“利用微型ct扫描评估卡里亚科盆地翼足类膨胀Heliconoides inflatus壳厚度的年度变化”补充材料

R. Oakes, J. Sessa
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引用次数: 2

摘要

摘要翼足类动物被戏称为海洋酸化的“煤矿金丝雀”,因为据预测,它们是首批受到未来海洋化学变化影响的生物之一。这是由于它们脆弱的文石壳和在极地和亚极地地区的高丰度,海洋酸化的影响将首先表现出来。为了最有效地利用翼足类作为海洋酸化的指标,需要对它们在现代海洋中的自然变异性进行量化和了解。在这里,我们测量了近50个来自委内瑞拉卡里亚科盆地沉积物陷阱的翼足类Heliconoides inflatus标本的壳状态(即壳溶解的程度)和壳特征,包括大小、轮数、壳厚度和壳体积(即壳材料的数量)。由于热带辐合带(ITCZ)的运动,Cariaco盆地的水全年处于文石饱和状态,水文和化学性质随季节而变化。采用Limacina溶出指数(LDX)和不透明度法评价壳条件。不透明度法只捕捉到溶解早期的壳态变化,而LDX法记录的溶解变化范围要大得多。壳的状态不随时间的延长而恶化。相反,在水温最温暖的9月和10月收集的样本中,壳的变化最多,水柱中有机物降解的数量可能是最大的。一年四季,膨胀螺的壳在大小、轮数和厚度上都有变化。螺轮的数量与壳的直径无关,这表明壳的生长是可塑的。与从少营养雨季取样的标本相比,在上升流期间营养浓度高时,膨胀螺形成的壳厚40%,直径大20%。本研究建立了加勒比海盆地翼足类贝壳特征变异的基线数据集,并建立了一种方法,用于生成全球翼足类种群的类似基线记录。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Supplementary material to "Assessing annual variability in the shell thickness of the pteropod Heliconoides inflatus in the Cariaco Basin using micro-CT scanning"
Abstract. Pteropods have been nicknamed the canary in the coal mine for ocean acidification because they are predicted to be among the first organisms to be affected by future changes in ocean chemistry. This is due to their fragile, aragonitic shells and high abundances in polar and sub-polar regions where the impacts of ocean acidification will manifest first. For pteropods to be used most effectively as indicators of ocean acidification, their natural variability in the modern ocean needs to be quantified and understood. Here, we measured the shell condition (i.e., the degree to which a shell has dissolved) and shell characteristics, including size, number of whorls, shell thickness, and shell volume (i.e., amount of shell material) of nearly fifty specimens of the pteropod species Heliconoides inflatus from a sediment trap in the Cariaco Basin, Venezuela sampled over an 11-month period. The water in the Cariaco Basin is supersaturated with respect to aragonite year-round, and hydrographic and chemical properties vary seasonally due to the movement of the Inter Tropical Convergence Zone (ITCZ). Shell condition was assessed using with two methods: the Limacina Dissolution Index (LDX) and the opacity method. The opacity method captured changes in shell condition only in the early stages of dissolution, whereas the LDX recorded dissolution changes over a much larger range. Shell condition did not deteriorate with the length of time in the sediment trap. Instead, the most altered shells occurred in samples collected in September and October when water temperatures were warmest, and the amount of organic matter degradation in the water column was likely to have been the greatest. Shells of H. inflatus varied in size, number of whorls, and thickness throughout the year. The number of whorls did not correlate with shell diameter, suggesting that shell growth is plastic. H. inflatus formed shells that were 40 % thicker and 20 % larger in diameter when nutrient concentrations were high during times of upwelling, compared to specimens sampled from the oligotrophic rainy season. This study produces a baseline dataset of the variability in shell characteristics of H. inflatus in the Cariaco Basin and establishes a methodology for generating similar baseline records for pteropod populations globally.
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