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1 June 2002 A Comparative Study of Osmoregulation in Four Fiddler Crabs (Ocypodidae: Uca)
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This study aims to give an integrative description of the correlation of physiological parameters of osmoregulation and the habitats of the four common Uca species in Taiwan. Uca arcuata inhabits areas close to fresh water in the upper beach. Uca formosensis is only found in the areas near the mean high water of spring tide where there is a clear dry-wet transition within a single semilunar cycle. Uca vocans is found in the lower intertidal zone. Uca lactea, the most widely distributed species, can easily be found on most muddy sand shores. The number of gills was observed and histological sectioning performed on each species. The range of salinity in which the fiddler crabs maintained their hemolymph osmolality without any significant change (i.e. osmoregulatory homeostasis) and the gill Na , K -ATPase activity were determined by transferring individuals to different salinity tanks. The results suggest that U. formosensis and U. lactea can sustain a wider range of salinity change through both modification in gill morphology and Na , K -ATPase activity. Uca arcuata can regulate in a hypo-osmotic condition and U. vocans tends to be a weak-osmoregulator.


Euryhaline fiddler crabs inhabit estuaries and intertidal regions where the salinity can fluctuate from almost fresh water to suprasaline (D'Orazio and Holliday, 1985; Rabalais and Cameron, 1985; Luquet et al., 1995; Zanders and Rojas, 1996). Brachyuran crabs typically have 9 pairs of gills, but the number of gills tends to decrease as the degree of terrestriality increases (Gray, 1957; McMahon and Burggren, 1988; Taylor and Taylor, 1992). In those crabs, which live in brackish water or intertidal areas, the anterior gills are usually for respiration and the posterior gills for both respiration and osmoregulation (Copeland, 1968; Luquet et al., 1995; Péqueux, 1995 for review; Takeda et al., 1996). The respiratory lamellae consist of a thin layer of epithelia without any accumulation of mitochondria. On the contrary, a lot of ionocytes with many mitochondria can be found in the epithelial layer of osmoregulatory lamellae (Greenaway, 1988; Taylor and Taylor, 1992; Luquet, 1995; Takeda et al., 1996).

Previous studies have reported that Na+, K+-ATPase located in the basal infolding system of the ionocytes will change its activity with environmental salinity, implying a role in regulation of the internal ionic composition (D'Orazio and Holliday, 1985; Holliday, 1985, 1988; Corotto and Holliday, 1996; McLaughlin et al., 1996). This can be correlated with the habitat of the species. When transferred to hypo- or hyper-osmotic conditions, brachyuran crabs response differently in respect of branchial Na+, K+-ATPase activity. An increase in Na+, K+-ATPase activity was observed when brachyuran crabs, including Uca pugnax, Hemigrapsus nudus, Carcinus maenas, Uca pugilator, and Pseudosesarma moeschi, were transferred to hypoosmotic conditions (D'Orazio and Holliday, 1985; Holliday, 1985; Péqueux, 1995; Corotto and Holliday, 1996; McLaughlin et al., 1996). On the other hand, when transferred to hyperosmotic conditions, H. nudus (Corotto and Holliday, 1996) and C. maenas (Péqueux, 1995) had no change in Na+, K+ATPase activity, while U. pugilator decreased (D'Orazio and Holliday, 1985) and P. moeschi increased (McLaughlin et al., 1996). These studies, however, focused more on discussion at a physiological level rather than on the relation between physiological diversity and its ecological implications.

In this study, four of the most common Uca species (U. vocans, U. arcuata, U. formosensis and U. lactea) which live in mid- to supra-tidal zones in Taiwan were compared, especially in gill morphology, hemolymph osmolality and Na+, K+ATPase activity.


Field Observation

Environmental parameters were recorded for the mudflat of the south Tadu estuary, Taiwan, where the four Uca species were collected. Four transect lines were prepared, each 50 m apart. Each transect line was 600 m long, and a sampling area (10×10 m2) was established every 200 m. There were four sampling areas per line. The total number of each species of crabs present during low tide, and salinity in crab burrows or on the surface, were recorded daily for 14 days. On the day after a neap tide when the tidal water first reached the burrows of U. formosensis in the April of 1998, salinity of water sampled from 10 burrows of each species was determined.

Laboratory Preparation

Adult male specimens of U. arcuata, U. formosensis, U. vocans and U. lactea were collected from the Tadu estuary (120°30′N, 24°13′E) in mid-Taiwan. They were transported to the laboratory and three individuals per species were sacrificed immediately for gill number determination and histological sectioning of the gills. The rest were maintained in 200 L holding aquaria (90×45×60 cm3, one aquarium for each species) before experiments. All animals were kept at 26–28°C under a 14 L/10 D photoperiod.

Holding aquaria had a layer of 3-cm coarse coral reef sand and contained about 80 L of 25 ppt artificial seawater (ASW) made directly by mixing local tap water and salts (Coralife scientific grade marine salt, USA). The water level was about 12–15 cm. The water was aerated and filtered continuously. Several plastic racks (18×12×13 cm3) with nylon mesh were provided as a platform for the crabs to stay in air. They were allowed to enter or leave the water and acclimated at least a week (but less than one month) before the salinity transfer experiment. Salinity was monitored by refractometry (ATAGO model S/Mill-E, Japan) every other day. A stock solution of 60 ppt ASW was prepared for experimental use and subsequently diluted to 0, 5, 15, 25, 35, 45 and 60 ppt ASW. The respective osmolalities were as follows: 0, 36, 438, 736, 996, 1274 and 1679 mosmol kg−1 H2O. The 0 ppt ASW was obtained from a 2000 × dilution. This was to simulate the result of the mixing of fresh water and seawater under the natural environment.

Twenty liters of experimental saline water were introduced into 25 L white plastic tanks (50×20×25 cm3) with lids. Each tank had coral reef sand on the bottom and the water was aerated and filtered continuously.

Weighed crabs were wrapped in a paper towel and kept on ice. As soon as they could no longer move, the carapace was carefully removed and the right side gills were cut off for determination of gill morphology and Na+, K+-ATPase activity.

Branchial morphology

The degree of branchial development and/or reduction was compared among the four species of Uca, following the method of Takeda et al. (1996). Briefly, three of the largest individuals of each species were chosen for dissection. After the carapace was removed, the gills on the right side were removed from the articulation, appendage, or sternite, and their length, number, and arrangement were recorded. The positions and numbers of the gills with the abbreviations for them are presented in Table 1.

Table 1

Gill morphology in the four species of Uca.



To investigate the osmoregulatory function of the gills, histology of the four most prominent gills (gills 5–8) of each species was examined. The podobranchiae on the second and third appendages (gills 1 and 3) and anterior arthrobranchiae (gill 4) on the third thoracic segment were too small to examine. Excised gills were fixed in FAA fixative (formalin, acetic acid, 70% alcohol, 1:1:18) without further dissection, followed by t-butonal-alcohol series dehydration. Sections (8 μm thick) were sliced from each gill and stained with hematoxylin and eosin. Gills with a marked increase in tissue thickness were considered to be highly osmoregulatory, while those with a thin layer of epithelium underneath the cuticular layer were recorded as respiratory gills. The criteria for determination are based on the review paper by Péqueux (1995) in which a thin epithelium of 1 to 5 μm is recognized as the site of gas exchange and a thick epithelium of 10 to 20 μm as the site of ion transport. Gills with only a small increase in thickness were recorded as weakly osmoregulatory gills.

Hemolymph osmolality (HO)

The range of salinity in which the fiddler crabs maintained their hemolymph osmolality was examined in the four species of crabs. By keeping 3-5 crabs in a mesh cage (18×12×13 cm3), four to eight cages were submerged in one experimental tank. Crabs were forced to remain fully immersed in 25 ppt ASW for 72 hr and transferred to 0, 5, 15, 25, 35, 45 or 60 ppt ASW, respectively. D'Orazio and Holliday (1985) indicated that the hemolymph of U. pugilator would show little change if they were allowed to enter or leave the media freely. Therefore, crabs were kept submerged throughout the experiment. The HO was measured at 0, 1, 4 hr and 2, 7, 14 days after submersion. Three to five individuals were used to determine the HO at each sampling period for each species.

The hemolymph samples were taken through the arthrodial membrane at the base of the large chela with a 27-gauge needle and quickly expelled into a 0.5 ml plastic tube. Hemolymph osmolality (8 μL aliquot of hemolymph) was immediately determined by an osmometer (Wescor Model 5500 vapor pressure osmometer). Laboratory temperature was kept at 25–26°C during osmolality measurement.

Na+, K+-ATPase activity

Due to mortality of individuals of some species kept at extreme salinities (0 and 60 ppt ASW) in the HO experiment, only three levels of salinity (5, 25 and 45 ppt ASW) were included in this experiment. Two sampling periods, 4 hr and 14 d, would represent respectively the time of one ebb or flow tide and of one spring tide. Similar to the preparation in the HO experiment, individuals (3 per mesh cage) were first submerged into the experimental tanks with 25 ppt ASW for 72 hr before being transferred directly to 5, 25 or 45 ppt ASW. Assays were performed and three individuals per species were collected at 0 hr, 4 hr and 14 days. The right side of the four most prominent gills (gills 5, 6, 7 and 8) was sampled for enzyme activity determination.

Each weighed gill was rinsed in ice-cold homogenizing medium (HM: 0.25 M sucrose, 6 mM EDTA). Because the gills differed in size, the amount of HM added for homogenization varied. Basically, the volume (in μL) of HM was equal to 10–20 times the mass (in mg) of the gills. The gills were homogenized by a motor-driven, glass homogenizer (Hsiangtai Model DC-2RM, Taiwan) at 600 rpm for approximately 30 sec or until lamellae were not seen. Crude homogenate was then centrifuged at 4°C for 15 min at 4000 rpm (Hettich with rotor 1412) to remove cellular debris. The super-natant was collected, diluted 10 times with HM and rehomogenized in a hand-held homogenizer. Aliquots of 66.7 μL homogenate were prepared in 1.0 ml Eppendorf vials on ice and assayed immediately.

The method to determine Na+, K+-ATPase enzyme specific activity (ESA) was that of Holliday (1985). One of two reaction media (200 μl each) was added to aliquots of the 66.7 μL homogenate. One reaction medium had the complete formulus of all ions (167 mM NaCl, 50 mM KCl and 33.3 mM imidazole, pH 7.2) while the other had no potassium but contained 1.67 mM ouabain (an Na+, K+-ATPase specific inhibitor) (217 mM NaCl, 33.3 mM imidazole and 1.67 mM ouabain (Sigma), pH 7.2). They were mixed and preincubated at 30°C for 5 min in a water bath before 66.7 μL of the starting solution (25 mM Na2ATP (Sigma) and 50 mM MgCl26H2O (Sigma), pH adjusted to 7.2 with crystalline imidazoleHCl) was added and mixed well. After another incubation at 30°C for exactly 15 min, the reaction was stopped by adding 1.5 ml ice-cold Bonting's reagent (560 mM H2SO4, 8.10 mM ammonium molybdate and 176 mM FeSO4) and color was allowed to develop for 20 min at 20°C. Phosphate concentration was measured spec-trophotometrically at 700 nm as the reduced phosphomolybdate complex.

The protein contents in the homogenates were determined spectrophotometrically at 595 nm using bovine serum albumin as a standard. Enzyme specific activity (ESA) of Na+, K+-ATPase was calculated as the difference between phosphate (Pi) liberated by each homogenate in the two media and expressed as mmol PO42– per mg homogenate protein per h.


All results were expressed as mean value ± standard error. In the hemolymph osmolality experiment, the significance of difference in transfer time in various media was determined by one-way ANOVA followed by Duncan's Multiple Range Test (SAS 6.12).

For the comparisons of Na+, K+-ATPase activity, because of the non-independence of the ESA of each gill within an individual and because the ESA among gills was measured at the same time, a repeated-measures ANOVA was performed (Tabachnick and Fidell, 1989) on the four most prominent gills. The grouping variable was salinity, divided into (1) control, which was crabs acclimated to 25 ppt at the beginning of the experiment, (2) 5 ppt, (3) 25 ppt and (4) 45 ppt. Three individuals of each species were collected 4 hr and 14d after transfer. SAS GLM profile analysis (SAS 6.12) was used. Additionally, pair-wise comparisons were performed between certain data subsets.


Field Observation

Uca arcuata was mostly found on wet muddy substrate along tidal creeks and canals. The environmental salinity of U. arcuata was less than 5 ppt during low tide and between 20 to 30 ppt during high tide. The salinity range for U. formosensis recorded in the field ranged from 0 to 38 ppt. Uca formosensis lives on open mudflats of supratidal regions where seawater does not reach for 3 to 5 days during neap tides. Nevertheless, water can be sampled from the bottom of their burrows and the average salinity of water collected in the burrows during neap tides was lower than 5 ppt. The species, which lives at the lowest tidal location, is U. vocans. Tidal water reaches here everyday and daily salinity changes during the 14 days of recording ranged from 23 to 35 ppt. The most widely distributed U. lactea was found in all three habitats. Since there were more U. lactea in the low to mid-tidal region than in the rest of the area, we recorded its habitat characteristics in this area. The salinity range of this low to mid-tidal area was between 24 to 38 ppt during the 14 days of observation.

The salinity determined from 10 burrows for each species were as follows: 11.3±2.7 ppt for U. arcuata, 41.9±1.1 ppt for U. formosensis, 39.3±0.8 ppt for U. vocans and 36.1± 0.8 ppt for U. lactea.

Gill morphology

None of the four species had gills 2 and 9. On all four species of Uca, the posterior four pairs of gills (gills 5–8) were more prominent than the anterior three pairs (gills 1, 3 and 4). For all species, the anterior arthrobranchiae attached to the forth appendages (gill 6) were the longest. A species-specific variation was found in the degree of reduction in the three anterior gills (gills 1, 3 and 4) (Table 1). There were 7 complete gills in U. vocans. Both U. arcuata and U. formosensis had 6 complete gills. Gill 3, which was completely absent in U. formosensis, is reduced to a rod shape without lamellae in U. arcuata. The least number of gills was found in U. lactea, which had only 5 gills, with a reduction of gill 4 and a complete reduction of gills 3 and 9.


Histology of the four most obvious gills (gills 5–8) of Uca indicated further morphological variation. In U. formosensis, many ionocytes, easily noticed by the tissue thickening, were observed in the lamellae of all four gills. Although a highly osmoregulatory type of gill was suggested, the degree of lamella thickening was more evident in gills 7 and 8 than in gills 5 and 6.

Highly osmoregulatory type gills were also found in gills 7 and 8 of the other three Uca species, except gill 7 in U. vocans. In U. lactea, respiratory and weakly osmoregulatory gills were recorded respectively for gills 5 and 6. Gill 6, but not gill 5, of U. arcuata was determined to be weakly osmo-regulatory. Both gills 5 and 6 of U. vocans were classified as respiratory (Table 2).

Table 2

Osmoregulatory and respiratory functions in the four most apparent gills of Uca.


Hemolymph osmolality

After acclimation to 25 ppt ASW for 72 hr, the four species of fiddler crabs had average hemolymph osmolality as follows: U. arcuata 755.8±5.5 mosmol kg−1 H2O (N=26), U. formosensis 860.9±2.0 mosmol kg−1 H2O (N=31), U. vocans 786.0±4.7 mosmol kg−1 H2O (N=29) and U. lactea 840.1± 4.7 mosmol kg−1 H2O (N=30). Results following transfer to different salinities are presented by species.

U. arcuata. Hemolymph osmolality (HO) did not change significantly within 14 days for those individuals transferred to 15 or 25 ppt ASW (Fig. 1A). Comparing the osmolality at 0 hr (crabs were collected immediately after being transferred) and 4 hr after transfer, a significant difference was found in those transferred to 0, 35, 45 and 60 ppt ASW. All individuals in 0 ppt ASW died shortly after 7-day observation. In 35 ppt ASW, HO increased significantly 4 hr after transfer, reached environmental condition at 7 d (1012.6± 2.9 mosmol kg−1 H2O) and recovered slightly thereafter. Dramatic increases in HO were recorded in those individuals transferred to 45 and 60 ppt ASW and all individuals died shortly after 2 days (Fig. 1A).

Fig. 1

Time course of changes in hemolymph osmolality (HO) in (A) Uca arcuata, (B) U. formosensis, (C) U. vocans and (D) U. lactea after transfer of crabs from 25 ppt to various salinities. Each symbol represents the mean value of hemolymph samples from 3 to 5 crabs. For a better recognition of the symbols, only those standard errors larger than 35 were displayed. Asterisks indicate significant differences between mean values of HO at time zero and 4 hr after transfer.


U. formosensis. Only individuals in 0 ppt ASW displayed a significant decrease in HO after 4 hr of transfer (Fig. 1B). HO declined to 487.2±8.9 mosmol kg−1 H2O prior to their death on day 2. It was the seventh day before a significantly lower HO was noticed in either 5 or 15 ppt ASW (as compared to the HO at 0 hr in their respective salinity) (Fig. 1B). For those in 35 or 45 ppt ASW, maximal HO was observed on day 7 (979.8±14.6 mosmol kg−1 H2O and 1329.6±8.4 mosmol kg−1 H2O, respectively). Although HO in both salinities recovered significantly on day 14 (compared to day 7), they were still significantly higher than their respective controls. Individuals in 60 ppt ASW did not increase their HO until 2 days after transfer and they survived for at least 7 days.

U. vocans. It took only 4 hr for U. vocans to show a significant difference in HO after they were transferred to 0, 5, 35, 45 or 60 ppt ASW (Fig. 1C). U. vocans survived in 0 or 60 ppt ASW for 2 days only. There were slight variations through time in those submerged in 5, 15 and 25 ppt ASW. When kept in 35 ppt ASW, individuals of U. vocans had a significant rise in HO by 4 hr. Their HO was close to environmental conditions on day 2 (981.2±15.3 mosmol kg−1 H2O) and day 7 (1001.6±11.5 mosmol kg−1 H2O). By the end of the 14 days, the HO was significantly lower than that at the end of 7 days and recovered to the level recorded after 4 hr. Similarly, when U. vocans was maintained in 45 ppt ASW SW, a drastic increase was noticed by day 7 (1364.3±4.9 mosmol kg−1 H2O) and a slight decline thereafter (1276.6±21.3 mosmol kg−1 H2O) on day 14. U. vocans only survived in 60 Fppt ASW SW up to 2 days with its HO (1747.5±7.4 mosmol kg−1 H2O) almost equivalent to the external milieu.

U. lactea. Among the seven salinity levels, 25 ppt ASW was the only salinity treatment that did not cause significant change in HO within the 14-day observation. Four hours after transfer, significant changes in HO were found in organisms from 0, 5 and 60 ppt ASW (Fig. 1D). All specimens of U. lactea had a significantly lower HO and they died shortly after the second day in 0 ppt ASW. Although there was a significant change in HO when specimens of U. lactea were held in 5 ppt ASW, HO did not change further. At 35 ppt ASW, a significant rise in HO was found 2 d after transfer. In 45 ppt ASW, HO peaks in specimens of U. lactea on day 7 (1329.5±7.5 mosmol kg−1 H2O), thereafter declining significantly by day 14. The HO of specimens of U. lactea in 60 ppt ASW rose to 1157.6±43.6 mosmol kg−1 H2O within 4 hr and was iso-osmotic to the environment by day 7 (1718.5±16.6 mosmol kg−1 H2O), but no specimen of U. lactea survived 14 days exposure to this salinity.

In summary, the salinity range for osmoregulatory homeostasis was species-specific. Upon four hours after transfer, U. formosensis had the widest range (5 to 60 ppt ASW), followed by U. lactea (15 to 45 ppt ASW) and U. arcuata (5 to 25 ppt ASW), and U. vocans had the narrowest (15 to 25 ppt ASW). Response to salinity over a longer period of time was also species-specific.

Na+, K+-ATPase activity assay (ESA)

This experiment compared the time course of branchial Na+, K+-ATPase activity of the four crab species salinity transfer after salinity transfer. An increase in the Na+, K+ATPase activity was taken as an indication of an active physiological regulation in response to salinity change.

Among all four species studied, the two posterior gills (gills 7 and 8) had a higher ESA than the two anterior to them (gills 5, 6). The test statistics for each species and time periods are summarized in Table 3.

Table 3

Univariate repeated-measures ANOVA of the effects of salinity on the Na+, K+-ATPase activity in the gills of four Uca species.


U. arcuata. Within 4 hr after transfer to 45 ppt, salinity had a significant effect on ESA (Fig. 2A, Table 3A). But this difference disappeared by the end of the 14 d experiment (Fig. 2B, Table 3B). Instead, the difference among gills was significant. However, the standard error of each of the 4 hr treatment combinations was also high, making further comparisons insignificant. None of the individuals submerged in 45 ppt survived to the end of the 14 d experiment.

Fig. 2

Na+, K+-ATPase ESA in the gills of (A, B) U. arcuata, (C, D) U. formosensis, (E, F) U. vocans and (G, H) U. lactea. Crabs were first acclimated at 25 ppt for 72 hr before being transferred to 5, 25 and 45 ppt ASW. Na+, K+-ATPase ESA at 4 hr and 14 days was determined from 3 to 5 crabs. Error bars represent±1 SE.


U. formosensis. Specimens of U. formosensis had the lowest ESA among the four Uca species (Fig. 2C, D). However, in addition to a significant difference in ESA among salinity treatments, a difference was found among gills in both sampling periods (Table 3C, D). There was no significant difference in ESA between these two sampling periods (Fig. 2C, D).

U. vocans. Four hours after transfer, the salinity effect on ESA was not significant, while the difference among gills was significant (Table 3E). The ESA changed significantly, especially in the two posterior gills at low salinity on day 14 (Table 3F and Fig. 2E, F).

U. lactea. Although the gills have significantly different ESA, salinity did not have an effect on the ESA of U. lactea at either 4 hr or 14 d after transfer (Table 3G, H and Fig. 2G, H).


In this study, discussion of physiological responses to salinity fluctuation in the natural environment is possible since several species were studied at the same time and both the ecological data on salinity fluctuation and laboratory investigation on enzyme activity were included.

Gray (1957) reported that the reduction in gills was correlated with the degree of terrestrial adaptation in crabs. This correlation was observed in our study, with U. lactea having only 5 pairs of functional gills, U. formosensis and U. arcuata each having 6 and U. vocans having 7. Similar results were also reported by Takeda et al. (1996) in their study of 16 species of ocypodid and grapsid crabs. Uca annulipes, whose distribution is highest on the shore has the fewest pairs of gills (5), while U. tetragonon and the subspecies U. vocans vocans, both of which live near the low tide mark, each have 7 pairs (Takeda et al., 1996). However, it is inappropriate to predict the degree of terrestrial adaptation by the number of gills when the crab species vary greatly in size or are phylogenetically distant. For example, Gecarcinus lateralis, which lives in supratidal zone and is completely terrestrial, has 7 functional gills plus 2 vestiges (Copeland, 1968) and it would have been misleading to compare its terrestrial adaptation with those of Uca species. In our study, U. lactea is significantly smaller than the other three species and it is uncertain whether this would have any association with the extent of gill reduction.

For most terrestrial crabs, gas exchange takes place in the specialized vascular system on the inner lining of cara-pace, while osmoregulation is performed in thickened gill lamellae filled with ionocytes (Mantel and Farmer, 1983; Greenaway, 1988). In our study, Uca formosensis and U. arcuata had increases in thickness in the four most prominent gills. Similar results were also reported in two supratidal fiddler crabs, U. annulipes and U. forcipata (Takeda et al., 1996).

The four Uca species exhibited various degrees and ranges of osmoregulatory homeostasis when transferred to different salinities. The ability to maintain HO was well correlated with the habitat of each species described in the first paragraph in the Result. From our results for crabs submerged in various salinities for up to 14 days, U. formosensis is a better hyper-hypoosmoregulator than U. lactea, and both U. arcuata and U. vocans are hyper-osmoregulators.

For those species such as U. longisignalis, U. rapax and U. subcylindrica which live in a habitat similar to or more terrestrial than that of U. formosensis, their salinity tolerance ranges (or the salinity ranges of survival) are much larger than in other intertidal Uca species (Rabalais and Cameron, 1985; Zanders and Rojars, 1996). The salinity tolerance ranges of U. longisignalis and U. subcylindrica were 0.008 to 110 g L−1 NaCl (about 0 to 110 ppt) and 2 to 90 g L−1 NaCl (2 to 90 ppt), respectively (Rabalais and Cameron, 1985), while that of U. rapax was 7 to 139 g L−1 NaCl (7 to 139 ppt)(Zanders and Rojars, 1996). Although their ranges were much larger than that of U. formosensis, the gradual transfer (instead of our direct transfer) to extreme salinity may explain this difference.

Several studies have indicated that enzyme activity of branchial Na+, K+-ATPase varies with species and their acclimation conditions (Corotto and Holliday, 1996; McLaughlin et al., 1996; Castilho et al., 2001). In brief, an increase in Na+, K+-ATPase ESA was found in the intertidal crustaceans exposed to diluted seawater. The increase is especially apparent in the posterior gills. Increase in Na+, K+-ATPase ESA at low salinity has been observed in U. pugilator (D'Orazio and Holliday, 1985) and U. pugnax (Holliday, 1985) acclimated for 21 d. U. vocans, which is distributed in the lower intertidal areas, had a significantly higher Na+, K+ATPase ESA in the two posterior gills when they were kept at low salinity for 14 d, presumably to increase ion uptake. However, this response did not occur in the rest of the three Uca species in Taiwan. Uca lactea was collected from a similar tidal location as U. vocans. Uca lactea exhibited a similar but insignificant trend of change in Na+, K+-ATPase ESA when transferred to low salinity for 14 days. Neither U. arcuata nor U. formosensis had a significant change in Na+, K+-ATPase ESA at low salinity. In addition to species-specific variation, different length of acclimation (i.e. 21 d in the studies by D'Orazio and Holliday (1985) and Holliday (1985) and 14 d in the present study) should be taken into account.

There are far fewer studies of Na+, K+-ATPase ESA in crabs acclimated to hyperosmotic conditions and the results are inconclusive. No significant change was observed in Na+, K+-ATPase ESA of U. pugnax at high salinity (150% or 200% SW) (about 53 or 71 ppt, respectively) (Holliday, 1985), while a significant decrease in Na+, K+-ATPase ESA was reported for the posterior gills of U. pugilator acclimated to 200% seawater (approximately 71 ppt) (D'Orazio and Holliday, 1985). In our study, the change in Na+, K+-ATPase ESA of both U. formosensis and U. vocans after 14 d of acclimation may not necessarily be biologically significant, due to small sample size, large standard deviation and partial mortality. In the future, it would be particularly interesting to examine the plasticity of branchial morphology and Na+, K+-ATPase ESA in a certain widely distributed species such as U. lactea from different types of habitats.


This study was supported by National Science Council, Taiwan, R.O.C. (NSC 89-2313-B-029-015) to HCL.



P. C. Castilho, I. A. Martins, and A. Bianchini . 2001. Gill Na+, K+-ATPase and osmoregulation in the estuarine crab, Chasmagnathus granulata Dana, 1851 (Decapoda, Grapsidae). J Exp Mar Biol Ecol 256:215–227. Google Scholar


D. E. Copeland 1968. Fine structure of salt and water uptake in the land-crab, Gecarcinus lateralis. Am Zool 8:117–132. Google Scholar


F. S. Corotto and C. W. Holliday . 1996. Branchial Na+, K+-ATPase and osmoregulation in the purple shore crab, Hemigrapsus nudus (Dana). Comp Biochem Physiol 113/A:361–368. Google Scholar


S. E. D'Orazio and C. W. Holliday . 1985. Gill Na+, K+- ATPase and osmo-regulation in the sand fiddler crab, Uca pugilator. Physiol Zool 58/4:364–373. Google Scholar


I. E. Gray 1957. A comparative study of gill area of crabs. Biol Bull 112:34–42. Google Scholar


R. Greenaway 1988. Ion and water balance. In “Biology of the Land Crabs”. Ed by W. W. Burggren and B. R. McMahon . Cambridge University Press. London. pp. 211–248. Google Scholar


C. W. Holliday 1985. Salinity-induced changes in gill Na+, K+-ATPase activity in the mud fiddler crab, Uca pugnax. J Exp Zool 23:199–208. Google Scholar


C. W. Holliday 1988. Branchial Na+, K+-ATPase and osmoregulation in the isopod, Idotea wosnesenskii. J Exp Biol 136:259–272. Google Scholar


C. M. Luquet, G. Pellerano, and J. M. DeCarlo . 1995. Gill morphology and terrestrial adaptation in the estuarine crab Uca uruguarensis (Nobili, 1901) (Decapoda, Brachyura). Crustaceana 68/7:882–892. Google Scholar


L. H. Mantel and L. L. Farmer . 1983. Osmotic and ionic regulation. In “The Biology of Crustacea. Volume 5. Internal Anatomy and Physiological Regulation”. Ed by L. H. Mantel Academic Press. New York. pp. 53–161. Google Scholar


R. McLaughlin, N. Firooznia, and C. W. Holliday . 1996. Branchial Na+, K+ATPase activity and osmotic and chloride ion regulation in the Thai Crab, Pseudosesarma moeschi. J Penn Acad Sci 70:45–52. Google Scholar


B. R. McMahon and W. W. Burggren . 1988. Respiration. In “Biology of the Land Crabs”. Ed by W. W. Burggren and B. R. McMahon . Cambridge University Press. London. pp. 249–297. Google Scholar


A. Péqueux 1995. Osmotic regulation in crustaceans. J Crust Biol 15/1:1–60. Google Scholar


N. N. Rabalais and J. N. Cameron . 1985. Physiological and morphological adaptations of adult Uca subcylindrica to semi-arid environments. Biol Bull 168:135–146. Google Scholar


B. G. Tabachnick and L. S. Fidell . 1989. Using Multivariate Statistics. 2nd ed. Harper Row. New York. Google Scholar


S. Takeda, M. Matsumasa, S. Kikuchi, S. Poovachiranon, and M. Murai . 1996. Variation in the branchial formula of semi-terrestrial crabs (Decapoda: Brachyura: Grapside and Ocypodidae) in relation to physiological adaptations to the environment. J Crust Biol 125:315–320. Google Scholar


H. H. Taylor and E. W. Taylor . 1992. Gills and lungs: the exchange of gases and ions. In “Microscopic Anatomy of Invertebrates Vol 10”. Ed by F. W. Harrison and A. G. Humes . Wiley-Liss. New York. pp. 103–293. Google Scholar


I. P. Zanders and W. E. Rojas . 1996. Osmotic and ionic regulation in the fiddler crab Uca rapax acclimated to dilute and hypersaline sea-water. Mar Biol 125:315–320. Google Scholar
Hui-Chen Lin, Yong-Chao Su, and Shan-Hui Su "A Comparative Study of Osmoregulation in Four Fiddler Crabs (Ocypodidae: Uca)," Zoological Science 19(6), 643-650, (1 June 2002).
Received: 26 December 2001; Accepted: 1 April 2002; Published: 1 June 2002

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