School of Natural Sciences & Centre for Marine Ecosystems Research, Faculty of Health, Engineering and Science, Edith Cowan University, Joondalup 6027, WA, Australia; The UWA Oceans Institute, The University of Western Australia, Crawley, WA, Australia.
School of Natural Sciences & Centre for Marine Ecosystems Research, Faculty of Health, Engineering and Science, Edith Cowan University, Joondalup 6027, WA, Australia.
Sci Total Environ. 2016 Jan 15;541:883-894. doi: 10.1016/j.scitotenv.2015.09.017. Epub 2015 Oct 2.
The study of a Posidonia australis sedimentary archive has provided a record of changes in element concentrations (Al, Fe, Mn, Pb, Zn, Cr, Cd, Co, As, Cu, Ni and S) over the last 3000 years in the Australian marine environment. Human-derived contamination in Oyster Harbor (SW Australia) started ~100 years ago (AD ~1900) and exponentially increased until present. This appears to be related to European colonization of Australia and the subsequent impact of human activities, namely mining, coal and metal production, and extensive agriculture. Two contamination periods of different magnitude have been identified: Expansion period (EXP, AD ~1900-1970) and Establishment period (EST, AD ~1970 to present). Enrichments of chemical elements with respect to baseline concentrations (in samples older than ~115 cal years BP) were found for all elements studied in both periods, except for Ni, As and S. The highest enrichment factors were obtained for the EST period (ranging from 1.3-fold increase in Cu to 7.2-fold in Zn concentrations) compared to the EXP period (1.1-fold increase for Cu and Cr to 2.4-fold increase for Pb). Zinc, Pb, Mn and Co concentrations during both periods were 2- to 7-fold higher than baseline levels. This study demonstrates the value of Posidonia mats as long-term archives of element concentrations and trends in coastal ecosystems. We also provide preliminary evidence on the potential for Posidonia meadows to act as significant long-term biogeochemical sinks of chemical elements.
对波西多尼亚海草(Posidonia australis)沉积档案的研究提供了过去 3000 年来澳大利亚海洋环境中元素浓度(Al、Fe、Mn、Pb、Zn、Cr、Cd、Co、As、Cu、Ni 和 S)变化的记录。牡蛎港(澳大利亚西南部)的人为污染始于大约 100 年前(公元 1900 年),并呈指数增长,一直持续到现在。这似乎与澳大利亚的欧洲殖民化以及随后人类活动的影响有关,即采矿、煤炭和金属生产以及广泛的农业。已经确定了两个不同规模的污染期:扩张期(EXP,公元 1900-1970 年)和建立期(EST,公元 1970 年至今)。在两个时期中,除了 Ni、As 和 S 之外,所有研究元素相对于基线浓度(在早于约 115 年的样本中)都出现了化学元素的富集。在 EST 期间(Cu 浓度增加了 1.3 倍,Zn 浓度增加了 7.2 倍)与 EXP 期间(Cu 和 Cr 增加了 1.1 倍,Pb 增加了 2.4 倍)相比,最高的富集因子出现在 EST 期间。在两个时期中,Zn、Pb、Mn 和 Co 的浓度比基线水平高 2-7 倍。本研究证明了波西多尼亚海草垫作为沿海生态系统中元素浓度和趋势的长期档案的价值。我们还提供了波西多尼亚草甸可能作为重要的长期生物地球化学元素汇的初步证据。