Metabolic plasticity and critical temperatures for aerobic scope in a eurythermal marine invertebrate (Littorina saxatilis, Gastropoda: Littorinidae) from different latitudes
Inna M. Sokolova* and
Hans-Otto Pörtner
Lab. Ecophysiology and Ecotoxicology, Alfred-Wegener-Institute for
Polar and Marine Research, Columbusstr., 27568 Bremerhaven, Germany

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Fig. 1. Temperature dependence of the respiration rates in (A) North Sea and (B)
White Sea Littorina saxatilis acclimated to 13°C and 4°C.
High critical temperatures (Tc IIc and
Tc IIw in cold- and warm-acclimated animals,
respectively) are indicated by arrows. These are the temperatures where an
onset of anaerobiosis occurred as determined by significant succinate
accumulation compared with the respective control level (see
Fig. 3). N=6-16 for
each data point.
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Fig. 2. Activation energy of aerobic respiration in North Sea and White Sea
Littorina saxatilis acclimated to 13° and 4°C. Arrhenius
breakpoint temperatures (ABTs) are given above the respective columns.
Activation energy (Ea) values below and above the
respective ABTs were determined in the temperature range 0-28°C.
Ea values beyond ABT were significantly lower than
Ea values above the ABT in all experimental groups
(P<0.05). On the x-axis, the population of origin (North
Sea vs White Sea) and acclimation temperatures (4°C vs
13°C) are indicated.
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Fig. 3. Changes in (A,B) succinate and (C,D) malate levels in foot muscle tissue of
Littorina saxatilis during temperature incubations. High critical
temperatures (Tc IIc and Tc
IIw in cold- and warm-acclimated animals, respectively) are
indicated by arrows. These are the temperatures where an onset of anaerobiosis
occurred as determined by significant succinate accumulation compared with the
respective control level. Open symbols denote values that are significantly
different from the respective controls (P<0.05). N=5-10
for each data point.
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Fig. 4. Changes in (A,B) phospho-L-arginine (PLA) and (C,D) L-arginine (L-Arg)
levels in foot muscle tissue of Littorina saxatilis during
temperature incubations. High critical temperatures (Tc
IIc and Tc IIw in cold- and
warm-acclimated animals, respectively) are indicated by arrows. These are the
temperatures where an onset of anaerobiosis occurred as determined by
significant succinate accumulation compared with the respective control level.
Open symbols denote values that are significantly different from the
respective controls (P<0.05). N=5-10 for each data
point.
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Fig. 5. Changes in the (A,B) phosphagen/aphosphagen ratio
(RPLA) and (C,D) ATP levels in foot muscle tissue of
Littorina saxatilis during temperature incubations. High critical
temperatures (Tc IIc and Tc
IIw in cold- and warm-acclimated animals, respectively) are
indicated by arrows. These are the temperatures where an onset of anaerobiosis
occurred as determined by significant succinate accumulation compared with the
respective control level. Open symbols denote values that are significantly
different from the respective controls (P<0.05). N=5-10
for each data point.
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Fig. 6. Aerobic and anaerobic ATP turnover rates
( ATP) at 32°C in North
Sea and White Sea Littorina saxatilis acclimated at 13°C and
4°C. The rate of ATP turnover during anaerobiosis (amount of ATP consumed
per g wet mass per hour) was calculated from end product accumulation and ATP
and phospho-L-arginine (PLA) depletion as described in the text, assuming an
ATP equivalent of 2.75 µmol per µmol of succinate. The aerobic ATP
turnover rate was calculated from routine oxygen consumption rates, assuming
that 6 mol ATP produced 1 mol O2.
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Fig. 7. Relative contribution of succinate accumulation and depletion of
high-energy phosphates to anaerobic ATP turnover in Littorina
saxatilis at 32°C in water. Upper row, White Sea snails; lower row,
North Sea snails.
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© The Company of Biologists Ltd 2003