Lucas J M, Knapp L W
Department of Biological Sciences, University of South Carolina, Columbia, SC 29208, USA.
J Exp Biol. 1997 Oct;200(Pt 20):2653-62. doi: 10.1242/jeb.200.20.2653.
The union of calcium cations with carbonate anions to form calcium carbonate (CaCO3) is a fundamentally important physiological process of many marine invertebrates, in particular the corals. In an effort to understand the sources and processes of carbon uptake and subsequent deposition as calcium carbonate, a series of studies of the incorporation of 14C-labeled compounds into spicules was undertaken using the soft coral Leptogorgia virgulata. It has been surmised for some time that dissolved inorganic carbon in sea water is used in the biomineralization process. Furthermore, it was suspected that metabolically generated CO2 is also available for calcification. As a means of testing these possible sources of carbon in spicule calcification, key enzymes or transport systems in each pathway were inhibited. First, the enzyme carbonic anhydrase was specifically inhibited using acetazolamide. Second, the active transport of bicarbonate was inhibited using DIDS (4,4'-diisothiocyanato-stilbene-2,2'-disulfonic acid). Third, CO2 generation resulting from glycolysis and the citric acid cycle was arrested using iodoacetic acid, which interferes specifically with the enzyme glyceraldehyde-3-phosphate dehydrogenase. The results indicate that dissolved CO2 is the largest source of carbon used in the formation of calcitic sclerites, followed by HCO3- from dissolved inorganic carbon. In L. virgulata, the dissolved inorganic carbon is responsible for approximately 67% of the carbon in the sclerites. The other 33% comes from CO2 generated by glycolysis. Two important conclusions can be drawn from this work. First, carbon for spiculogenesis comes not only from dissolved inorganic carbon in the environment but also from metabolically produced carbon dioxide. While the latter has been theorized, it has never before been demonstrated in octocorals. Second, regardless of the carbon source, the enzyme carbonic anhydrase plays a pivotal role in the physiology of spicule formation in Leptogorgia virgulata.
钙阳离子与碳酸根阴离子结合形成碳酸钙(CaCO3)是许多海洋无脊椎动物,尤其是珊瑚的一个极其重要的生理过程。为了了解碳吸收及随后以碳酸钙形式沉积的来源和过程,利用软珊瑚细指海葵开展了一系列将14C标记化合物掺入骨针的研究。一段时间以来人们一直推测海水中溶解的无机碳用于生物矿化过程。此外,有人怀疑代谢产生的CO2也可用于钙化。作为测试骨针钙化中这些可能碳源的一种方法,每条途径中的关键酶或转运系统都受到了抑制。首先,使用乙酰唑胺特异性抑制碳酸酐酶。其次,使用4,4'-二异硫氰酸根合芪-2,2'-二磺酸(DIDS)抑制碳酸氢根的主动转运。第三,使用碘乙酸阻止糖酵解和柠檬酸循环产生CO2,碘乙酸特异性干扰甘油醛-3-磷酸脱氢酶。结果表明,溶解的CO2是形成钙质骨针所用碳的最大来源,其次是来自溶解无机碳的HCO3-。在细指海葵中,溶解的无机碳约占骨针中碳的67%。另外33%来自糖酵解产生的CO2。这项研究可以得出两个重要结论。第一,骨针形成所用的碳不仅来自环境中溶解的无机碳,也来自代谢产生的二氧化碳。虽然后者已有理论推测,但此前从未在八放珊瑚中得到证实。第二,无论碳源如何,碳酸酐酶在细指海葵骨针形成的生理过程中都起着关键作用。