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首页> 外文期刊>Climate of the past >An inter-laboratory investigation of the Arctic sea ice biomarker proxy IP_(25) in marine sediments: key outcomes and recommendations
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An inter-laboratory investigation of the Arctic sea ice biomarker proxy IP_(25) in marine sediments: key outcomes and recommendations

机译:北极海洋沉积物中北极海冰生物标志物代理IP_(25)的实验室间研究:主要成果和建议

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摘要

We describe the results of an inter-laboratory investigation into the identification and quantification of the Arctic sea ice biomarker proxy IP_(25) in marine sediments. Seven laboratories took part in the study, which consisted of the analysis of IP_(25) in a series of sediment samples from different regions of the Arctic, sub-Arctic and Antarctic, additional sediment extracts and purified standards. The results obtained allowed 4 key outcomes to be determined. First, IP_(25) was identified by all laboratories in sediments from the Canadian Arctic with inter-laboratory variation in IP_(25) concentration being substantially larger than within individual laboratories. This greater variation between laboratories was attributed to the difficulty in accurately determining instrumental response factors for IP_(25), even though laboratories were supplied with appropriate standards. Second, the identification of IP_(25) by 3 laboratories in sediment from SW Iceland that was believed to represent a blank, was interpreted as representing a better limit of detection or quantification for such laboratories, contamination or mis-identification. These alternatives could not be distinguished conclusively with the data available, although it is noted that the precision of these data was significantly poorer compared with the other IP_(25) concentration measurements. Third, 3 laboratories reported the occurrence of IP_(25) in a sediment sample from the Antarctic Peninsula even though this biomarker is believed to be absent from the Southern Ocean. This anomaly is attributed to a combined chromatographic and mass spectrometric interference that results from the presence of a di-unsaturated highly branched isoprenoid (HBI) pseudo-homologue of IP_(25) that occurs in Antarctic sediments. Finally, data are presented that suggest that extraction of IP_(25) is consistent between Accelerated Solvent Extraction (ASE) and sonication methods and that IP_(25) concentrations based on 7-hexylnonadecane as an internal standard are comparable using these methods. Recoveries of some more unsaturated HBIs and the internal standard 9-octylheptadecene, however, were lower with the ASE procedure, possibly due to partial degradation of these more reactive chemicals as a result of higher temperatures employed with this method. For future measurements, we recommend the use of reference sediment material with known concentration(s) of IP_(25) for determining and routinely monitoring instrumental response factors. Given the significance placed on the presence (or otherwise) of IP_(25) in marine sediments, some further recommendations pertaining to quality control are made that should also enable the two main anomalies identified here to be addressed.
机译:我们描述了对海洋沉积物中北极海冰生物标志物代理IP_(25)的鉴定和量化的实验室间调查结果。七个实验室参与了这项研究,其中包括对来自北极,亚北极和南极不同地区的一系列沉积物样品,其他沉积物提取物和纯化标准液中IP_(25)的分析。获得的结果可以确定4个关键结果。首先,所有实验室在加拿大北极地区的沉积物中鉴定出IP_(25),实验室间IP_(25)浓度的变化比单个实验室大得多。实验室之间更大的差异归因于即使为实验室提供了适当的标准,也难以准确确定IP_(25)的仪器响应因子。其次,被认为来自冰岛西南部的沉积物中3个实验室对IP_(25)的识别被认为是空白,这被解释为对此类实验室,污染物或错误识别的更好的检测或定量限制。尽管要注意的是,与其他IP_(25)浓度测量相比,这些数据的精度明显较差,但这些替代方法无法与可用数据进行最终区分。第三,尽管据认为该生物标记物在南大洋中不存在,但有3个实验室报告了南极半岛沉积物样品中IP_(25)的发生。该异常归因于南极沉积物中IP_(25)的双不饱和高支化类异戊二烯(HBI)假同源物的存在,导致色谱和质谱相结合。最后,提供的数据表明,加速溶剂萃取(ASE)和超声处理方法之间IP_(25)的萃取是一致的,并且使用这些方法可比较基于7-己基壬二烷作为内标的IP_(25)浓度。但是,采用ASE方法,一些不饱和HBI和内标9-辛基十七碳烯的回收率较低,这可能是由于该方法采用较高的温度导致这些更具活性的化学物质部分降解。对于将来的测量,我们建议使用已知浓度为IP_(25)的参考沉积物来确定和常规监测仪器响应因子。考虑到对海洋沉积物中IP_(25)的存在(或其他方面)的重要性,提出了一些与质量控制有关的其他建议,这些建议还应能够解决此处确定的两个主要异常。

著录项

  • 来源
    《Climate of the past》 |2014年第1期|155-166|共12页
  • 作者单位

    Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK;

    Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK;

    Department of Geological Sciences, Stockholm University, 106 91 Stockholm, Sweden;

    Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK;

    Alfred Wegener Institute for Polar and Marine Research, Am Alten Hafen 26, 27568 Bremerhaven, Germany;

    Department of Geosciences, University of Massachusetts Amherst, Amherst, MA 01075, USA;

    UMI 3376 TAKUVIK, CNRS & Universite Laval, 1045 Avenue de la Medecine, G1V 0A6 Quebec, Canada;

    Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK;

    MOE Key Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing 100871, PR China;

    MOE Key Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing 100871, PR China;

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