Wong Charles S, Pakdeesusuk Usarat, Morrissey Joshua A, Lee Cindy M, Coates John T, Garrison Arthur W, Mabury Scott A, Marvin Christopher H, Muir Derek C G
Department of Chemistry, University of Alberta, Edmonton, Alberta T6G 2G2, Canada.
Environ Toxicol Chem. 2007 Feb;26(2):254-63. doi: 10.1897/06-164r.1.
Enantiomer fractions (EFs) of seven chiral polychlorinated biphenyls (PCBs) were measured in dated sediment cores of Lake Hartwell (SC, USA) and Lake Ontario (USA) to detect, quantify, and gain insight regarding microbial reductive dechlorination of PCBs in lake sediments with high and low concentrations, respectively. Lake Hartwell sediments had high total PCBs (5-60 microg/g), with significantly nonracemic EFs that generally were consistent with those from previous laboratory microcosm reductive dechlorination experiments using sediments from these sites. Thus, stereoselective reductive dechlorination had occurred in situ, including at total PCB concentrations of less than the threshold of approximately 30 to 80 microg/g suggested as being necessary for reductive dechlorination. Enantiomer fractions of PCBs 91, 95, 132, and 136 in Lake Hartwell cores were significantly correlated both with concentrations of those individual congeners and with total PCB concentration for some sites. This result indicates that enantioselective microbial dechlorination activity increases with higher concentrations within sediments for these congeners. Enantiomer composition reversed with depth for PCBs 91, 132, and 176, suggesting that multiple microbial populations may be present within the same core that are enantioselectively dechlorinating PCBs. Such observations indicate that concentration and time are not the only factors affecting biotransformation, complicating prediction of enantioselectivity. Comparison of EFs with dates suggested biotransformation half-lives of approximately 30 years, which is on the same time scale as sequestration by burial. In contrast, Lake Ontario sediments (maximum total PCBs, 400 ng/g) had racemic or near-racemic amounts of most congeners throughout the core profile, which is consistent with achiral indicators suggesting no microbial biotransformation within Lake Ontario sediments. Thresholds for reductive dechlorination may exist, but they would be at concentrations of less than 30 to 80 microg/g.
在美国南卡罗来纳州的哈特韦尔湖和美国安大略湖的年代测定沉积物岩芯中,测量了七种手性多氯联苯(PCBs)的对映体分数(EFs),以分别检测、量化并深入了解高浓度和低浓度湖泊沉积物中多氯联苯的微生物还原脱氯情况。哈特韦尔湖沉积物中的多氯联苯总量较高(5 - 60微克/克),其对映体分数显著偏离外消旋,总体上与之前使用这些地点沉积物进行的实验室微观还原脱氯实验结果一致。因此,原位发生了立体选择性还原脱氯,包括在多氯联苯总浓度低于约30至80微克/克的阈值时,而该阈值被认为是还原脱氯所必需的。哈特韦尔湖岩芯中多氯联苯91、95、132和136的对映体分数,在某些地点与这些单个同系物的浓度以及多氯联苯总浓度均显著相关。这一结果表明,对于这些同系物而言,沉积物中对映选择性微生物脱氯活性随浓度升高而增加。多氯联苯91、132和176的对映体组成随深度发生逆转,这表明同一岩芯中可能存在多个对多氯联苯进行对映选择性脱氯的微生物种群。这些观察结果表明,浓度和时间并非影响生物转化的唯一因素,这使得对映选择性的预测变得复杂。将对映体分数与年代进行比较表明,生物转化半衰期约为30年,这与通过埋藏进行封存的时间尺度相同。相比之下,安大略湖沉积物(多氯联苯总量最高为400纳克/克)在整个岩芯剖面中大多数同系物的对映体为外消旋或接近外消旋,这与非手性指标一致,表明安大略湖沉积物中没有微生物生物转化。还原脱氯可能存在阈值,但它们将低于30至80微克/克的浓度。