
pyruvate kinase and lactate dehydrogenase reactions
(Bergmeyer, 1983
).
Cytochromes and ANT concentrations
Cytochromes a, b, c and c1 in the
mitochondrial preparations were quantified by difference spectra. The electron
transport chain components in 2% deoxycholate-dispersed mitochondria were
reduced by 5 mmol l-1 ascorbate and the oxygen in the solution was
eliminated by the addition of dithionite
(Williams, 1964
). The reduced
samples were read against the samples oxidised with 5 mmol l-1
ferricyanide. We used the solution to the simultaneous equations required to
assess the individual cytochrome concentrations
(Williams, 1964
). Difference
spectra were obtained using a double-beam UV/Vis spectrophotometer
(Varian-Cary 210, Mississauga, Ontario, Canada). The concentration of adenine
nucleotide translocase (ANT) was measured in mitochondrial suspensions by
titration with its noncompetitive irreversible inhibitor, carboxyatractyloside
(CAT) (Guderley et al., 2005
).
State 3 respiration was gradually inhibited and the inhibition was considered
complete when addition of CAT had no further effect on oxygen uptake. The
quantity of ANT in mitochondrial suspensions corresponded to the amount of CAT
needed for inhibition.
Protein concentrations
The protein concentration in mitochondrial suspensions was determined by
the bicinchoninic acid method (Smith et
al., 1985
) using bovine serum albumin (BSA) as the standard.
Before analysis, an aliquot of each mitochondrial preparation was resuspended
in the reaction buffer minus BSA and centrifuged at 9000 g at
room temperature for 10 min. The supernatant was discarded and the pellet
resuspended, washed and centrifuged twice more to remove the BSA. These
preparations were conserved at -80°C until protein assays.
Cytochrome c oxidase activity
CCO activity was measured at 5°C and 15°C according to published
methods (Bouchard and Guderley,
2003
) except that mitochondrial suspensions were diluted in
phosphate buffer without Triton-X (45 mmol l-1 KH2
PO4 and 30 mmol l-1 K2HPO4, pH
6.8). We used an initial optimal cytochrome c concentration of 100
µmol l-1. All assays were run in triplicate using fresh
mitochondrial preparations. Activities were calculated using an extinction
coefficient of 19.1 mmol l-1 cm-1 and are expressed as
µmol cytochrome c transformed min-1 (first order
reaction).
Membrane lipid analysis
The membrane lipids of mitochondrial suspensions were extracted according
to the method described (Folch et al.,
1957
). Before lipid extraction, the aliquot of mitochondrial
preparation was resuspended in the reaction buffer minus BSA and centrifuged
at 9000 g at room temperature for 10 min. The supernatant was
discarded and the pellet resuspended, washed in reaction buffer and
centrifuged a further two times. The final extract was stored at -80°C
under nitrogen after adding 0.01% w/v butylated hydroxytoluene (BHT,
antioxidant).
Separation of polar lipids on silica gel microcolumns
An aliquot of the lipid extract was evaporated to dryness and lipids were
recovered with three washings of 500 µl of CHCl3/methanol (98:2,
v/v) and deposited at the top of a silica gel micro-column (30 mmx5 mm
i.d., packed with Kieselgel 60 (70-230 mesh, Merck, Darmstadt, Germany)
previously heated at 450°C and deactivated with 6 weight% H2O
(Marty et al., 1992
). Neutral
lipids were eluted with 10 ml of CHCl3/methanol (98:2, v/v) and
stored at -20°C for later cholesterol analysis. The polar lipid fraction
was recovered with 20 ml methanol and stored at -20°C for later
phospholipid class separation by high performance liquid chromatography (HPLC)
and FA composition analysis by gas chromatography (GC).
Cholesterol analysis
Cholesterol was analysed in a gas chromatograph (Chrompak 9002, Middelburg,
The Netherlands) equipped with RTX65 (65% diphenyl, 35% dimethylpolysiloxane)
fused silica capillary column (50 mx0.32 mm, 0.2 pm film thickness)
using an on-column injection system and hydrogen as carrier gas, with a
thermal gradient from 60°C to 280°C. Quantification of cholesterol was
achieved by adding a known quantity of cholestane to samples.
Separation of membrane lipid classes and FA analysis
Separation of the phospholipid classes and subclasses followed Kraffe et
al. (Kraffe et al., 2004
)
using two successive HPLC separations with two different mobile phases. This
method allowed the separate analysis of plasmalogen (1-alkenyl-2-acyl-) and
diacyl subclasses of PE and PC jointly with cardiolipin (CL),
phosphatidylinositol (PI), phosphatidylserine (PS), and natural
lysophosphatidylcholine (LysoPC). The remaining diacyl fraction of PE and PC
(diacylPE and diacylPC) presented and discussed in this paper likely contained
the 1-alkyl-2-acyl-form in addition to the 1,2-diacyl. Each fraction was
collected and, after transesterification (methanol/BF3), analysed
by GC for FA composition. Fatty acid methyl esters (FAME) obtained were
identified and quantified using both polar (CPWAX 52 CB, Varian, Middelburg,
The Netherlands; 50 mx0.25 mm i.d.; 0.2 µm thickness) and nonpolar
(CP-Sil 8 CB, Varian; 25 mx0.25 mm i.d.; 0.25 µm thickness) capillary
columns and C23:0 FA as an internal standard. FA were expressed as molar
percentage of the total FA content of each class or subclass. For plasmalogen
ethanolamine (PlsmPE) and plasmalogen choline (PlsmPC) subclasses, the total
percentage was adjusted to 50% to take into account the absence of alkenyl
chains of the sn-1 position hydrolysed by the acid mobile phase.
Calculation of amounts of phospholipid classes
The quantities of each class and subclass of phospholipid were determined
from their respective FA spectrum obtained by GC. To obtain the molar content
of each analysed fraction, a correction factor was applied to their respective
total FA molar contents: x1 for PlsmPE and PlsmPC fractions and for the
natural lysoPC fraction; x1/2 for the diacylPE, diacylPC, PS and PI
fractions, and x1/4 for the CL fraction.
Statistical analysis
Statistical comparisons and linear regressions were carried out with
StatGraphics Plus 5.1 (Sigma Plus Inc., Toulouse, France). One-way analysis of
variance (ANOVA) followed by a posteriori Tukey multiple comparisons
was used for intergroup comparisons of the impact of warm acclimation on
mitochondrial characteristics of trout. Differences were considered
significant when P
0.05.
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| Results |
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Mitochondrial concentrations of cytochromes and ANT
After short-term warm exposure, cytochrome levels were unchanged
(Fig. 1). Warm acclimation
decreased the levels of cytochromes b and c, but left those
of cytochromes a and c1 unchanged. The
protein-specific levels of ANT exceeded those of the cytochromes and were
slightly, but significantly, higher (P<0.05) in short-term warm
exposed trout compared to cold or warm acclimated trout.
Mitochondrial maximal oxidative capacities during warm acclimation
The isolation procedure yielded mitochondria with respiratory control
ratios (RCR; State 3/State 4) ranging from 3 to 9 throughout the experiment.
Maximal rates of pyruvate oxidation (nmol O min-1 mg-1
mitochondrial protein) changed markedly during warm acclimation. Rates were
stable after short-term warm exposure and dropped markedly with warm
acclimation at both assay temperatures (P<0.05)
(Fig. 2). State 4 rates (nmol O
min-1 mg-1 mitochondrial protein) showed a biphasic
pattern, with rates, particularly at 15°C, increasing during short-term
warm exposure and returning to initial values with warm acclimation
(Table 2). These patterns led
the mean RCR values to decrease from 5 to 3.3 with warm acclimation. The
thermal sensitivity (Q10) of maximal rates of pyruvate oxidation
did not change between cold acclimated and short-term warm exposed trout (mean
values of 1.36±0.12 and 1.49±0.07, respectively), but increased
in warm acclimated trout (mean value of 1.84±0.07, P<0.05).
The phosphorylation capacity of mitochondria, expressed by the molar ratio
between added ADP and consumed oxygen (ADP/O), reached significantly higher
values in mitochondria of short-term warm exposed trout at both assay
temperatures compared to cold and warm acclimated trout: 5°C (mean values
of 2.8±0.1 for cold and warm acclimated trout; 3.3±0.2 for
short-term warm exposed) and 15°C (3.1±0.1 for cold and warm
aclimated trout; 3.8±0.1 for short-term warm exposed).
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The denominator typically used to standardise mitochondrial rates is the amount of protein (mg) in the mitochondrial preparation. This reflects protein located both in the matrix and in the membrane. As the adjustments of membrane composition that are a major focus of our study would primarily affect membrane-bound complexes, we examined oxidative capacities relative to the concentrations of cytochromes and ANT, all located in the mitochondrial membrane. For State 3 rates measured at 5°C expressed over cytochrome a, c1 and ANT, the same pattern was observed as with protein specific rates: stability during short-term warm exposure and a decrease with warm acclimation (Fig. 2). On the other hand, at 15°C, use of cytochromes a and c1 as the denominator revealed a biphasic response, with State 3 rates increasing during short-term warm exposure (significant only for cytochrome c1) and then decreasing during warm acclimation. State 4 rates expressed over the cytochromes and ANT changed less with warm acclimation than protein-specific State 4 rates (Table 2).
Changes in cytochrome c oxidase activity during warm acclimation
The time course of warm acclimation changed the activity of CCO in a
similar fashion as the protein-specific capacities of isolated mitochondria
(Fig. 3). CCO activity in
mitochondrial suspensions increased slightly, but not significantly, in
short-term warm exposed trout when assayed at 5°C. Warm acclimation
significantly decreased CCO activity compared to cold acclimated or short-term
warm exposed trout (P<0.05) at both assay temperatures. The same
pattern was found when CCO activity was expressed over cytochrome a
levels. The Q10 for CCO remained between 1.4 and 1.6 during our
experiment. Throughout the experiment, only 4-5% of mitochondrial CCO activity
was used during maximal rates of pyruvate oxidation (State 3/CCO activity
expressed in mU).
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ADP affinity
During the time course of warm acclimation, mitochondria from red muscle
changed their apparent ADP affinity (Km,app), as well as
its thermal sensitivity (Table
3). At 5°C, the highest value for the
Km,app was obtained for cold acclimated trout with
short-term warm exposed and warm acclimated trout having significantly lower
values. On the other hand, at 15°C, short-term warm exposed trout had a
higher Km,app than trout in the other groups. Thus, while
both cold and warm acclimated trout show a 50% decrease of
Km,app with an increase in assay temperature, for
short-term warm exposed trout the apparent Km values did
not differ between 5 and 15°C (t-test, P>0.05).
|
At the assay temperature of 5°C, the Vmax (maximal velocity) calculated by iterative fitting of the Michaelis-Menten equation was close to the values of State 3 respiration (Table 3) and showed the same changes during the acclimation protocol. Thus, the ADP-dependence of mitochondrial oxidative capacities at 5°C was well described by the Michaelis-Menten equation. At 15°C, the calculated Vmax was considerably lower than the measured State 3 rates.
Mitochondrial compositions of membrane phospholipid classes and subclasses during the time course of warm acclimation
Throughout the study, glycerophospholipids (PE, PC, PS, PI, CL and LysoPC)
were the predominant phospholipid classes in mitochondria. Plasmalogen forms
were only found in PE (PlsmPE) and PC (PlsmPC), those in PE being more
prominent. Sphingomyelin was always found in trace amounts, indicating that
the mitochondrial membranes were not significantly contaminated by other
cellular membranes.
During warm acclimation, the relative levels of the phospholipid classes and subclasses changed (Fig. 4), with particularly marked changes in diacylPE, diacylPC, PlsmPE, PlsmPC and LysoPC. The proportion of the diacyl form of PE declined during warm acclimation from 33.95% in cold acclimated trout to 22.94% in warm acclimated trout (P<0.05). With short-term warm exposure, diacylPE levels decreased, but not significantly, to 30.14%. The changes in PlsmPE showed an inverse pattern over the time course of the experiment compared to diacylPE. Indeed, while values of PlsmPE remained stable in short-term warm exposure, levels doubled after 8 weeks of warm acclimation. Thus, warm acclimated trout mitochondria have the highest proportion of plasmalogen in PE (35.6%) while this value was only 14.4 and 16.3%, respectively in cold acclimated and short-term warm exposed trout. Although proportions of diacylPC were similar between cold and warm acclimated trout, the level of diacylPC rose significantly in short-term warm exposed trout concomitant with a decrease, albeit not significant, of lysoPC. PlsmPC content relative to total phospholipids varied in the same way as PlsmPE, remaining stable in short-term warm exposure and doubling in warm acclimation. Although the proportion of plasmalogens in PC was markedly lower than that in PE, the proportion of plasmalogens in PC also reached the highest level in warm acclimated trout (2.7%). The proportions of CL, PS and PI did not vary significantly between acclimation groups. However, LysoPC increased in mitochondria from warm acclimated trout (P<0.05).
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Fatty acyl chain composition of phospholipid classes and subclasses during warm acclimation
Changes in acyl chain composition during the time course of warm
acclimation differed when examined for the total phospholipids
(Table 5) or for the specific
classes (Tables 6,
7 and
8). The acyl chain composition
of plasmalogen subclasses of PE and PC also changed during warm acclimation,
suggesting that FA of these subclasses may influence membrane dynamics. For
the overall phospholipids, saturated fatty acids (SFA) were dominated by 16:0
while 22:6n-3 was the main unsaturated FA. The other major FA were 18:0,
18:1n-9, 18:2n-6, 20:4n-6, 20:5n-3 and 22:5n-3. The time course of warm
acclimation did not greatly affect the FA composition of total phospholipids.
When FA levels differed, it was the mitochondria of warm acclimated trout that
were distinct from those obtained from the other states. The levels of 22:6n-3
rose slightly, but not significantly, before returning to initial values with
warm acclimation. 20:5n-3 decreased with warm acclimation, whereas 18:1n-9 and
18:2n-6 rose. The n-3/n-6 ratio was decreased (P<0.05),
monounsaturated fatty acids (MUFA) were increased (P<0.05),
saturated were decreased (but not significantly) while polyunsaturated (PUFA)
were stable at the different stages of acclimation. Dimethylacetals (DMA),
obtained from the fatty aldehydes bound as vinyl ethers to the sn-1
position of plasmalogen phospholipids, increased in long-term warm acclimated
trout (P<0.05). A modest, but not statistically significant,
decrease in unsaturation index (UI) was noted for warm acclimated trout.
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Changes in the FA compositions of the two prominent mitochondrial phospholipid classes, PE and PC, in both their diacyl and plasmalogen forms (Tables 6 and 7), were similar in magnitude to those in the total phospholipids. For diacylPC, the more unsaturated FA (20:5n-3 and 22:6n-3) decreased in warm acclimation (P<0.05). Correspondingly, 18:1n-9 increased with the same time course. SFA, dominated by 16:0, increased in short-term warm exposed trout, only to fall to initial levels in warm acclimated trout. The plasmalogen form of PC showed fairly constant levels of individual FA. However, warm acclimation increased PUFA and decreased SFA with significant differences between warm and cold acclimated trout. The FA composition of diacylPE differed from that of diacylPC in that 18:0 was also a major SFA and in that 22:6n-3 and 20:5n-3 were respectively higher and lower than in diacylPC. In diacylPE, all statistically significant effects distinguished warm acclimated trout from the other groups, except for 22:6n-3, for which warm acclimated trout only differed from warm exposed trout. Among SFA, 16:0 increased slightly and 18:0 decreased slightly leading to constant total SFA in diacylPE during warm acclimation. As observed for diacylPC, 20:5n-3 and 22:6n-3 decreased in warm acclimated trout (P<0.05), whereas 18:1n-9 tended to increase. The levels of 22:5n-3 became higher than those of 20:5n-3 in mitochondria from warm acclimated trout. Interestingly, 22:5n-3 is the sole PUFA that increased significantly during warm acclimation. These PUFA showed much the same patterns of change in PlsmPE.
More dramatic modifications during the time course of warm acclimation were noted when considering the FA composition of the minor phospholipid classes CL and LysoPC (Table 8). Effectively, warm acclimation caused more marked alterations in acyl composition of these phospholipids than for PC and PE, with many FA being halved or doubled in their levels. In CL, the decrease in 16:0 and monounsaturated FA, mainly 18:1n-7, was accompanied by a marked increase in 18:2n-6 during warm acclimation. The 18:2n-6, appeared to be an important fatty acid in CL compared to other phospholipids, and accounted for more than 20 mol% of total FA of CL in warm acclimated trout. In contrast, 22:6n-3, which was the most abundant fatty acid in CL, stayed constant during time course of warm acclimation. For LysoPC, the same PUFA varied as in diacylPC, diacylPE and PlsmPE, but the changes were more dramatic. Marked decreases in 22:6n-3 (from 53.4% to 32.4%) and in 20:5n-3 in warm acclimated trout (P<0.05) were accompanied by virtual doubling of 18:1n-9 and 16:0 (P<0.05). Few modifications in FA composition were noted for PI and PS (data not shown).
| Discussion |
|---|
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|---|
Mitochondrial properties
Role of membrane proteins
Warm acclimation led to the expected shifts in mitochondrial oxidative
capacities. Transfer of trout from 5°C to 15°C led to a slight
increase in mitochondrial maximal oxidative capacity measured at 15°C in
short-term warm exposed trout followed by a marked drop after warm acclimation
at both assay temperatures The increase in capacity in short-term warm exposed
trout was most pronounced for State 3 respiration rates expressed relative to
cytochrome a and c1 levels. Non-phosphorylating
(State 4) rates of oxygen uptake increased with transfer from 5°C to
15°C before returning to initial levels after long-term thermal
acclimation. These functional characteristics of muscle mitochondria and their
modification during warm acclimation confirmed the biphasic responses
previously found for State 3 and 4 rates
(Bouchard and Guderley, 2003
).
Maximal rates of oxygen uptake accounted for approximately 4% of the maximal
capacity of CCO, as observed for Arctic char and rainbow trout muscle
mitochondria (Blier and Lemieux,
2001
; Bouchard and Guderley,
2003
). The thermal sensitivity of the ADP affinity was
dramatically modified during short-term warm exposure, when the ADP/O ratio
increased, but warm acclimation returned these values to those observed in
cold acclimated trout. In addition, an increase in ADP affinity was observed
after warm acclimation. A loss of apparent ADP affinity with a decrease in
temperature characterises rainbow trout mitochondria over much of their annual
cycle (Blier and Guderley,
1993
; Guderley and St Pierre,
1999
), but thermal independence of the apparent ADP
Km (as for the short-term warm acclimated trout) occurs at
both the coldest and the warmest periods of the year
(Guderley and St Pierre,
1999
). As the changes in mitochondrial functional properties we
observed were similar to those previously determined, causal mechanisms
uncovered are also likely to apply broadly.
Trout oxidative muscle mitochondria had similar cytochrome and ANT
concentrations and relative levels as muscle mitochondria from carp, cane
toads, chickens, guinea pig and rats
(Williams, 1968
;
Wodtke, 1981a
;
Guderley et al., 2005
). The
increase of ANT during short-term warm exposure resembles the changes observed
previously in trout muscle mitochondria
(Bouchard and Guderley, 2003
).
Changes in the relative levels or concentrations of electron transport chain
complexes could modify the catalytic capacity of the mitochondria
(Sidell, 1983
). Differences in
cytochrome ratios and ANT in muscle mitochondria from rats, cane toads and
bearded dragon lizards may contribute to interspecific variability in
oxidative capacities (Guderley et al.,
2005
). However, the relative levels of cytochromes and ANT were
quite constant during warm acclimation of trout, although warm acclimation of
trout decreased the levels of cytochromes b and c.
Cytochrome b is situated in Complexes II and III. If the portion
associated with Complex III became less abundant, it could reduce the capacity
for pyruvate oxidation. As cytochrome c is a substrate for Complexes
III and IV, reductions in its availability could decrease mitochondrial
oxidative capacity (Lesnefsky et al.,
2001
). On the other hand, the constant levels of cytochrome
a, a component of Complex IV (CCO), suggest that the concentrations
of Complex IV were maintained in warm acclimated trout. Carp acclimated to
30°C also maintain constant levels of cytochrome a in muscle
mitochondria and decrease levels of c+c1
(Wodtke, 1981a
). Since warm
acclimation caused parallel decreases in mitochondrial oxidative capacity and
CCO activity, and since cytochrome a levels did not change, we
conclude that the decreases in oxidative capacity were not caused by a change
in the concentration of CCO.
Role of membrane lipid composition
Cholesterol. Our study evaluated potential means by which
mitochondrial membrane lipid composition sets mitochondrial oxidative
capacities during thermal change. To ensure proper functioning of
biomembranes, the physical and chemical environment of the membrane must be
regulated to maintain activity of membrane-associated proteins. Among membrane
components, changes in cholesterol are suggested to play such a role during
thermal acclimation (Crockett and Hazel,
1995
).
The basic stoichiometry of mitochondrial membranes from trout red muscle,
in particular the phospholipid to protein ratio, was in close agreement with
data from carp red muscle (Wodtke,
1981b
), and similar to the values obtained for mitochondria from
pig heart and rat liver (Comte et al.,
1976
; Hovius et al.,
1990
). The ratio of cholesterol to protein was in the range of
published values. Thermal acclimation led to substantial changes in overall
mitochondrial lipid composition, but left the ratio of cholesterol to protein
unchanged. Specifically, the ratio of total phospholipids to protein was
significantly decreased in mitochondrial membranes from warm acclimated trout.
As suggested (Wodtke, 1981b
),
these modifications were most likely due to a lower proportion of inner
membranes in mitochondria of warm acclimated trout. Indeed, although less
frequently observed during thermal acclimation than changes in mitochondrial
volume density, an increased mitochondrial cristae density occurs during
winter acclimatisation in oxidative muscle of rainbow trout
(St Pierre et al., 1998
).
Since cholesterol seems to be mainly associated with the outer mitochondrial
membrane (Daum, 1985
;
Echegoyen et al., 1993
),
specific modifications of the proportion of cholesterol in the outer
mitochondrial membrane with warm acclimation seem unlikely.
Phospholipid classes and subclasses restructuring. Phospholipids
that constitute mitochondrial membranes should be regarded as structural
partners of membrane proteins and as potential modulators of mitochondrial
processes (Daum, 1985
). Among
mechanisms of membrane remodeling during thermal acclimation, alterations in
phospholipid headgroup composition are a common response of poikiloterms
(Hazel and Carpenter, 1985
;
Hazel, 1988
;
Hazel and Landrey, 1988a
). In
trout muscle mitochondria, the proportion of PE and PC, in particular the
diacyl forms, responded the most to thermal change. These two phospholipid
subclasses represented more than 78 mol% of total phospholipids. These rapid
changes after short-term temperature change have been described in various
cell membranes and have led to the concept that phospholipid headgroup
alterations are central for regulation of physical and functional properties
of cell membranes during the initial stages of thermal change
(Hazel and Carpenter, 1985
;
Hazel, 1995
). As reported
(Hazel and Landrey, 1988a
) and
reviewed (Lee, 1991
), these
alterations in membrane lipid composition during warm acclimation are not
consistent with HVA because a reduction in the numbers of PE should decrease,
not increase, membrane order. The increase in lysoPC in warm acclimated trout
also would not favour homeoviscous adaptation, as lysoPC increases membrane
permeability when incorporated into PC bilayers
(Kumar et al., 1988
). On the
other hand, as PE has a smaller headgroup than PC, decreased proportions of PE
are believed to offset direct effects of high temperature on phospholipid
volume and maintain an appropriate balance between bilayer-stabilising
(lamellar phase forming, like PC) and -destabilising (hexagonal phase forming,
like PE) lipids. Several lines of evidence suggest the PC/PE ratio is a
primary determinant of membrane function
(Hazel, 1995
). The rapid
adjustments of PE and PC found in mitochondrial membranes suggest that
maintaining membrane status, even temporarily, within the time course of warm
acclimation is critical.
Our study demonstrated the novel finding that diacyl and plasmalogen
subclasses of PE and PC do not vary in parallel. Indeed, the proportion of
plasmalogens of both phosphatides rose only in warm acclimated trout while the
diacyl forms of PE and PC changed with short-term warm exposure, with diacylPC
increasing and diacylPE decreasing. Since temperature-induced changes in PE
and PC were different for plasmalogen and diacyl forms, care should be taken
when considering the `PC/PE ratio' in membranes. From the present study,
differences are evident since diacylPC/diacylPE ratios increased during warm
acclimation (from 1.4 in cold acclimated trout to 1.8 for short-term warm
exposed trout and 2.0 in warm acclimated) while diacylPC+PlsmPC/diacylPE+
PlsmPE ratios increased after short-term warm exposure and decreased slightly
with warm acclimation (1.2, 1.5 and 1.4, respectively, in cold acclimated,
short-term warm exposed and warm acclimated trout). Few data exist concerning
modifications of plasmalogen levels in biological membranes during thermal
acclimation. However, the increase in total plasmalogen in warm acclimated
trout is consistent with data from carp red muscle mitochondria
(Wodtke, 1981b
), goldfish
brain (Roots and Johnston,
1968
; Chang and Roots,
1985
) and marine invertebrates
(Dembitsky, 1979
). To the best
of our knowledge, ours are the first data on the time course of modifications
in plasmalogen levels during thermal acclimation. The functional significance
of these changes in membrane plasmalogens is unclear. Plasmalogens are
glycerophospholipids characterised by an alk-l'-enylether bond in
position sn-1 instead of an acyl bond in diacyl homologue. It has
been suggested that the lack of the carbonyl oxygen in position sn-1
affects the hydrophilicity of the headgroup and allows stronger intermolecular
hydrogen-bonding between headgroups. These properties would favour the
formation of the non-lamellar structures, reflecting the propensity of
ethanolamine plasmalogen to adopt the inverse hexagonal phase
(Lohner, 1996
). Plasmalogens
were also reported to reduce transmembrane solute fluxes at high growth
temperatures (Hazel and Williams,
1990
). This could help minimise proton leak across mitochondrial
membranes at elevated temperature. In vitro, the higher
susceptibility of the vinyl-ether bond to oxidative attack led to the
hypothesis that plasmalogens may act as anti-oxidants, protecting cells from
oxidative stress (Brosche and Platt,
1998
; Maeba and Ueta,
2003
; Brites et al.,
2004
). Generation of free radical species of oxygen during
mitochondrial electron transport chain can damage mitochondrial membranes and
hinder function by generating lipid peroxides from unsaturated FA
(Chang and Roots, 1985
;
Genova et al., 2004
). For
example, peroxidation of mitochondrial CL in aged rats is followed by losses
of peroxidised CL and parallel decreases in CCO activity
(Paradies et al., 1997
).
Warming exacerbates the formation of reactive oxygen species (ROS) in marine
invertebrates (Keller et al.,
2004
). Beside other mechanisms (i.e. higher activities of
antioxidant enzymes), increases in PlsmPE in trout mitochondria during warm
acclimation may compensate for thermally enhanced rates of lipid peroxidation
reactions at warm temperatures. Interestingly, changes in the proportion of PE
(no distinctions being made between plasmalogens and the corresponding diacyl)
during thermal acclimation are largely restricted to the inner membrane of
rainbow trout liver mitochondria (Miranda
and Hazel, 1996
). Such an asymmetrical distribution of PlsmPE in
the inner membrane of mitochondria would facilitate that interaction with free
radical species.
FA restructuring
Modification of phospholipid FA composition is the most commonly observed
cellular response to thermal change. Ectotherms are thought to adapt their
temperature-sensitive membranes by increasing lipid unsaturation in response
to low temperature (Hazel and Williams,
1990
). This cellular response has been extensively related to
compensation of membrane function and modification of activities of
membrane-bound enzymes (Van Der Thillart
and Modderkolk, 1978
; Wodtke,
1981a
; Wodtke,
1981b
; Itoi et al.,
2003a
; Guderley,
2004
). In the present study, the levels of the cytochromes or ANT
could not explain the decrease in mitochondrial capacity or CCO activity
during warm acclimation. These functional modifications could result from HVA
acting through changes in the mitochondrial membrane FA composition. However,
only modest variations in the UI or in the ratio of unsaturated to saturated
FA in the total phospholipids occurred during warm acclimation. This suggests
that the remarkable modulations in mitochondrial oxidative capacities, CCO
activity and ADP affinity occur through mechanisms that may not significantly
alter fluidity. This agrees with a compelling body of evidence indicating that
many aspects of membrane organisation can influence function more than simple
changes in lipid order (for reviews, see
Lee, 1991
;
Hazel, 1995
).
At the level of individual FA, inverse variations of the main unsaturated
FA in the mitochondrial membranes occurred. In particular, the PUFA, 20:5n-3
and 22:6n-3, decreased during warm acclimation while 18:1n-9 and 18:2n-6
increased. These modifications are not dramatic but agree with the shift of
mitochondrial FA composition of total phospholipids from rainbow trout red
muscle with seasonal acclimatisation
(Guderley et al., 1997
) and
with the increase of 18:2n-6 and decrease of 22:6n-3 and 20:5n-3 in total
lipids from red muscle mitochondria of warm acclimated carp
(Wodtke, 1981b
) and warm
acclimated goldfish (Van Der Thillart and
Modderkolk, 1978
). They are also consistent with reports for sea
bass liver and heart mitochondria (Trigari
et al., 1992
). Because cis double bonds introduce a kink
into the acyl chain, unsaturated FA pack less compactly and thus offset, to a
significant degree, the increase in membrane lipid order caused by a drop in
temperature. However, considerations of modulation of lipid order cannot
explain why trout and other winter-active poikilotherms accumulate PUFA rather
than monoenes in their membrane lipids at low temperature
(Hazel and Williams, 1990
),
since monoenoic FA are superior to PUFA with respect to the magnitude
(expressed on a per double bond basis) of the changes in fluidity they produce
and the lower metabolic cost of their production
(Stubbs and Smith, 1984
;
Rabinovich and Ripatti, 1991
;
Williams and Hazel, 1993
). As
suggested (Lee, 1991
;
Hazel, 1995
), modification of
overall membrane unsaturation may not be the primary aim of restructuring of
membrane FA during thermal adaptation.
Only a small number of lipid molecules are thought to separate membrane
proteins or protein aggregates, particularly in the protein dense
mitochondrial membranes (Hazel and
Williams, 1990
). The lipid-protein associations required for
appropriate protein conformations may demand specificity of acyl chain length
and unsaturation more than an appropriate overall fluidity. Thus,
modifications in specific phospholipid classes or subclasses may account for
the modifications of mitochondrial activity, CCO activity and ADP affinity.
Warm acclimation did not lead to the same FA changes in all phospholipid
classes. Indeed, while warm acclimation led to mitigated FA changes of total
phospholipids, changes largely reflecting the FA composition of diacylPE and
diacylPC, which together represented
80% of the phospholipids, warm
acclimation caused marked alterations in LysoPC and CL, two minor phospholipid
classes. In addition, while warm acclimation led to similar FA modifications
for diacylPC, diacylPE, PlsmPC and PlsmPE, LysoPC and CL presented distinct FA
alterations. In LysoPC, 16:0 rose with warm acclimation, while it decreased in
PE and PC. In CL, both 18:1n-7 and 18:1n-9 decreased with warm acclimation
(the former more than the latter), whereas they changed little or increased in
PE and PC. Few analyses of FA composition of phospholipid classes are
available for fish mitochondria, and even fewer consider minor classes. To the
best of our knowledge, this study represents the first comprehensive report on
changes of the FA composition of natural lysoPC with thermal acclimation.
Although the function of lysoPC during thermal acclimation remains unclear,
many functions in biological membranes have been attributed to it
(Watanabe et al., 2006
).
LysoPC may regulate mediated membrane processes in highly curved bilayer
domains (Kumar et al., 1988
).
The shorter lysoPC FA moities in warm acclimated trout may also constrain
membrane curvature (Rigoni et al.,
2005
).
The remarkable specificity of FA modifications in CL with thermal
acclimation is suggestive of interactions with membrane proteins. CL only
occurs in mitochondria and plays an important role in the micro-environment of
mitochondrial enzymes involved in oxidative phosphorylation, including
cytochrome c oxidase, cytochrome bc1 complex,
ATPase, ANT and NADH reductase (Paradies
et al., 2002
; Schlame et al.,
2000
). The influence of cardiolipin on the micro-environment of
mitochondrial complexes requires certain types of fatty acids
(Schlame et al., 2005
) and, in
mammals, alteration of CL acyl composition modulates the activity of these
membrane complexes (Yamaoka et al.,
1988
; Berger et al.,
1993
; Watkins et al.,
1998
). Warm acclimation of rainbow trout led to similar changes in
the acyl composition of CL of muscle mitochondria as in carp even if the acyl
chain composition differs between these species
(Wodtke, 1981b
). As in our
study, changes in CCO activity during thermal adaptation of carp accompanied
FA modifications of this annular phospholipid
(Wodtke, 1981a
). We therefore
propose that the specific reduction of CCO activity in warm acclimation is
due, at least in part, to an increase in 18:2n-6 in CL, concomitant with a
decrease in 18:1n-7 and 16:0.
Parallels between membrane lipid composition and mitochondrial capacities
During thermal acclimation, phospholipids from trout muscle changed their
proportions and FA composition following a time course similar to that shown
for plasma membranes from trout kidney
(Hazel and Landrey, 1988a
;
Hazel and Landrey, 1988b
).
Remodelling of phospholipid headgroups (diacyl forms) was the earliest
detectable response, while FA compositions primarily changed with prolonged
acclimation. Logically, the functional properties that changed during
short-term warm exposure probably reflected the proportions of phospholipid
classes, whereas those changing with warm acclimation likely followed both
changes in phospholipid proportions and FA composition. Short-term warm
exposure enhanced State 3 and 4 rates and changed the thermal sensitivity of
the apparent ADP affinity. The adjustment of the diacylPE/diacylPC ratio
during short-term warm exposure should modify the tendency of the bilayer to
form reversed hexagonal phases, thus modifying the activity of membrane
proteins. ANT activity in rats is strongly correlated with the membrane
content of hexagonal phase-forming lipids (PE/PC)
(Mak et al., 1983
). Replacing
PC with PE increases ADP/ATP exchange in liposomes
(Krämer and Klingerberg,
1980
). As ANT may help set mitochondrial affinity for ADP, the
inverted thermal sensitivity of the ADP affinity after short-term warm
exposure is consistent with such effects. The changes in acyl chain
composition of specific phospholipids during warm acclimation coincided with
the marked reduction of oxidative capacity and CCO activity. This reduction in
capacity and CCO activity is unlikely to be due to removal of cardiolipin from
the mitochondrial inner membrane (Stuart
et al., 1998
; Paradies et al.,
2000
; Schlame et al.,
2000
). Rather, the striking parallel between the modifications of
FA composition of CL and oxidative capacities/CCO activities
(Fig. 5) suggest that
regulation by membrane lipids occurs, at least in part, via the acyl
chain composition of CL. As ANT activity also depends on interactions with CL
(Paradies et al., 1994
;
Schlame et al., 2000
), the
increased ADP affinity after warm acclimation may reflect the changed FA
composition of CL.
|
| Acknowledgments |
|---|
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|---|
|
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