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Measurements of the stable carbon isotope composition of dissolved inorganic carbon in the northeastern Atlantic and Nordic Seas during summer 2012

机译:2012年夏季东北大西洋和北欧海域溶解无机碳稳定碳同位素组成的测量

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摘要

The stable carbon isotope composition of dissolved inorganic carbon (?13CDIC) in seawater was measured in a batch process for 552 samples collected during two cruises in the northeastern Atlantic and Nordic Seas from June to August 2012. One cruise was part of the UK Ocean Acidification research programme, and the other was a repeat hydrographic transect of the Extended Ellett Line. In combination with measurements made of other variables on these and other cruises, these data can be used to constrain the anthropogenic component of dissolved inorganic carbon (DIC) in the interior ocean, and to help to determine the influence of biological carbon uptake on surface ocean carbonate chemistry. The measurements have been processed, quality-controlled and submitted to an in-preparation global compilation of seawater ?13CDIC data, and are available from the British Oceanographic Data Centre. The observed ?13CDIC values fall in a range from ?0.58 to +2.37 ‰, relative to the Vienna Pee Dee Belemnite standard. The mean of the absolute differences between samples collected in duplicate in the same container type during both cruises and measured consecutively is 0.10 ‰, which corresponds to a 1? uncertainty of 0.09 ‰, and which is within the range reported by other published studies of this kind. A crossover analysis was performed with nearby historical ?13CDIC data, indicating that any systematic offsets between our measurements and previously published results are negligible.
机译:在2012年6月至2012年8月于东北大西洋和北欧海的两次航行中,通过分批过程测量了552个样品的海水中溶解的无机碳(?13CDIC)的稳定碳同位素组成。一次航行是英国海洋酸化的一部分研究计划,另一个是Extended Ellett Line的重复水文横断面。结合在这些航行和其他航行中对其他变量进行的测量,这些数据可用于约束内部海洋中人为溶解的无机碳(DIC)的人为成分,并有助于确定生物碳吸收对表层海洋的影响碳酸盐化学。这些测量值已经过处理,质量控制,并已提交给准备中的全球海水13CDIC数据汇编,可从英国海洋学数据中心获得。相对于Vienna Pee Dee Belemnite标准,观测到的?13CDIC值在?0.58至+2.37‰的范围内。在两次巡航期间,在同一容器类型中一式两份采集并连续测量的样品之间的绝对差的平均值为0.10‰,对应于1?不确定度为0.09‰,并且在其他此类已发表研究报告的范围内。使用附近的历史Δ13CDIC数据进行了交叉分析,表明我们的测量值与先前发表的结果之间的任何系统性偏差都可以忽略不计。

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