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Query: HUMANGGP:003739 (CO2)
 48,959 document(s) hit in 31,850,051 MEDLINE articles (0.00 seconds)

The effects of birth and morepinephrine on hepatic glucose production, glycogenolysis, and gluconeogenesis were examined in livers isolated from fetal dogs at term, littermates 3 hr after delivery, and newborn dogs 1-5 days old. Livers were perfused in pairs with medium containing (6-3H)glucose (6 mM) and (3-14C)lactate (10 mM +/- a pharmacologic amount of norepinephrine (10(-6)M). Changes in glucose production rates were correlated with changes in the enzymatic activities controlling gluconeogenesis. Net glucose production was less than 0.48 mumol/min-g liver both fetal and 3 hr liver but stablized above 1 mumol/min-g later during the first day. Initially, mobilization of the fetal hepatic glycogen accounted for glucose output. Subsequently, incorporation of lactate into glucose rose from negligible fetal rates to 0.19 mumol/min-g and accounted for 21% of net glucose production on day 3. Mazimal pyruvate carboxylase activity and mitochondrial CO2 fixation increased postnatally and correlated directly with net glucose production, glucose production from glycogen, and glucose production from lactate. Fetal liver did not respond to norepinephrine. Thereafter, norepinephrine increase hepatic glucose production by stimulating glycogen breakdown. Postnatal acceleration of glucose production and the response to norepinephrine occurred only after indiction of mitochondrial CO3 fixation. During day 1 the decline of hepatic glycogen in response to norepinephrine correlated with both CO2 fixation and lactate incorporation into glucose. Thus, initiation of gluconegenesis after birth may have been required for the postnatal acceration of hepatic glucose production and for the regulation of glycogenolysis by norpinephrine.
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PMID:Glucose production in the newborn dog. II. Evaluation of autonomic and enzymatic control in the isolated perfused canine liver. 17 17

Tubular fragments from rat kidney cortex were isolated by collagenase and suspended in an incubation medium containing a combination of several renal substrates. Substrate concentrations were in the physiological range. O2 uptake, total CO2 production, and the 14CO2 production from U-14C-labeled palmitate and oleate were measured. During the first minutes of incubation the CO2 production from palmitate and oleate was 10.5% or 6.3%, respectively, of the total CO3 produced. The RQ was 0.897. A subsequent decrease of the total CO2 production at a constant uptake of oxygen indicated a rising contribution of fatty acids to the fuel of respiration. The renal preference for substrates other than longchain fatty acids is discussed.
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PMID:Contribution of long chain fatty acids to the energy supply of the rat kidney cortex. 17 58

The initial and long-term drift of tcPO2 microcathode electrodes has been shown to be substantially less when chloride is removed from the electrolyte, despite the probability that reference electrode EMF is less well defined. In addition to virtually eliminating drift, these electrolytes eliminate silver deposition on the cathode. The most successful electrolyte tested thus far has been 0.2 M K2B4O7 in 95% ethylene glycol, 5% water, both with and without cellophane spacers. The buffering produced by borate appears to prevent the downward drift in CO2 free air probably caused by Ag2 CO3 formation on the anode, after exposure to skin.
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PMID:Alkaline chloride-free oxygen electrolytes. 27 4

Lake Mendota sediments and the immediate overlying water column were studied to better understand the metabolism of the methanogenic precursors H2/CO2 and acetate in nature. The pool size of acetate (3.5 microns M) was very small, and the acetate turnover time (0.22h) was very rapid. The dissolved inorganic carbon pool was shown to be large (6.4 to 8.3 mM), and the turnover time was slow (111 H.). CO2 was shown to account for 41 +/- 5.5% of the methane produced in sediment. Acetate and H2/CO2 were simultaneously converted to CH4. The addition of H2 to sediments resulted in an increase specific activity of CH4 from H(14)CO3- and a decrease in specific activity of CH4 from [2-14C]acetate. Acetate addition resulted in a decrease in specific activity of CH4 from H(14)CO3-. The metabolism of H(14)CO3- or [2-14C]acetate to 14CH4 was not inhibited by addition of acetate or H2. After greater than 99% of added [2-14C]acetate had been turned over, 42% of the label was recovered as 14CH4 20% was recovered as 14CO2 and 38% was incorporated into sediment. Inhibitor studies of [2-14C]acetate metabolism in sediments demonstrated that CHCl3 completely inhibited CH4 formation, but not CO2 production. Air and nitrate addition inhibited CH4 formation and stimulated CO2 production, whereas fluoroacetate addition totally inhibited acetate metabolism. The oxidation of [2-14C]acetate to 14CO2 was shown to decrease with time when sediment was incubated before the addition of label, suggesting depletion of low levels of an endogenous sediment electron acceptor. Acetate metabolism varied seasonally and was related to the concentration of sulfate in the lake and interstitial water. Methanogenesis occurred in the sediment and in the water immediately overlying the sediment during period of lake stratification and several centimeters below the sediment-water interface during lake turnovers. These data indicate that methanogenesis in Lake Mendota sediments was limited by "immediate" methane precursor availability (i.e., acetate and H2), by competition for these substrates by nonmethanogens, and by seasonal variations which altered sediment and water chemistry.
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PMID:Anaerobic metabolism of immediate methane precursors in Lake Mendota. 43 7

Larval Taenia taeniaeformis in vivo accumulates 45Ca2+ in soft tissues and calcareous corpuscles. Radioactivity was demonstrable in the corpuscles six months after a single dose of 45Ca2+ was administered to the host by means of a stomach tube. Ca2+ also was taken up by isolated larvae. Accumulation in vitro was more rapid then in vivo and was correlated with the external Ca2+ concentration. Temperature variation, oxygen availability, and metabolic inhibitors had little effect on the Ca2+ uptake, indicating that active transport of Ca2+ is unlikely in this parasite. Variations in the external Pi concentrations had no effect on Ca2+ accumulation or on its distribution. Addition of 5% CO2 increased the uptake of Ca2+ by the calcareous corpuscles under anaerobic conditions. Radioactivity from NaH14CO3 also was accumulated in soft tissues and corpuscles of T. taeniaeformis. Assuming that the 14C taken up by the corpuscles was in the form of 14CO3(2-), the ratio of Ca2+ to CO3(2-) accumulation in the corpuscles approximates the ratio of these constituents in dolomite: CaMg(CO3)2.
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PMID:Incorporation of calcium into the soft tissues and calcareous corpuscles of larval Taenia taeniaeformis. 122 Mar 60

HCO3- exit across the basolateral membrane of the kidney proximal tubule cell is mediated via an electrogenic Na+:HCO3- cotransporter. We have studied the effect of pH on the activity of this cotransport system in basolateral membrane vesicles isolated from rabbit renal cortex. At constant internal pH 6.0, increasing the external pH and [HCO3-] increased the rate of 4,4'-diisothiocyanostilbene-2,2'-disulfonic acid-sensitive 22Na+ influx into the vesicles. To determine the role of internal pH on the activity of the Na+:HCO3- cotransport system, the influx of 22Na+ via HCO3-dependent Na(+)-Na+ exchange was measured in the absence of an initial pH and [HCO3-] gradient (pH(i) = pH(o), 5% CO2). Increasing the pH from 6.8 to 7.2 increased whereas, increasing the pH from 7.4 to 8.0 decreased the rate of 22Na+ influx via this exchange. Increasing pH at constant [HCO3-] (pH(i) = pH(o) = 8.0, 1.5% CO2 versus pH(i) = pH(o) = 7.2, 10% CO2) reduced the influx of 22Na+ via HCO3-dependent Na(+)-Na+ exchange. Increasing pH at constant [CO3(2-)](pH(i) = pH(o) = 8.0, 1.5% CO2 versus pH(i) = pH(o) = 7.2, 60% CO2) was associated with reduced 22Na+ uptake. Decreasing the pH (pH(i) = pH(o) = 6.3, 60% CO2 versus pH(i) = pH(o) = 7.2, 5% CO2) was associated with a reduced rate of HCO3(-)-dependent Na(+)-Na+ exchange. We conclude that the Na+:HCO3- cotransporter displays a significant pH sensitivity profile with the cotransporter being more functional at pH 7.0-7.4 and less active at more acid or alkaline pH. In addition, the results suggest that the pH sensitivity arises at the inner surface of the basolateral membrane.
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PMID:pH sensitivity of the Na+:HCO3- cotransporter in basolateral membrane vesicles isolated from rabbit kidney cortex. 152 75

Calcium carbonate is a major component of gallstones, but there are few data on calcium and carbonate (CO3(2-)) concentrations in human bile. Therefore, in patients undergoing cholecystectomy for gallstones, total [CaTOT] and free ionized [Ca2+] calcium concentrations, pH, PCO2, and total [CO2] were measured and [CO3(2-)] was derived in gallbladder and hepatic bile (aspirated anaerobically at surgery or from T tubes). Gallbladder bile had lower pH (6.96 vs. 7.30) and total [CO2] (14.1 vs. 21.6 mmol/L), higher PCO2 (53.8 vs. 40.2 mm Hg), lower [CO3(2-)] (2.52 vs. 6.11 x 10(5) mol/L) and lower [Ca2+] x [CO3(2-)] ion product (1.88 vs. 4.74 x 10(-8) mol/L) than did hepatic bile. Gallbladder bile pH correlated positively with total [CO2], [CO3(2-)], and [Ca2+] x [CO3(2-)] but negatively with PCO2. Patients with surface gallstone calcification had similar gallbladder bile [CaTOT] and [Ca2+] but higher gallbladder bile pH (7.30 vs. 6.90), lower PCO2 (42.9 vs. 57.2 mm Hg), higher [CO3(2-)] (7.29 vs. 1.84 x 10(-5) mol/L), and higher [Ca2+] x [CO3(2-)] ion product [4.73 vs. 1.45 x 10(-8) (mol/L)2] than those with radiolucent gallstones. There were no differences in these parameters between patients with cholesterol stones and those with pigment stones. These data suggest that the human gallbladder acidifies bile by secreting hydrogen ion and that impairment of this secretion is one cause of calcified gallstone formation in humans.
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PMID:Calcium and carbonate ion concentrations in gallbladder and hepatic bile. 850 Jul 51

The solubility of enamel mineral (a carbonated apatite) formed at various stages of porcine amelogenesis was investigated at controlled partial pressures of CO2. Enamel samples were obtained from the outer (young) secretory, inner (old) secretory, early (soft) and late (hard) mature enamel of the permanent dentition of slaughtered piglets. The dissected enamel was pulverized and subjected to a plasma ashing at low temperature to remove organic matter. The composition (Ca, total P, HPO4, and CO3) of the enamel mineral was determined chemically. The enamel mineral contained significant amounts of carbonate and acid phosphate; the model adopted for its stoichiometry was [Ca]5-x [HPO4]v[CO3]w[PO4]3-x[OH]1-x. Each enamel sample was equilibrated in dilute phosphoric acid solutions (0.01-1.2 mM) under Pco2 = 1.86 and 1.75%. Equilibration of the enamel samples usually took 20-25 days; the solution composition (pH, concentrations of Ca, P, Mg, Na, and K, and activity of Ca2+) was determined periodically. The composition of the solution at equilibrium showed that (1) the outer (younger) secretory mineral was the most soluble and the solubility of enamel mineral decreased with advancing developmental stages; (2) the mean activity product in the saturated solutions for the outer secretory enamel was the same as that calculated on the basis of the reported composition of the enamel fluid; and (3) the solubility data obtained with most of the enamel samples were consistent with a model in which the equilibration includes two processes: dissolution of the original enamel mineral and precipitation of a new carbonatoapatite. Analyses of the equilibrated samples, particularly the mature enamel, by electron microscopy, supported the precipitation of carbonatoapatite.(ABSTRACT TRUNCATED AT 250 WORDS)
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PMID:Changes in the solubility of enamel mineral at various stages of porcine amelogenesis. 161 2

The ESR spectrum of X-irradiated carbonated apatites precipitated from aqueous solutions was studied as a function of their carbonate content and drying temperature. When the latter increases from 25 to 400 degrees C, the ESR spectrum is gradually modified and becomes similar to the spectrum of carbonated apatites, synthesized at high temperatures by solid state reactions. The latter ESR spectrum is dominated by CO3(3-)-contributions whereas the spectrum of precipitated samples dried at 25 degrees C can mainly be interpreted in terms of CO2-, CO3-, and O- ions. The behavior of these earlier-reported CO2-, CO3-, and O- centers is now studied as a function of drying temperature. In addition, the Spin Hamiltonian parameters of the CO3(3-) centers are determined and some other new paramagnetic radicals are discussed. It is shown that a CO3(2-) ion at a phosphate lattice site (B-type substitution) may give rise to either a CO2-, CO3-, or CO3(3-) radical on X-irradiation, depending on the sample preparation conditions. A surface CO3(2-) ion may cause a surface CO2-, CO3-, or O- radical. From the reported results it is not unambiguously clear whether the CO3(3-) ion detected in the samples with the relatively lowest carbonate content should be located on the surface or on a hydroxyl lattice site (A-type substitution). An important result is that the absolute concentration of the B-type CO3(3-) ion increases with increasing carbonate content as was also the case for the earlier reported B-type radicals (isotropic CO2- and CO3-). On the other hand, the absolute concentration of the surface radicals decreases with increasing carbonate content. The reported results show that similar deconvolution techniques can be applied in the future for the study of ESR spectra of calcified tissues. This will allow a more efficient phenomenological investigation of the latter.
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PMID:The effect of carbonate content and drying temperature on the ESR-spectrum near g = 2 of carbonated calciumapatites synthesized from aqueous media. 164 44

Carbonic acid buffer anions, HCO3- and CO3(2-), play an instrumental role in a host of vital processes in animal cells and tissues. Yet study of carbonic acid buffer species is hampered because no means are available to simultaneously monitor them at a cellular level in a rapid and dynamic fashion. An ion-selective cocktail, previously reported to measure changes in bicarbonate activity (alpha HCO3-), was instead shown to be principally selective for alpha CO3(2-). Ion-selective micropipettes (ISMs) based on this exchanger and consisting of a 3:1:6 (volume) mixture of tri-n-octylpropylammonium chloride, 1-octanol, and trifluoroacetyl-p-butylbenzene showed no significant interference from bicarbonate, chloride, phosphate, ascorbate, lactate, glutamate, acetate, or hydroxyl ions at concentrations expected in vivo. Intracellular and triple-barrel ISMs, consisting of a CO3(2-) sensitive, pH-sensitive, and reference barrel, were fabricated. Skeletal muscle cells (n = 17) were penetrated in vivo and showed values of 74 +/- 7 mV for membrane potential, 6.94 +/- 0.09 pHi, and 11 +/- 5 microM intracellular alpha CO3(2-), from which intracellular alpha HCO3- of 25 +/- 10 mM and CO2 tension of 120 +/- 55 Torr were calculated. All ion measurements reached a new steady state in 9 +/- 2 s after cell penetration. Thus measurements of intracellular alpha CO3(2-) and pH and associated levels of alpha HCO3(2-) and CO2 tension can be determined in biological tissues and cells with a spatial and temporal resolution previously unattainable.
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PMID:Carbonic acid buffer species measured in real time with an intracellular microelectrode array. 165 44


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