Hall B D, Aiken G R, Krabbenhoft D P, Marvin-Dipasquale M, Swarzenski C M
Environmental Chemistry and Technology Program, University of Wisconsin-Madison, Madison, WI 53706, USA.
Environ Pollut. 2008 Jul;154(1):124-34. doi: 10.1016/j.envpol.2007.12.017. Epub 2008 Feb 20.
It is widely recognized that wetlands, especially those rich in organic matter and receiving appreciable atmospheric mercury (Hg) inputs, are important sites of methylmercury (MeHg) production. Extensive wetlands in the southeastern United States have many ecosystem attributes ideal for promoting high MeHg production rates; however, relatively few mercury cycling studies have been conducted in these environments. We conducted a landscape scale study examining Hg cycling in coastal Louisiana (USA) including four field trips conducted between August 2003 and May 2005. Sites were chosen to represent different ecosystem types, including: a large shallow eutrophic estuarine lake (Lake Pontchartrain), three rivers draining into the lake, a cypress-tupelo dominated freshwater swamp, and six emergent marshes ranging from a freshwater marsh dominated by Panicum hemitomon to a Spartina alterniflora dominated salt marsh close to the Gulf of Mexico. We measured MeHg and total Hg (THg) concentrations, and ancillary chemical characteristics, in whole and filtered surface water, and filtered porewater. Overall, MeHg concentrations were greatest in surface water of freshwater wetlands and lowest in the profundal (non-vegetated) regions of the lake and river mainstems. Concentrations of THg and MeHg in filtered surface water were positively correlated with the highly reactive, aromatic (hydrophobic organic acid) fraction of dissolved organic carbon (DOC). These results suggest that DOC plays an important role in promoting the mobility, transport and bioavailability of inorganic Hg in these environments. Further, elevated porewater concentrations in marine and brackish wetlands suggest coastal wetlands along the Gulf Coast are key sites for MeHg production and may be a principal source of MeHg to foodwebs in the Gulf of Mexico. Examining the relationships among MeHg, THg, and DOC across these multiple landscape types is a first step in evaluating possible links between key zones for Hg(II)-methylation and the bioaccumulation of mercury in the biota inhabiting the Gulf of Mexico region.
人们普遍认识到,湿地,尤其是那些富含有机物质且接收大量大气汞(Hg)输入的湿地,是甲基汞(MeHg)产生的重要场所。美国东南部广袤的湿地具有许多有利于促进高甲基汞产生率的生态系统属性;然而,在这些环境中进行的汞循环研究相对较少。我们进行了一项景观尺度研究,考察美国路易斯安那州沿海地区的汞循环,包括在2003年8月至2005年5月期间进行的四次实地考察。选择的地点代表不同的生态系统类型,包括:一个大型浅水富营养化河口湖(庞恰特雷恩湖)、三条流入该湖的河流、一个以柏木-水紫树为主的淡水沼泽,以及六个从以半穗雀稗为主的淡水沼泽到靠近墨西哥湾以互花米草为主的盐沼的挺水沼泽。我们测量了整个地表水和过滤后的地表水以及过滤后的孔隙水中的甲基汞和总汞(THg)浓度以及辅助化学特征。总体而言,甲基汞浓度在淡水湿地的地表水中最高,在湖泊和河流主干的深层(无植被)区域最低。过滤后的地表水中总汞和甲基汞的浓度与溶解有机碳(DOC)的高反应性、芳香族(疏水性有机酸)部分呈正相关。这些结果表明,DOC在促进这些环境中无机汞的迁移、运输和生物可利用性方面起着重要作用。此外,海洋和咸淡水湿地中孔隙水浓度升高表明,墨西哥湾沿岸的沿海湿地是甲基汞产生的关键场所,可能是墨西哥湾食物网中甲基汞的主要来源。研究这些多种景观类型中甲基汞、总汞和DOC之间的关系,是评估汞(II)甲基化关键区域与墨西哥湾地区生物群中汞生物积累之间可能联系的第一步。