Studies on chitin and calcification in the inner layers of the shell of Anodonta cygnea

Summary An orthorhombic structure -chitin, probably in the form of a chitin-protein complex, was identified in the matrix of the shell of Anodonta cygnea by X-ray diffraction. Aragonite crystals of pseudohexagonal symmetry were also found by a Lauegram on the nacreous layer of the shell. The orthorhombic structure of these two compounds together with the identical reticular spacing d₁₁₀ corroborate, in Anodonta cygnea, the indirect chitin-aragonite relationships already suggested for molluscan shells.Observations with SEM in the inner surface of the shell showed CaCO₃ crystals with irregular geometrical shapes in spring and summer and regular geometrical shapes in autumn and winter. The more elaborate aspect appearing in winter corresponds to an accurate hexagonal shape. This suggests that the observed variability may depend on the balance between calcium and hydrogen ions in the extrapallial fluid.Abbreviations OME outer mantle epithelium - SEM scanning electron microscopy     

Characterization of a Monoclonal Antibody Directed against Mytilus spp Larvae Reveals an Antigen Involved in Shell Biomineralization

The M22.8 monoclonal antibody (mAb) developed against an antigen expressed at the mussel larval and postlarval stages of Mytilus galloprovincialis was studied on adult samples. Antigenic characterization by Western blot showed that the antigen MSP22.8 has a restricted distribution that includes mantle edge tissue, extrapallial fluid, extrapallial fluid hemocytes, and the shell organic matrix of adult samples. Other tissues such as central mantle, gonadal tissue, digestive gland, labial palps, foot, and byssal retractor muscle did not express the antigen. Immunohistochemistry assays identified MSP22.8 in cells located in the outer fold epithelium of the mantle edge up to the pallial line. Flow cytometry analysis showed that hemocytes from the extrapallial fluid also contain the antigen intracellularly. Furthermore, hemocytes from hemolymph have the ability to internalize the antigen when exposed to a cell-free extrapallial fluid solution. Our findings indicate that hemocytes could play an important role in the biomineralization process and, as a consequence, they have been included in a model of shell formation. This is the first report concerning a protein secreted by the mantle edge into the extrapallial space and how it becomes part of the shell matrix framework in M. galloprovincialis mussels.     

Gas exchange and blood gases of Puna teal (Anas versicolor puna) embryos in the Peruvian Andes

Oxygen consumption, air cell gases, hematology, blood gases and pH of Puna teal (Anas versicolor puna) embryos were measured at the altitude at which the eggs were laid (4150 m) in the Peruvian Andes. In contrast to the metabolic depression described by other studies on avian embryos incubated above 3700 m, O₂ consumption of Puna teal embryos was higher than even that of some lowland avian embryos at equivalent body masses. Air cell O₂ tensions dropped from about 80 toor in eggs with small embryos to about 45 toor in eggs containing a 14-g embryo; simultaneously air cell CO₂ tension rose from virtually negligible amounts to around 26 torr. Arterial and venous O₂ tensions (32–38 and 10–12 toor, respectively, in 12- to 14-g embryos) were lower than described previously in similarly-sized lowland wild avian embryos or chicken embryos incubated in shells with restricted gas exchange. The difference between air cell and arterial O₂ tensions dropped significantly during incubation to a minimum of 11 torr, the lowest value recorded in any avian egg. Blood pH (mean 7.49) did not vary significantly during incubation. Hemoglobin concentration and hematocrits rose steadily throughout incubation to 11.5 g · 100 ml^-1 and 39.9%, respectively, in 14-g embryos.Abbreviations PO₂ partial pressure gradient of O₂ - BM body mass - D diffusion coefficient - G gas conductance (cm³·s^-1·torr^-1) - conductance to water vapor - IP internal pipping of embryos - P _ACO₂ partial pressure of carbon dioxide in air cell - P _AO₂ partial pressure of oxygen in air cell - P _aCO₂ partial pressure of carbon dioxide in arterial blood - P _aCO₂ partial pressure of oxygen in arteries - P _H barometric pressure (torr) - PCO₂ partial pressure of carbon dioxide - P _IO₂ partial pressure in ambiant air - PO₂ partial pressure of oxygen - P _VCO₂ venous carbon dioxide partial pressure - P _VO₂ mixed venous oxygen partial pressure - SE standard error - VO ₂ oxygen consumption     

Morphological studies on the mantle of the fresh-water mussel Amblema (UNIONIDAE): Scanning electron microscopy

The scanning electron microscope has been used to describe the surface morphology of the mantle in mantle-shell preparations from the fresh-water mussel Amblema. In some regions (adductor muscle insertions), the mantle is firmly attached to the shell. In other areas (along the main course of the mantle), transient adhesions between the outer mantle epithelial cells and the nacre appear to temporally further compartmentalize the extrapallial fluid possibly as a prerequisite for the initial crystallization phenomenon. At the mantle edge, as well as at the isthmus, the periostracum was seen to extrude from the periostracal groove. At the siphonal edge, peculiar fingerlike processes were identified; these may represent primitive photoreceptors. The epithelial cells of the outer mantle epithelium are all microvillated whereas those of the inner mantle epithelium are both microvillated and ciliated. Specific differences in surface morphology are described for various regions of the outer mantle epithelium. These may be related to precise regionalized functional differences of this tissue. Several functions of the mantle, in addition to shell formation, and based on its various morphologies, are also discussed.     

Decalcification at the Mantle-Shell Interface in Molluscs

Decalcification at the mantle-shell interface in Mercenariatnercenaria was studied through the changes in the chemicalcomposition of the extrapallial fluid, and by the measurementof Ca⁴⁵-deposition and solution. Measurements of O₂-tensiondemonstrated that the clam was anaerobic soon after the valveswere closed. Measurements of calcium, carbon dioxide, and hydrogenion concentration showed that all of these components of theextrapallial fluid increase with increasing time of closure.These measurements, and measurements of calcium and succinicacid in the tissues and fluids of the clam, indicated thatsuccinicacid produced by the anaerobic metabolism of the clam was neutralizedby the dissolution of previously deposited shell.     

Zona Localization of Shell Matrix Proteins in Mantle of <Emphasis Type="Italic">Haliotis tuberculata</Emphasis> (Mollusca,Gastropoda)

Organic matrix from molluscan shells has the potential to regulate calcium carbonate deposition and crystallization. Control of crystal growth thus seems to depend on control of matrix protein secretion or activation processes in the mantle cells, about which little is known. Biomineralization is a highly orchestrated biological process. The aim of this work was to provide information about the source of shell matrix macromolecule production, within the external epithelium of the mantle. An in vivo approach was chosen to describe the histologic changes in the outer epithelium and in blood sinus distribution, associated with mantle cells implicated in shell matrix production. Our results characterized a topographic and time-dependent zonation of matrix proteins involved in shell biomineralization in the mantle of Haliotis.     

Cationic responses of organs and haemolymph of Biomphalaria pfeifferi (Krauss), Biomphalaria glabrata (Say) and Helisoma trivolvis (Say) (Gastropoda: Planorbirdae) to cationic alterations of the medium

The cationic responses of haemolymph, mantle collar, headfoot, gut + digestive diverticulum and ovotestis + albumin gland of three planorbids to cationic changes in the media are explored. Body organs exhibited cationic homeostasis, although attained with difficulty under very low Ca : Mg and Ca : Na ratios. Haemolymph imbalances were obtained at very low calcium concentrations and at very low Ca : Mg and Ca : Na ratios in the medium; this may be linked to competition for Ca²⁺ uptake sites in the epithelium by Mg²⁺ and possibly Na⁺ ions.Fecundity and shell growth in relation to calcium concentrations and to Ca : Mg and Ca : Na ratios are examined.Normal internal cationic levels, under optimal conditions, were obtained for each species. Significant interspecific differences for haemolymph sodium were found; magnesium levels were slightly higher in Biomphalaria spp. than in Helisoma trivolvis; potassium levels were all similar. Amounts of tissue calcium decreased as follows: Mantle collar head-foot ovotestis + albumin gland-gut + diverticulum. Tissue magnesium levels in the gut were low. H. trivolvis had highest tissue calcium and sodium; B. glabrata had highest tissue potassium.     

Amorphous Calcium Carbonate Precipitation by Cellular Biomineralization in Mantle Cell Cultures of Pinctada fucata

The growth of molluscan shell crystals is generally thought to be initiated from the extrapallial fluid by matrix proteins, however, the cellular mechanisms of shell formation pathway remain unknown. Here, we first report amorphous calcium carbonate (ACC) precipitation by cellular biomineralization in primary mantle cell cultures of Pinctada fucata. Through real-time PCR and western blot analyses, we demonstrate that mantle cells retain the ability to synthesize and secrete ACCBP, Pif80 and nacrein in vitro. In addition, the cells also maintained high levels of alkaline phosphatase and carbonic anhydrase activity, enzymes responsible for shell formation. On the basis of polarized light microscopy and scanning electron microscopy, we observed intracellular crystals production by mantle cells in vitro. Fourier transform infrared spectroscopy and X-ray diffraction analyses revealed the crystals to be ACC, and de novo biomineralization was confirmed by following the incorporation of Sr into calcium carbonate. Our results demonstrate the ability of mantle cells to perform fundamental biomineralization processes via amorphous calcium carbonate, and these cells may be directly involved in pearl oyster shell formation.     

Effects of bafilomycin A1 and amiloride on the apical potassium and proton gradients in Drosophila Malpighian tubules studied by X-ray microanalysis and microelectrode measurements

The intracellular distribution of potassium in Malpighian tubules from Drosophila larva was measured by electron probe X-ray microanalysis of freeze-dried cryosections. Application of amiloride alone to the haemolymph space had no effect on the intracellular potassium concentration in the region of intermediate cytoplasm (between the basal region of basal membrane infoldings and the apical brush border), whereas a potassium increase as well as a chloride increase was observed after simultaneous blocking of the potassium conductance of the basal membrane with barium. Injected bafilomycin and amiloride applied in the haemolymph caused an increase of the potassium content in the basal cytoplasm but not in the microvilli. In addition, the intracellular water portion was decreased by bafilomycin. pH measurements in isolated larval anterior tubules with proton-selective microelectrodes showed that bafilomycin added to the bathing solution caused a decrease in intracellular pH. Addition of amiloride had no significant effect on intracellular pH, but the pH of the luminal fluid was decreased within 1 min by 0.5 pH units. The amiloride-induced luminal pH decrease could be inhibited by the metabolic blocker KCN as well as by bafilomycin. Furthermore, removing potassium from the bathing saline caused a slow luminal acidification, which could be blocked by KCN. Our results support the hypothesis of a functionally coupled transport system in the apical membrane consisting of a bafilomycin-sensitive V-ATPase and a K⁺-dependent, amiloride-sensitive K⁺/H⁺ exchange system.Abbreviation C _a element concentration related to water - C _d element content related to dry weight - dw dry weight - DMSO dimethylsulphoxide - emf electromotive force - NBD-Cl 7-chloro-4-nitrobenz-2-oxa-1,3-diazole - NEM N-ethylmaleimide - NMDG⁺ N-methyl-d-glucamine - PD potential difference - pH_i intracellular pH value - pH_lu luminal pH value - pmf protonmotive force - SD standard deviation - SE standard error - STEM scanning transmission electron microscopy - V _a apical potential difference - V _b basal potential difference - V _t transepithelial potential difference     

Arterial blood pressure during voluntary diving in the tufted duck,Aythya fuligula

Arterial blood pressure was monitored in voluntarily diving tufted ducks. Mean arterial blood pressure while diving increased during the pre-dive tachycardia, fell to resting levels on submersion, then gradually increased before peaking on surfacing. Estimated total peripheral resistance fell during the pre-dive and post-dive tachycardia, presumably to allow the oxygen stores to be loaded and replenished respectively and/or for carbon dioxide levels to be reduced. Changes in mean arterial blood pressure and total peripheral resistance suggest that peripheral vasoconstriction occurs in some vascular beds during a dive. An increase in arterial blood pressure (and therefore perfusion pressure) may be employed to increase blood flow and oxygen delivery to the active leg muscles.Abbreviations ecg Electrocardiogram, f _H, heart rate - MABP mean arterial blood pressure - P _b blood pressure(s) - TPR total peripheral resistance - V _b cardiac output     

Aerial and Aquatic Respiration in the River Crab Potamonautes Warreni Calman with Notes on Gill Structure

Summary

The oxygen consumption rate (?O₂) for Potamonauteus warreni Calman (= Potamon warreni (Calman) kept in 25 °C water was 34,4 μmol 1^?1 O₂ kg^?1 and after 72 hours in 98% R.H. air the rate was 31,9 μmol 1^?1 O₂ kg^?1 min^?1. The ?O₂ values for each of the two groups are not significantly different (P > 0,05). The partial oxygen tension of pre-branchial (v = venous) haemolymph (P_vCO₂) is 15,3 mm Hg in water and 13,0 mm Hg in air); partial carbon dioxide tension of pre-branchial (v) haemolymph (P_vCO₂) is 13,2 mm Hg in water and 13,0 mm Hg in air); the total carbon dioxide concentration in pre-branchial (v) haemolymph (C_vCO₂) tot. is 12,3 mmol 1^?1 in air and 13,9 mmol 1^?1 in water) are not significantly different for the two groups (P > 0,05). The haemolymph pH and the lactate concentration for crabs in water was found to be 7,51 and 0,38 mmol 1^?1 respectively. No significant differences were found in pre-branchial haemolymph oxygen tension, carbon dioxide tension, total carbon dioxide content, haemolymph pH, lactate level, chloride concentration, P₅₀ and haemocyanin-oxygen cooperativity in control crabs kept in water, and experimental crabs held in air for 72 hours. The chloride concentration, (327,0 mmol 1^?1) for crabs kept in water does not differ from that of crabs held in air for 72 hours but is at least 15% higher than the sodium concentration (255 mmol 1^?1) for crabs kept in water. The gill surface area is 520 mm² g^?1 wet body mass; on average 9,2 gill platelets (lamellae) can be found on a gill length of one millimetre. Each lamella is spaced 60–70 μm apart, each with a thickness of 30–40 μm. It is concluded that P. warreni may be described as a truly amphibious fresh-water crab.     

Seasonal variations of pH, pCO2, pO2, HCO3- and Ca2+ in the haemolymph: implications on the calcification physiology in Anodonta cygnea

A study about the relationship between the physical–chemical parameters and the calcium carbonate balance between the haemolymph fluid and mantle calcareous structures was carried out in Anodonta cygnea. An intense peak of HCO₃ ⁻ and a highest pH in December–January months may be understood as a preparation period for creating alkaline conditions. An intense pH decrease from January to February in parallel with the HCO₃ ⁻ reduction seems to indicate the beginning process of carbonate precipitation. On the other hand, the following calcium and HCO₃ ⁻ increases in February–May associated with a continuous and gradual pH fall profile may infer two combined aspects: calcium and HCO₃ ⁻ absorption from external environment and a simultaneous intense calcium carbonate deposition in the haemolymph. So, the pCO₂ peak in this period reflects a subsequent result on equilibrium balance between HCO₃ ⁻ absorption and deposition. The only significant pO₂ increase in the next period, from February to June, is related with an energetic increase to support the metabolic activity favouring the posterior intense pCO₂ peaks. The extended time of CO₂ production in the haemolymph from May to November should induce an increased metabolic acidosis with subsequent intense formation of both HCO₃ ⁻ and Ca²⁺ ions in the same period. This seems to result from CaCO₃ deposits dissolution in the haemolymph, the most direct calcareous source. Additionally, the later increase of metabolic succinic acid during autumn may greatly potentiate this acidosis increasing the dissolution process. Consequently, the pH profile present two simultaneous alkaline peaks in July and October, probably due to a strong HCO₃ ⁻ release from the CaCO₃ dissolution. So, the present seasonal results indicate that in the freshwater bivalve A. cygnea, the low metabolism with higher pH from the early winter is the main cause which may favour a calcareous precipitation, while the high metabolism with lower pH from the early summer may function as an inductor of calcareous dissolution in the haemolymph.     

Effectors of metabolic depression in an estivating pulmonate snail (Helix aspersa): whole animal and in vitro tissue studies

 We have examined metabolic depression in the land snail (Helix aspersa) during estivation, and have developed a tissue model of metabolic depression using an in vitro mantle preparation. The metabolic rate of H. aspersa is depressed by 84% in vivo within 4 weeks of onset of estivation, and this metabolic depression is accompanied by a decrease in haemolymph PO₂ and pH, and an increase in haemolymph PCO₂. The in vitro mantle preparation has a stable O₂ consumption and energy charge, and an energy charge similar to that of mantle in vivo. The in vitro mantle is an O₂-conforming tissue, with VO₂ varying curvilinearly with PO₂. Consequently, we have developed a mathematical method of calculating tissue VO₂ at any PO₂. These calculations show that under appropriate incubation conditions of pH and PO₂, the mantle from estivating animals shows a stable in vitro metabolic depression of 48% compared to mantle from control snails. The extrinsic effects of PO₂ and pH account for 70% of the total in vitro metabolic depression of mantle tissue; intrinsic effectors contribute a further 30%. Accepted April 26, 1996     

PO2 and pH changes in the retina of the crab Ocypode ryderi: evidence for aerobic glycolysis

Summary The isolated retina of the terrestrial crab Ocypode ryderi exhibits a pronounced lactate production in spite of being supplied with sufficient O₂ (140 torr). To determine whether this lactate production is caused by hypoxic areas in the tissue or represents aerobic glycolysis, oxygen partial pressure and pH measurements with two-channel glass microelectrodes and additional biochemical analyses were carried out on this organ. Distinct profiles were obtained for O₂ partial pressure and pH inside the tissue. At a depth of 200 m different O₂ partial pressure levels could be observed depending on the O₂ partial pressure in the medium (85 torr at 280 torr and 36 torr at 130 torr, respectively). The extracellular pH displays a similar pattern; it reaches a stable value of 7.15 at 100 m inside the tissue. Lowering bath O₂ partial pressure from 280 torr to about 15 torr (hypoxia) induces a decrease of the O₂ partial pressure in the tissue with different time-courses for different tissue depths. However, hypoxia did not change the extracellular pH. Addition of antimycin A (100 mol · 1^-1) to the medium abolishes the O₂ partial pressure gradient and the delayed recovery of the tissue O₂ partial pressure after hypoxia. These results and the biochemical data suggest that in the crab retina a high glycolytic activity occurs simultaneously with oxydative carbohydrate degradation (aerobic glycolysis).Abbreviations AEC Atkinson energy charge - DC bioelectric potential - dw dry weight - HEPES N-[2-Hydroxyethyl]piperazine-N-[2-ethanesulphonic acid] - PCO₂ carbon dioxide partial pressure - PO₂ oxygen partial pressure - P _tO₂ oxygen partial pressure inside the tissue - P _mO₂ oxygen partial pressure in the medium - pH_t pH inside the tissue - pH_m pH in the superfusion medium     

Ionoregulatory and urinary responses to emersion in the mangrove crab Ucides cordatus and the intertidal crab Carcinus maenas

The mangrove crab Ucides cordatus showed a significant reduction in its output of isosmotic urine (to 60% of submerged rates) in humid, emersed conditions when in apparent water balance. A similar, but lesser, reduction was observed in the intertidal temperature species Carcinus maenas. Some of the decrease is effected by increased water withdrawal of an isosmotic fluid in the antennal gland (inulin urine to haemolymph concentration ratio=1.27) in Ucides but most is due to the reduced filtration rate which decreases from 3.41 to 2.19 ml·100 g^-1·day^-1 (in Carcinus from 7.37 to 5.88). In Carcinus, inulin urine to haemolymph concentration ratios are within the range 1.34–1.41 and show significant change on emersion. Comparisons of ion and inulin clearance ratios revealed interspecific differences in renal handling of Na⁺ and Cl^-. During emersion total Na⁺ efflux is markedly reduced in both species. Urinary Na⁺ losses are responsible for most of the efflux in Carcinus but represent only 50% of the total in Ucides. Significant Na⁺ uptake from interstitial water occurs in Ucides. REductions in ion and water loss appear to be mainly dependent on decreases in urine output (clearance rate). However, some released urine was found to accumulate in the branchial chambers in both species. Whether or not extrarenal reabsorption of ions from released urine occurs in the gill chambers in either crab species remains to be proved.Abbreviations CPM counts per minute - ECF extracellular fluid - k rate constant for inulin clearance - k ^Na rate constant for sodium efflux - J _out ^Na sodium efflux rate - Q _tot total radioactivity injected - SEM standard error of mean - SW sea water - 9-SW sea water, salinity 9 mg·ml^-1 (ppt) - 26-SW sea water, salinity 26 mg·ml^-1 (ppt) - U/B ratio of urine (U) to haemolymph (B) concentrations - V _c1 clearance rate - V _u urine output - V _a inulin space     

Light induces an increase in the pH of and a decrease in the ammonia concentration in the extrapallial fluid of the giant clam Tridacna squamosa

The objective of this study was to examine whether 12 h of light exposure would lead to an increase in the pH of and a decrease in the concentration of total ammonia in the extrapallial fluid of the giant clam Tridacna squamosa. We also aimed to elucidate indirectly whether movements of ammonia and/or protons (H(+)) occurred between the extrapallial fluid and the outer mantle epithelium. The pH of the extrapallial fluid of T. squamosa exposed to 12 h of light was significantly higher than that of clams exposed to 12 h of darkness. Conversely, the total ammonia concentration in the extrapallial fluid of the former was significantly lower than that of the latter. In addition, the glutamine content in the mantle adjacent to the extrapallial fluid of clams exposed to 12 h of light was significantly greater than that of clams exposed to 12 h of darkness. These results suggest that in the extrapallial fluid of T. squamosa exposed to light, NH(3) combined with H(+) as NH(+)(4) and that NH(+)(4) was transported into the mantle and used as a substrate for glutamine formation. Injection of NH(4)Cl into the extrapallial fluid led to an instantaneous increase in the total ammonia concentration therein, but the total ammonia concentration decreased subsequently and returned to the control value within 1 h. This is in support of the proposition that NH(+)(4) could be transported from the extrapallial fluid to the mantle. Injection of HCl into the extrapallial fluid led to an instantaneous decrease in the pH of the extrapallial fluid. However, there was a significant increase in pH within 1 h in light or darkness, achieving a partial recovery toward the control pH value. The increase in pH within this 1-h period in light or darkness was accompanied by a significant decrease in the total ammonia concentration in the extrapallial fluid, which supports the proposition that H(+) could be transported in combination with NH(3) as NH(+)(4). Therefore, our results prompt a reexamination of the previous proposition that the removal of H(+) by NH(3) can facilitate calcification in molluscs in general and an investigation of the relationship between H(+) removal through NH(+)(4) transport and light-enhanced calcification in T. squamosa.     

Haemocyte response associated with induction of shell regeneration in the deep-sea vent mussel Bathymodiolus azoricus (Bivalvia: Mytilidae)

This study reports on the haemocyte responses after induction of shell regeneration in the hydrothermal mussel Bathymodiolus azoricus. Haemolymph was drawn from live mussels collected at Menez Gwen hydrothermal vent site (850 m depth) at the Mid Atlantic Ridge (MAR) and was compared with those collected following laboratory acclimatisation (1 atm and Ca-rich algal diet) and also with induced specimen for up to 30 days. Simultaneously, histological changes in mantle micro-morphology with the histochemical detection of Ca mobilisation in tissues were conducted.On the basis of light- and transmission electron microscopy, it is concluded that the physiological equipment involved in shell regeneration in the deep sea bivalve closely resembles that in littoral mytilids, a group that B. azoricus is closely related. This in spite of previously alleged molecular and cellular adaptations to extreme conditions typical at deep sea hydrothermal vents. Three types of blood cells were identified sharing various morphological similarities with those in many non-vent bivalves. Significant increase in the number of circulating haemocytes was detected from day 5 after induction shell regeneration. It is suggested that the increase may be a result of migration of haemocytes from the connective tissue, probably to the shell growth frontline. It is alleged that a first peak in haemocyte number is a non-specific immune response related wound healing, which renders changes in the pallial fluid that are favourable for CaCO₃ deposition. The conspicuous presence of an unidentified, acid soluble, highly refractive structure in the haemolymph of induced mussels was detected, which may play a role in Ca nucleation.This study has set the stage for investigations underway on the influence of hydrostatic pressure on shell biomineralisation in B. azoricus subjected to post-capture hyperbaric simulations.     

Hemolymph oxygen content,oxyhemocyanin, protein levels and ammonia excretion in the shrimp Penaeus monodon exposed to ambient nitrite

Subadult Penaeus monodon (21.03±3.19 g) were exposed individually in sea water (30 mg·ml^-1) to 0.02 (control), 1.04, 5.02, 10.11 and 20.06 mg·l^-1 nitrite-N for 24h. Hemolymph pH, partial pressures of oxygen and carbon dioxide, bicarbonate concentration, oxyhemocyanin and protein levels, and whole animal ammonia-N excretion and nitrite-N uptake were determined. Ammonia-N excretion and hemolymph oxygen partial pressure increased, whereas hemolymph pH, HCO ₃ ^- , oxyhemocyanin, protein and the ratio of oxyhemocyanin/protein levels decreased with increasing ambient nitrite-N. It is suggested that accumulated nitrite of P. monodon following exposure to ambient nitrite causes reduction of oxyhemocyanin, protein and the ratio of oxyhemocyanin/protein in the hemolymph, and affects nitrogen metabolism and acid-base balance at low hemolymph pH.Abbreviations bw body weight - EC₅₀ concentration reducing growth rate by 50% that of controls - LC₅₀ median lethal concentration - nitrite-N nitrite concentration measured as nitrogen - PO₂ partial pressure of O₂ in hemolymph - PCO₂ partial pressure of CO₂ in hemolymph - sw sea water - ww wet weight     

Ventilatory responses to temperature variation in the fresh water turtle,Mauremys caspica leprosa

A study of lung gas exchange in the fresh water turtle Mauremys caspica leprosa at normal physiological body temperatures (15, 25 and 35 °C) was extended to extreme temperatures (5 and 40 °C) to determine whether the direct relationship between body temperature and ventilatory response found in many lung-breathing ectotherms including other chelonian species was maintained. From 5 to 35 °C the lung ventilation per unit of O₂ uptake and CO₂ removed declined with temperature. Consequently, lung CO₂ partial pressure increased with temperature. Its value was maintained within narrow limits at each thermal constant, suggesting a suitable control throughout the complete ventilatory cycle. At 40 °C the ventilatory response showed the opposite trend. The ratios of ventilation to lung gas exchange increased compared to their values at 35 °C. The impact of this increased breathing-lowering the estimated mean alveolar CO₂ partial pressure-was nevertheless less than expected due to an increase in calculated physiological dead space. This suggests that the relative hyperventilation in response to hyperthermia found in Mauremys caspica leprosa is related to evaporative heat loss.Abbreviations BTPS body temperature, ambient pressure, saturated with water vapour - CTM critical thermal maximum - F_N2 fractional concentration of nitrogen - PA _CO2or PL _CO2 alveolar or lung CO₂ pressure - PA_O2or PL_O2 alveolar or lung O₂ pressure - PI_O2 inspired O₂ pressure - R respiratory exchange ratio - STPD standard temperature, standard pressure, dry - T _a ambient temperature - T _b body temperature - VA alveolar ventilation - VA/VCO₂ relative alveolar ventilation (alveolar ventilation per unit of CO₂ removed) - VO₂ O₂ uptake - VCO₂ CO₂ output - V _D anatomical dead space volume - V _D physiological dead space volume - VE/VO₂ ventilatory equivalent for O₂ - VE pulmonary ventilation or expiratory minute volume - VE/VCO₂ ventilatory equivalent for CO₂ - V _T tidal volume