Centre for Earth Observation Sciences (CEOS), Department of Environment and Geography, University of Manitoba, Winnipeg, Canada; Environmental & Resource Studies Program, Trent University, Peterborough, Canada.
Centre for Earth Observation Sciences (CEOS), Department of Environment and Geography, University of Manitoba, Winnipeg, Canada.
Sci Total Environ. 2015 Feb 15;506-507:430-43. doi: 10.1016/j.scitotenv.2014.11.002. Epub 2014 Nov 26.
With declining sea ice conditions in Arctic regions owing to changing climate, the large prospective reservoirs of oil and gas in Baffin Bay and Davis Strait are increasingly accessible, and the interest in offshore exploration and shipping through these regions has increased. Both of these activities are associated with the risk of hydrocarbon releases into the marine ecosystem. However, hydrocarbons are also present naturally in marine environments, in some cases deriving from oil seeps. We have analyzed hydrocarbon concentrations in eleven sediment cores collected from northern Baffin Bay during 2008 and 2009 Amundsen expeditions and have examined the hydrocarbon compositions in both pre- and post-industrial periods (i.e., before and after 1900) to assess the sources of hydrocarbons, and their temporal and spatial variabilities. Concentrations of ΣPAHs ranged from 341 to 2693 ng g(-1) dw, with concentrations in cores from sites within the North Water (NOW) Polynya generally higher. Individual PAH concentrations did not exceed concentrations of concern for marine aquatic life, with one exception found in a core collected within the NOW (one of the seven sediment core samples). Hydrocarbon biomarkers, including alkane profiles, OEP (odd-to-even preference), and TAR (terrigenous/aquatic ratios) values indicated that organic carbon at all sites is derived from both terrigenous higher plants and marine algae, the former being of greater significance at coastal sites, and the latter at the deepest sites at the southern boundary of the NOW. Biomarker ratios and chemical profiles indicate that petrogenic sources dominate over combustion sources, and thus long-range atmospheric transport is less significant than inputs from weathering. Present-day and historic pre-1900 hydrocarbon concentrations exhibited less than an order of magnitude difference for most compounds at all sites. The dataset presented here provides a baseline record of hydrocarbon concentrations in Baffin Bay sediments in advance of offshore exploration and increased shipping activities.
由于气候变化,北极地区的海冰条件正在下降,巴芬湾和戴维斯海峡的大量潜在石油和天然气储量越来越容易获得,对这些地区的近海勘探和航运的兴趣也有所增加。这两种活动都伴随着碳氢化合物释放到海洋生态系统中的风险。然而,碳氢化合物在海洋环境中也自然存在,有些来自石油渗漏。我们分析了 2008 年和 2009 年阿蒙森探险队在巴芬湾北部采集的 11 个沉积物岩芯中的碳氢化合物浓度,并检查了工业前和工业后(即 1900 年之前和之后)的碳氢化合物组成,以评估碳氢化合物的来源及其时空变异性。ΣPAHs 的浓度范围为 341-2693ng g(-1)dw,北水域(NOW)Polynyas 内的站点的浓度通常较高。个别 PAH 浓度没有超过对海洋水生生物的关注浓度,只有一个例外是在 NOW 内采集的岩芯中发现的(七个沉积物岩芯样本之一)。碳氢化合物生物标志物,包括烷烃分布、OEP(奇数对偶数偏好)和 TAR(陆源/水生比值)值表明,所有站点的有机碳均来自陆生高等植物和海洋藻类,前者在沿海站点更为重要,后者在 NOW 南部边界的最深站点更为重要。生物标志物比值和化学分布表明,生源碳氢化合物源占主导地位,燃烧源的影响较小,因此长距离大气传输的重要性小于风化输入。在大多数情况下,目前和历史上 1900 年前的碳氢化合物浓度在所有站点的大多数化合物中都没有相差一个数量级。本数据集提供了巴芬湾沉积物中碳氢化合物浓度的基线记录,以便在进行近海勘探和增加航运活动之前进行记录。