Unionid shells (Hyriopsis cumingii) record manganese cycling at the sediment-water interface in a shallow eutrophic lake in China (Lake Taihu)

被引:29
|
作者
Zhao, Liqiang [1 ]
Walliser, Eric O. [1 ]
Mertz-Kraus, Regina [1 ]
Schoene, Bernd R. [1 ]
机构
[1] Johannes Gutenberg Univ Mainz, Inst Geosci, Joh J Becher Weg 21, D-55128 Mainz, Germany
关键词
Bivalve shell; Manganese-to-calcium ratio; Manganese biogeochemistry; Sediment-water interface; Eutrophication; Lake Taihu; TRACE-ELEMENT ANALYSIS; FRESH-WATER; ICP-MS; METAL BIOAVAILABILITY; CYANOBACTERIAL BLOOMS; AQUATIC ENVIRONMENTS; MARINE ECOSYSTEMS; CRASSOSTREA-GIGAS; COASTAL WATERS; PECTEN-MAXIMUS;
D O I
10.1016/j.palaeo.2017.03.010
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Aquatic eutrophication is becoming a serious environmental problem throughout the world. The utility of bi-valves as bio-filters to improve water quality and reduce algal blooms has been widely acknowledged, but the potential usefulness of bivalve shells as retrospective monitors of eutrophication-induced environmental change has received little attention. Here, we present the first multi-year, high-resolution Mn/Ca-shell records of the freshwater mussel, Hyriopsis cumingii (Lea, 1852) from a shallow eutrophic lake (Lake Taihu, China). Mn/Ca-shell time series of the two studied shells exhibit a high degree of synchrony after being placed in a precise temporal context by means of growth pattern analysis. There is a large inter-annual variability of Mn/Casheii records during 20112015, with the highest value occurring in 2013. Mn/Ca-shell also displays a pronounced intra-annual variability with maxima consistently occurring during late spring/early summer. The high reproducibility of Mn/Ca-shell time-series among contemporaneous specimens highlights the existence of strong environmental rather than biological control on the incorporation of Mn into the shells. In particular, the striking feature of late spring/early summertime Mn/Cashell maxima is synchronous with the occurrence of reducing conditions beneath the sediment-water interface (SWI). The latter results in substantial increases of biologically available Mn2+ in the sediment pore water and organic particles, the element being rapidly taken up from these sources by the mussels with subsequent incorporation of Mn into their shells. Therefore, Mn/Ca-shell can potentially serve as a high-resolution proxy of the mobility of Mn at the SWI. As demonstrated by the present study, documenting and understanding geochemical properties of bivalve shells can help to retrospectively monitor eutrophication-induced environmental change in aquatic ecosystems. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:97 / 108
页数:12
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