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波西多尼亚海草海洋沉积物记录:全新世重金属污染档案。

The Posidonia oceanica marine sedimentary record: A Holocene archive of heavy metal pollution.

机构信息

Centro de Estudios Avanzados de Blanes, c/Accés a la Cala St. Francesc, 14. 17300 Blanes, Girona, Spain.

出版信息

Sci Total Environ. 2011 Oct 15;409(22):4831-40. doi: 10.1016/j.scitotenv.2011.08.001. Epub 2011 Sep 1.

Abstract

The study of a Posidonia oceanica mat (a peat-like marine sediment) core has provided a record of changes in heavy metal abundances (Fe, Mn, Ni, Cr, Cu, Pb, Cd, Zn, As and Al) since the Mid-Holocene (last 4470yr) in Portlligat Bay (NW Mediterranean). Metal contents were determined in P. oceanica. Both, the concentration records and the results of principal components analysis showed that metal pollution in the studied bay started ca. 2800yr BP and steadily increased until present. The increase in Fe, Cu, Pb, Cd, Zn and As concentrations since ca. 2800yr BP and in particular during Greek (ca. 2680-2465cal BP) and Roman (ca. 2150-1740cal BP) times shows an early anthropogenic pollution rise in the bay, which might be associated with large- and short-scale cultural and technological development. In the last ca. 1000yr the concentrations of heavy metals, mainly derived from anthropogenic activities, have significantly increased (e.g. from ~15 to 47μg g(-1) for Pb, ~23 to 95μg g(-1) for Zn and ~8 to 228μg g(-1) for As). Our study demonstrates for the first time the uniqueness of P. oceanica meadows as long-term archives of abundances, patterns, and trends of heavy metals during the Late Holocene in Mediterranean coastal ecosystems.

摘要

对波蒂略湾(西北地中海)中一片海草床(类似于泥炭的海洋沉淀物)岩芯的研究提供了从中世纪中期(距今 4470 年)以来重金属丰度(铁、锰、镍、铬、铜、铅、镉、锌、砷和铝)变化的记录。对波西多尼亚海草中的金属含量进行了测定。浓度记录和主成分分析的结果均表明,研究湾的金属污染始于约 2800 年前,并持续增加至今。自约 2800 年前以来,铁、铜、铅、镉、锌和砷浓度的增加,特别是在希腊时期(约公元前 2680-2465 年)和罗马时期(约公元前 2150-1740 年),表明湾内存在早期人为污染上升的情况,这可能与大规模和短期的文化和技术发展有关。在过去约 1000 年里,主要源自人为活动的重金属浓度显著增加(例如,铅的浓度从约 15 微克/克增加到 47 微克/克,锌的浓度从约 23 微克/克增加到 95 微克/克,砷的浓度从约 8 微克/克增加到 228 微克/克)。本研究首次证明,波西多尼亚海草床作为地中海沿海生态系统晚全新世重金属丰度、模式和趋势的长期档案具有独特性。

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