Byrne Maria, Fitzer Susan
School of Medical Science and School of Life and Environmental Science, The University of Sydney, NSW 2006, Australia.
Institute of Aquaculture, University of Stirling, Stirling, FK9 4LA, UK.
Conserv Physiol. 2019 Nov 11;7(1):coz062. doi: 10.1093/conphys/coz062. eCollection 2019.
Ocean acidification (OA), from seawater uptake of anthropogenic CO has a suite of negative effects on the ability of marine invertebrates to produce and maintain their skeletons. Increased organism CO causes hypercapnia, an energetically costly physiological stress. OA alters seawater carbonate chemistry, limiting the carbonate available to form the calcium carbonate (CaCO) minerals used to build skeletons. The reduced saturation state of CaCO also causes corrosion of CaCO structures. Global change is also accelerating coastal acidification driven by land-run off (e.g. acid soil leachates, tannic acid). Building and maintaining marine biomaterials in the face of changing climate will depend on the balance between calcification and dissolution. Overall, in response to environmental acidification, many calcifiers produce less biomineral and so have smaller body size. Studies of skeleton development in echinoderms and molluscs across life stages show the stunting effect of OA. For corals, linear extension may be maintained, but at the expense of less dense biomineral. Conventional metrics used to quantify growth and calcification need to be augmented by characterisation of the changes to biomineral structure and mechanical integrity caused by environmental acidification. Scanning electron microscopy and microcomputed tomography of corals, tube worms and sea urchins exposed to experimental (laboratory) and natural (vents, coastal run off) acidification show a less dense biomineral with greater porosity and a larger void space. For bivalves, CaCO crystal deposition is more chaotic in response to both ocean and coastal acidification. Biomechanics tests reveal that these changes result in weaker, more fragile skeletons, compromising their vital protective roles. Vulnerabilities differ among taxa and depend on acidification level. Climate warming has the potential to ameliorate some of the negative effects of acidification but may also make matters worse. The integrative morphology-ecomechanics approach is key to understanding how marine biominerals will perform in the face of changing climate.
海洋酸化(OA)是由于海水吸收人为排放的二氧化碳所致,它对海洋无脊椎动物生成和维持其骨骼的能力产生一系列负面影响。生物体二氧化碳增加会导致高碳酸血症,这是一种耗能巨大的生理应激。海洋酸化改变了海水碳酸盐化学性质,限制了用于形成构建骨骼的碳酸钙(CaCO₃)矿物的碳酸盐。碳酸钙饱和度降低还会导致碳酸钙结构的腐蚀。全球变化也在加速由陆地径流(如酸性土壤渗滤液、单宁酸)驱动的沿海酸化。面对气候变化构建和维持海洋生物材料将取决于钙化和溶解之间的平衡。总体而言,为应对环境酸化,许多钙化生物产生的生物矿物减少,因此体型较小。对棘皮动物和软体动物整个生命阶段骨骼发育的研究表明了海洋酸化的发育迟缓效应。对于珊瑚来说,可能会维持线性生长,但代价是生物矿物密度降低。用于量化生长和钙化的传统指标需要通过表征环境酸化引起的生物矿物结构和机械完整性变化来加以补充。对暴露于实验(实验室)和自然( vents、沿海径流)酸化环境下的珊瑚、管虫和海胆进行扫描电子显微镜和微型计算机断层扫描显示,生物矿物密度较低,孔隙率更高,空隙空间更大。对于双壳类动物,碳酸钙晶体沉积在应对海洋和沿海酸化时更加混乱。生物力学测试表明,这些变化导致骨骼更脆弱,从而损害了它们至关重要的保护作用。不同分类群的脆弱性各不相同,并取决于酸化程度。气候变暖有可能减轻酸化的一些负面影响,但也可能使情况变得更糟。综合形态学 - 生态力学方法是理解海洋生物矿物在气候变化面前将如何表现的关键。