...
首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Multi-biomarker characterization of sedimentary organic carbon in small rivers draining the Northwestern United States
【24h】

Multi-biomarker characterization of sedimentary organic carbon in small rivers draining the Northwestern United States

机译:美国西北部小河中沉积有机碳的多生物标志物表征

获取原文
获取原文并翻译 | 示例
           

摘要

The sources of sedimentary organic carbon in various river systems draining the Pacific Northwest (USA) were assessed using a biomarker approach. Sediment samples were collected in creeks and small rivers from Oregon and Washington states (Cascades and Coastal Range ecoregions) and analyzed as total and silylated total extracts using gas chromatography-mass spectrometry (GC-MS). In general, the individual organic compounds were similar in the river samples from both the Cascades and the Coast Range, with apparent higher averaged abundances (normalized to organic carbon content) observed for the Cascades sediments. Major contributions in the river samples were from sterols and triterpenoids derived mainly from the vegetation bordering the rivers, followed by n-alkanols and n-alkanes from epicuticular plant wax. Fatty acids (16:0, 16:1, 18:0, 18:1, 18:2), cholesterol, monoacylglycerols (e.g., 1-O-hexadecanoyl glycerol) and glucose were important organic tracers detected especially in higher altitude systems, presumably due to autochthonous production, namely from algal blooms during late spring. Resin acids (e.g., dehydroabietic acid, a biomarker for conifers) were expected to be the major tracer input to these sediments. However, diterpenoids were detected in significant amounts only at sites directly bordering conifer forests, suggesting that those compounds are not transported downstream during normal river flow. (c) 2007 Elsevier Ltd. All rights reserved.
机译:使用生物标记法评估了西北太平洋(美国)的各种河流系统中沉积有机碳的来源。在俄勒冈州和华盛顿州(喀斯喀特和沿海山脉生态区)的小河和小河中收集了沉积物样品,并使用气相色谱-质谱法(GC-MS)分析了总提取物和甲硅烷基化的总提取物。通常,在喀斯喀特山脉和海岸山脉的河流样本中,单个有机化合物是相似的,并且在喀斯喀特山脉的沉积物中观测到的平均平均丰度(相对于有机碳含量标准化)明显更高。河流样品的主要贡献来自主要来自河流沿岸植被的固醇和三萜类化合物,其次是来自表皮植物蜡的正构烷醇和正构烷烃。脂肪酸(16:0、16:1、18:0、18:1、18:2),胆固醇,单酰基甘油(例如1-O-十六烷酰甘油)和葡萄糖是重要的有机示踪剂,尤其是在高海拔系统中,大概是由于自生,即春末的藻华。预计树脂酸(例如,脱氢松香酸,一种针叶树的生物标记)将成为这些沉积物中主要的示踪剂输入。但是,仅在与针叶林直接接壤的地点才检测到大量的二萜类化合物,这表明这些化合物在正常河水流动期间并未被下游输送。 (c)2007 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号