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Effects of seawater pCO_2 and temperature on shell growth, shell stability, condition and cellular stress of Western Baltic Sea Mytilus edulis (L.) and Arctica islandica (L.)

机译:海水pCO_2和温度对西波罗的海紫草(Mytilus edulis(L.))和北极小岛(Arctica islandica(L.))的壳生长,壳稳定性,状况和细胞胁迫的影响

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摘要

Acidification of the World's oceans may directly impact reproduction, performance and shell formation of marine calcifying organisms. In addition, since shell production is costly and stress in general draws on an organism's energy budget, shell growth and stability of bivalves should indirectly be affected by environmental stress. The aim of this study was to investigate whether a combination of warming and acidification leads to increased physiological stress (lipofuscin accumulation and mortality) and affects the performance [shell growth, shell breaking force, condition index (C_i)] of young Mytilus edulis and Arctica islandica from the Baltic Sea. We cultured the bivalves in a fully-crossed 2-factorial experimental setup (seawater (sw) pCO_2 levels "low", "medium" and "high" for both species, temperature levels 7.5, 10,16, 20 and 25 ℃ for M. edulis and 7.5, 10 and 16 ℃ for A. islandica) for 13 weeks in summer. Mytilus edulis and A. islandica appeared to tolerate wide ranges of sw temperature and pCO_2. Lipofuscin accumulation of M. edulis increased with temperature while the C_i decreased, but shell growth of the mussels only sharply decreased while its mortality increased between 20 and 25 ℃. In A. islandica, lipofuscin accumulation increased with temperature, whereas the C_i, shell growth and shell breaking force decreased. The pCO_2 treatment had only marginal effects on the measured parameters of both bivalve species. Shell growth of both bivalve species was not impaired by under-saturation of the sea water with respect to aragonite and calcite. Furthermore, independently of water temperatures shell breaking force of both species and shell growth of A. islandica remained unaffected by the applied elevated sw pCO_2 for several months. Only at the highest temperature (25 ℃), growth arrest of M. edulis was recorded at the high sw pCO_2 treatment and the C_i of M. edulis was slightly higher at the medium sw pCO_2 treatment than at the low and high sw pCO_2 treatments. The only effect of elevated sw pCO_2 on A. islandica was an increase in lipofuscin accumulation at the high sw pCO_2 treatment compared to the medium sw pCO_2 treatment. Our results show that, despite this robustness, growth of both M. edulis and A. islandica can be reduced if sw temperatures remain high for several weeks in summer. As large body size constitutes an escape from crab and sea star predation, this can make bivalves presumably more vulnerable to predation-with possible negative consequences on population growth. In M. edulis, but not in A. islandica, this effect is amplified by elevated sw pCO_2. We follow that combined effects of elevated sw pCO_2 and ocean warming might cause shifts in future Western Baltic Sea community structures and ecosystem services; however, only if predators or other interacting species do not suffer as strong from these stressors.
机译:世界海洋的酸化可能直接影响海洋钙化生物的繁殖,性能和壳形成。此外,由于壳生产成本高昂,并且压力通常来自生物体的能量预算,因此壳生长和双壳类动物的稳定性应间接受到环境压力的影响。这项研究的目的是研究变暖和酸化的结合是否会导致生理压力(脂褐素的积累和死亡)的增加,并影响可食幼小紫贻贝和北极的性能[壳的生长,破壳力,状况指数(C_i)]波罗的海的小岛。我们在完全交叉的2因子实验装置中培养了双壳类动物(两个物种的海水(sw)pCO_2水平分别为“低”,“中”和“高”,M的温度水平分别为7.5、10、16、20和25℃)夏季在13个月内可食(7.5℃,10℃和16℃)。美味的Mytilus edulis和A. islandica耐受宽范围的sw温度和pCO_2。在20-25℃之间,贻贝的脂褐素积累随温度增加而C_i降低,但贻贝的壳生长仅急剧下降而死亡率增加。在岛南曲霉中,脂褐素积累随温度增加,而C_i,壳生长和壳破坏力降低。 pCO_2处理仅对两种双壳类物种的测量参数产生边际影响。海水对文石和方解石的欠饱和度不会损害两种双壳类物种的壳生长。此外,与水温无关,物种的壳破坏力和小岛曲霉的壳生长在数月内均不受施肥sw pCO_2的影响。仅在最高温度(25℃)下,在高sw pCO_2处理下才记录到了蓝靛果的生长停滞,在中等sw pCO_2处理下蓝靛果的C_i略高于在低sw pCO_2处理下的蓝靛果。与中等sw pCO_2处理相比,在高sw pCO_2处理下,升高的sw pCO_2对小岛曲霉的唯一影响是脂褐素积累的增加。我们的结果表明,尽管具有这种鲁棒性,但是如果夏季夏季气温保持较高水平,则可降低食用蓝藻和小岛曲霉的生长。由于较大的体形构成了逃避螃蟹和海星捕食活动的原因,因此这可能会使双壳类动物更容易受到捕食活动的影响,从而可能对人口增长产生负面影响。在可食的分支杆菌中,但在岛状曲霉中却没有,这种作用被升高的sw pCO_2所放大。我们认为,sw pCO_2升高和海洋变暖的综合影响可能会导致未来的西波罗的海群落结构和生态系统服务发生变化。但是,只有当捕食者或其他相互作用的物种没有受到这些压力源的强烈影响时,才可以。

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  • 来源
    《Marine biology》 |2013年第8期|2073-2087|共15页
  • 作者单位

    Helmholtz-Zentrum fuer Ozeanforschung, GEOMAR, Duesternbrooker Weg 20, 24105 Kiel, Germany;

    Institut fuer Klinische Molekularbiologie, Universitaetsklinikum Schleswig-Holstein, Christian-Albrechts-Universitaet zu Kiel, Schittenhelmstr. 12, 24105 Kiel, Germany;

    Helmholtz-Zentrum fuer Ozeanforschung, GEOMAR, Wischhofstr. 1-3, 24148 Kiel, Germany;

    Helmholtz-Zentrum fuer Ozeanforschung, GEOMAR, Duesternbrooker Weg 20, 24105 Kiel, Germany;

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