INTRODUCTION
The northern quahog, Mercenaria mercenaria (Linnaeus, 1758), occurs over a wide geographical range in North America, from the Bay of Chaleurs, Gulf of St Lawrence, south to the Florida Keys (Harte, Reference Harte, Kraeuter and Castagna2001), surviving temperatures between 0 and 30°C (McHugh, Reference McHugh1984). Following introduction to England during the late 19th and early 20th Centuries a naturalized breeding population of M. mercenaria became established in Southampton Water (Harte, Reference Harte, Kraeuter and Castagna2001). The population increased from the 1950s, possibly occupying the vacant niche left by the elimination of Mya arenaria by cold winters in 1947 and 1962/1963 (Mitchell, Reference Mitchell1974). The elevation of estuarine temperatures by industrial and power station cooling water discharges and physiological adaptation to spawning at lower temperatures than populations in areas of origin (Mitchell, Reference Mitchell1974), resulted in an increasing population that supported a fishery from the 1960s (Eno et al., Reference Eno, Clark and Sanderson1997).
Recently this fishery has become severely depleted (Eno et al., Reference Eno, Clark and Sanderson1997). Differences between the age–frequency distribution observed in the Southampton Water population and those in other study areas indicate that Southampton Water is a marginal habitat for the species (Fegley, Reference Fegley, Kraeuter and Castagna2001). Poor recruitment observed (Richardson & Walker, Reference Richardson and Walker1991) may result from large numbers of animals removed by the fishery and damage to the physical environment (Eno et al., Reference Eno, Clark and Sanderson1997), and/or from adverse environmental conditions, e.g. temperature effects (Loosanoff et al., Reference Loosanoff, Miller and Smith1951; Loosanoff, Reference Loosanoff1959). The status of introduced populations in The Netherlands, Belgium and on the west coast of France is unknown (Fegley, Reference Fegley, Kraeuter and Castagna2001). Data on the physiological ecology of M. mercenaria, including metabolic rate and growth across the original North American biogeographical range, have been reviewed by Grizzle et al. (Reference Grizzle, Bricelj, Shumway, Kraeuter and Castagna2001). Although ontogenetic growth models have been established across a wide latitudinal range in North America, indicating a latitudinal gradient of decreasing growth rate from south to north, no model has been constructed for the naturalized Southampton Water population. Additionally, allometric relationships have been established for M. mercenaria indicating increasing oxygen consumption rate with increasing body mass (Loveland & Chu, Reference Loveland and Chu1969), and with increasing temperature (Hibbert, Reference Hibbert1977). Examination of growth and metabolic rates for the Southampton Water population at the edge of the biogeographical limits may elucidate evidence of the impact of adverse environmental conditions on M. mercenaria.
In this study functions for age-specific metabolic rate, growth and derived somatic production and respiration were calculated and compared with other findings from the literature to assess the contribution of physiological impairment to the observed biogeographical limit of M. mercenaria in the UK to Southampton Water.
MATERIALS AND METHODS
Sampling and maintenance
Mercenaria mercenaria were collected by local fishermen from onboard a small vessel, from the western shore of Southampton Water (50°51.7′N 001°22.7′W), with a small benthic dredge. After sampling, animals were immediately transported to the National Oceanography Centre, Southampton, where they were maintained in a recirculating aquarium at ambient salinities (31 – 35), temperature following seasonal changes (minimum 12; maximum 20°C), and a 12:12-hour dark/light cycle. They were fed a mixed diet of Phaeodactylum tricornutum, Isochrysis galbana, Pavlova lutheri, Chaetoceros ceratosporum and Tetraselmis suecica microalgal cultures ad libitum three times each week, until used in experiments.
Metabolic rate
Oxygen consumption rates of unfed (deprived of food for at least 3 days), unstressed and inactive animals were used as a proxy for standard metabolic rate as described by Bayne & Newell (Reference Bayne, Newell, Saleuddin and Wilbur1983). Measurements were taken at aquarium ambient temperature (19.5±0.9°C). The largest size-range of animals available was used for sampling.
Oxygen content of water was assessed using oxygen microoptodes connected to a Microx TX3 array (PreSens, Germany) and a flow-through system, modified from the intermittent flow system described by Heilmayer & Brey (Reference Heilmayer and Brey2003). Oxygen microoptodes were used to record oxygen content of water flowing into and out of the respiration chambers at 30 second intervals. Individual metabolic rates (VO2) were obtained by comparison with control chambers (no animals) (for details Heilmayer & Brey, Reference Heilmayer and Brey2003).
For size–mass relationships the shell height (H), the greatest distance from the umbo to the dorsal margin (Fritz, Reference Fritz, Kraeuter and Castagna2001), of each animal was measured to the nearest 0.1 mm using vernier callipers before animals were dissected, and soft tissue wet mass was weighed to the nearest mg. Soft tissue dry mass (DM) was calculated (using 1 mg soft tissue wet mass = 0.176 mg soft tissue dry mass (Brey, Reference Brey2001)) and linear regression analysis was carried out on log-transformed data estimating constant a and height scaling exponent b of the size–mass allometric equation:
The VO2 was expressed as a function of DM with a model fitted by linear regression analysis after logarithmic transformation of both variables:
where c is constant and d is the mass scaling exponent.
Age and growth
Shell growth bands in bivalves result from seasonal oscillations in growth, but also from changes in food availability, spawning events or predation attempts. Identification and interpretation of annual growth bands in M. mercenaria were based on that described by Fritz (Reference Fritz, Kraeuter and Castagna2001). Winter growth cessations were indicated by thick microgrowth increment boundaries in the outer shell layer microstructure associated with a V shaped notch in the outer layer, and with dark bands in the middle shell layer microstructure (see figure 2.12 in Fritz, Reference Fritz, Kraeuter and Castagna2001).
Valve preparation followed a method modified from that described by Schöne et al. (Reference Schöne, Fiebig, Pfeiffer, Gleβ, Hickson, Johnson, Dreyer and Oschmann2005). Prior to analysis the shell was cleaned of organic matter with warm 5% NaOCl solution, rinsed with water and dried. A quick-drying metal epoxy resin (J-B KWIK) was applied to the axis of shell height, and allowed to dry overnight before cutting perpendicular to the annual growth lines with a FKS/E table saw (PROXXON MICROMOT), using a 0.7 mm thick diamond coated cutting disc. The section edge of the left valve was ground and polished using an Alpha dual speed grinder–polisher (Buehler) with 180, 400, 1000, 2400 and 4000 SiC grit, before the number of microscopically visible annual growth bands and correlating shell height were analysed using an SZX12 stereo microscope system with U-CMAD3 camera adapter and Color View I digital colour camera (Olympus), and analySIS 5.0 image-processing software (Olympus).
Valve preparation and growth band identification and analysis were conducted in the Sclerochronology Laboratory at the Alfred Wegener Institute (AWI, Germany). A von Bertalanffy growth function was fitted to the resulting size-at-age data pairs using a non-linear iterative Newton algorithm (Brey, Reference Brey2001):
where H∞ is the mean asymptotic shell height in mm, K is the Brody growth coefficient, t the age in years and t0 the theoretical age in years at which shell height equals zero.
Somatic production and respiration
Individual age-specific somatic production (Ps) was calculated from the increment between consecutive age-classes in soft tissue dry mass, derived using the size–mass allometric relationship and von Bertalanffy growth function, and the conversion factor (C) 1 mg dry mass = 18.393 J (Brey, Reference Brey2001):
Individual age-specific respiration rate (R) was calculated from the average soft tissue dry mass over consecutive age-classes using the metabolic rate equation:
derived from the size–mass allometric relationship, von Bertalanffy growth function, and using the constant x and mass scaling exponent y from the equation for mass-specific respiration rate:
calculated by linear regression analysis, where VO2 is in J y−1 and DM is in J with oxygen consumed converted to energy using 1 ml O2 = 20.1 J (Brey, Reference Brey2001).
RESULTS
Metabolic rate
The range in shell height and soft tissue dry mass of the 18 animals used were from 14.7 to 92.2 mm and from 14 to 8692 mg, respectively. The allometric relationship of soft tissue dry mass in mg and shell height in mm in Mercenaria mercenaria can be described by the linear model:
The effect of soft tissue dry mass in mg on individual metabolic rate in ml O2 h−1 can be described by the linear model (Figure 1):
The DM range of organisms used corresponded to a VO2 range from 0.06 to 2.62 ml O2 h−1.
Age and growth
A total of 227 size-at-age data pairs of 18 specimens were fitted best by the von Bertalanffy equation:
The range of shell height of animals used was from 14.7 to 92.2 mm. The age range of animals used was from two to 30 years old.
Somatic production and respiration
Individual age-specific somatic production can be described by the equation:
and demonstrated increase to a maximum 3.88 kJ y−1 at an age of ten years, decreasing thereafter (Figure 3).
Mass-specific respiration rate can be described by the equation:
and mean mass-specific respiration rate over the DM range was 5.65 J y−1 J−1.
Individual age-specific respiration can therefore be described by the equation:
and demonstrated asymptotic increase to 231.37 kJ y−1 at an age of 30 years (Figure 3).
DISCUSSION
The broad geographical range over which Mercenaria mercenaria occurs naturally in North America, and the broad 0 to 30°C temperature range which this corresponds to, indicate that this species is strongly eurythermal sensu Pörtner et al. (Reference Pörtner, Storch and Heilmayer2005). Reported growth functions from across the species' biogeographical range demonstrate a latitudinal gradient of decreasing growth rate from south to north (Figure 4A), suggesting that temperature is the major cause of this variation. Mean annual growth of M. mercenaria has been shown to be highly correlated (r = 0.88) to mean annual water temperature (Jones et al., Reference Jones, Arthur and Allard1989), and previous analysis has evaluated optimum temperature for shell growth as approximately 20°C, with shell growth ceasing below 9°C or above 31°C (Ansell, Reference Ansell1968). The strong resemblance of the growth function derived in this study to those across the biogeographical range indicates that growth in M. mercenaria in Southampton Water is not physiologically impaired. Composite indices of overall growth performance (e.g. log (K)+log (H∞)) can be used to indirectly compare these non-linear growth patterns (Heilmayer et al., Reference Heilmayer, Brey, Storch, Mackensen and Arntz2004), and support this conclusion (Figure 4B). The maximum longevity of 30 years observed within the population studied here, falls in the range reported for representative sites for North American populations, e.g. 28 years in Florida (Jones et al., Reference Jones, Quitmeyer, Arnold and Marelli1990) and 46 years in North Carolina (Peterson, Reference Peterson1986). Additionally, the metabolic rate observed falls within the range described by existing models (Figure 5). The absence of physiological impairment of M. mercenaria necessitates a consideration of the ecological factors that may influence the biogeographical limitation of the species in the UK to Southampton Water.
Age–frequency data reported for Southampton Water by Richardson & Walker (Reference Richardson and Walker1991) suggest that environmental constraints on larval development may contribute to the limitation of the species' range. Spawning across the North American distribution of M. mercenaria focuses around peak water temperatures, and durations decrease with increasing latitude shifting from semi-annual to annual gametogenic cycles (Eversole, Reference Eversole, Kraeuter and Castagna2001). Annual spawning in the Southampton Water population has been reported at 18°C (Mitchell, Reference Mitchell1974), and appears unusually low when compared with spawning temperature amongst natural North American populations. Larval growth rates are significantly affected by temperature with individuals successfully reared from egg to metamorphosis between 18 and 30°C (Loosanoff et al., Reference Loosanoff, Miller and Smith1951) reaching metamorphosis after 16–24 days and 5–7 days, respectively (Loosanoff, Reference Loosanoff1959). Outside this temperature range rates of normal development were low (Loosanoff et al., Reference Loosanoff, Miller and Smith1951). Larval development indicates that higher temperatures are more favourable. Southampton Water experiences considerable interannual variability in monthly mean water temperature, rarely exceeding 18°C for three months, and seldom exceeding 20°C (Richardson & Walker, Reference Richardson and Walker1991). Peaks in temperature outside the estuary are lower and it therefore appears likely that the effect of temperature on larval development will contribute significantly to the observed limitation of M. mercenaria to Southampton Water.
Growth and metabolic data presented here yield no indication of physiological impairment of Mercenaria mercenaria from the study area. The explanation for the biogeographical limitation of this species in the United Kingdom must therefore lie elsewhere. Further detailed analysis of the ecological factors affecting this species throughout its life cycle is required to clearly establish this.
ACKNOWLEDGEMENTS
The collection of samples by local shellfish fishermen, and the aquarium-maintenance of Mercenaria mercenaria by Jenny Mallinson and Chris Hauton are gratefully acknowledged. We are also grateful for sclerochronological technical support provided by Kerstin Beyer (AWI, Germany). The present work was conducted within the frame of the Marine Biodiversity and Ecosystems Functioning Network of Excellence MarBEF (Contract no. GOCE-CT-2003-505446) of the 6th European Framework Programme (FP6).