念珠藻对岩溶水中 Ca2＋、HCO－3利用效率实验研究

岩溶碳汇过程中石灰石溶解将大气/土壤中 CO 2转移到水体形成 HCO －3促进水生藻类的生长.该文为了研究水生藻类光合作用将岩溶水中无机碳转化为有机碳的效率,采用从岩溶水生生态系统中筛选出的念珠藻作为研究对象,探讨在封闭体系中藻细胞光合作用时对典型岩溶水中 Ca2＋、HCO －3利用、藻细胞生物量的变化与 Ca2＋、HCO －3的利用关系以及体系 pH、DO 的变化.结果表明：念珠藻通过光合作用能吸收利用岩溶水中27．38％的 Ca2＋,同时将29．54％的 Ca2＋通过物理化学作用以“藻体-CaCO 3”复合体形式沉淀而返回到无机环境.pH 漂移实验表明念珠藻光合作用过程中先利用水体中游离 CO 2,然后以岩溶水中 HCO －3为碳源.由于水体中岩溶作用产生的 HCO －3不断被光合作用利用而引起体系 pH 和 DO 的升高.念珠藻光合作用将岩溶水中65％的 HCO －3转化为稳定化合物,其中18．46％以胞外 CaCO 3形式被沉淀,81．54％被藻类转化为有机物,表现为净碳汇效应.     

丝藻光合作用无机碳利用研究

丝藻pH补偿点为9．2,表明其具有较低的CO2补偿点,不同pH值下丝藻光合作用放氧速率明显大于理论上从HCO3－脱水来的CO2供应速率,表明其具有利用HCO3－的能力,未检测到丝藻有胞外碳酸酐酶活性,胞内碳酸酐酶的活性随培养液中CO2浓度的升高而降低。     

小球藻吸附水中Pb2+影响因素的初步研究

对小球藻生物吸附水中Pb2 + 的影响因素作了初步研究。实验表明 :在小球藻处于指数生长期和静止期时加入Pb2 + ,去除率达 6 0 %以上 ;当藻细胞密度一定时 ,随着Pb2 + 浓度的增加 ,Pb2 + 的去除率增大 ;当Pb2 + 浓度一定时 ,随着藻细胞密度的增加 ,小球藻对Pb2 + 的去除率增大 ,藻细胞密度为 1 2 9× 10 8个 /ml时 ,去除率可达 92 82 % ;加强光照可以促进小球藻对Pb2 + 的吸附 ;在pH值为 5～ 10的范围内 ,pH对Pb2 + 吸附影响不大 ,较佳的pH值在 7左右。实验最佳条件的去除率在 90 %以上 ,去除效果较好。     

模拟酸沉降对鼎湖山季风常绿阔叶林地表径流水化学特征的影响

通过模拟酸沉降实验,研究了旱季期间(10-3月份)鼎湖山季风常绿阔叶林在4种不同pH模拟酸雨处理(对照、pH 4.0、pH 3.5、pH 3.0)下地表径流水化学输出特征.结果显示:(1)地表径流pH随酸处理强度增强呈“U”型变化模式,酸沉降对地表径流pH的影响不显著(P＞0.05),表明模拟酸沉降尚未引起地表水的酸化.(2)地表径流中NO3-、SO24-浓度随酸处理强度增强略有增加;HCO3-浓度的变化模式与地表径流pH类似.酸根离子浓度与地表径流pH相关性分析表明,SO24-、HCO3-有助于提高地表水抗酸化能力而NO3-则有助于促进地表水酸化.(3)地表径流中盐基离子对酸沉降的响应不尽相同.pH 3.0处理显著提高地表径流中Ca2+、Na+浓度;Mg2+浓度具有随酸处理梯度增强而增加的趋势;K+受模拟酸度的影响小.表明强酸(pH3.0)处理将导致土壤Na+、Ca2+、Mg2+盐基离子流失.(4)酸沉降具有诱发土壤可溶性有机碳(DOC)流失的倾向,增加地表水受有机污染的风险.     

pH对小球藻Chlorella sp. XQ-200419光合作用、生长和产油的影响

以一种生长快、油脂含量高的小球藻(Chlorella sp. XQ-200419)为实验材料, 利用测定净光合放氧速率的方法研究了pH对其光合作用的影响; 使用改良的BG-11培养基在微藻环形培养池模拟系统中进行分批培养, 培养周期为8d, 培养过程中使用 pH控制仪在线监测藻液的pH, 根据pH变化, 自动接通、关闭CO2通气管道, 将藻液pH分别控制在5.06.0, 7.08.0, 8.09.0, 9.010.0, 10.011.0内, 研究pH对生长速率、生物质面积产率、总脂含量和总脂面积产率的影响。主要结果如下: 藻液pH对小球藻Chlorella sp. XQ-200419光合放氧、生长速率、生物质产率、总脂含量和产率都有显著影响, 适宜的pH范围是7.09.0, 在此范围内, 光合放氧、生长速率、生物质产率、总脂含量和产率均保持较高水平, 且pH的影响不显著; pH低于7.0, 高于9.0, 其光合放氧、生长速率、生物质产率、总脂含量和产率都显著降低。这表明pH对小球藻Chlorella sp. XQ-200419光合作用的影响和对生长、产油的影响是一致的。pH 7.08.0, 小球藻的生物质平均面积产率和总脂平均面积产率都达到最大值, 分别是8.9 g/(m2d)和2269.5 mg/(m2d); 当藻液pH超过10.0, 生物质平均面积产率和总脂平均面积产率分别降低42.1%和60.0%。适合于小球藻生长的pH也有利于其积累油脂, 所以, pH对小球藻产油的影响是一种适宜模式, 而非胁迫模式。规模化培养小球藻Chlorella sp. XQ-200419, 通过补充CO2将藻液pH控制在7.09.0内, 可以获得高生物质产率和总脂产率。研究结果反映出pH对小球藻光合作用、生长和产油影响的规律, 也为规模化培养小球藻生产微藻油脂过程中合理控制藻液pH提供了依据。       

蛋白核小球藻生长和无机碳利用对不同光照强度和CO_2浓度的响应

为了探讨光照强度和CO_2浓度对蛋白核小球藻(Chlorella pyrenoidosa)生长、无机碳利用的复合效应,丰富绿藻中无机碳浓缩机制的资料,该文设置两种光照强度(40和120μmol photons×m–2×s–1)和两种CO_2浓度(0.04%和0.16%)组合成4种条件,比较了蛋白核小球藻生长、无机碳浓度、pH补偿点、光合放氧速率、碳酸酐酶(CA)活性和α-CA基因转录表达对这4种培养条件的响应。结果发现:蛋白核小球藻在高光强高CO_2浓度组生长最快;低光强高CO_2浓度组培养体系中总无机碳浓度为1 163.3μmol×L–1,显著高于其他3组;高光强低CO_2浓度组藻的p H补偿点最高(9.8),而低光强高CO_2浓度组藻的p H补偿点最低(8.6);低光强高CO_2浓度组藻的最大光合速率(Vmax)和最大光合速率一半时的无机碳浓度(K0.5)最高,分别是其他3组的1.28-1.91倍和1.61-2.00倍;高光强低CO_2浓度组藻的胞外CA活性最高;而低光强低CO_2浓度组藻的胞外α-CA基因表达量显著高于其他3组。以上结果表明低CO_2浓度可促进蛋白核小球藻的pH补偿点和无机碳亲和力的提高,诱导胞外CA活性及α-CA基因的表达;该藻主要以HCO_3~–为无机碳源,其对无机碳的利用受光照的调节。     

水体无机碳条件对常见沉水植物生长和生理的影响

为了解水华引起的水体无机碳变化对沉水植物生长的影响,对8种沉水植物:金鱼藻、穗花狐尾藻、篦齿眼子菜、光叶眼子菜、微齿眼子菜、伊乐藻、菹草和黑藻在不同无机碳浓度下的生物量、株高、叶绿素以及光合和呼吸速率进行了比较研究.结果表明8种沉水植物均能利用HCO3-作为光合无机碳源,在1.5 mmoL/L外源HCO3-浓度下能促进金鱼藻、菹草和伊乐藻的生长,提高其光合速率;在2.5 mmol/L外源HCO3-浓度下能促进狐尾藻、光叶眼子菜、黑藻、微齿眼子菜和蓖齿眼子菜的生长,提高其光合速率.在CO32-为优势碳源时,8种沉水植物表现出不同的适应性,发现微齿眼子菜、篦齿眼子菜和黑藻在整个实验范围内生长未受抑制,且在不同浓度下表现生长和光合速率的促进,说明这三种沉水植物对[HCO3-]/[CO32-]比值和pH具有较广适应范围.而当CO32-成为优势碳源时,金鱼藻和伊乐藻的生长受到抑制,狐尾藻、菹草和光叶眼子菜均死亡,表明[HCO3-]/[CO32-]比值和pH是这5种沉水植物生长的重要限制因子.     

蛋白核小球藻生长和无机碳利用对不同光照强度和CO2浓度的响应

为了探讨光照强度和CO₂浓度对蛋白核小球藻(Chlorella pyrenoidosa)生长、无机碳利用的复合效应, 丰富绿藻中无机碳浓缩机制的资料, 该文设置两种光照强度(40和120 µmol photons•m^-2•s^-1)和两种CO₂浓度(0.04%和0.16%)组合成4种条件, 比较了蛋白核小球藻生长、无机碳浓度、pH补偿点、光合放氧速率、碳酸酐酶(CA)活性和α-CA基因转录表达对这4种培养条件的响应。结果发现: 蛋白核小球藻在高光强高CO₂浓度组生长最快; 低光强高CO₂浓度组培养体系中总无机碳浓度为1163.3 µmol•L^-1, 显著高于其他3组; 高光强低CO₂浓度组藻的pH补偿点最高(9.8), 而低光强高CO₂浓度组藻的pH补偿点最低(8.6); 低光强高CO₂浓度组藻的最大光合速率(V_max)和最大光合速率一半时的无机碳浓度(K_0.5)最高, 分别是其他3组的1.28-1.91倍和1.61-2.00倍; 高光强低CO₂浓度组藻的胞外CA活性最高; 而低光强低CO₂浓度组藻的胞外α-CA基因表达量显著高于其他3组。以上结果表明低CO₂浓度可促进蛋白核小球藻的pH补偿点和无机碳亲和力的提高, 诱导胞外CA活性及α-CA基因的表达; 该藻主要以HCO₃^-为无机碳源, 其对无机碳的利用受光照的调节。     

两株绿藻响应CO2浓度变化的生长和生理特性的研究

以小球藻FACHB-1580和栅藻FACHB-1618为研究对象,比较了两株绿藻在0.04%CO_2、5%CO_2和20%CO_2(v/v)三种通气培养条件下的生长和生理特性的响应,试图阐述与无机碳利用相关生理参数和微藻利用CO_2能力的关系。结果表明,两株绿藻均能高效利用CO_2,在5%(v/v)条件下均表现出最大生物量积累、最大比生长速率和最大二氧化碳固定速率。小球藻FACHB-1580和栅藻FACHB-1618最大生物量分别为3.5和5.4g/L,分别是0.04%CO_2(v/v)条件的1.41和1.46倍。在高达20%CO_2(v/v)条件下,两株绿藻的生物量均显著高于空气组(P0.05)。随着CO_2浓度的增加,两株绿藻的无机碳亲和力、胞内和胞外CA活性、初始Rubisco活性,及Rubisco活化度均有下降趋势,总的Rubisco活性变化不明显。另外,小球藻FACHB-1580存在较高的胞外和胞内CA活性;而栅藻FACHB-1618胞外CA活性几乎为零,胞内CA活性显著低于小球藻FACHB-1580。由此推测,小球藻FACHB-1580能同时吸收介质中的HCO_3~-和CO_2,其胞内CA催化胞内HCO?3快速转化为CO_2,从而为Rubisco提供充足的CO_2来源;而栅藻FACHB-1618主要吸收介质中的CO_2,其胞内CA活性较低,推测其通过提高胞内CA含量,或增强Rubisco对CO_2的亲和力等促进光合固碳作用。     

光照强度、温度、pH、盐度对小球藻（Chlorella）光合作用的影响

利用测定净光合放氧速率的方法研究了光照强度、温度、pH、盐度对小球藻（Chlorella sp.XQ-200419）和海洋小球藻（Chlorella marina NJ-016）光合作用的影响。小球藻（Chlorella sp.XQ-200419）的适宜光照强度范围为100～〉1600μmo·lm-2·s-1,光饱和点在500μmo·lm-2·s-1附近;适宜温度范围为25～42.5℃,最适温度为37.5℃;适宜pH值范围为6.5～9.0,最适pH值为7.0;对盐度的适应范围较广,在0～0.6mol/L范围内,随着盐度的升高,净光合放氧速率有下降趋势。海洋小球藻（Chlorella marina NJ-016）的适宜光照强度范围为400～〉1600μmol·m-2·s-1,光饱和点在1400μmo·lm-2.s-1附近;适宜温度范围为25～42.5℃,最适温度为37.5℃;适宜pH值范围为5.0～9.0,最适pH值为8.0;对盐度有很好的适应性,在0～0.6mol/L范围内,随着盐度升高,净光合放氧速率明显上升。小球藻和海洋小球藻的净光合放氧速率随光照强度、温度、pH值和盐度变化的规律,表明了两种小球藻的基本生理生态学特性：能适应较强的光照强度、较高的温度、中性偏碱的环境和较高的盐度。研究结果有助于小球藻培养条件的优化。两种小球藻对光照强度、温度、pH值和盐度变化的反应也有所不同：与小球藻（Chlorella sp.XQ-200419）相比,海洋小球藻（Chlorella marina NJ-016）对光照强度有更好的适应性,对pH值变化有更宽的适应范围,适当提高盐度对其光合作用有明显的促进作用。这表明海洋小球藻（Chlorella marina NJ-016）在快速生长繁殖方面具有更大的潜力,这一研究结果为筛选适合于大量培养的优良藻种提供了依据。     

海洋浮游藻类无机碳利用机理的研究

为了认识海洋浮游藻类在碳充足和碳受限条件下对水体中溶解无机碳(DIC)的利用方式与可能机理,对13种海洋浮游藻类在不同pH和CO2浓度及不同DIC条件下细胞外碳酸酐酶(CA)的活性进行了分析测定.结果显示:13种藻中,只有Amphidinium carterae和Prorocentrum minimum在碳充足条件下具细胞外CA活性.Melosira sp.、Phaeodactylum tricornutum、Skeletonema costatum、Thalassiosira rotula、Emiliania huxleyi和Pleurochrysis carterae则在碳受限条件下才具细胞外CA活性.Chaetoceros compressus、Glenodinium foliaceum、Coccolithus pelagicus、 Gephrocapsa oceanica和Heterosigma akashiwo即使在碳受限条件下也未检测到细胞外CA活性.应用封闭系统中pH漂移技术和阴离子交换抑制剂4′4′-diisothiocyanatostilbene-2,2-disulfonic acid (DIDS)等的研究表明,Coc. pelagicus和G. oceanica可通过阴离子交换机制进行HCO-3的直接利用.H. akashiwo没有潜在的HCO-3直接利用或细胞外CA催化的HCO-3利用.     

Inorganic-carbon uptake by the marine diatom Phaeodactylum tricornutum

Air-grown cells of the marine diatom Phaeodactylum tricornutum showed only 10% of the carbonic-anhydrase activity of air-grown Chlamydomonas reinhardtii. Measurement of carbonic-anhydrase activity using intact cells and cell extracts showed all activity was intracellular in Phaeodactylum. Photosynthetic oxygen evolution at constant inorganic-carbon concentration but varying pH showed that exogenous CO₂ was poorly utilized by the cells. Sodium ions increased the affinity of Phaeodactylum for HCO ₃ ^- and even at high HCO ₃ ^- concentrations sodium ions enhanced HCO ₃ ^- utilization. The internal inorganic-carbon pool (HCO ₃ ^- +CO₂] was measured using a silicone-oil-layer centrifugal filtering technique. The internal [HCO ₃ ^- +CO₂] concentration never exceeded 15% of the external [HCO ₃ ^- +CO₂] concentration even at the lowest external concentrations tested. It is concluded that an internal accumulation of inorganic carbon relative to the external medium does not occur in P. tricornutum.Abbreviation Hepes 4-(2-hydroxyethyl)-1-piperazineethane-sulfonic acid     

A requirement of bicarbonate for Ca2+-induced elevations of cyclic AMP in guinea pig spermatozoa

Ca2+ causes less than 2-fold elevations of guinea pig sperm cyclic AMP concentrations when cells are incubated in a minimal culture medium in the absence of bicarbonate (HCO3-). However, in the presence of HCO3-, Ca2+ increases cyclic AMP by as much as 25-fold within 1 min. The (Ca2+, HCO3-)-induced elevations occur in either the presence or absence of the permeant anions, pyruvate and lactate. In the absence of extracellular Ca2+, HCO3- elevates cyclic AMP only slightly. The effect of HCO3- is concentration-dependent, with maximal responses obtained at concentrations of greater than 25 mM. Ca2+ (25 mM HCO3-) at concentrations of less than 100 microM causes one-half-maximal elevations of cyclic AMP. The (Ca2+, HCO3-)-induced elevations of cyclic AMP are observed at various extracellular pH values (7.5-8.5) and in the presence or absence of extracellular Na+ or K+. NH4Cl does not elevate sperm cyclic AMP concentrations and does not greatly alter the (Ca2+, HCO3-)-induced elevations. the putative Ca2+ transport antagonist, D-600 (100 microM), completely blocks the (Ca2+, HCO3-)-induced elevations of cyclic AMP. A23187, in the presence but not in the absence of extracellular Ca2+, increases sperm cyclic AMP but does not further elevate cyclic AMP in HCO3(-)-treated cells. These studies establish that Ca2+-dependent elevations of cyclic AMp in guinea pig spermatozoa are dependent on the presence of HCO3- and suggest that HCO3- is required for the uptake (exchange) or membrane sequestration of small amounts of physiologically active Ca2+.     

Importance of bicarbonate ion for intracellular pH regulation in antigen- and ionomycin-stimulated RBL-2H3 mast cells.

In RBL-2H3 rat basophilic leukemia cells, Ca2+ influx and secretion are activated by antigens that crosslink IgE-receptor complexes and by the Ca2+ ionophore, ionomycin. Here we report that antigen-stimulated Ca2+ influx and secretion are impaired and ionomycin-induced responses are strongly inhibited following the removal of HCO3- from the medium. These results raised the possibility that HCO3(-)-dependent pH regulation mechanisms play a role in the cascade of events leading to mast cell activation. To test this hypothesis, intracellular pH (pHi) was measured by ratio imaging microscopy in individual RBL-2H3 cells labeled with 2',7'-bis-(2-carboxyethyl)-5-(6) carboxyfluorescein (BCECF). In unstimulated cells, it was found that basal pHi in the presence of HCO3- is 7.26, significantly greater than pHi in its absence, 7.09 (P less than 10(-6]. These results, as well as evidence that pHi increases rapidly when HCO3- is added to cells initially incubated in HCO3(-)-free medium, indicate that unstimulated cells use a HCO3(-)-dependent mechanism to maintain cytoplasmic pH. Further analyses comparing unstimulated with stimulated cells showed that antigen causes a small transient acidification in medium containing HCO3- and a larger sustained acidification in HCO3(-)-depleted medium. Ionomycin is a more potent acidifying agent, stimulating a sustained acidification in complete medium and causing further acidification in HCO3(-)-free medium. These results support the hypothesis that the inhibition of antigen- and ionomycin-induced 45Ca2+ influx and secretion in cells incubated in HCO3(-)-free medium is at least partially due to the inactivation of HCO3(-)-dependent mechanisms required to maintain pH in unstimulated cells and to permit pH recovery from stimulus-induced acidification.     

Bicarbonate- and calcium-dependent induction of rapid guinea pig sperm acrosome reactions by monovalent ionophores

The monovalent cationic ionophores monensin and nigericin stimulated rapid guinea pig sperm acrosome reactions in the presence of extracellular Na+, Ca2+ and bicarbonate (HCO3-/CO2). Extracellular K+ (mM concentrations), in contrast, was not required for the stimulatory effect of the ionophores. The effect of HCO3-/CO2 is concentration, pH and temperature dependent, with maximal responses obtained with 50 microM monensin or 25 microM nigericin at a concentration of 30 mM HCO3-, 2.5% CO2 and pH 7.8 at 25 degrees C. At a constant HCO3- concentration (30 mM), monensin stimulated acrosome reactions within the pH range 7.5-7.8, whereas a higher or lower pH did not support acrosome reactions at 25 degrees C. At constant extracellular pH (7.8), monensin stimulated acrosome reactions in the presence of 30 mM HCO3-, whereas higher and lower concentrations did not support acrosome reactions at 25 degrees C. The permeant anions pyruvate and lactate were essential to maintain sperm motility when treated with monensin under these conditions. NH4Cl, sodium acetate and 4,41-diisothiocyano-2, 21-disulfonic acid stibene (DIDS; 25 microM), an anion transport inhibitor, blocked the ability of monensin to stimulate acrosome reactions. Verapamil (100 microM), a putative Ca2+ transport antagonist, in contrast, did not prevent the monensin-induced acrosome reactions. Physiological concentrations of Na+ were needed for monensin to stimulate acrosome reactions, but high concentrations of Mg2+ prevented the monensin stimulation. The Ca2+ ionophore A23187 (75 nM) also required physiological concentrations of Na+ for the rapid induction of maximal acrosome reactions at an elevated pH (8.3) but did not require the presence of extracellular HCO3-. These studies suggest that a monovalent ionophore-induced rise in sperm intracellular Na+ concentrations is a pre-Ca2+ entry event, that stimulates an endogenous Ca2+/Na+ exchange that allows a Ca2+ influx which in turn induces the acrosome reaction. The possible regulatory role of the sperm intracellular pH and Na+, K+-ATPase during the capacitation process under physiological conditions is discussed.     

The role of HCO3- and Na+/H+ exchange in the response of rat parotid acinar cells to muscarinic stimulation

The intracellular pH (pHi) of a rat parotid acinar preparation was monitored using the pH-sensitive fluorescent dye, 2',7'-bis(2-carboxyethyl)-5(6)-carboxyfluorescein. Under resting (unstimulated) conditions both Na+/H+ exchange and CO2/HCO3- buffering contribute to the regulation of pHi. Muscarinic stimulation (carbachol) of the acini produced a gradual rise in pHi (approximately 0.1 unit by 10 min) possibly due to activation of the Na+/H+ exchanger. When the exchanger was blocked by amiloride or sodium removal, carbachol induced a dramatic (atropine inhibitable) decrease in pHi (approximately 0.4 pH unit with t1/2 approximately 0.5 min at 1 mM carbachol). The rate of this acidification was reduced by removal of exogenous HCO3- and by the carbonic anhydrase inhibitor methazolamide. Also, acini stimulated with carbachol in Cl- -free solutions showed a more pronounced acidification than in the corresponding Cl- -replete media. Taken together, these data indicate that the carbachol-induced acidification of rat parotid acinar cells unmasked by inhibition of the Na+/H+ exchanger is due to a rapid loss of intracellular HCO3-. Carbachol induced acidification was inhibited by the Cl- channel blocker diphenylamine 2-carboxylate but not by 4-acetomido-4'-isothiocyanostilbene-2,2'-disulfonic acid, an inhibitor of Cl-/HCO3- exchange. In addition, this acidification could not be sustained in Ca2+-free media and was totally blocked by chelation of intracellular Ca2+. Interpreted in terms of HCO3- loss, these results closely parallel the pattern of carbachol-induced Cl- release from this same preparation and indicate that HCO3- is secreted in response to muscarinic stimulation via the same or a very similar exit pathway, presumably an apical anion channel. Under normal physiological conditions the intracellular acidification resulting from HCO3- secretion is buffered by the Na+/H+ exchanger.     

Critical role of bicarbonate and bicarbonate transporters in cardiac function

Bicarbonate is one of the major anions in mammalian tissues and extracellular fluids. Along with accompanying H+, HCO3- is generated from CO2 and H2 O, either spontaneously or via the catalytic activity of carbonic anhydrase. It serves as a component of the major buffer system, thereby playing a critical role in pH homeostasis. Bicarbonate can also be utilized by a variety of ion transporters, often working in coupled systems, to transport other ions and organic substrates across cell membranes. The functions of HCO3- and HCO3--transporters in epithelial tissues have been studied extensively, but their functions in heart are less well understood. Here we review studies of the identities and physiological functions of Cl-/HCO3- exchangers and Na+/HCO3-cotransporters of the SLC4 A and SLC26 A families in heart. We also present RNA Seq analysis of their cardiac mRNA expression levels. These studies indicate that slc4a3(AE3) is the major Cl-/HCO3- exchanger and plays a protective role in heart failure, and that Slc4a4(NBCe1) is the major Na+/HCO3- cotransporter and affects action potential duration. In addition, previous studies show that HCO3- has a positive inotropic effect in the perfused heart that is largely independent of effects on intracellular Ca2+. The importance of HCO3- in the regulation of contractility is supported by experiments showing that isolated cardiomyocytes exhibit sharply enhanced contractility, with no change in Ca2+ transients, when switched from Hepes-buffered to HCO3-- buffered solutions. These studies demonstrate that HCO3- and HCO3--handling proteins play important roles in the regulation of cardiac function.     

Investigation of adenosinetriphosphatase activity of rat liver and thymus cell nuclei]

The activity of ATPase was studied in highly purified rat liver and thymus cell nuclei, HCO3-, CO3(2-) and SO3(2-) stimulated nuclear ATPase in 1.5--2 times. HSO3- did not affect the enzyme activity, and NO3-, J-, ClO4-,F- and SCN- inhibited it. Bicarbonate increased V and decreased Ka for ATP. SCN- inhibited HCO3--ATPase activity non-competitively with respect to HCO3-. Mg2+-ATPase activity did not depend on pH, and HCO3-component of the activity was decreased under alkaline pH. Mg2+, Mn2+ and Co2+ increased the initial ATPase activity and helped its stimulation with HCO3-. Ba2+, Ni2+ and Zn2+ inhibited the ATPase activity, and Ca2+ did not affect it, Nuclear ATPase is sensitive to 2,4-dinitrophenol and DNAase. It is suggested that cell nuclei have their own H+-ATPase differing for some characteristics from mitochondrial H+-ATPase.     

Quenching of Chlorophyll a Fluorescence in Response to Na+-Dependent HCO3- Transport-Mediated Accumulation of Inorganic Carbon in the Cyanobacterium Synechococcus UTEX 625

In the cyanobacterium Synechococcus UTEX 625, the yield of chlorophyll a fluorescence decreased in response to the transport-mediated accumulation of intracellular inorganic carbon (CO2 + HCO3- + CO32- = dissolved inorganic carbon [DIC]) and subsequently increased to a near-maximum level following photosynthetic depletion of the DIC pool. When DIC accumulation was mediated by the active Na+-dependent HCO3- transport system, the initial rate of fluorescence quenching was found to be highly correlated with the initial rate of H14CO3- transport (r = 0.96), and the extent of fluorescence quenching was correlated with the size of the internal DIC pool (r = 0.99). Na+-dependent HCO3- transport-mediated accumulation of DIC caused fluorescence quenching in either the presence or absence of the CO2 fixation inhibitor glycolaldehyde, indicating that quenching was not due simply to NADP+ reduction. The concentration of Na+ required to attain one-half the maximum rate of H14CO3- transport, at 20 [mu]M external HCO3-, declined from 9 to 1 mM as the external pH increased from 8 to 9.6. A similar pH dependency was observed when fluorescence quenching was used to determine the kinetic constants for HCO3- transport. In cells capable of Na+-dependent HCO3- transport, both the initial rate and extent of fluorescence quenching increased with increasing external HCO3-, saturating at about 150 [mu]M. In contrast Na+-independent HCO3- transport-mediated fluorescence quenching saturated at an HCO3- concentration of about 10 [mu]M. It was concluded that measurement of chlorophyll a fluorescence emission provided a convenient, but indirect, means of following Na+-dependent HCO3- transport and accumulation in Synechococcus.