Exchange of oxygen between solvent H 2 O and the CO 2 produced in Cypridina bioluminescence

Bioluminescent oxidation of $\text{Cypridina}$ luciferin yields CO₂ besides oxyluciferin and light. The exchange of oxygen between the CO₂ and H₂O of the solvent becomes significant when less than approximately 1 μmol of luciferin is reacted in 4 ml of buffer solution, and the exchanged oxygen in CO₂ markedly increases by decreasing the amount of luciferin. Such an exchange is to be expected in any such system which produces CO₂ in aqueous solution, and must be taken into account in interpreting the results of experiments.     

Use of 14C-carboxyl-luciferin in determining the mechanism of the firefly luciferase catalyzed reactions

The use of ¹⁴C-carboxyl-labelled luciferin as a substrate for the firefly luciferase catalyzed reaction produces ¹⁴CO₂ as a product. We have studied this reaction in the presence of ¹⁷O₂ and H¹⁸OH, using an excess of luciferin over luciferase. The initial collection of CO₂ contained close to one oxygen from ¹⁷O₂ for each molecule of ¹⁴CO₂ derived from luciferin, which is consistent with a cyclic peroxide mechanism. About half of the ¹⁴CO₂ remained bound to the enzyme and was collected after acidification of the medium. This CO₂ contained less than 0.1 of an atom of oxygen from ¹⁷O₂ for each molecule of ¹⁴CO₂ derived from luciferin. Exchange of medium CO₂-HCO₃ su? with water was not sufficiently great to account for the loss of any ¹⁷O previously incorporated. The most likely explanation appears to be a preferential exchange of oxygens of enzyme-bound CO₂ with water oxygens. Such exchange, and dilution of CO₂ from luciferin by medium CO₂, may explain previous results in which little incorporation of atmospheric oxygen was noted.     

cAMP mediated decrease in membrane phosphorylation.

Mass spectral analyses of the CO₂ liberated in the $\text{Cypridina}$ luciferin-luciferase and firefly luciferin-luciferase reactions run in the presence of ¹⁷O₂ and H₂¹⁸O show that the product is predominantly C¹⁸O¹⁶O (mass 46) and not C¹⁷O¹⁶O (mass 45). Incorporation of ¹⁸O into medium CO₂ by exchange does not account for the observed results. These experiments provide evidence that the $\text{Cypridina}$ and firefly bioluminescence reactions proceed via a linear peroxide mechanism rather than the dioxetane mechanism and suggest that a common mechanism may underly many bioluminescence reactions.     

ON THE QUANTA OF LIGHT PRODUCED AND THE MOLECULES OF OXYGEN UTILIZED DURING CYPRIDINA LUMINESCENCE

A study of the oxygen consumed per lumen of luminescence during oxidation of Cypridina luciferin in presence of luciferase, gives 11.4 x 10^–5 gm. oxygen per lumen or 88 molecules per quantum of λ = 0.48µ, the maximum in the Cypridina luminescence spectrum. For reasons given in the text, the actual value is probably somewhat less than this, perhaps of the order of 6.48 x 10^–5 gm. per lumen or 50 molecules of oxygen and 100 molecules of luciferin per quantum. It is quite certain that more than 1 molecule per quantum must react. On the basis of a reaction of the type: luciferin + 1/2 O₂ = oxyluciferin + H₂O + 54 Cal., it is calculated that the total efficiency of the luminescent process, energy in luminescence/heat of reaction, is about 1 per cent; and that a luciferin solution containing 4 per cent of dried Cypridina material should rise in temperature about 0.001°C. during luminescence, and contain luciferin in approximately 0.00002 molecular concentration.     

Mechanism of the enzyme-catalyzed bioluminescent oxidation of coelenterate-type luciferin.

The use of a fully active, synthetic analogue of coelenterate-type luciferin labeled in the carbonyl position with ¹⁴C and ¹⁸O was used to probe the mechanism of the $\text{Renilla}$ luciferase catalyzed oxidative decarboxylation of this compound. In the presence of ¹⁷O₂, the CO₂ produced in this oxidation can be shown to contain approximately one ¹⁷O atom per CO₂ molecule. This result is consistent with a cyclic peroxide or dioxetanone-type mechanism. In the presence of luciferase, the oxygen in the luciferin carbonyl group is rapidly exchanged with solvent water prior to the production of CO₂. Thus, the $\text{reaction}$ CO₂ contains considerable oxygen derived from water, via exchange with the carbonyl group, and about one oxygen from O₂ via a cyclic peroxide.     

Sodium azide as a specific quencher of singlet oxygen during chemiluminescent detection by luminol and Cypridina luciferin analogues

Reactive oxygen species (ROS) are presently thought to play important role in an increasing number of the physiological and pathological processes in living organisms. Various chemiluminescent (CL) compounds have been studied in order to find suitable and specific probes for the detection of particular ROS species. The CL of luminol is known to be non‐specific and can be induced by various oxidants. Two Cypridina luciferin analogues, CLA and MCLA, have been used for the detection of ROS in vivo. CLAs are thought to emit light only when reacting with superoxide and singlet oxygen. It is possible to distinguish the particular ROS by using a specific quencher or scavenger, e.g. superoxide dismutase (SOD) or sodium azide (NaN₃). The CL reactions of luminol (3‐aminophthalhydrazide), CLA [2‐methyl‐6‐phenyl‐3,7‐dihydroimidazo(1,2α) pyrazin‐3‐one] and MCLA [2‐methyl‐6‐(p‐methoxyphenyl)‐3,7‐dihydroimidazo(1,2α) pyrazin‐3‐one] were studied in three hydrogen peroxide decomposition systems (H₂O₂–HRP; H₂O₂–CuSO₄; and H₂O₂–NaOCl). The measurements were carried out in phosphate buffer, pH 7.4, at 25 °C, using a luminometer (Fluoroskan Ascent FL and Sirius C). NaN₃ was used as the specific quencher of singlet oxygen. The results demonstrate that the proclaimed specifity of the CL of Cypridina luciferin analogues towards singlet oxygen has to be discussed. Copyright © 2011 John Wiley & Sons, Ltd.     

The CO2 permeability of the plasma membrane of Chlamydomonas reinhardtii: mass-spectrometric 18O-exchange measurements from 13C18O2 in suspensions of carbonic anhydrase-loaded plasma-membrane vesicles

The unicellular green alga Chlamydomonas reinhardtii possesses a CO₂-concentrating mechanism. In order to measure the CO₂ permeability coefficients of the plasma membranes (PMs), carbonic anhydrase (CA) loaded vesicles were isolated from C. reinhardtii grown either in air enriched with 50 mL CO₂ · L?1} (high-C_i cells) or in ambient air (350 μL CO₂ · L?1}; low-C_i cells). Marker-enzyme measurements indicated less than 1% contamination with thylakoid and mitochondrial membranes, and that more than 90% of the PMs from high and low-C_i cells were orientated right-side-out. The PMs appeared to be sealed as judged from the ability of vesicles to accumulate [¹⁴C]acetate along a proton gradient for at least 10 min. Carbonic anhydrase-loaded PMs from high and low-C_i cells of C. reinhardtii were used to measure the exchange of ¹⁸O between doubly labelled CO₂ (¹³C¹⁸O₂) and H₂O in stirred suspensions by mass spectrometry. Analysis of the kinetics of the ¹⁸O depletion from ¹³C¹⁸O₂ in the external medium provides a powerful tool to study CO₂ diffusion across the PM to the active site of CA which catalyses ¹⁸O exchange only inside the vesicles but not in the external medium (Silverman et al., 1976, J Biol Chem 251: 4428–4435). The activity of CA within loaded PM vesicles was sufficient to speed-up the ¹⁸O loss to H₂O to 45360–128800 times the uncatalysed rate, depending on the efficiency of CA-loading and PM isolation. From the ¹⁸O-depletion kinetics performed at pH 7.3 and 7.8, CO₂ permeability coefficients of 0.76 and 1.49·10?3} cm·s?1}, respectively, were calculated for high C_i cells. The corresponding values for low-C_i cells were 1.21 and 1.8·10?3} cm·s?1}. The implications of the similar and rather high CO₂ permeability coefficients (low CO₂ resistance) in high and low-C_i cells for the CO_i-concentrating mechanism of C. reinhardtii are discussed.     

Enzymatic preparation of carboxyl oxygen-18 labeled prostaglandin F2α and utility for quantitative mass spectrometry

A nonspecific liver esterase was found to not only catalyze the hydrolysis of the methyl ester of prostaglandin F2α (PGF2α) but also to catalyze the exchange of the carboxyl oxygen atoms with water leading to the production of [¹⁸O₂]PGF2α when the enzymatic hydrolysis is carried out in H₂¹⁸O. The kinetics of this oxygen-18 exchange reaction are briefly discussed. The [¹⁸O₂]PGF2α was found to be relative stable toward back exchange in methanol, aqueous buffer, and urine, but rapidly back exchanged to the native PGF2α in plasma with a half-life of 1 h. The [¹⁸O₂]PGF2α was relatively stable in plasma to which alcohol had been added. The utility of the oxygen-18 labeled prostaglandin as an internal standard in a gas chromatography-mass spectrometry assay was demonstrated at the picomole range.     

Evidence for 18O labeling of photorespiratory CO2 in photoautotrophic cell cultures of higher plants illuminated in the presence of 18O2

The ¹⁸O-enrichment of CO₂ produced in the light or during the post-illumination burst was measured by mass spectrometry when a photoautotrophic cell suspension of Euphorbia characias L. was placed in photorespiratory conditions in the presence of molecular ¹⁸O₂. The only ¹⁸O-labeled species produced was C¹⁸O¹⁶O; no C¹⁸O¹⁸O could be detected. Production of C¹⁸O¹⁶O ceased after addition of two inhibitors of the photosynthetic carbon-oxidation cycle, aminooxyacetate or aminoacetonitrile, and was inhibited by high levels of CO₂. The average enrichment during the post-illumination burst was estimated to be 46 ± 15% of the enrichment of the O₂ present during the preceding light period. Addition of exogenous carbonic anhydrase, by catalyzing the exchange between CO₂ and H₂O, drastically diminished the ¹⁸O-enrichment of the produced CO₂. The very low carbonio-anhydrase level of the photoautotrophic cell suspension probably explains why the ¹⁸O labeling of photorespiratory CO₂ could be observed for the first time. These data allow the establishment of a direct link between O₂ consumption and CO₂ production in the light, and the conclusion that CO₂ produced in the light results, at least partially, from the mitochondrial decarboxylation of the glycine pool synthesized through the photosynthetic carbon-oxidation cycle. Analysis of the C¹⁸O¹⁶O and CO₂ kinetics provides a direct and reliable way to assess in vivo the real contribution of photorespiratory metabolism to CO₂ production in the light.     

The Human Enzyme That Converts Dietary Provitamin A Carotenoids to Vitamin A Is a Dioxygenase

β-Carotene 15–15′-oxygenase (BCO1) catalyzes the oxidative cleavage of dietary provitamin A carotenoids to retinal (vitamin A aldehyde). Aldehydes readily exchange their carbonyl oxygen with water, making oxygen labeling experiments challenging. BCO1 has been thought to be a monooxygenase, incorporating oxygen from O₂ and H₂O into its cleavage products. This was based on a study that used conditions that favored oxygen exchange with water. We incubated purified recombinant human BCO1 and β-carotene in either ¹⁶O₂-H₂¹⁸O or ¹⁸O₂-H₂¹⁶O medium for 15 min at 37 °C, and the relative amounts of ¹⁸O-retinal and ¹⁶O-retinal were measured by liquid chromatography-tandem mass spectrometry. At least 79% of the retinal produced by the reaction has the same oxygen isotope as the O₂ gas used. Together with the data from ¹⁸O-retinal-H₂¹⁶O and ¹⁶O-retinal-H₂¹⁸O incubations to account for nonenzymatic oxygen exchange, our results show that BCO1 incorporates only oxygen from O₂ into retinal. Thus, BCO1 is a dioxygenase.     

Fate of oxygen species from O2 activation at dimetal cofactors in an oxidase enzyme revealed by 57Fe nuclear resonance X-ray scattering and quantum chemistry

Oxygen (O₂) activation is a central challenge in chemistry and catalyzed at prototypic dimetal cofactors in biological enzymes with diverse functions. Analysis of intermediates is required to elucidate the reaction paths of reductive O₂ cleavage. An oxidase protein from the bacterium Geobacillus kaustophilus, R2lox, was used for aerobic in-vitro reconstitution with only ⁵⁷Fe(II) or Mn(II) plus ⁵⁷Fe(II) ions to yield [FeFe] or [MnFe] cofactors under various oxygen and solvent isotopic conditions including ^16/18O and H/D exchange. ⁵⁷Fe-specific X-ray scattering techniques were employed to collect nuclear forward scattering (NFS) and nuclear resonance vibrational spectroscopy (NRVS) data of the R2lox proteins. NFS revealed Fe/Mn(III)Fe(III) cofactor states and Mössbauer quadrupole splitting energies. Quantum chemical calculations of NRVS spectra assigned molecular structures, vibrational modes, and protonation patterns of the cofactors, featuring a terminal water (H₂O) bound at iron or manganese in site 1 and a metal-bridging hydroxide (μOH⁻) ligand. A procedure for quantitation and correlation of experimental and computational NRVS difference signals due to isotope labeling was developed. This approach revealed that the protons of the ligands as well as the terminal water at the R2lox cofactors exchange with the bulk solvent whereas ¹⁸O from ¹⁸O₂ cleavage is incorporated in the hydroxide bridge. In R2lox, the two water molecules from four-electron O₂ reduction are released in a two-step reaction to the solvent. These results establish combined NRVS and QM/MM for tracking of iron-based oxygen activation in biological and chemical catalysts and clarify the reductive O₂ cleavage route in an enzyme.     

Influence of vegetation and soil CO2 exchange on the concentration and stable oxygen isotope ratio of atmospheric CO2 within a Pinus resinosa canopy

Measurements were made of the concentration and stable oxygen isotopic ratio of carbon dioxide in air samples collected on a diurnal basis at two heights within a Pinus resinosa canopy. Large changes in CO₂ concentration and isotopic composition were observed during diurnal time courses on all three symple dates. In addition, there was strong vertical stratification in the forest canopy, with higher CO₂ concentrations and more negative ¹⁸O values observed closer to the soil surface. The observed daily increases in ¹⁸O values of forest CO₂ were dependent on relative humidity consistent with the modelled predictions of isotopic fractionation during photosynthetic gas exchange. During photosynthetic gas exchange, a portion of the CO₂ that enters the leaf and equilibrates with leaf water is not fixed and diffuses back out of the leaf with an altered oxygen isotopic ratio. The oxygen isotope ratio of CO₂ diffusing out of a leaf depends primarily on the ¹⁸O content of leaf water which changes in response to relative humidity. In contrast, soil respiration caused a decline in the ¹⁸O values of forest CO₂ at night, because CO₂ released from the soil has equilibrated with soil water which has a lower ¹⁸O content than leaf water. The observed relationship between diurnal changes in CO₂ concentration and oxygen isotopic composition in the forest environment were consistent with a gas mixing model that considered the relative magnitudes of CO₂ fluxes associated with photosynthesis, respiration and turbulent exchange between the forest and the bulk atmosphere.     

Determination of horserdish peroxidase concentration using the chemiluminescence of Cypridina luciferin analogue, 2 methyl-6-(p-methyoxyphenyl)-3,7-dihydroimidazo[1,2-a]pyrazin-3-one

The chemiluminescence of the Cypridina luciferin analogue, 2-methyl-6-(p-methoxyphenyl)-3,7-dihydroimidazo[1,2-a]pyrazin-3-one (MCLA) was observed at 462nm in the presence of horseradish peroxidase (HRP) and the total spectrum of light emitted was found to depend linearly on HRP concentration. Methods for the determination of HRP concentration using the chemiluminescence was investigated. HRP could be detected in the range from 100 pmol/L to 100nmol/L under the optimum condition, H₂O₂ (10mmol/L) and MCLA (10μmol/L) at pH 5.8.     

Heme-Dependent Rubber Oxygenase RoxA of Xanthomonas sp. Cleaves the Carbon Backbone of Poly(cis-1,4-Isoprene) by a Dioxygenase Mechanism

Oxidative cleavage of poly(cis-1,4-isoprene) by rubber oxygenase RoxA purified from Xanthomonas sp. was investigated in the presence of different combinations of ¹⁶O₂, ¹⁸O₂, H₂¹⁶O, and H₂¹⁸O. 12-Oxo-4,8-dimethyl-trideca-4,8-diene-1-al (ODTD; m/z 236) was the main cleavage product in the absence of ¹⁸O-compounds. Incorporation of one ¹⁸O atom in ODTD was found if the cleavage reaction was performed in the presence of ¹⁸O₂ and H₂¹⁶O. Incubation of poly(cis-1,4-isoprene) (with RoxA) or of isolated unlabeled ODTD (without RoxA) with H₂¹⁸O in the presence of ¹⁶O₂ indicated that the carbonyl oxygen atoms of ODTD significantly exchanged with oxygen atoms derived from water. The isotope exchange was avoided by simultaneous enzymatic reduction of both carbonyl functions of ODTD to the corresponding dialcohol (12-hydroxy-4,8-dimethyl-trideca-4,8-diene-1-ol (HDTD; m/z 240) during RoxA-mediated in vitro cleavage of poly(cis-1,4-isoprene). In the presence of ¹⁸O₂, H₂¹⁶O, and alcohol dehydrogenase/NADH, incorporation of two atoms of ¹⁸O into the reduced metabolite HDTD was found (m/z 244), revealing that RoxA cleaves rubber by a dioxygenase mechanism. Based on the labeling results and the presence of two hemes in RoxA, a model of the enzymatic cleavage mechanism of poly(cis-1,4-isoprene) is proposed.     

Evaporation and carbonic anhydrase activity recorded in oxygen isotope signatures of net CO2 fluxes from a Mediterranean soil

The oxygen stable isotope composition (δ¹⁸O) of CO₂ is a valuable tool for studying the gas exchange between terrestrial ecosystems and the atmosphere. In the soil, it records the isotopic signal of water pools subjected to precipitation and evaporation events. The δ¹⁸O of the surface soil net CO₂ flux is dominated by the physical processes of diffusion of CO₂ into and out of the soil and the chemical reactions during CO₂–H₂O equilibration. Catalytic reactions by the enzyme carbonic anhydrase, reducing CO₂ hydration times, have been proposed recently to explain field observations of the δ¹⁸O signatures of net soil CO₂ fluxes. How important these catalytic reactions are for accurately predicting large‐scale biosphere fluxes and partitioning net ecosystem fluxes is currently uncertain because of the lack of field data. In this study, we determined the δ¹⁸O signatures of net soil CO₂ fluxes from soil chamber measurements in a Mediterranean forest. Over the 3 days of measurements, the observed δ¹⁸O signatures of net soil CO₂ fluxes became progressively enriched with a well‐characterized diurnal cycle. Model simulations indicated that the δ¹⁸O signatures recorded the interplay of two effects: (1) progressive enrichment of water in the upper soil by evaporation, and (2) catalytic acceleration of the isotopic exchange between CO₂ and soil water, amplifying the contributions of ‘atmospheric invasion’ to net signatures. We conclude that there is a need for better understanding of the role of enzymatic reactions, and hence soil biology, in determining the contributions of soil fluxes to oxygen isotope signals in atmospheric CO₂.     

Two-tier vessel for photoautotrophic high-density cultures

Two-tier vessels, developed for culturing of microalgae and cyanobacteria at high cell density on a shaken platform, were assembled from a flat lower chamber to be filled with a CO₂ buffer and an upper flat sterile chamber for the culture that was separated from the lower chamber by a porous polypropylene membrane. Diffusive gas exchange with the atmosphere was controlled by the O₂ outlet channel. Referred to surface area, rates of CO₂ transfer to a shaken weakly alkaline buffer solution across the membrane were higher than those reached on the conventional pathway through the free upper liquid surface. Membrane-mediated CO₂ supply enabled rapid growth of Synechocystis sp. PCC 6803 and Synechococcus sp. PCC 7002 up to ultrahigh cell density. The biomass (dry weight) concentration of Synechococcus cultures reached more than 30 g L^?1 on a buffered medium with adequate concentrations of mineral nutrients. An increase of 15 to 20 g L^?1 was observed during repeated two-day cycles. Separate pathways for CO₂ supply and oxygen outlet prevented significant loss of CO₂. Convective gas flow through the oxygen outlet channel enabled the estimation of the O₂ generation rate. The permeability of the channel for diffusive O₂/N₂ exchange limited the O₂ concentration to a moderate value. It is concluded that shaken flat cultures using CO₂ supply through a porous hydrophobic membrane and diffusive release of O₂ through a separate pathway are promising for research on microalgae and cyanobacteria.     

18O Labeling of Chlorophyll d in Acaryochloris marina Reveals That Chlorophyll a and Molecular Oxygen Are Precursors

The cyanobacterium Acaryochloris marina was cultured in the presence of either H₂¹⁸O or ¹⁸O₂, and the newly synthesized chlorophylls (Chl a and Chl d) were isolated using high performance liquid chromatography and analyzed by mass spectroscopy. In the presence of H₂¹⁸O, newly synthesized Chl a and d, both incorporated up to four isotopic ¹⁸O atoms. Time course H₂¹⁸O labeling experiments showed incorporation of isotopic ¹⁸O atoms originating from H₂¹⁸O into Chl a, with over 90% of Chl a ¹⁸O-labeled at 48 h. The incorporation of isotopic ¹⁸O atoms into Chl d upon incubation in H₂¹⁸O was slower compared with Chl a with ∼50% ¹⁸O-labeled Chl d at 115 h. The rapid turnover of newly synthesized Chl a suggested that Chl a is the direct biosynthetic precursor of Chl d. In the presence of ¹⁸O₂ gas, one isotopic ¹⁸O atom was incorporated into Chl a with approximately the same kinetic incorporation rate observed in the H₂¹⁸O labeling experiment, reaching over 90% labeling intensity at 48 h. The incorporation of two isotopic ¹⁸O atoms derived from molecular oxygen (¹⁸O₂) was observed in the extracted Chl d, and the percentage of double isotopic ¹⁸O-labeled Chl d increased in parallel with the decrease of non-isotopic-labeled Chl d. This clearly indicated that the oxygen atom in the C3¹-formyl group of Chl d is derived from dioxygen via an oxygenase-type reaction mechanism.     

Lack of photosynthetic or stomatal regulation after 9 years of elevated [CO2] and 4 years of soil warming in two conifer species at the alpine treeline

Alpine treelines are temperature‐limited vegetation boundaries. Understanding the effects of elevated [CO₂] and warming on CO₂ and H₂O gas exchange may help predict responses of treelines to global change. We measured needle gas exchange of Larix decidua Mill. and Pinus mugo ssp. uncinata DC trees after 9 years of free air CO₂ enrichment (575 µmol mol^?1) and 4 years of soil warming (+4 °C) and analysed δ¹³C and δ¹⁸O values of needles and tree rings. Tree needles under elevated [CO₂] showed neither nitrogen limitation nor end‐product inhibition, and no down‐regulation of maximal photosynthetic rate (A_max) was found. Both tree species showed increased net photosynthetic rates (A_n) under elevated [CO₂] (L. decidua: +39%; P. mugo: +35%). Stomatal conductance (g_H2O) was insensitive to changes in [CO₂], thus transpiration rates remained unchanged and intrinsic water‐use efficiency (iWUE) increased due to higher A_n. Soil warming affected neither A_n nor g_H2O. Unresponsiveness of g_H2O to [CO₂] and warming was confirmed by δ¹⁸O needle and tree ring values. Consequently, under sufficient water supply, elevated [CO₂] induced sustained enhancement in A_n and lead to increased C inputs into this ecosystem, while soil warming hardly affected gas exchange of L. decidua and P. mugo at the alpine treeline.     

Trichothecene Biosynthesis in Fusarium sporotrichioides: Origin of the Oxygen Atoms of T-2 Toxin

Mass spectral analysis of T-2 toxin formed during the growth of Fusarium sporotrichioides (ATCC 24043) in the presence of H₂¹⁸O showed incorporation of up to three ¹⁸O atoms per toxin molecule. The carbonyl oxygens of the acetates at C-4 and C-15 and of the isovalerate at C-8 were derived from H₂O. Toxin formed in the presence of ¹⁸O molecular oxygen incorporated up to six ¹⁸O atoms per toxin molecule. The overall incorporation was 78 and 92% of toxin molecules labeled for H₂¹⁸O and ¹⁸O₂ labeled samples, respectively. The oxygens of position 1, the 12,13-epoxide, and the hydroxyl groups at C-3, C-4, C-8, and C-15 were all derived from molecular oxygen.     

Active transport of CO2 by three species of marine microalgae

The occurrence of an active CO₂ transport system and of carbonic anhydrase (CA) has been investigated by mass spectrometry in the marine, unicellular rhodophyte Porphyridium cruentum (S.F. Gray) Naegeli and two marine chlorophytes Nannochloris atomus Butcher and Nannochloris maculata Butcher. Illumination of darkened cells incubated with 100 μM H¹³CO₃^? caused a rapid initial drop, followed by a slower decline in the extracellular CO₂ concentration. Addition of bovine CA to the medium raised the CO₂ concentration by restoring the HCO₃^?–CO₂ equilibrium, indicating that cells were taking up CO₂ and were maintaining the CO₂ concentration in the medium below its equilibrium value during photosynthesis. Darkening the cell suspensions caused a rapid increase in the extracellular CO₂ concentration in all three species, indicating that the cells had accumulated an internal pool of unfixed inorganic carbon. CA activity was detected by monitoring the rate of exchange of ¹⁸O from ¹³C¹⁸O₂ into water. Exchange of ¹⁸O was rapid in darkened cell suspensions, but was not inhibited by 500 μM acetazolamide, a membrane‐impermeable inhibitor of CA, indicating that external CA activity was not present in any of these species. In all three species, the rate of exchange was completely inhibited by 500 μM ethoxyzolamide, a membrane‐permeable CA‐inhibitor, showing that an intracellular CA was present. These results demonstrate that the three species are capable of CO₂ uptake by active transport for use as a carbon source for photosynthesis.