Acquisition of Ca2+ and HCO3 −/CO3 2− for shell formation in embryos of the common pond snail Lymnaea stagnalis
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Embryos of the freshwater common pond snail Lymnaea stagnalis develop to hatch within 10 days under control conditions (22°C, Miami-Dade tap water) and this development is impaired by removal of ambient calcium. In contrast, embryos did not exhibit dependence upon an ambient HCO3 −/CO3 2− source, developing and hatching in HCO3 −/CO3 2−-free water at rates comparable to controls. Post-metamorphic, shell-laying embryos exhibited a significant saturation-type calcium uptake as a function of increasing ambient calcium concentration. However, changes in ambient bicarbonate concentration did not influence calcium or apparent titratable alkalinity uptake. There was a distinct shift from no significant flux in pre-metamorphic embryos to net uptake of calcium in post-metamorphic stages as indicated by an increased uptake from the micro-environment surrounding the egg mass and increased net uptake in 24-h, whole egg mass flux measurements. Furthermore, HCO3 −/CO3 2− acquisition as measured by titratable alkalinity flux is at least partially attributable to an endogenous carbonate source that is associated with acid extrusion. Thus, calcium requirements for embryonic shell formation are met via uptake but HCO3 −/CO3 2−, which is also necessary for shell formation is acquired in part from endogenous sources with no detectable correlation to ambient HCO3 −/CO3 2− availability.
KeywordsCalcium uptake kinetics Carbonate Development Freshwater Calcification Snail metamorphosis
In addition to carbohydrates and proteins (Bayne 1968; Plesch et al. 1971; Taylor 1973), snail egg masses have been found to contain maternal stores of shell-forming and other ions in concentrations exceeding that in surrounding waters (Taylor 1973). Using excised eggs with pre-gastrula embryos, Beadle (1969a) studied L. stagnalis and found mean calculated perivitelline fluid volume for L. stagnalis to be 0.70 mm3. In his study, the capsular membrane was found to be more permeable to water than ions. In a series of experiments using excised egg capsules that were exposed to either a large sugar (raffinose), solutes of large molecular weight polyethylene glycols (m.w. 500–600 or 3,000), or standard lake water; Beadle (1969a) found that molecules of approximately m.w. 600 could move across the capsular membrane in both directions. Furthermore, an intact gelatinous matrix and outer envelope retarded inward diffusion of raffinose but did not prevent it. Beadle (1969a) also determined that the undifferentiated pre-gastrula embryo could maintain itself in lake water for more than 24 h suggesting that it is capable of actively regulating its salt and water levels. This agrees with later findings by Taylor (1977) who reported that ion uptake and water excretion systems are developed in the earliest cleavage stages in L. stagnalis to cope with the problems of osmotic and ionic regulation. Compared to another pulmonate snail examined in the Beadle (1969a) study, Biomphalaria sudanica, the gelatinous matrix that surrounds the eggs is thicker in the egg mass of L. stagnalis and thus provides a greater buffer between the embryo and the ambient environment considering that the egg capsule provides no significant barrier to the diffusion of water and ions (Beadle 1969a).
In a related study, Beadle (1969b) focused on the Na+ requirements of developing B. sudanica and found that active Na+ uptake occurred during development, increasing embryonic Na+ content to seven times that of pre-blastula stage levels. Additionally, and pertinent to our study, he found that the embryos developed normally under reduced [Na+] of 1/7 normal levels (standard lake water: 0.56 meq l−1 Na+), but total ion reduction to 1/10 of normal resulted in the onset of water balance disruption. This suggests that B. sudanica can tolerate a wide range of [Na+] and possibly other cations with no effect on embryonic snail development when varied individually. Lastly, Taylor (1977) determined that the exchangeable Ca+ content of the embryos increases by five orders of magnitude (1.3 pmol to 130 nmol) over the period from the blastula stage through hatching, clearly demonstrating Ca2+ absorption from the egg mass and/or the water.
Considering the ion requirements for calcification, and the ability of L. stagnalis embryos to complete direct development in freshwater conditions in a relatively short period of time, we sought to determine whether our target species is provided with adequate quantities of shell-forming ions via maternal stores or actively extract the necessary inorganic ions from ambient waters. Thus, our objectives were to determine [Ca2+] in the perivitelline fluid and gelatinous matrix encasing the eggs over the course of development to determine whether there are significant fluctuations, particularly when comparing pre- and post-metamorphic stages of development. Additionally, we measured fluxes of shell-forming Ca2+ ions on the microscale and whole egg mass scale to determine whether egg masses of L. stagnalis acquire the necessary Ca2+ from environmental sources or are provided with them as maternal stores within the egg mass. Based on preliminary findings it became essential to also determine whether HCO3 −/CO3 2− sources were from exogenous sources or endogenously produced in egg masses containing post-metamorphic embryos as suggested in early respiratory studies on these embryos by Baldwin (1935) and as proposed and modeled by Greenaway (1971a) in adults of this species.
Materials and methods
Egg masses of the common pond snail L. stagnalis were collected in 24-h intervals from mass cultures with the day of collection considered day zero post-oviposition, for age determination. Embryos were incubated at room temperature (20–22°C) in aerated, dechlorinated Miami-Dade County tap water (Grosell et al. 2007). Prior to flux experiments, the egg masses were weighed (g), measured (mm), and viability was determined. Egg masses with less than 80% development were excluded from experiments and analyses.
Visual characterization of development
Nominal chemical concentrations for artificial waters
Miami-Dade tap water (μmol l−1)
Ca2+-free media (μmol l−1)
HCO3 −-free media (μmol l−1)
680 HCO3 −
110 SO4 2−
Voltage and Ca2+-selective microelectrodes
Microelectrodes, used for recordings of voltage across the tunica capsulis or the membrana interna and externa, were pulled from filamented 1.5 mm diameter borosilicate capillary glass (WPI, Sarasota, FL, USA). The microelectrodes were filled with 3 mol l−1 KCl and had tip resistances of approximately 30 MΩ. Ca2+-selective microelectrodes used to measure Ca2+ concentration in the tunica interna and perivitelline fluid were pulled from unfilamented 1.5 mm borosilicate capillary glass (A-M systems, Carlsborg, WA, USA), silanized by exposure to the vapors of dimethyldichlorosilane at 200°C and stored over silac gel until use. Microelectrodes were backfilled with 100 mmol l−1 CaCl2 and tip-filled with a 300–500 μm column of Ca2+ ionophore I, cocktail A (Fluka, Buchs, Switzerland). Microelectrodes were mounted on micromanipulators (Marzhauser MM33, Fine Science Tools, North Vancouver, BC, Canada) and observed through a dissecting microscope (Wild-Leitz, Heidelberg, Germany).
For measurement of Ca2+ concentration in the tunica interna of day 2 egg masses, it was necessary to cut two slits, each approximately 300 μm long, in the tunica capsulis using the tip of a 25 gauge syringe needle. This incision was necessary because the outer integument of the tunica capsulis was too rigid to pierce with the microelectrode without compromising the electrode. The outer integument became increasingly fluidic over the course of development, making the pre-incision necessary only for day 2 measurements. For older egg masses it was feasible to advance the microelectrodes directly across the tunica capsulis and into the tunica interna. A voltage electrode was then inserted through one slit and advanced 1–2 mm into the tunica interna and the Ca2+-selective microelectrode was inserted through the second slit. The voltage detected by the voltage microelectrode was subtracted from that detected by the Ca2+-selective microelectrode, yielding a signal proportional to Ca2+ concentration. Voltage and Ca2+-selective microelectrodes were connected through a high impedance (>1014 Ω) electrometer (pH/ion Amp, A-M systems, Carlsborg, WA, USA) to a PC-based data acquisitions and analysis system (PowerLab 4/25, AD Instruments, Colorado Springs, CO, USA) running CHART software (AD Instruments).
Time course of Ca2+, titratable alkalinity, and ammonia fluxes—whole egg masses
To evaluate whether the embryos were developing fully from maternal stores or were extracting necessary Ca2+ and HCO3 −/CO3 2− from the water over the course of development, eight egg masses were selected from mass cultures, scored, and placed in individual flux chambers that contained 20 ml of Miami-Dade tap water. Daily 10 ml initial stock and final water samples were collected for each egg mass. Daily net Ca2+ flux was determined using the difference in [Ca2+] between the initial and final waters following the 24-h flux as measured by flame atomic absorption spectrophotometry (Varian SpectrAA220, Mulgrave, Victoria, Australia), mass of egg mass (g), and elapsed time (h). Daily net titratable alkalinity flux was calculated from the change in titratable alkalinity from the initial and final flux media samples as determined via double-endpoint titration, mass of egg mass (g), and elapsed time (h). The double-endpoint titration, rather than a standard titration method, was used to determine titratable alkalinity because the double-endpoint titration method is insensitive to non-bicarbonate/carbonate buffering in the media. This technique has been suggested (Hills 1973) and since modified (Wilson et al. 1996) and used successfully for this type of titratable alkalinity determination (Wilson et al. 1996; Grosell et al. 1999). In experiments with low volume:biomass ratios the potential for release of organic material with buffer capacity exists which could lead to erroneous conclusions based on single-endpoint titrations. For the double-endpoint titration procedure, which avoids this problem, a 5 ml flux media sample with 5 ml of pH electrode-stabilization media (450 mmol l−1 NaCl) were gassed with N2 for 30 min after which starting pH was noted. Using a Gilmont micro-burette syringe filled with 0.02 N HCl, the sample was titrated down to pH 3.8 and 15 min was allowed for CO2 degassing. Sample pH was then returned to the original pH value using a second Gilmont micro-burette syringe filled with 0.02 N NaOH while continuously gassed. Using the difference in the amount of acid and base necessary to titrate to 3.800 and the start pH, HCO3 −/CO3 2− titratable alkalinity equivalents were determined. To evaluate whether the changes in titratable alkalinity were attributable to ammonia flux, we determined ammonia excretion rates over the course of development by calculating total ammonia concentration in initial and final water samples from the 24-h flux. Total ammonia was assessed using a modified colorimetric ammonia assay (Verdouw et al. 1978) in which ammonia was reacted with salicylate and hypochlorite to form a blue indophenol in a sodium nitroprusside-catalyzed reaction. The assay was measured on a micro-plate reader (Molecular Devices ThermoMax, Sunnyvale, CA, USA) at 640 nm. Final values for Ca2+ and titratable alkalinity net flux as well as total ammonia excretion were presented as μmol g−1 h−1.
Time course of Ca2+ fluxes-microscale measurements using the scanning ion electrode technique
Transport of Ca2+ into or out of egg masses produces gradients in [Ca2+] in the unstirred layer adjacent to the surface of the tissue. These gradients can be calculated from the voltages recorded by a Ca2+-selective microelectrode moved between two points within the unstirred layer. Calcium flux can then be calculated from the concentration gradients using Fick’s law, as described below. Measurement of fluxes in this way is the basis of the scanning ion electrode technique (SIET), which allows fluxes to be repeatedly measured in near real-time at sites along the length of an egg mass. Extensive descriptions of the use of SIET are reported in Rheault and O’Donnell (2001, 2004) and Donini and O’Donnell (2005).
SIET measurements were made using hardware from Applicable Electronics (Forestdale, MA, USA) and automated scanning electrode technique (ASET) software (version 2.0) from Science Wares Inc. (East Falmouth, MA, USA). Egg masses were placed in 35 mm diameter petri dishes filled with 5 ml of artificial Miami-Dade water. Reference electrodes were made from 10 cm lengths of 1.5 mm borosilicate glass capillaries that were bent at a 45° angle, 1–2 cm from the end, to facilitate placement in the sample dish. Capillaries were filled with boiling 3 mol l−1 KCl in 3% agar and connected to the ground input of the Applicable Electronics amplifier through an Ag/AgCl half cell.
Ca2+ and HCO3 −/CO3 2− kinetics
For Ca2+ uptake kinetics experiments, day 7 egg masses were incubated for 24 h in 20 ml of media with nominal ion concentrations approximating that of Miami-Dade tap water except for Ca2+, which was adjusted to nominal concentrations of 10, 20, 60, 90, 100, 200, 600, or 900 μmol l−1 Ca2+ using CaCl2 (Sigma–Aldrich). Egg masses were dip-rinsed in appropriate flux media prior to the start of the flux. For determination of fluxes, 10 ml of initial media stock and 10 ml of final media from flux chambers were collected for each treatment. Calcium and titratable alkalinity net flux were determined for each [Ca2+] as described above in the time course section and presented as μmol g−1 h−1.
For HCO3 − kinetics experiments, [Ca2+] was maintained at 310 μmol l−1 and [HCO3 −] was adjusted to either 200, 400, 800, or 1,200 μmol l−1 HCO3 − with choline bicarbonate (Sigma–Aldrich, [2-hydroxyethyl] trimethylammonium, C5H14NO·HCO3). Both Ca2+ net flux and titratable alkalinity net flux were determined for each [HCO3 −]. Ammonia fluxes were not included here due to the nearly undetectable concentrations measured during the time course experiments. Egg masses and flux procedures were handled in the same manner as described above for time course and Ca2+ kinetics experiments.
Fluxes in HCO3 −/CO3 2−-free HEPES-buffered media
Day 7 egg masses were scored and dip-rinsed then placed in individual chambers with 20 ml of flux media that contained either 680 μmol l−1 HCO3 −, which is comparable to Miami-Dade tap water, or HCO3 −/CO3 2−-free HEPES-buffered media (1.5 mmol l−1 each HEPES-free H+ and HEPES-Na+ salt; Sigma–Aldrich) with all other ions maintained at concentrations comparable to Miami-Dade tap water. This concentration of HEPES provided for adequate buffering under bicarbonate-free conditions while still allowing for measurements of changes in apparent titratable alkalinity (Grosell and Taylor 2007). Egg masses were incubated for 24 h. Then 15 ml of the initial and final media samples were taken and analyzed for [Ca2+], titratable alkalinity, and total ammonia. Net Ca2+ flux was determined as described above. Net titratable alkalinity flux was calculated from results of single-endpoint titrations on initial and final media samples as outlined in Grosell and Taylor (2007). In the absence of HCO3 −/CO3 2−, changes in apparent titratable alkalinity would be a result of H+ excretion and its effects (i.e. NH4 + trapping). Therefore, it was not necessary to complete double-endpoint titrations as in the HCO3 −/CO3 2−-buffered solutions. For the single-endpoint procedure, aliquots of 10 ml were collected and gassed continuously in 50 ml Falcon tubes with N2 for 30 min prior to and during the titration to insure the absence of CO2. pH was noted following the initial 30 min gassing and then the 10 ml sample was titrated using a Gilmont micro-burette syringe filled with 0.02 N HCl down to pH 7.0 noting the pH and amount of 0.02 N HCl added at the final pH and for no less than three points along the titration curve. Linearity was conserved down to pH 7.0 but was lost below that value thus [H+] values below pH 7.0 were not used in the H+ excretion calculation. Initial and final samples were titrated on the same pH electrode and with the same burette. All curves were fit by non-linear regression analysis and only those curves for which R 2 > 0.95 were included. The titratable alkalinity net flux (=acid excretion) was calculated using the difference between the H+ added to reach the known pH of 7.0 for both the initial and final flux media, the mass of the egg mass (g), and the elapsed flux time (h). Total ammonia excretion was determined as described above.
Uptake kinetic constants, apparent affinity (k m) and capacity (V max), were determined assuming Michaelis–Menten saturation kinetics and using the non-linear regression function in SigmaPlot for Windows version 11.00. Comparisons among experimental groups were completed using an ANOVA with pairwise comparisons where appropriate following the Holm–Sidak method after an evaluation for whether the data sets were normally distributed with the Shapiro–Wilk test. All values are mean ± SEM and statements of statistical difference were reserved for a P value < 0.05.
Endogenous Ca2+ sources
The visible onset of shell formation, an indicator of metamorphosis, at approximately day 5, was concurrent with significantly decreased [Ca2+] in the tunica interna of post-metamorphic egg masses to levels below pre-metamorphic concentrations. Also, perivitelline fluid from post-metamorphic (day 7 and 9) eggs had significantly lower [Ca2+] than eggs containing pre-metamorphic embryos (Fig. 4). Results from the aforementioned experiments indicated a need to consider the likelihood of important interactions between the egg mass and its contents with the surrounding environment, particularly in post-metamorphic stages.
Exogenous Ca2+ sources
Using Ca2+-selective and voltage microelectrodes for measurements of [Ca2+] and transmembrane voltage difference, respectively, we were able to quantify the net electrochemical potential (ΔμCa/F) across these barriers in peri- and post-metamorphic stages. Day 7 ΔμCa/F (−19.7 mV) and ΔV (−9.2 ± 0.60 mV) values were negative across the tunica capsulis membrane. After emergence of the embryos from the egg capsules on day 10, but prior to their emergence from the egg mass, mean ΔμCa/F became more negative (−51.0 mV) with no significant change in transmembrane voltage difference (−8.7 ± 1.11 mV, inside negative). For excised eggs, mean ΔμCa/F across the membrana interna and externa was more negative on day 9 (−26.4 mV) relative to peri-metamorphic values (day 5, −3.7 mV); however, the voltage difference across these membranes became less negative over the same time period (day 5: −21.4 ± 0.92 mV, day 9: −9.1 ± 0.77 mV).
Flux of acid–base equivalents
Developing embryos of L. stagnalis showed visible dependency on environmental Ca2+ sources after depletion of maternal stores in the form of reduced growth rates (Figs. 3, 4), but no apparent dependence on exogenous HCO3 −/CO3 2− sources (Fig. 2). We also observed a distinct difference in the structural integrity of the egg mass membrane (i.e., resistant to penetration during early development but more permeable in post-metamorphic stages) and significant differences in the Ca2+ content and ΔμCa/F over the course of development, but particularly during peri- and post-metamorphic stages. Thus, it was important to consider interactions between the contents of the egg mass and the surrounding environment that may facilitate the process of embryonic acquisition of shell-forming ions.
The saturation-type kinetics that we observed in the post-metamorphic embryos of L. stagnalis were remarkably similar to those reported by Greenaway (1971b) in adults of the species. Greenaway calculated a half-saturation point of 300 μmol Ca2+ l−1 and determined that the uptake pathway reached the maximum of 0.5 μmol g−1 h−1 at 1,000–1,500 μmol Ca2+ l−1. That maximum value was comparable to the maximum of 0.4 μmol g−1 h−1 at above 600 μmol Ca2+ that we found here. However, our half-saturation value (91 μmol Ca2+ l−1) was nearly 1/3 of his calculated value. This may be due to the difference in developmental stage (embryonic versus adult), difference in pre-experimental [Ca2+], or other parameters.
Over the course of development, we noted changes in the penetrability of the integument of the tunica capsulis, and fluctuations in [Ca2+] in the perivitelline fluid consistent with the presence and use of maternal stores during pre-metamorphic stages. The earliest studies on various vertebrate eggs including Raja, Triton, Bufo, and salmonid species in freshwater environments indicated changes in their permeability to water and ions during development from impermeability to semi-permeability (Gray 1920; Krogh and Ussing 1937; Krogh et al. 1939). The changes in the degree of permeability to water and/or ions were attributed to changes in the protoplasmic membrane (limiting layer) coupled with embryonic activation of osmoregulatory mechanisms. At the egg and embryonic level of development, Krogh (1965) clearly stated that there was no reason to distinguish between vertebrates and invertebrates in freshwater because the problem of preserving maternal ionic stores against the strong outward gradient is universal particularly until the mechanisms for osmoregulation have developed and become active. In preliminary whole egg mass experiments, we observed net uptake of Ca2+ from incubation media with developing L. stagnalis egg masses but not when the embryos were dead (data not shown). In later time course experiments we found that egg masses incubated in nominally Ca2+-free and HCO3 −-free media were affected by lack of Ca2+ availability in the incubation media but not by HCO3 −-free conditions, which suggests that there is an alternative HCO3 −/CO3 2− source for shell formation. The increased Ca2+ uptake in HCO3 −-free HEPES-buffered conditions points to a likely connection between Ca2+ uptake and apparent HCO3 −/CO3 2− acquisition under depleted HCO3 −, yet buffered, conditions.
The presence of internal Ca2+ stores may explain why when embryos had essentially no exogenous Ca2+ sources available they still developed shell but exhibited retarded growth relative to controls. We measured 2 mmol Ca2+ l−1 in perivitelline fluid of in situ eggs containing pre-metamorphic embryos (Fig. 4). This is less but on the same order of magnitude as the 6–7.5 mmol Ca2+ l−1 (12–15 meq Ca2+ l−1) measured by Taylor (1973). There are procedural and possibly population differences to take into consideration between the two studies. Within his study there were greater differences in [Ca2+] between perivitelline fluids of eggs from different egg masses compared to those taken from the same egg mass. This suggests that [Ca2+] in perivitelline fluids of eggs from different snails may differ and account for part of the difference between our observations and those of Taylor (1973). Also around the onset of shell formation, when internal Ca2+ stores were depleted, substantial Ca2+ uptake from the water occurred as evident from both net flux measurements on whole egg masses and microscale measurements whereas there was no significant net movement of either shell-forming ion in pre-metamorphic stages (Fig. 5). Nonetheless, Taylor (1973) calculated that Ca2+ activity in the perivitelline fluid was 4.8 mequiv l−1 (i.e., 2.4 mmol l−1), in good agreement with our value of 2 mmol l−1 in pre-metamorphic embryos. The difference between activity and concentration in the perivitelline fluid may reflect interactions of Ca2+ with polyvalent anions and binding of Ca2+ by macromolecules. As a result, the Ca reserves in the tunica interna and PVF are probably considerably larger than indicated by measurements of Ca2+ based on microelectrodes, which measure Ca2+ activity.
Measurements of perivitelline fluid using a Ca2+-selective microelectrode revealed that there were significant Ca2+ stores in the perivitelline fluid (5–7 times that of the incubation media, Fig. 4) and gelatinous matrix (3–4 times incubation media, Fig. 3) surrounding the eggs of the egg masses during early developmental stages but that these stores apparently become depleted around the time of shell formation. During metamorphosis or at least by day 7, an inside negative ΔμCa/F exists across the membranes separating the embryo from the aquatic environment. This potential was more strongly negative with emergence of the embryos from the egg capsules on day 10. This change in ΔμCa/F was attributed to decreased [Ca2+] in the perivitelline fluid and tunica interna. After metamorphosis, but prior to emergence of embryos from the egg mass, mean ΔμCa/F across the tunica capsulis became more negative (day 7: −19.7 mV, day 10: −51.0 mV) despite a lack of significant change in transmembrane voltage difference (day 7: −9.2 ± 0.60 mV, day 10: −8.7 ± 1.11 mV). However, the strengthening in ΔμCa/F from day 7 to day 10 was accompanied by decreased [Ca2+] in the tunica interna to 20% of day 7 values (Fig. 3). For excised eggs, mean ΔμCa/F across the membrana interna and externa was more negative on day 9 (−26.4 mV) relative to peri-metamorphic values (day 5, −3.7 mV), but the voltage difference across these membranes became less negative over the same time period (day 5: −21.4 ± 0.92 mV, day 9: −9.1 ± 0.77 mV). Thus, the increase in ΔμCa/F was likely due to the decrease in [Ca2+] to 13% of day 5 values (Fig. 4). The depletion of maternal stores available for calcification to concentrations below aquatic levels (Figs. 3, 4) thus favors diffusive Ca2+ influx in these later stages (i.e. movement of Ca2+ down the concentration gradient from the ambient media to the Ca2+-depleted perivitelline fluid).
Considering the aforementioned findings as well as our observations of changes in tunica capsulis integrity over the development of the embryos and findings by Beadle (1969a) that Biomphalaria sudanica embryos have osmoregulatory capabilities, we propose that around the time of embryonic metamorphosis there is also a concurrent change in the membranes of the egg mass. The altered state may allow for Ca2+ diffusion and/or uptake as influenced by Ca2+ removal from the perivitelline fluid by the embryo for calcification. Thus, the tunica interna and tunica capsulis may serve to resist ion efflux during early developmental phases but allow Ca2+ uptake during shell formation. Our techniques did not allow us to isolate what role, if any, the limiting membrane, which is located between the tunica interna and tunica capsulis, plays in this development of permeability.
High calcium accretion of nearly fivefold over the course of development (Taylor 1977) apparently leads to a reduction in [Ca2+] in the tunica interna by day 7 (Fig. 3) and perivitelline fluid by at least day 9 (Fig. 4) to concentrations below ambient media. This provides a reasonable explanation for the observed increase in the inside negative ΔμCa/F over the post-metamorphic stages. One point for further consideration is that reduced [Ca2+]PVF to below water concentrations may allow for less energy consumptive Ca2+ uptake. Similar measurements were made by Taylor (1973) on pre-gastrula (pre-metamorphic) stage embryos. Taylor excised pre-gastrula stage (<24 h old) egg capsules from the tunica interna and allowed them to equilibrate with experimental media for at least 24 h at 22–25°C. In contrast, the microelectrode measurements reported as part of the present study for post-metamorphic embryos were taken immediately after eggs were excised and completed within 1–2 h.
The concomitant occurrence of several events have lead us to consider that it may not be just the embryo that metamorphoses but that the embryo–egg mass complex transforms over the course of development. Maternal Ca2+ reserves provided in the perivitelline fluid apparently decrease over development. This reduction is concurrent with strengthening of inward negative ΔμCa/F across the membranes between the developing embryo and the aquatic environment. Around this same time, active Ca2+ uptake from the surrounding medium also begins. In the SIET measurements, day 7 egg masses exhibited a net Ca2+ flux of 0.04 μmol cm−2 h−1, which translates to 0.48 μmol g−1 h−1 for an egg mass 2 cm long and 0.43 cm diameter. This was of the same order of magnitude as the 0.29 μmol g−1 h−1 that we measured in whole egg mass net Ca2+ fluxes. Furthermore, documented accumulation of 0.13 μmol Ca2+/embryo in isolated eggs over the period from the blastula stage through hatching (Taylor 1977) equates to 7.7 μmol Ca2+ over the time period for an average egg mass with 59 eggs. The blastula stage occurs during the latter half of day 1 for L. palustris embryos maintained at 25°C (Morrill 1982). In whole egg mass fluxes, our embryos, which were maintained at 20–22°C, removed 16.9 μmol Ca2+ from flux media over the period of day 2–11. Thus, our flux measurements using microscale and whole egg mass methods produced similar results and were in reasonable agreement with literature values.
Similar trends were expected in titratable alkalinity kinetics as those observed for Ca2+ kinetics over a range of ambient bicarbonate and/or [Ca2+]. However, considering (1) that embryos developed in HCO3 −/CO3 2−-free media, (2) the lack of a significant relationship between HCO3 −/CO3 2− transport and either Ca2+ or HCO3 − availability, and (3) a significant apparent titratable alkalinity flux under HCO3 −-free, HEPES-buffered conditions there is apparently another source of HCO3 −/CO3 2− for these post-metamorphic embryos. The likely HCO3 −/CO3 2− source in L. stagnalis is hydration of endogenous, metabolic CO2. The notion of retaining and using endogenously produced HCO3 −/CO3 2− for calcification was suggested by Baldwin (1935) following measurements of oxygen consumption and bound CO2 in L. stagnalis embryos. He reported significantly greater O2 uptake rates with developmental progress. Furthermore, the onset of the formation of true shell, which was labeled as stage II in the study, was concurrent with a spiked increase in CO2 content and O2 consumption. In a study on the adults of this species, Greenaway (1971a) proposed a model in which Ca2+ was exchanged between the external medium, blood, fresh tissues, and shell compartments. Additionally, H+ and HCO3 − that were produced through the hydration of metabolic CO2 were exchanged for Ca2+ from the external medium and used for CaCO3 deposition, respectively. To maintain HCO3 −/CO3 2− production from CO2 hydration (CO2 + H2O → HCO3 − + H+ → CO3 2− + H+) and allow for continued shell formation, H+ extrusion is necessary. Indeed, such H+ extrusion likely accounts for the apparent titratable alkalinity uptake in HCO3 −-free media because net acid excretion would be expressed as apparent base uptake when measuring changes in concentrations of absolute alkalinity equivalents. This suggestion is supported by Taylor (1973), who reported that lowering the pH in the bathing medium from 8.5 to 4.0 reduced the concentration of Ca2+ in the perivitelline fluid by up to 85%. We propose that the increase in water [H+] in the Taylor (1973) study would drastically reduce the capacity to excrete H+. Cation uptake in freshwater fish (Bury and Wood 1999; Fenwick et al. 1999; Grosell and Wood 2002; Lin and Randall 1991) and in L. stagnalis (Ebanks and Grosell 2008) has been linked to an electrochemical gradient that is in part established by excretion of the H+ from carbonic anhydrase-mediated hydration of respiratory CO2. Calcium uptake in Lymnaea exposed to low ambient pH would likely be impaired, explaining the earlier observations by Taylor (1973) of reduced [Ca2+] in the perivitelline fluid.
Lastly, the observed increase in ammonia excretion and Ca2+ uptake under HCO3 −/CO3 2−-free HEPES-buffered conditions was another indicator of the use of endogenously produced HCO3 −/CO3 2− in post-metamorphic embryos. Under these conditions the embryos would be forced to rely exclusively on the hydration of CO2 to produce the necessary HCO3 −/CO3 2− for shell formation thus producing greater amounts of H+ to be excreted to the surrounding media in order to maintain acid–base balance and favorable internal conditions for calcification. Increased ammonia excretion, as a result of further acidification of boundary layers and consequent diffusion trapping of NH3 as NH4 +, may thereby explain the observations of elevated ammonia excretion in absence of ambient HCO3 −/CO3 2−. The increased H+ excretion under HCO3 −/CO3 2−-free HEPES-buffered conditions would possibly also enhance hyperpolarization of the apical membrane, which would provide a stronger electrochemical gradient leading to the observed increased Ca2+ uptake.
Utilizing whole egg mass and microscale analytical techniques, we have confirmed the need for aquatic Ca2+ for proper development and timely hatching of embryos of the freshwater common pond snail Lymnaea stagnalis. The embryos apparently utilize an endogenous source of HCO3 −/CO3 2− because they can develop in the absence of ambient HCO3 −/CO3 2−. Furthermore, increased Ca2+ uptake under HCO3 −/CO3 2−-depleted conditions indicates a connection between Ca2+ transport pathways and endogenous HCO3 −/CO3 2− production and thus H+ extrusion. Therefore, we propose that while Ca2+ requirements for complete embryonic shell formation and development are met via uptake, the necessary HCO3 −/CO3 2− is acquired in part from endogenous sources, likely via carbonic anhydrase-catalyzed hydration of CO2 coupled with H+ extrusion with no significant correlation to ambient HCO3 −/CO3 2− availability. Lastly, excretion of H+ from hydration of CO2 seems to facilitate uptake of Ca2+, a subject of ongoing studies.
We thank Drs. Lynne Fieber and Michael Schmale of the University of Miami, RSMAS for use of their cameras & microscopes and Andrea Kocmarek and Erin Leonard, M.Sc. of McMaster University for their technical assistance during S. Ebanks’ visit to the O’Donnell laboratory. This research was funded in part by the NOAA Educational Partnership Program, Environmental Cooperative Science Center and the RSMAS Marine Science Graduate Student Organization Student Travel Fund.
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