Anion uptake and acid-base and ionic effects during isolated and combined exposure to hypercapnia and nitrite in the freshwater crayfish, Astacus astacus

Nitrite influx into crayfish showed saturation kinetics, supporting a carrier-mediated uptake. Addition of 4,4′-diisothiocyanatostilbene-2,2′-disulfonate (DIDS: at 10⁻⁵, 10⁻⁴ and 10⁻³M) and bumetanide (at 10⁻⁵ M and 10⁻⁴ M) to the ambient water did not significantly affect nitrite influx. Rather than suggesting that neither Cl⁻/HCO₃ ⁻ exchange nor K⁺/Na⁺/2Cl⁻ cotransport were involved in the transport, this may reflect that the gill cuticle has a low permeability to the pharmacological agents, or that the sensitivity of the transport mechanism to the inhibitors is low. Nitrite accumulation in the haemolymph was significantly decreased during hypercapnic conditions compared to normocapnic conditions. This supports the idea that an acid–base regulatory decrease in Cl⁻(influx)/HCO₃ ⁻ (efflux) induced by hypercapnia should decrease NO₂ ⁻ uptake if NO₂ ⁻ and Cl⁻ share this uptake route. The respiratory acidosis caused by exposure to hypercapnia alone was partially compensated by HCO₃ ⁻ accumulation in the haemolymph. Combined exposure to hypercapnia and nitrite improved pH recovery, mainly by augmenting the [HCO₃ ⁻] increase, but also by decreasing haemolymph PCO₂. Exposure to nitrite in normocapnic water induced an initial increase in haemolymph [HCO₃ ⁻] and later also a decrease in PCO₂. Thus, the improved acid-base compensation during combined hypercapnia and nitrite exposure was an amplification of this nitriteinduced response. Haemolymph base excess rose much more than haemolymph [Ca], suggesting that transfer of acid-base equivalents between animal and water was more important than H⁺ buffering by exoskeletal CaCO₃ in mediating the increase in haemolymph [HCO₃ ⁻]. Accepted: 27 June 2000     

Coral calcification responds to seawater acidification: a working hypothesis towards a physiological mechanism

The decrease in the saturation state of seawater, Ω, following seawater acidification, is believed to be the main factor leading to a decrease in the calcification of marine organisms. To provide a physiological explanation for this phenomenon, the effect of seawater acidification was studied on the calcification and photosynthesis of the scleractinian tropical coral Stylophora pistillata. Coral nubbins were incubated for 8 days at three different pH (7.6, 8.0, and 8.2). To differentiate between the effects of the various components of the carbonate chemistry (pH, CO₃²⁻, HCO₃⁻, CO₂, Ω), tanks were also maintained under similar pH, but with 2-mM HCO₃⁻ added to the seawater. The addition of 2-mM bicarbonate significantly increased the photosynthesis in S. pistillata, suggesting carbon-limited conditions. Conversely, photosynthesis was insensitive to changes in pH and pCO₂. Seawater acidification decreased coral calcification by ca. 0.1-mg CaCO₃ g⁻¹ d⁻¹ for a decrease of 0.1 pH units. This correlation suggested that seawater acidification affected coral calcification by decreasing the availability of the CO₃²⁻ substrate for calcification. However, the decrease in coral calcification could also be attributed either to a decrease in extra- or intracellular pH or to a change in the buffering capacity of the medium, impairing supply of CO₃²⁻ from HCO₃⁻.     

Acquisition of Ca2+ and HCO3 −/CO3 2− for shell formation in embryos of the common pond snail Lymnaea stagnalis

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.     

The impact of seawater saturation state and bicarbonate ion concentration on calcification by new recruits of two Atlantic corals

Rising concentrations of atmospheric CO₂ are changing the carbonate chemistry of the oceans, a process known as ocean acidification (OA). Absorption of this CO₂ by the surface oceans is increasing the amount of total dissolved inorganic carbon (DIC) and bicarbonate ion (HCO₃ ⁻) available for marine calcification yet is simultaneously lowering the seawater pH and carbonate ion concentration ([CO₃ ²⁻]), and thus the saturation state of seawater with respect to aragonite (Ω_ar). We investigated the relative importance of [HCO₃ ⁻] versus [CO₃ ²⁻] for early calcification by new recruits (primary polyps settled from zooxanthellate larvae) of two tropical coral species, Favia fragum and Porites astreoides. The polyps were reared over a range of Ω_ar values, which were manipulated by both acid-addition at constant pCO₂ (decreased total [HCO₃ ⁻] and [CO₃ ²⁻]) and by pCO₂ elevation at constant alkalinity (increased [HCO₃ ⁻], decreased [CO₃ ²⁻]). Calcification after 2 weeks was quantified by weighing the complete skeleton (corallite) accreted by each polyp over the course of the experiment. Both species exhibited the same negative response to decreasing [CO₃ ²⁻] whether Ω_ar was lowered by acid-addition or by pCO₂ elevation—calcification did not follow total DIC or [HCO₃ ⁻]. Nevertheless, the calcification response to decreasing [CO₃ ²⁻] was nonlinear. A statistically significant decrease in calcification was only detected between Ω_ar = <2.5 and Ω_ar = 1.1–1.5, where calcification of new recruits was reduced by 22–37% per 1.0 decrease in Ω_ar. Our results differ from many previous studies that report a linear coral calcification response to OA, and from those showing that calcification increases with increasing [HCO₃ ⁻]. Clearly, the coral calcification response to OA is variable and complex. A deeper understanding of the biomineralization mechanisms and environmental conditions underlying these variable responses is needed to support informed predictions about future OA impacts on corals and coral reefs.     

Deposition and cycling of carbon and nitrogen in carbonate mud of the lagoons of Arlington and Sudbury Reefs, Great Barrier Reef

The dynamics of carbon and nitrogen in carbonate mud were examined in the lagoons of Arlington and Sudbury Reefs, Great Barrier Reef. Most (89–93%) of the organic carbon and total nitrogen depositing to the carbonate mud zones was mineralized over a sediment depth of 1 m, with ∼50% of CO₂ produced during microbial decomposition involved in carbonate precipitation/dissolution reactions. There was proportionally little burial of organic carbon (10–11%) or nitrogen (7–10%). Nitrogen budgets suggest rapid turnover of porewater inorganic N pools on the order of hours to a few days. Incubation experiments indicate carbonate dissolution in surface deposits (≤20 cm depth) and carbonate precipitation in deeper sediments. Depth-integrated reaction rates indicate net carbonate precipitation of 7–10 mol CaCO₃ m² year⁻¹ over a depth of 1 m. Budget calculations at the whole-reef scale imply that deposition of CaCO₃ in the mud zones of both lagoons may equate to 50–90% of total reef carbonate production, with organic carbon fluxes equating to nearly all net primary production on each reef. These biogeochemical estimates point to the functional importance of carbonate mud zones in the lagoons of the shelf reefs of the Great Barrier Reef.     

The long-term culture of the coccolithophore Pleurochrysis carterae (Haptophyta) in outdoor raceway ponds

The calcareous marine haptophyte algae, the coccolithophorids, are of global environmental significance because of the impact of their blooms on the carbon cycle. The coccolithophorid, Pleurochrysis carterae was grown semi-continuously in paddlewheel-driven outdoor raceway ponds over a period of 13 months in Perth, Western Australia. The mean total dry weight productivity of P. carterae was 0.19 g.L⁻¹.d⁻¹ with cell lipid and CaCO₃ contents of up to 33% and 10% of dry weight respectively, equivalent to an annual total biomass productivity of about 60 t.ha⁻¹.y⁻¹ and 21.9 t.ha⁻¹.y⁻¹ total lipid and 5.5 t.ha⁻¹.y⁻¹ total calcium carbonate production. Throughout the culture period there was little protozoan contamination or contamination by other algae. The pH of the growth medium increased to pH 11 during the day and was found to be a useful variable for monitoring the state of the culture. A comparison of the growth of P. carterae and Dunaliella salina in the raceway ponds showed no significant differences between these two species with regard to areal total dry weight productivity and lipid content.     

Calcium carbonate budgets for two coral reefs affected by different terrestrial runoff regimes, Rio Bueno, Jamaica

A process-based carbonate budget was used to compare carbonate framework production at two reef sites subject to varying degrees of fluvial influence in Rio Bueno, Jamaica. The turbid, central embayment was subjected to high rates of fluvial sediment input, framework accretion was restricted to ≤30 m, and net carbonate production was 1,887 g CaCO₃ m⁻² year⁻¹. Gross carbonate production (GCP) was dominated by scleractinians (97%), particularly by sediment-resistant species, e.g. Diploria strigosa on the reef flat (<2 m). Calcareous encrusters contributed very little carbonate. Total bioerosion removed 265 g CaCO₃ m⁻² year⁻¹ and was dominated by microborers. At the clear-water site, net carbonate production was 1,236 g CaCO₃ m⁻² year⁻¹; the most productive zone was on the fore-reef (10 m). Corals accounted for 82% of GCP, and encrusting organisms 16%. Bioerosion removed 126 g CaCO₃ m⁻² year⁻¹ and was dominated by macroborers. Total fish and urchin grazing was limited throughout (≤20 g CaCO₃ m⁻² year⁻¹). The study demonstrates that: (1) carbonate production and net reef accretion can occur where environmental conditions approach or exceed perceived threshold levels for coral survival; and (2) although live coral cover (and carbonate production rates) were reduced on reef-front sites along the North Jamaican coast, low population densities of grazing fish and echinoids to some extent offset this, thus maintaining positive carbonate budgets.     

External HCO3 − dehydration maintained by acid zones in the plasma membrane is an important component of the photosynthetic carbon uptake in Ruppia cirrhosa

Ruppia cirrhosa, a temperate seagrass growing in brackish water, featured a high capacity for HCO₃ ⁻ utilisation, which could operate over a wide pH range (from 7.5 up to 9.5) with maintained efficiency. Tris buffer inhibited this means of HCO₃ ⁻ utilisation in a competitive manner, while addition of acetazolamide, an inhibitor of extracellular carbonic anhydrase activity, caused a 40–50% inhibition. A mechanism involving periplasmic carbonic anhydrase-catalysed HCO₃ ⁻ dehydration in acid zones, followed by a (probably diffusive) transport of the formed CO₂ across the plasma membrane was thus, at least partly, responsible for the HCO₃ ⁻ utilisation. This mechanism, which comprises a CO₂-concentrating mechanism (CCM) associated with the plasma membrane, is thus shown for the first time in an aquatic angiosperm. Additional mechanisms involved in the Tris-sensitive HCO₃ ⁻ utilisation could be direct HCO₃ ⁻ uptake (e.g., in an H⁺/HCO₃ ⁻symport) or (more likely) non-catalysed HCO₃ ⁻ dehydration in the acid zones. Based on these results, and on earlier investigations on Zostera marina, a general model for analysis of HCO₃ ⁻ utilisation mechanisms of seagrasses is suggested. In this model, three `systems' for HCO₃ ⁻ utilisation are defined which are characterised (and can to some extent be quantified) by their capability to operate at high pH in combination with their response to acetazolamide and Tris. Some consequences of the fact that HCO₃ ⁻ utilisation and osmoregulation probably depend on the same energy source (ATP via H⁺-ATPase in the plasma membrane) are discussed. This revised version was published online in August 2006 with corrections to the Cover Date.     

Bicarbonate,the most important factor inducing iron chlorosis in vine grapes on calcareous soil

Summary In pot experiments grape vine was grown on a calcareous and on a non calcareous soil with a low and with a high water saturation. During the growing period soil solution samples were collected and analyzed for their pH and for HCO ₃ ⁻ , phosphate, Fe, and Ca. High water saturation resulted in a pH increase and in an increase of the HCO ₃ ⁻ concentration in both soils. The level in pH and HCO ₃ ⁻ , however, was much higher in the calcareous soil than in the non calcareous soil. The Fe concentration varied much throughout the experimental period, but there was no major differences between soils and water saturation treatments. The Ca concentration of the soil solution increased with time in the calcareous soil; for the non calcareous soil rather the reverse was true. The phosphate level in the soil solution of the non calcareous soil was about 10 times higher than in the calcareous soil. After 3 weeks growth all plants of the calcareous soil with the high water saturation showed first symptoms of Fe deficiency. These became more intense from day to day. Plants of the other treatments did not show any chlorotic symptoms. In the treatment with the chlorotic plants the HCO ₃ ⁻ concentration of the soil solution was the highest, the phosphate concentration the lowest from all treatments. It is therefore concluded that HCO ₃ ⁻ and not phosphate is the primary cause for lime induced Fe chlorosis. Despite the low phosphate concentration in the soil solution, the P concentration in the chlorotic leaves was more than twice as high as the P concentration in green leaves grown on the same soil. It is thus assumed that the high P content frequently found in chlorotic leaves is the result and not the cause for Fe chlorosis.     

Bioerosion caused by foraging of the tropical chiton Acanthopleura gemmata at One Tree Reef, southern Great Barrier Reef

The bioerosive potential of the intertidal chiton Acanthopleura gemmata on One Tree Reef was determined by quantification of CaCO₃ in daily faecal pellet production of individuals transplanted into mesocosms after nocturnal-feeding forays. Mean bioerosive potential was estimated at 0.16 kg CaCO₃ chiton⁻¹ yr⁻¹. Bioerosion rates were estimated for populations on two distinct chiton habitats, reef margin (0.013 kg CaCO₃ m⁻² yr⁻¹) and beachrock platform (0.25 kg CaCO₃ m⁻² yr⁻¹). Chiton density on the platform was orders of magnitude greater than on the reef margin. The surface-lowering rate (0.16 mm m⁻² yr) due to bioerosion by the beachrock population is a substantial contribution to the total surface-lowering rate of 2 mm m⁻² yr⁻¹ previously reported for One Tree Reef across all erosive agents. At high densities, the contribution of A. gemmata to coral reef bioerosion budgets may be comparable to other important bioeroders such as echinoids and fish.     

The cationic composition and pH in the moulting fluid of Porcellio scaber (Crustacea, Isopoda) during calcium carbonate deposit formation and resorption

Before moulting, terrestrial isopods resorb calcium carbonate (CaCO₃) from the posterior cuticle and store it in sternal deposits. These consist mainly of amorphous calcium carbonate (ACC) spherules that develop within the ecdysial space between the anterior sternal epithelium and the old cuticle. Ions that occur in the moulting fluid, including those required for mineral deposition, are transported from the hemolymph into the ecdysial space by the anterior sternal epithelial cells. The cationic composition of the moulting fluid probably affects mineral deposition and may provide information on the ion-transport activity of the sternal epithelial cells. This study presents the concentrations of inorganic cations within the moulting fluid of the anterior sternites during the late premoult and intramoult stages. The most abundant cation is Na⁺ followed by Mg²⁺, Ca²⁺ and K⁺. The concentrations of these ions do not change significantly between the stages whereas the mean pH changed from 8.2 to 6.9 units between mineral deposition in late premoult, and resorption in intramoult, respectively. Measurements of the transepithelial potential show that there is little driving force for passive movements of calcium across the anterior sternal epithelium. The results suggest a possible role of magnesium ions in ACC formation, and a contribution of pH changes to CaCO₃ precipitation and dissolution.     

Biomass, carbonate standing stock and production of the mediterranean coralCladocora caespitosa (L.)

Summary The Mediterranean coralCladocora caespitosa often occurs in large beds, i.e. populations of hemispherical clonies with stock densities varying between 1.9 and 4 coloneis ·m⁻². Laboratory measurements of volume, skeleton weight, surface and number of corallites per colony, coupled with mean annual growth rates evaluated through sclerochronology, allowed for the estimation of biomass, skeleton bulk density, calcimass (carbonate standing stock) and secondary production (both organic and inorganic) of twoC. caespitosa beds at 4 and 9 m depth. The mean colony biomass varied between 0.73 and 0.99 kg dw ·m⁻², corresponding to a calcimass between 2 and 5 kg CaCO₃·m⁻². Organic secondary production was 215.5–305.4 g dw of polyps ·m⁻²·y⁻¹, while the potential (mineral) production was 1.1–1.7 kg CaCO₃·m⁻²·y⁻¹, for the year 1996–1997. These values show thatC. caespitosa is one of the major carbonate producers within the Mediterranean and one of the major epibenthic species originating stable carbonate frameworks both in recent and past times.     

Carbonate precipitates and bicarbonate secretion in the intestine of sea bass, <Emphasis Type="Italic">Dicentrarchus labrax</Emphasis>

The aim of this paper was to study the chemical composition of the precipitates found in the intestine of Dicentrarchus labrax and the source of HCO₃ ⁻ secreted into the intestinal lumen. The chemical analysis was performed by employing the potentiometric double titration method and by means of an electron microscope coupled with a spectrometer and X-ray powder diffraction. The results obtained suggest the presence of very insoluble intestinal precipitates, presumably formed by a mixture of CaCO₃ and MgCO₃, with a higher quantity of the former with respect to the latter. HCO₃ ⁻ secretion rate was investigated with the aid of the pH stat method in isolated tissues mounted in Ussing chamber, where the transepithelial electrical parameters were also measured. When the serosal surface of the intestinal mucosa was bathed in HCO₃ ⁻-Ringer bubbled with 1% CO₂ in O₂ while the serosal surface was bathed in HCO₃ ⁻ free Ringer solution bubbled with pure O₂, bicarbonate secretion proceeded at an almost stable rate of 0.9 ± 0.05 μeq cm⁻² h⁻¹ for about 3 h while I _sc maintained a constant value of 38 ± 1.5 μA cm⁻². The carbonic anhydrase inhibitor ethoxyzolamide elicited a progressive reduction of HCO₃ ⁻ secretion that was about 75% of the initial value after 80 min. When serosal HCO₃ ⁻–CO₂ saline was substituted with Hepes–O₂ saline base secretion progressively declined reaching a value of about 20% of the initial value. It was also strongly inhibited when Na⁺ was substituted with the impermeant cation choline and when either DIDS or ouabain were added to the basolateral side. These results suggest that most of the bicarbonate secreted is of extracellular source and is probably transported across the basolateral membrane by both Na⁺ independent mechanism and Na⁺ dependent transporter, presumably a NaHCO₃ cotransport.     

Effect of high rates of sulphur on the CaCO3 and CaSO4 content of calcareous soils

Samples of two calcareous soils from central Iraq were amended with 2, 6 and 10 mg g⁻¹ soil of agriculturegrade sulphur and incubated for 4, 8 and 12 weeks at 30°C and 70% water-holding capacity. At the end of each incubation period, soils were analyzed for sulphate, CaCO₃ and CaSO₄. The sulphate content of the soils increased, whereas the CaCO₃ content decreased, with increasing S levels and incubation time. The gypsum formed was in proportion to the sulphur oxidised and the calcium released from CaCO₃.     

The role of external carbonic anhydrase in the photosynthetic use of inorganic carbon in the deep-water alga Phyllariopsis purpurascens (Laminariales, Phaeophyta)

Mechanisms of inorganic carbon assimilation were investigated in the deep-water alga Phyllariopsis purpurascens (C. Agardh) Henry et South (Laminariales, Phaeophyta). The gross photosynthetic rate as a function of external pH, at a constant concentration of 2 mM dissolved inorganic carbon (DIC), decreased sharply from pH 7.0 to 9.0, and was not substantially different from 0 above pH 9.0. These data indicate that P. purpurascens is inefficient in the use of external HCO₃ ⁻ as a carbon source in photosynthesis. Moreover, the photosynthetic rate as a function of external DIC and the highest pH (9.01 ± 0.07) that this species can achieve in a closed system were consistent with a low capacity to use HCO₃ ⁻, in comparison to many other species of seaweeds. The role of external carbonic anhydrase (CA; EC 4.2.1.1) on carbon uptake was investigated by measuring both the HCO₃ ⁻-dependent O₂ evolution and the CO₂ uptake, at pH 5.5 and 8.0, and the rate of pH change in the external medium, in the presence of selected inhibitors of extra- and intracellular CA. Photosynthetic DIC-dependent O₂ evolution was higher at pH 5.5 (where CO₂ is the predominant form of DIC) than at pH 8.0 (where the predominant chemical species is HCO₃ ⁻). Both intra- and extracellular CA activity was detected. Dextran-bound sulfonamide (DBS; a specific inhibitor of extracellular CA) reduced the photosynthetic O₂ evolution and CO₂ uptake at pH 8.0, but there was no effect at pH 5.5. The pH-change rate of the medium, under saturating irradiance, was reduced by DBS. Phyllariopsis purpurascens has a low efficiency in the use of HCO₃ ⁻ as carbon source in photosynthesis; nevertheless, the ion can be used after dehydration, in the external medium, catalyzed by extracellular CA. This mechanism could explain why the photosynthetic rate in situ was higher than that supported solely by the diffusion of CO₂ from seawater. Received: 6 March 1998 / Accepted: 22 June 1998     

Control of Cell pH in the T84 Colon Cell Line

Cell pH regulation was investigated in the T84 cell line derived from epithelial colon cancer. Cell pH was measured by ratiometric fluorescence microscopy using the fluorescent probe BCECF. Basal pH was 7.17 ± 0.023 (n= 48) in HEPES Ringer. After acidification by an ammonium pulse, cell pH recovered toward normal at a rate of 0.13 ± 0.011 pH units/min in the presence of Na⁺, but in the absence of this ion or after treatment with 0.1 mm hexamethylene amiloride (HMA) no significant recovery was observed, indicating absence of Na⁺ independent H⁺ transport mechanisms in HEPES Ringer. In CO₂/HCO⁻ ₃ Ringer, basal cell pH was 7.21 ± 0.020 (n= 35). Changing to HEPES Ringer, a marked alkalinization was observed due to loss of CO₂, followed by return to the initial pH at a rate of −0.14 ± 0.012 (n= 8) pH/min; this return was retarded or abolished in the absence of Cl⁻ or after addition of 0.2 mm DIDS, suggesting extrusion of bicarbonate by Cl⁻/HCO⁻ ₃ exchange. This exchange was not Na⁺ dependent. When Na⁺ was added to cells incubated in 0 Na⁺ Ringer while blocking Na⁺/H⁺ exchange by HMA, cell alkalinization by 0.19 ± 0.04 (n= 11) pH units was observed, suggesting the presence of Na⁺/HCO⁻ ₃ cotransport carrying HCO⁻ ₃ into these cells, which was abolished by DIDS. These experiments, thus, show that Na⁺/H⁺ and Cl⁻/HCO⁻ ₃ exchange and Na⁺/HCO⁻ ₃ cotransport participate in cell pH regulation in T84 cells. Received: 3 April 2000/Revised: 22 June 2000     

A Mathematical Model of the Pancreatic Ductal Epithelium

A mathematical model of the HCO⁻ ₃-secreting pancreatic ductal epithelium was developed using network thermodynamics. With a minimal set of assumptions, the model accurately reproduced the experimentally measured membrane potentials, voltage divider ratio, transepithelial resistance and short-circuit current of nonstimulated ducts that were microperfused and bathed with a CO₂/HCO⁻ ₃-free, HEPES-buffered solution, and also the intracellular pH of duct cells bathed in a CO₂/HCO⁻ ₃-buffered solution. The model also accurately simulated: (i) the effect of step changes in basolateral K⁺ concentration, and the effect of K⁺ channel blockers on basolateral membrane potential; (ii) the intracellular acidification caused by a Na⁺-free extracellular solution and the effect of amiloride on this acidification; and (iii) the intracellular alkalinization caused by a Cl⁻-free extracellular solution and the effect of DIDS on this alkalinization. In addition, the model predicted that the luminal Cl⁻ conductance plays a key role in controlling both the HCO⁻ ₃ secretory rate and intracellular pH during HCO⁻ ₃ secretion. We believe that the model will be helpful in the analysis of experimental data and improve our understanding of HCO⁻ ₃-transporting mechanisms in pancreatic duct cells. Received: 18 October 1995/Revised: 5 July 1996     

Mineral composition and growth of Colorado spruce (Picea pungens) seedlings under calcareous soil conditions

Summary Field studies were conducted to assess the mineral nutrition and growth of Colorado spruce (Picea pungens Engln) seedlings (2–4 yr) from provenances selected for superior growth on calcareous prairie soils. Tissue nutrient concentrations and response to nitrogen were determined by use of foliar analysis and growth pattern studies. Soil conditions ranged from 7.6–7.8 for pH, 12–23% for total CaCO₃, and 5–6% for active CaCO₃. Foliage mineral composition showed relatively low phosphorus (0.09–0.15%) and high calcium (0.45–1.52%) assimilation. Seasonal growth and seedling response to added nitrogen was not adversely affected by the calcareous soil condition. Levels of nitrogen in the foliage required for optimum growth ranged from 1.5–2.0% and were similar to that of other conifer species.     

Mechanisms of inorganic carbon acquisition in Gracilaria gaditana nom. prov. (Rhodophyta)

The mechanisms for acquisition of dissolved inorganic carbon (DIC) in the red macroalga Gracilaria gaditana nom. prov. have been investigated. The capacity for HCO₃ ⁻ use by an extracellular carbonic anhydrase (CA; EC 4.2.1.1), and by an anion exchanger with similar properties to that of red blood cells (AE1), has been quantified. It was illustrated by comparing O₂ evolution rates with those theoretically supported by CO₂, as well as by photosynthesis-pH curves. Both external and internal CA, and a direct uptake were involved in HCO₃ ⁻ use, since photosynthesis and pH evolution were affected by acetazolamide, 6-ethoxyzolamide (inhibitors of external and total CA, respectively) and 4,4′-diisothiocyanatostilbene-2,2′-disulfonate, (DIDS; an inhibitor of HCO₃ ⁻ exchanger protein). The activity of the external CA was detected by a potentiometric method and by an alternative method based on the study of O₂ evolution after addition of CO₂ and acetazolamide. The latter method showed a residual photosynthetic rate due to direct HCO₃ ⁻ use. Inhibitors caused a reduction in the pH compensation points in pH-drift experiments. The CO₂ compensation points for photosynthesis increased when the inhibitors were applied, indicating a suppresion of the pathways involved in the carbon-concentrating mechanism. The net photosynthesis rates as a function of DIC concentration displayed a biphasic pattern that could be supported by the occurrence of the two mechanisms of HCO₃ ⁻ use. The potential contribution to HCO₃ ⁻ acquisition by the DIDS-sensitive mechanism was higher after culturing at a high pH. Our results suggest that the HCO₃ ⁻ use by Gracilaria gaditana is carried out by the two DIC uptake mechanisms. These operate simultaneously with different affinities for DIC, the indirect HCO₃ ⁻ use by an external CA activity being the main pathway. The presence of a carbon-concentrating mechanism confers eco-physiological advantages in a fluctuating ecosystem subjected daily to high pHs and low DIC concentrations. Received: 3 July 1998 / Accepted: 30 November 1998     

Intracellular pH regulation and buffer capacity in CO2/HCO− 3-buffered media in cultured epithelial cells from rainbow trout gills

The influence of a CO₂/HCO⁻ ₃-buffered medium on intracellular pH regulation of gill pavement cells from freshwater rainbow trout was examined in monolayers grown in primary culture on glass coverslips; intracellular pH (pH_i) was monitored by continuous spectrofluorometric recording from cells loaded with 2′,7′-bis(2-carboxyethyl)-5(6)-carboxy-fluoroscein. When cells in HEPES-buffered medium at normal pH=7.70 were transferred to normal CO₂/HCO⁻ ₃-buffered medium {P _CO2=3.71 mmHg, [HCO⁻ ₃]= 6.1 mmol l⁻¹, extracellular pH (pH_e)=7.70}, they exhibited a brief acidosis but subsequently regulated the same pHi (∼7.41) as in HEPES. Buffer capacity (β) increased by the expected amount (5.5–8.0 slykes) based on intracellular [HCO⁻ ₃], and was unaffected by most drugs and treatments. However, after transfer to high P _CO2=11.15 mmHg, [HCO⁻ ₃]= 18.2 mmol l⁻¹ at the same pH_e=7.70, the final regulated pHi was elevated (∼7.53). The rate of correction of alkalosis caused by washout of this high P _CO2, high-HCO⁻ ₃ medium was unaffected by removal of extracellular Cl⁻. Removal of extracellular Na⁺ lowered resting pH_i and greatly inhibited the rate of pH_i recovery from acidosis. Bafilomycin A₁ (3 μmol l⁻¹) had no effect on these responses. However amiloride (0.2 mmol l⁻¹) inhibited recovery from acidosis caused by washout of an ammonia prepulse, but did not affect resting pH_i, the latter differing from the response in HEPES where amiloride also lowered resting pH_i. Similarly 4-acetamido-4′- isothiocyanatostilbene-2,2′-disulfonic acid, sodium salt (0.1 mmol l⁻¹) did not affect resting pH_i but slowed the rate of recovery from acidosis, though to a lesser extent than amiloride. Removal of extracellular Cl⁻ also slowed the rate of recovery but greatly increased β by an unknown mechanism; when this was taken into account, H⁺ extrusion rate was unaffected. These results are consistent with the presence of Na⁺-(HCO⁻ ₃)_N co-transport and/or Na⁺-dependent HCO⁻ ₃/Cl⁻ exchange, in addition to Na⁺/H⁺ exchange, as mechanisms contributing to “housekeeping” pH_i regulation in gill cells in CO₂/HCO⁻ ₃ media, whereas only Na⁺/H⁺ exchange is seen in HEPES. Both Na⁺-independent Cl⁻/HCO⁻ ₃ exchange and V-type H⁺-ATPase mechanisms appear to be absent from these cells cultured in isotonic media. Accepted: 30 November 1999