ABSTRACT
The mechanism of fluid absorption at ecdysis was investigated in the stenohaline marine decapod, Homarus americanas.
Sea-water uptake began approximately 1 h before ecdysis, increased rapidly during ecdysis, and was completed 2 h after ecdysis.
Increased drinking rates were measured during and just after ecdysis. The quantity of water ingested was equal to the total amount of water absorbed during moult, indicating that fluid entered the haemolymph exclusively via the lining of the digestive tract.
It was estimated that 91 % of the ingested sea water appeared in the haemolymph by 2·5 h postecdysis.
The midgut appeared to be the principal part of the digestive tract involved in the absorption of fluid into the haemolymph. X-radiography of lobsters that ingested a suspension of barium sulphate during ecdysis demonstrated that accumulation and concentration of this compound occurred within the midgut during the 2·5 h of haemolymph expansion following ecdysis. Elevated net water fluxes across perfused midgut were observed in late proecdysis and 0-5 h after ecdysis.
INTRODUCTION
In aquatic arthropods, shedding of the exuvium at ecdysis is accompanied by a rapid increase in wet weight as a result of water uptake (Olmsted & Baumberger, 1923 ; Drach, 1939; Lowndes & Panikkar, 1941; Corrivault & Tremblay, 1948; Travis, 1954; Robertson, 1960; Born, 1970; Dall, 1974). Uptake of water leads to an increase in haemolymph volume; diluting blood constituents and providing space for subsequent addition of tissue mass (Drilhon, 1935; Drach, 1939; Hollett, 1943; Robertson, 1960; Glynn, 1968; Barlow & Ridgway, 1969; Born, 1970; Bursey & Lane, 1971; Dall, 1974; Hepper, 1977).
Most authors agree that the gut lining is the major surface for water absorption (Drach, 1939; Passano, 1960; Robertson, 1960; Mykles & Ahearn, 1978). However, other investigators present qualitative evidence that the gills and/or general body surface are the primary absorptive surfaces at moult (Travis, 1954; Dandrifosse, 1966; Bocquet-Védrine, 1976). But previous studies have not presented quantitative information comparing the amount of water absorbed via a particular route to total water uptake, and thus the relative contribution of a specific absorptive surface to water uptake at moult is not known.
It is generally thought that water is driven across the lining of the digestive tract by osmotic and hydrostatic pressures (Passano, 1960; Robertson, 1960). In the mechanism proposed by Passano, blood osmotic pressure is said to increase as the animal approaches moult. At ecdysis, ‘water is swallowed, increasing the hydrostatic pressure in the digestive tract lumen, and the combined effects of filtration and osmotic uptake cause water to pass into the hemolymph’ (Passano, 1960, p. 492).
It would appear that the filtration-osmotic theory of Passano (1960) is not applicable to all decapod crustaceans. Elevated blood osmolalities during proecdysis have been observed only in strong osmoregulators such as Pachygrapsus crassipes (Baumberger & Olmsted, 1928), Callinectes sapidus (Baumberger & Dill, 1928), Carcinus maenas (Robertson, 1960), and Eriocheir sinensis (De Leersnyder, 1967). In contrast, blood osmolalities of stenohaline marine forms, such as Homarus gammarus (= vulgaris) (Lowndes & Panikkar, 1941; Glynn, 1968), Pugettia producta (Born, 1970), and Penaeus duorarum (Bursey & Lane, 1971), remain essentially iso-osmotic to sea water during the moulting cycle. Therefore, in many marine decapods, the absorption of water into the haemolymph is accomplished in the absence of any obvious osmotic gradient between blood and environment. For this reason, Born (1970) and Smith (1976) have hypothesized that water absorption is linked to active salt transport, which establishes local osmotic gradients at or just beneath the absorptive surfaces. The American lobster, Homarus americanus, is a poor osmoregulator (Dall, 1970). The present investigation examines the dynamics of fluid absorption in this species. It establishes the surface across which fluid is absorbed into the haemolymph and suggests a mechanism by which fluid absorption is accomplished.
MATERIALS AND METHODS
Juvenile American lobsters (1-13 g), Homarus americanus Milne Edwards, were raised in the aquaculture facility at the Bodega Marine Laboratory. Lobsters were fed food pellets and live brine shrimp (Artemia) and maintained at 19 ± 1 °C. The intermoult interval under these conditions was 3–8 weeks. All experiments were performed at room temperature (20 ± 2 °C).
For determination of haemolymph osmolality, approximately 0 ·2 ml of blood was withdrawn from the ventral sinus. Whole blood and sea-water osmolalities were determined with an Osmette Precision Osmometer (Precision Systems, Inc.).
Measurement of drinking rate was made on lobsters placed in a 200 ml sea-water bath containing 25 μCi [14C]inulin (inulin-carboxyl-14C ; ICN, 1·4 μCi/mg) for 1 h. After exposure, individuals were rinsed in unlabelled sea water and frozen. A 1 ml sample of labelled bath was taken at each exposure. While still frozen, the entire gut was removed and placed in a tared scintillation vial, dried to a constant weight at 60–70 °C, and weighed to the nearest 10−4 g. Distilled water (1 ml) was added to each vial to hydrate the tissue sample. Gut tissue was solubilized with 5 ml Protosol (New England Nuclear) at 50 °C for approximately 8 h, cooled to room temperature, and decolourized with 3% hydrogen peroxide (25 drops) at 50 °C for 30 min. Aquasol (NEN; 10 ml) was added to each vial, which was set aside for 12 h before counting. Protosol (5 ml), hydrogen peroxide (25 drops), and Aquasol (10 ml) were added to the vials containing the 1 ml samples of labelled bath. All samples were counted in a Packard Tri-Carb liquid scintillation spectrometer.
X-radiography was performed on lobsters that had ingested a suspension of barium sulphate. Individuals undergoing ecdysis or immediately following ecdysis (stage were placed in a 500 ml sea-water bath containing 30 g BaSO4 kept in suspension by vigorous aeration. After an exposure of variable duration (20–65 min), animals were periodically X-rayed with a Picker Industrial Mini-Shot X-ray unit at 80 kV for 10 s (source-to-target distance = 65 cm).
The measurement of transepithelial net water transport employed the method of Burg & Orloff (1968) as modified for the midgut of freshwater prawn (Ahearn et al. 1977; Mykles & Ahearn, 1978). The entire midgut was removed from each lobster and flushed with lobster saline to remove faecal material. The saline, modified from Welsh, Smith & Kammer (1968), contained, in mM: NaCl, 462·8; KC1, 15·7; CaCl2, 25·9; MgCl2, 8·3; Na2SO4, 8·4; D-glucose, 5·0; Tris-HCl (pH 7·4), 5·0 (995 m-osmol/ kg H2O).
The midgut was mounted on blunted 20-gauge syringe needles in a lucite chamber containing 10 ml saline as serosal bath and perfused with saline at approximately 100/d/min by means of a peristaltic pump (Sage Instruments). To determine the magnitude and direction of net water transport, the difference in perfusate concentration of radioactively labelled non-absorbed volume marker ([14C]inulin) before and after passage through the midgut was measured.
The composition of perfusate and serosal bath was identical except that the perfusate contained [14C]inulin (0·25 μCi/ml) and 0·05% unlabelled inulin to minimize adsorption of radioactivity upon the walls of the tubing. Midgut preparations were perfused for 20–30 min before initiation of sampling. Usually six 5 min collections were obtained from each preparation. Bath samples (1 ml) were taken at the end of the collection period to determine extent of leakage. Preparations with leakages greater than 0·10% of the perfusion rate were eliminated from further consideration. Distilled water (2·5 ml) and 10 ml Aquasol were added to vials containing either 0·5 ml initial perfusate samples, collected perfusate effluent (approximately 0·5 ml), or bath samples (1 ml). The vials were set aside for at least 24 h before counting in a Packard Tri-Carb liquid scintillation spectrometer.
Classification of moult stages was based on that of Drach (1939) and Drach & Tchemigovtzeff (1967). Proecdysis (stage D) subdivisions were as defined by Aiken (1973). For juvenile lobsters raised at 19 °C, moult stages are as follows. Stage DJ animals are within 24–36 h of ecdysis. Stage D4 begins 45–60 min before ecdysis when sea-water uptake commences. At this time the carapace swells and begins to lift. Stage E, or ecdysis, is restricted to exuviation, or the active withdrawal of the animal from the exoskeleton, and lasts 15–20 min.
In postmoult stage A, the cuticle is soft, supple, and easily deformed. Stage Aj are animals immediately following ecdysis. Uptake of water continues through the duration of this stage (0–2 h postecdysis). Stage begins when water ingestion is completed (2 h postecdysis). Final distension of the new cuticle, particularly that of the chelae, occurs during this stage (2–4 h postecdysis). The beginning of stage A2 is defined as the time at which the cuticle is fully distended. Stage A2 has been subdivided on the basis of time after ecdysis. Stage and individuals are 4·5 and 8·5 h postecdysis, respectively. Consumption of the shed exuvium begins 12–18 h after ecdysis. Most of the exuvium is consumed by stage B (3–4 days postecdysis) ; the cuticle has hardened to a parchment-like consistency. The exoskeleton of stage C4 animals (14–15 days postecdysis) is hard and fully formed.
RESULTS
Haemolymph osmolality of juvenile Homarus americanus remained essentially iso-osmotic to sea water (982 m-osmol/kg H2O) during the moulting cycle (Table 1). The blood of stages C4 and D3 individuals was slightly hyper-osmotic to sea water (991-4 and 993·7 m-osmol/kg H2O, respectively). Osmolality of stage A animals declined to 980·5 m-osmol/kg H2O, which was significantly different from the means pf the other moult stages (P < 0·05).
A large increase in whole-animal wet weight occurred at moult (Fig. 1), commencing at stage D4. A transient weight loss accompanied the loss of the exuvium (18% of Dg weight). But this was followed by a rapid weight increase in the 2 h following ecdysis. Weight then increased more slowly. By 4 h after ecdysis, lobsters weighed 30·2% more than in late premoult. The total amount of water absorbed at moult (IFg) was equal to 48·2 ± 1·6% of the premoult weight.
The drinking rate of lobsters varied significantly with stage of the moulting cycle and was greatest during the period of weight increase (Fig. 2). Drinking rate can be seen to rise considerably at ecdysis and 0·5 h postecdysis. The mean values for these stages (E and ) were significantly greater (P < 0·01, Newman-Keuls test of Zivin & Bartko, 11976) than the means of the other groups (stages , D4, , B, and C4).
Table 2 shows that there is no significant difference between the total quantity of water absorbed and the quantity of water ingested during and immediately following ecdysis.
Both water content and haemolymph volume varied significantly during the moulting cycle (Fig. 3). Water content was lowest at stage and rose steadily to maximum values 2·5–8·5 h after ecdysis (stages ). Water content then steadily declined. All group means were significantly different from each other (P < 0·05, Newman-Keuls test) except those between stages D4 and C4 individuals and between stages , , and animals. Change in haemolymph volume followed a similar pattern. Approximately 91 % of the sea water ingested appeared within the haemolymph by 2·5 h after ecdysis. All group means were significantly different from each other (P < 0·05, Newman-Keuls test) except those of stages , D4, C4 stages D4 and B, and stages , and .
X-radiography of lobsters that had ingested a suspension of barium sulphate during ecdysis demonstrated that the compound entered the midgut within 45–60 min after individuals were placed in the suspension (Fig. 4). Immediately following ecdysis, the proventriculus was filled with gastrolith fragments and barium sulphate. During the first hour after ecdysis, barium sulphate accumulated rapidly in the anterior midgut. There was no apparent accumulation in the hepatopancreas, and gastrolith fragments remained within the proventriculus. By 45 min postecdysis, a well-defined faecal strand had formed. It darkened and became more distinct in the radiographs during the subsequent 1·5 h (1–2·5 h postecdysis). There was no further changes in the opacity of the faecal strand 2·5 and 3 h postecdysis.
Significant alterations in transepithelial net water flux, Jv, were observed in the perfused midgut during the moulting cycle (Fig. 5). The group means of stages and preparations were significantly greater (P < 0·05, Newman-Keuls test) than those of stages C4, , and B preparations.
DISCUSSION
The rapid absorption of water at ecdysis in juvenile lobster occurs in the absence of an osmotic gradient between haemolymph and sea water. Water uptake begins about an hour before ecdysis and is completed 2 h after ecdysis. The duration of water uptake is longer in adult Homarus americanus, being completed 4–6 h postecdysis (Corrivault & Tremblay, 1’948). In other decapods, weight gain as a result of water uptake is completed within 4–7 h after ecdysis (Olmsted & Baumberger, 1923; Drilhon, 1935; Drach, 1939; Travis, 1954; Robertson, 1960; Mykles, 1979a).
Dall & Smith (1978) have measured large net influxes of tritiated water in the rock lobster, Panulirus longipes, during stages D4 and E, but the surfaces across which the water entered the haemolymph were not determined. The data presented in this investigation provide convincing evidence that the digestive tract of Homarus is the sole site of water uptake at moult. The amounts of fluid absorbed and sea water ingested during and immediately following ecdysis are equal. Also, drinking of large quantities of sea water coincides with the weight gain observed. The proventriculus is distended to 2–3 times its normal volume in lobsters immediately following ecdysis (Mykles, 1979a).
Haemolymph volume measurements demonstrate that movement of fluid from the gut lumen into the blood space and ingestion of sea water occur simultaneously and are completed by 2–5 h postecdysis. It is estimated that 91% of the sea water ingested appears in the haemolymph by stage . The data suggest that blood volume expansion may begin before lobsters initiate drinking. Perfused midgut preparations obtained from stage animals have elevated net water fluxes, even though intact animals have low drinking rates at this stage. About midway in stage D4, as lobsters drink sea water, haemolymph volume has already increased about 46% above that of stage animals. The large variability of stage blood volumes (Fig. 3) suggests that at least some individuals have initiated fluid absorption.
The generation of internal hydrostatic pressure is caused by drinking the medium, which distends the gut (Drach, 1939; Passano, 1960). Hydrostatic pressure is believed essential in loosening and lifting the carapace before exuviation can occur. The extent to which the gut lining can be distended is limited; the absorption of fluid into the haemolymph would allow the animal to ingest greater quantities of sea water, resulting in the generation of greater hydrostatic pressures.
Fig. 6 summarizes the changes in magnitude of the major compartments within a hypothetical 100 g lobster during the moulting cycle. The columns comprising the whole-animal wet weight are divided into three major components; dry weight, extra-haemolymph space, and haemolymph volume. Before ecdysis, dry weight is divided between the exuvium and tissue mass. At moult, 18 g (10·6 g dry weight and 7·4 g water) is lost when the exuvium is shed. Tissue dry weight remains relatively constant through moult (stages D4, , and ). In stages B and C4, dry weight increases because of the combined effects of synthesis and mineralization of the remainder of the cuticle and tissue proliferation (Passano, 1960).
Extra-haemolymph space is the remainder of the body water not contained within the haemolymph and comprises gut fluid, the contents of the antennal gland (urine), intracellular water, and water in the exoskeleton. As haemolymph volume increases from stages D4 through and , extra-haemolymph space decreases. Because it is improbable that intracellular water, cuticular hydration, or antennal gland volume is changing in such a short interval, the decline in extra-haemolymph space, particularly from stage to stage , may reflect a decrease in gut volume as fluid is absorbed into the haemolymph. Blood volume decreases substantially in the days following ecdysis (stages B and C4). The reasons appear to be complex. Addition of tissue mass and cuticular materials, as well as the expansion of extra-haemolymph space are responsible. As more cuticle continues to be secreted, more water is invested in the exoskeleton. The gut volume may be larger as digestive enzymes and emulsifiers are secreted upon resumption of feeding by stage B individuals.
The midgut appears to be the principal part of the digestive tract of Homarus involved in absorption of ingested sea water into the haemolymph. X-radiography of lobsters that had ingested a barium sulphate suspension at moult (Fig. 4) indicates that formation and consolidation of the faecal strand within the midgut parallels haemolymph expansion during the 2·5 h after ecdysis. Concentration of the compound results presumably from the net absorption of fluid from the lumen. Also correlated with haemolymph expansion, increased net water fluxes across the perfused midgut occur in stages and . Elevated net water fluxes are also observed in the perfused midgut of the freshwater prawn, Macrobrachium rosenbergii, during stage D (Mykles & Ahearn, 1978).
Drach (1939) has calculated that a solution similar in composition to sea water is absorbed by the spider crab, Maia squinado, at ecdysis. In stenohaline marine decapods, it appears that a fluid iso-osmotic to sea water is transported into the haemolymph because blood solute concentration does not change during the moulting cycle (Lowndes & Panikkar, 1941 ; Glynn, 1968; Born, 1970; Bursey & Lane, 1971). Both Ahearn et al. (1977) and Mykles (1979a) have shown that net water transport is linked to solute transport in perfused midgut preparations from Macrobrachium and Homarus, respectively. The ultrastructural organization of the midgut and midgut caeca of Homarus (Mykles, 19796) as well as that of other decapods (Komuor & Yamamoto, 1968; Talbot, Clark & Lawrence, 1972; Mykles, 1977, 1979b; Smith, 1978) resembles that of other epithelia capable of active ion transport (Berridge & Oschman, 1972). The basal cytoplasm contains numerous mitochondria and an anastomosing system of smooth endoplasmic reticulum contiguous with the basolateral cell membrane. The ultrastructural and physiological information suggests that solutes, primarily Na+ and Cl−, are transported into the lumina of the smooth endoplasmic reticulum, creating a local osmotic gradient that draws water across the apical membrane and leads to an iso-osmotic flow of ions and water across the epithelium and into the haemolymph.
ACKNOWLEDGEMENTS
I thank Professors Ralph I. Smith, Howard A. Bern, Richard M. Eakin, and Robert I. Macey for their continued interest and support. Professor Cadet Hand, Director of Bodega Marine Laboratory, and Dr Douglas Conklin of its Aquaculture Project did much to aid this investigation. I am grateful to Professor David Wake, Director of the Museum of Vertebrate Zoology, University of California, Berkeley, for use of the X-ray unit, to Ms Phyllis Thompson for preparing the illustrations, to Mr. John Underhill for printing the radiographs, and to Professors R. I. Smith, H. A. Bern, C. Hand, and Dr Dorothy M. Skinner for critical reading of the manuscript. This research was sponsored by NOAA Office of Sea Grant, Department of Commerce, under Grant no. 04-7-158-44121. Additional funding was provided by NSF Grant PCM 75-16345 to Professor H. A. Bern.
REFERENCES
Note added in proof
Dall and Smith (J. exp. mar. Biol. Ecol., 1978, vol. 35, pp. 165–76) have recently investigated water uptake at ecdyais in the western rock lobster, Panulirus longipes. Their findings differ from those presented here in two respects: (1) the quantity of water ingested (13·7 % of premoult weight) was less than the total increase in weight (18·4–01·4% premoult weight) at moult and (2) the hepatopancreas, rather than the midgut proper, is the major site of absorption of fluid into the haemolymph. The midgut of Panulirus is limited to a short segment where the hepatopancreatic ducts join the digestive tract. Thus, it is probable that the absorptive function has been assumed by one or mote cell types in the hepatopancreas of Panulirus.