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希腊西北部浅湖潘沃蒂斯湖近期的环境变化:来自沉积有机质、碳氢化合物和稳定同位素的证据

Recent environmental changes in the shallow Lake Pamvotis (NW Greece): evidence from sedimentary organic matter, hydrocarbons, and stable isotopes.

作者信息

Daskalou Victoria, Vreca Polona, Muri Gregor, Stalikas Constantine

机构信息

Department of Chemistry, University of Ioannina, Greece.

出版信息

Arch Environ Contam Toxicol. 2009 Jul;57(1):21-31. doi: 10.1007/s00244-008-9246-y. Epub 2008 Oct 19.

Abstract

Lake Pamvotis is a shallow Mediterranean lake located in northwestern Greece that has been recognized as an internationally important conservation site. Here, an unprecedented investigation was undertaken to obtain and evaluate data related to sedimentary organic matter, hydrocarbon content, and stable isotopes of Lake Pamvotis sediments, thus tracking the origin of organic inputs and providing a record of environmental status. The study revealed a distinct spatial distribution of polycyclic aromatic hydrocarbons (PAHs) with values between 34.7 and 1600 microg/kg and a rather uniform pattern for n-alkanes with concentrations falling below 41.4 microg/g. A significant contribution of an unresolved complex mixture indicated anthropogenic petroleum contamination. Further study of relevant indexes and geochemical biomarkers supported a mixed-source input of aliphatic hydrocarbons. With regard to PAHs, there was strong evidence that their dominant origin is pyrogenic. Finally, considerable excursion in delta(13)C(org) was attributed to changes in dissolved inorganic carbon accompanied by increased input of effluents and recycling of organic carbon within the lake, whereas the rise in isotopic composition of nitrogen was associated with agricultural runoff and sewage input from the town of Ioannina.

摘要

帕姆沃蒂斯湖是位于希腊西北部的一个浅水地中海湖泊,已被认定为具有国际重要性的保护地点。在此,开展了一项前所未有的调查,以获取和评估与帕姆沃蒂斯湖沉积物中的沉积有机质、碳氢化合物含量及稳定同位素相关的数据,从而追踪有机输入的来源并提供环境状况记录。研究揭示了多环芳烃(PAHs)的明显空间分布,其含量在34.7至1600微克/千克之间,而正构烷烃呈现出相当均匀的分布模式,浓度低于41.4微克/克。未解析复杂混合物的显著贡献表明存在人为石油污染。对相关指标和地球化学生物标志物的进一步研究支持了脂肪族碳氢化合物的混合源输入。关于多环芳烃,有强有力的证据表明其主要来源是热解成因。最后,δ(13)C(org)的显著偏移归因于溶解无机碳的变化,同时伴随着湖泊内废水输入增加和有机碳的再循环,而氮同位素组成的上升与约阿尼纳镇的农业径流和污水输入有关。

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