CO2/H(+) sensing: peripheral and central chemoreception

H(+) is maintained constant in the internal environment at a given body temperature independent of external environment according to Bernard's principle of "milieu interieur". But CO2 relates to ventilation and H(+) to kidney. Hence, the title of the chapter. In order to do this, sensors for H(+) in the internal environment are needed. The sensor-receptor is CO2/H(+) sensing. The sensor-receptor is coupled to integrate and to maintain the body's chemical environment at equilibrium. This chapter dwells on this theme of constancy of H(+) of the blood and of the other internal environments. [H(+)] is regulated jointly by respiratory and renal systems. The respiratory response to [H(+)] originates from the activities of two groups of chemoreceptors in two separate body fluid compartments: (A) carotid and aortic bodies which sense arterial P(O2) and H(+); and (B) the medullary H(+) receptors on the ventrolateral medulla of the central nervous system (CNS). The arterial chemoreceptors function to maintain arterial P(O2) and H(+) constant, and medullary H(+) receptors to maintain H(+) of the brain fluid constant. Any acute change of H(+) in these compartments is taken care of almost instantly by pulmonary ventilation, and slowly by the kidney. This general theme is considered in Section 1. The general principles involving cellular CO2 reactions mediated by carbonic anhydrase (CA), transport of CO2 and H(+) are described in Section 2. Since the rest of the chapter is dependent on these key mechanisms, they are given in detail, including the role of Jacobs-Stewart Cycle and its interaction with carbonic anhydrase. Also, this section deals briefly with the mechanisms of membrane depolarization of the chemoreceptor cells because this is one mechanism on which the responses depend. The metabolic impact of endogenous CO2 appears in the section with a historical twist, in the context of acclimatization to high altitude (Section 3). Because low P(O2) at high altitude stimulates the peripheral chemoreceptors (PC) increasing ventilation, the endogenous CO2 is blown off, making the internal milieu alkaline. With acclimatization however ventilation increases. This alkalinity is compensated in the course of time by the kidney and the acidity tends to be restored, but the acidification is not great enough to increase ventilation further. The question is what drives ventilation during acclimatization when the central pH is alkaline? The peripheral chemoreceptor came to the rescue. Its sensitivity to P(O2) is increased which continues to drive ventilation further during acclimatization at high altitude even when pH is alkaline. This link of CO2 through the O2 chemoreceptor is described in Section 4 which led to hypoxia-inducible factor (HIF-1). HIF-1 is stabilized during hypoxia, including the carotid body (CB) and brain cells, the seat of CO2 chemoreception. The cells are always hypoxic even at sea level. But how CO2 can affect the HIF-1 in the brain is considered in this section. CO2 sensing in the central chemoreceptors (CC) is given in Section 5. CO(2)/H(+) is sensed by the various structures in the central nervous system but its respiratory and cardiovascular responses are restricted only to some areas. How the membranes are depolarized by CO2 or how it works through Na(+)/Ca(2+) exchange are discussed in this section. It is obvious, however, that CO2 is not maintained constant, decreasing with altitude as alveolar P(O2) decreases and ventilation increases. Rather, it is the [H(+)] that the organism strives to maintain at the expense of CO2. But then again, [H(+)] where? Perhaps it is in the intracellular environment. Gap junctions in the carotid body and in the brain are ubiquitous. What functions they perform have been considered in Section 6. CO2 changes take place in lung alveoli where inspired air mixes with the CO2 from the returning venous blood. It is the interface between the inspired and expired air in the lungs where CO2 change is most dramatic. As a result, various investigators have looked for CO2 receptors in the lung, but none have been found in the mammals. Instead, CO2/H(+) receptors were found in birds and amphibians. However, they are inhibited by increasing CO2/H(+), instead of stimulated. But the afferent impulses transmitted to the brain produced stimulation in the efferents. This reversal of afferent-efferent inputs is a curious situation in nature, and this is considered in Section 7. The NO and CO effects on CO2 sensing are interesting and have been briefly mentioned in Section 8. A model for CO2/H(+) sensing by cells, neurons and bare nerve endings are also considered. These NO effects, models for CO2/H(+) and O2-sensitive cells in the CNS have been considered in the perspectives. Finally, in conclusion, the general theme of constancy of internal environment for CO2/H(+) is reiterated, and for that CO2/H(+) sensors-receptors systems are essential. Since CO2/H(+) sensing as such has not been reviewed before, the recent findings in addition to defining basic CO2/H(+) reactions in the cells have been briefly summarized.     

Carbon dioxide signalling in plant leaves

The role of carbon dioxide (CO(2)) as a signal in biochemical regulation networks of plants is fathomed. Transport mechanisms of CO(2) and HCO3- are surveyed, which are the prerequisite for signalling. A CO(2) sensor is not known to date, but any reaction where CO(2)/HCO3- is a substrate can be a candidate. Carbon concentrating mechanisms, e.g., in higher plants C(4)-photosynthesis and crassulacean acid metabolism (CAM), generate high internal CO(2) concentrations, important for photosynthesis, but also as a basis for signalling via diffusion of CO(2). Spatiotemporal dynamics of desynchronization/synchronization of photosynthetic activity over leaves can be followed by chlorophyll fluorescence imaging. One example of desynchronization is based on patchiness of stomatal opening/closing in heterobaric leaves due to anatomic constraints of lateral CO(2) diffusion. During CAM, largely different internal CO(2) concentrations prevail in the leaves, offering opportunities to study the effect of lateral diffusion of CO(2) in synchronizing photosynthetic activity over the entire leaves.     

Mechanisms underlying CO2 diffusion in leaves

Plants provide an excellent system to study CO(2) diffusion because, under light saturated conditions, photosynthesis is limited by CO(2) availability. Recent findings indicate that CO(2) diffusion in leaves can be variable in a short time range. Mesophyll CO(2) conductance could change independently from stomata movement or CO(2) fixing reactions and it was suggested that, beside others, the membranes are mesophyll CO(2) conductance limiting components. Specific aquaporins as membrane intrinsic pore proteins are considered to have a function in the modification of membrane CO(2) conductivity. Because of conflicting data, the mechanism of membrane CO(2) diffusion in plants and animals is a matter of a controversy vivid debate in the scientific community. On one hand, data from biophysics are in favor of CO(2) diffusion limiting mechanisms completely independent from membrane structure and membrane components. On the other, there is increasing evidence from physiology that a change in membrane composition has an effect on CO(2) diffusion.     

Temperature, oxygen, and salt-sensing neurons in C. elegans are carbon dioxide sensors that control avoidance behavior

Homeostatic control of body fluid CO(2) is essential in animals but is poorly understood. C.?elegans relies on diffusion for gas exchange and avoids environments with elevated CO(2). We show that C.?elegans temperature, O(2), and salt-sensing neurons are also CO(2) sensors mediating CO(2) avoidance. AFD thermosensors respond to increasing CO(2) by a fall and then rise in Ca(2+) and show a Ca(2+) spike when CO(2) decreases. BAG O(2) sensors and ASE salt sensors are both activated by CO(2) and remain tonically active while high CO(2) persists. CO(2)-evoked Ca(2+) responses in AFD and BAG neurons require cGMP-gated ion channels. Atypical soluble guanylate cyclases mediating O(2) responses also contribute to BAG CO(2) responses. AFD and BAG neurons together stimulate turning when CO(2) rises and inhibit turning when CO(2) falls. Our results show that C.?elegans senses CO(2) using functionally diverse sensory neurons acting homeostatically to minimize exposure to elevated CO(2).     

The physiological and behavioral effects of carbon dioxide on Drosophila melanogaster larvae

Adult and larval insects are rapidly anesthetized by carbon dioxide (CO2); however, the mechanisms have not been addressed. In this study, we use larval Drosophila to investigate the actions of CO2 to explain the behavioral effects of rapid immobilization and cardiac arrest with acute exposure to CO2. To determine if the central nervous system (CNS) is required, studies were performed with and without the CNS. The effects of low pH induced by exposure to CO2 were also examined. An acidic saline increases the heart rate in contrast to saline containing CO2. Synaptic transmission at the skeletal neuromuscular junction (NMJ) is blocked by CO2 but not by low pH. The site of action is postsynaptic by a decreased sensitivity to glutamate, the neurotransmitter at Drosophila NMJs. The CNS remains active in synaptic transmission when exposed to CO2 which is in contrast to the synapses at the NMJ. In summary, the effects of CO2 are directly mediated on the heart to stop it and at skeletal NMJs by a reduced sensitivity to glutamate, the released neurotransmitter, from the motor nerve terminals. The rapid behavioral and physiological effects cannot be accounted for by action on the CNS within the larvae nor by a pH effect indirectly induced by CO2. The glutamate receptors in the D. melanogaster preparation are similar in function to ionotropic glutamate receptors in vertebrates which could account for the observational phenomena of CO2 not yet explained mechanistically in vertebrates.     

Conditions leading to high CO2 (>5 kPa) in waterlogged-flooded soils and possible effects on root growth and metabolism

AIMS: Soil waterlogging impedes gas exchange with the atmosphere, resulting in low P(O2) and often high P(CO2). Conditions conducive to development of high P(CO2) (5-70 kPa) during soil waterlogging and flooding are discussed. The scant information on responses of roots to high P(CO2) in terms of growth and metabolism is reviewed. SCOPE: P(CO2) at 15-70 kPa has been reported for flooded paddy-field soils; however, even 15 kPa P(CO2) may not always be reached, e.g. when soil pH is above 7. Increases of P(CO2) in soils following waterlogging will develop much more slowly than decreases in P(O2); in soil from rice paddies in pots without plants, maxima in P(CO2) were reached after 2-3 weeks. There are no reliable data on P(CO2) in roots when in waterlogged or flooded soils. In rhizomes and internodes, P(CO2) sometimes reached 10 kPa, inferring even higher partial pressures in the roots, as a CO2 diffusion gradient will exist from the roots to the rhizomes and shoots. Preliminary modelling predicts that when P(CO2) is higher in a soil than in roots, P(CO2) in the roots would remain well below the P(CO2) in the soil, particularly when there is ventilation via a well-developed gas-space continuum from the roots to the atmosphere. The few available results on the effects of P(CO2) at > 5 kPa on growth have nearly all involved sudden increases to 10-100 kPa P(CO2); consequently, the results cannot be extrapolated with certainty to the much more gradual increases of P(CO2) in waterlogged soils. Nevertheless, rice in an anaerobic nutrient solution was tolerant to 50 kPa CO2 being suddenly imposed. By contrast, P(CO2) at 25 kPa retarded germination of some maize genotypes by 50%. With regard to metabolism, assuming that the usual pH of the cytoplasm of 7.5 was maintained, every increase of 10 kPa CO2 would result in an increase of 75-90 mM HCO3(-) in the cytoplasm. pH maintenance would depend on the biochemical and biophysical pH stats (i.e. regulatory systems). Furthermore, there are indications that metabolism is adversely affected when HCO3(-) in the cytoplasm rises above 50 mM, or even lower; succinic dehydrogenase and cytochrome oxidase are inhibited by HCO3(-) as low as 10 mM. Such effects could be mitigated by a decrease in the set point for the pH of the cytoplasm, thus lowering levels of HCO3(-) at the prevailing P(CO2) in the roots. CONCLUSIONS: Measurements are needed on P(CO2) in a range of soil types and in roots of diverse species, during waterlogging and flooding. Species well adapted to high P(CO2) in the root zone, such as rice and other wetland plants, thrive even when P(CO2) is well over 10 kPa; mechanisms of adaptation, or acclimatization, by these species need exploration.     

Mechanism of mitochondrial carbamoyl-phosphate synthetase: synthesis and properties of active CO2, precursor of carbamoyl phosphate.

This paper demonstrates the formation of "active CO2" (CO2-P), a precursor of carbamoyl phosphate (CP), with frog liver carbamoyl-phosphate synthetase. Absence of ammonia is essential for the demonstration by pulse incubation with H14CO3- of CO2-P. Adenosine triphosphate (ATP) and acetylglutamate are required for the synthesis of CO2-P, which is highly unstable in aqueous solutions (t1/2 = 0.75 s at 24 degrees C at neutral pH). In the absence of ammonia, CO2-P attains rapidly a steady-state level, which depends on the concentration of ATP and HCO3-. The "apparent KM'S" are approximately equal to those found for the adenosine triphosphate (ATPase) activity of the enzyme. The maximum level of CO2-P is limited by the amount of enzyme, and approximates 4 mol of intermediate/mol of enzyme. The unprotonated form of ammonia seems to be the species reacting with CO2-P to produce CP. The reaction of CO2-P and NH3 is very fast (rate constant kn = 8 x 10(4) M-1 S-1) and does not consume free ATP. Therefore, the 2 mol of ATP necessary for CP synthesis binds or reacts with the enzyme and/or CO2 prior to reaction with NH3. The reaction of CO2-P with NH3 also takes place in acetone under conditions at which the enzyme is not active, suggesting little or no assistance from enzyme catalysis or that a part of the catalytic site is "frozen" by the solvent in the active conformation. In the light of these and other findings, a new scheme is proposed for the mechanism of frog liver carbamoyl-phosphate synthetase and some considerations are made on the chemical nature of the intermediate and on the possible evolutionary significance of the reaction of CO2-P with NH3 in acetone.     

Carbonyl sulfide inhibition of CO dehydrogenase from Rhodospirillum rubrum

Carbonyl sulfide (COS) has been investigated as a rapid-equilibrium inhibitor of CO oxidation by the CO dehydrogenase purified from Rhodospirillum rubrum. The kinetic evidence suggests that the inhibition by COS is largely competitive versus CO (Ki = 2.3 microM) and uncompetitive versus methylviologen as electron acceptor (Ki = 15.8 microM). The data are compatible with a ping-pong mechanism for CO oxidation and COS inhibition. Unlike the substrate CO, COS does not reduce the iron-sulfur centers of dye-oxidized CO dehydrogenase and thus is not an alternative substrate for the enzyme. However, like CO, COS is capable of protecting CO dehydrogenase from slow-binding inhibition by cyanide. A true binding constant (KD) of 2.2 microM for COS has been derived on the basis of the saturable nature of COS protection against cyanide inhibition. The ability of CO, CO2, COS, and related CO/CO2 analogues to reverse cyanide inhibition of CO dehydrogenase is also demonstrated. The kinetic results are interpreted in terms of two binding sites for CO on CO dehydrogenase from R. rubrum.     

Channeling of carbon monoxide during anaerobic carbon dioxide fixation

Carbon monoxide is an intermediate in carbon dioxide fixation by diverse microbes that inhabit anaerobic environments including the human colon. These organisms fix CO(2) by the Wood-Ljungdahl pathway of acetyl-CoA biosynthesis. The bifunctional CO dehydrogenase/acetyl-CoA synthase (CODH/ACS) catalyzes several key steps in this pathway. CO(2) is reduced to CO at a nickel iron-sulfur cluster called cluster C located in the CODH subunit. Then, CO is condensed with a methyl group and coenzyme A at cluster A, another nickel iron-sulfur cluster in the ACS subunit. Spectroscopic studies indicate that clusters A and C are at least 10-15 A apart. To gain a better understanding of how CO production and utilization are coordinated, we have studied an isotopic exchange reaction between labeled CO(2) and the carbonyl group of acetyl-CoA with the CODH/ACS from Clostridium thermoaceticum. When solution CO is provided at saturating levels, only CO(2)-derived CO is incorporated into the carbonyl group of acetyl-CoA. Furthermore, when high levels of hemoglobin or myoglobin are added to remove CO from solution, there is only partial inhibition of the incorporation of CO(2)-derived CO into acetyl-CoA. These results provide strong evidence for the existence of a CO channel between cluster C in the CODH subunit and cluster A in the ACS subunit. The existence of such a channel would tightly couple CO production and utilization and help explain why high levels of this toxic gas do not escape into the environment. Instead, microbes sequester this energy-rich carbon source for metabolic reactions.     

Stomatal density and stomatal index as indicators of paleoatmospheric CO(2) concentration

A growing number of studies use the plant species-specific inverse relationship between atmospheric CO(2) concentration and stomatal density (SD) or stomatal index (SI) as a proxy for paleo-CO(2) levels. A total of 285 previously published SD and 145 SI responses to variable CO(2) concentrations from a pool of 176 C(3) plant species are analyzed here to test the reliability of this method. The percentage of responses inversely responding to CO(2) rises from 40 and 36% (for SD and SI, respectively) in experimental studies to 88 and 94% (for SD and SI, respectively) in fossil studies. The inconsistent experimental responses verify previous concerns involving this method, however the high percentage of fossil responses showing an inverse relationship clearly validates the method when applied over time scales of similar length. Furthermore, for all groups of observations, a positive relationship between CO(2) and SD/SI is found in only 相似文献   

微藻固定CO2研究进展

空气中CO2浓度升高所导致的温室效应已成为重大的环境问题,受到人们普遍关注.概述了高效固定CO2微藻藻种的筛选和培养方法,分析了微藻固定CO2的无机碳利用形式和浓缩机制,讨论了高效光生物反应器设计和运行目标,简要介绍了微藻(酶)-膜生物反应器集成新技术.并认为今后的研究方向主要是在进一步探索微藻固定CO2有关机理的基础上,构建高效固定CO2的转基因微藻,开发高效膜生物反应集成系统.     

Carbon dioxide assimilation by leaves, isolated chloroplasts, and ribulose bisphosphate carboxylase from spinach

The relationship between rate of photosynthesis and CO(2) concentration has been reinvestigated using isolated spinach (Spinacia oleracea) chloroplasts. The apparently low CO(2) concentration required for half-maximal photosynthesis is shown to result partly from a ceiling imposed by electron transport. In double reciprocal plots of rate against CO(2) concentration, this ceiling results in departures from linearity at high CO(2) concentrations. If these rate limitations are disregarded in extrapolation the "true" CO(2) concentration required for half maximal carboxylation by intact chloroplasts is approximately 46 mum (CO(2)).When assayed under comparable conditions, ribulose bisphosphate carboxylase from these chloroplasts also shows an apparent Km (CO(2)) of approximately 46 mum, suggesting that its characteristics are not modified by extraction. An improved assay for ribulose bisphosphate carboxylase yielded rates of carboxylation considerably higher than those previously reported, the highest maximal velocities recorded approaching 1000 mumoles CO(2) fixed mg(-1) chlorophyll hr(-1) at 20 C. With such Km and V(max), values the carboxylase would be able to achieve, at concentrations of CO(2) less than atmospheric, rates of CO(2) fixation equal to those displayed by the parent tissue or by the average plant under favorable conditions in its natural environment.     

Life with CO or CO2 and H2 as a source of carbon and energy

An account is presented of the recent discovery of a pathway of growth by bacteria in which CO or CO2 and H2 are sources of carbon and energy. The Calvin cycle and subsequently other cycles were discovered in the 1950s, and in each the initial reaction of CO2 involved adding CO2 to an organic compound formed during the cyclic pathway (for example, CO2 and ribulose diphosphate). Studies were initiated in the 1950s with the thermophylic anaerobic organism Clostridium thermoaceticum, which Barker and Kamen had found fixed CO2 in both carbons of acetate during fermentation of glucose. The pathway of acetyl-CoA biosynthesis differs from all others in that two CO2 are combined with coenzyme A (CoASH) forming acetyl CoA, which then serves as the source of carbon for growth. This mechanism is designated the acetyl CoA pathway and some have called it the Wood pathway. A unique feature is the role of the enzyme carbon monoxide dehydrogenase (CODH), which catalyzes the conversion of CoASH, CO, and a methyl group to acetyl CoA, the final step of the pathway. The pathway involves the reduction of CO2 to formate, which then combines with tetrahydrofolate (THF) to form formyl THF. It in turn is reduced to CH3-THF. The methyl is then transferred to the cobalt on a corrinoid-containing enzyme. From there the methyl is transferred to CODH, and CO and CoASH bind with the enzyme at separate sites. Acetyl CoA is then synthesized. CODH would more properly be called carbon monoxide dehydrogenase-acetyl CoA synthase as it catalyzes oxidation of CO to CO2 and the synthesis of acetyl CoA. The solution of the mechanism of this pathway required more than 30 years, in part because the intermediate compounds are bound to enzymes, the enzymes are extremely sensitive to O2 and must be isolated under strictly anerobic conditions, and the role of a corrinoid and CODH was unprecedented. It is now apparent that this pathway occurs (perhaps with some modification) in many bacteria including the methane and sulfur bacteria. In some humans this pathway is catalyzed by the bacteria of the gut and acetate is produced rather than methane; it is calculated that 2.3 x 10(6) metric tons of acetate are formed daily from CO2. A similar synthesis occurs in the hind gut of termites. It is becoming apparent that the acetyl CoA pathway plays a significant role in the carbon cycle.(ABSTRACT TRUNCATED AT 400 WORDS)     

A 13C nuclear-magnetic-resonance study of CO2-HCO3-exchange catalyzed by human carbonic anhydrase C at chemical equilibrium.

The effects of human carbonic anhydrase C on the 13C nuclear magnetic resonance spectra of equilibrium mixtures of 13CO2 and NaH13CO3 were measured at 67.89 MHz. Enzyme-catalyzed CO2-HCO-3 exchange rates were estimated from the linewidths of the resonances. The results show that: (a) the maximal exchange rates are larger than the maximal turnover rates; (b) the exchange is equally rapid with 1H2O or with 2H2O as solvents; (c) the exchange is equally rapid in the presence or in the absence of added buffers; (d) the apparent substrate binding is weaker than predicted if steady-state Km values are assumed to represent substrate dissociation constants. The main conclusion concerning the catalytic mechanism of the enzyme is that the proton-transfer processes which limit turnover rates in the steady state are not directly involved in CO2-HCO-3 exchange. In addition, the results suggest that CO2-HCO-3 interconversion takes place by a nucleophilic mechanism, such as a reversible reaction of zinc-coordinated OH- with CO2.     

Bicarbonate, not CO2, is the species required for the stimulation of Photosystem II electron transport

Evidence is presented that the bicarbonate ion (HCO3-), not CO2, H2CO3 or CO32-, is the species that stimulates electron transport in Photosystem II from spinach (Spinacia oleracea). Advantage was taken of the pH dependence of the ratio of HCO3- to CO2 at equilibrium in order to vary effectively the concentration of one species while holding the other constant. The Hill reaction was stimulated in direct proportion with the equilibrium HCO3- concentration, but it was independent of the equilibrium CO2 concentration. The other two carbonic species, H2CO3 and CO32-, are also shown to have no direct involvement. It is suggested that HCO3- is the species which binds to the effector site.     

Metal centers in the anaerobic microbial metabolism of CO and CO2

Carbon dioxide and carbon monoxide are important components of the carbon cycle. Major research efforts are underway to develop better technologies to utilize the abundant greenhouse gas, CO(2), for harnessing 'green' energy and producing biofuels. One strategy is to convert CO(2) into CO, which has been valued for many years as a synthetic feedstock for major industrial processes. Living organisms are masters of CO(2) and CO chemistry and, here, we review the elegant ways that metalloenzymes catalyze reactions involving these simple compounds. After describing the chemical and physical properties of CO and CO(2), we shift focus to the enzymes and the metal clusters in their active sites that catalyze transformations of these two molecules. We cover how the metal centers on CO dehydrogenase catalyze the interconversion of CO and CO(2) and how pyruvate oxidoreductase, which contains thiamin pyrophosphate and multiple Fe(4)S(4) clusters, catalyzes the addition and elimination of CO(2) during intermediary metabolism. We also describe how the nickel center at the active site of acetyl-CoA synthase utilizes CO to generate the central metabolite, acetyl-CoA, as part of the Wood-Ljungdahl pathway, and how CO is channelled from the CO dehydrogenase to the acetyl-CoA synthase active site. We cover how the corrinoid iron-sulfur protein interacts with acetyl-CoA synthase. This protein uses vitamin B(12) and a Fe(4)S(4) cluster to catalyze a key methyltransferase reaction involving an organometallic methyl-Co(3+) intermediate. Studies of CO and CO(2) enzymology are of practical significance, and offer fundamental insights into important biochemical reactions involving metallocenters that act as nucleophiles to form organometallic intermediates and catalyze C-C and C-S bond formations.     

The impact of low levels of carbon dioxide on rats

The widespread use of individually ventilated cage (IVC) systems today has made the impact of CO(2) on rodents a highly important matter. Leaving cages from these systems without ventilation increases CO(2) concentrations inside the cages, as CO(2) generated from the animals is no longer removed actively. In modern IVC systems the CO(2) levels may reach 3-5% within a very short time, as the cages are very tightly sealed. The aim of the present study was to investigate the effects of 1%, 3%, and 5% CO(2) by studying the preferences of the animals as well as changes in the heart rate and systolic blood pressure as measured by telemetry. The rats avoided the cages, which contained 3% CO(2). In the telemetric study an anaesthetic effect on the rats were seen at 3% as a drop in the heart rate, and at 5% CO(2) a drop in the systolic blood pressure was also seen. The results from the present study could indicate that CO(2) levels of up to 3% do not affect the animals, or at least only to a minor extent, but that if the animals are exposed to CO(2) levels of higher than 3% they are affected directly as seen by changes in physiological parameters and preferences.