Grosell M, Genz J
Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, 4600 Rickenbacker Causeway, Miami, FL 33149-1098, USA.
Am J Physiol Regul Integr Comp Physiol. 2006 Oct;291(4):R1145-56. doi: 10.1152/ajpregu.00818.2005. Epub 2006 May 18.
The gulf toadfish (Opsanus beta) intestine secretes base mainly in the form of HCO3- via apical anion exchange to serve Cl- and water absorption for osmoregulatory purposes. Luminal HCO3- secretion rates measured by pH-stat techniques in Ussing chambers rely on oxidative energy metabolism and are highly temperature sensitive. At 25 degrees C under in vivo-like conditions, secretion rates averaged 0.45 micromol x cm(-2) x h(-1), of which 0.25 micromol x cm(-2) x h(-1) can be accounted for by hydration of endogenous CO2 partly catalyzed by carbonic anhydrase. Complete polarity of secretion of HCO3- and H+ arising from the CO2 hydration reaction is evident from equal rates of luminal HCO3- secretion via anion exchange and basolateral H+ extrusion. When basolateral H+ extrusion is partly inhibited by reduction of serosal pH, luminal HCO3- secretion is reduced. Basolateral H+ secretion occurs in exchange for Na+ via an ethylisopropylamiloride-insensitive mechanism and is ultimately fueled by the activity of the basolateral Na+-K+-ATPase. Fluid absorption by the toadfish intestine to oppose diffusive water loss to the concentrated marine environment is accompanied by a substantial basolateral H+ extrusion, intimately linking osmoregulation and acid-base balance.
海湾蟾鱼(Opsanus beta)的肠道主要通过顶端阴离子交换以HCO3-的形式分泌碱,以促进Cl-和水的吸收,从而实现渗透调节。在Ussing室中,通过pH计技术测量的管腔HCO3-分泌速率依赖于氧化能量代谢,并且对温度高度敏感。在25摄氏度的类似体内条件下,分泌速率平均为0.45微摩尔×厘米-2×小时-1,其中0.25微摩尔×厘米-2×小时-1可归因于部分由碳酸酐酶催化的内源性CO2的水合作用。由CO2水合反应产生的HCO3-和H+分泌的完全极性,从通过阴离子交换的管腔HCO3-分泌速率和基底外侧H+排出速率相等中可以明显看出。当通过降低浆膜pH部分抑制基底外侧H+排出时,管腔HCO3-分泌减少。基底外侧H+分泌通过一种对乙基异丙基amiloride不敏感的机制与Na+进行交换,最终由基底外侧Na+-K+-ATP酶的活性提供能量。蟾鱼肠道吸收液体以对抗向浓缩海洋环境的扩散性失水,同时伴随着大量的基底外侧H+排出,这将渗透调节和酸碱平衡紧密联系在一起。