A paleolimnological perspective on industrial-era metal pollution in the central Andes, Peru

被引:26
作者
Cooke, Colin A. [1 ,2 ]
Abbott, Mark B. [1 ,3 ]
机构
[1] Univ Alberta, Edmonton, AB T6G 2E3, Canada
[2] Univ Pittsburgh, Dept Geol, Pittsburgh, PA 15260 USA
[3] Carnegie Museum Nat Hist, Sect Anthropol, Pittsburgh, PA 15260 USA
关键词
Peru; Andes; pollution; lake sediment; trace metals;
D O I
10.1016/j.scitotenv.2007.12.034
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To date, few studies have investigated the environmental legacy associated with industrialization in the South American Andes. Here, we present an environmental archive of industrial pollution from Pb-210-dated lake cores recovered from Laguna Chipian, located near the Cerro de Pasco metallurgical region and Laguna Pirhuacocha, located near the Morococha mining region and the La Oroya smelting complex. At Laguna Chipian, trace metal concentrations increase beginning similar to 1900 AD, coincident with the construction of the central Peruvian railway, and the rapid industrial development of the Cerro de Pasco region. Trace metal concentrations and fluxes peak during the 1950s before subsequently declining up-core (though remaining well above background levels). While Colonial mining and smelting operations are known to have occurred at Cerro de Pasco since at least 1630 AD, our sediment record preserves no associated metal deposition. Based on our C-14 and Pb-210 data, we suggest that this is due to a depositional hiatus, rather than a lack of regional Colonial pollution. At Laguna Pirhuacocha, industrial trace metal deposition first begins similar to 1925 AD, rapidly increasing after similar to 1950 AD and peaking during either the 1970s or 1990s. Trace metal concentrations from these lakes are comparable to some of the most polluted lakes in North America and Europe. There appears to be little diagenetic alteration of the trace metal record at either lake, the exception being arsenic (As) accumulation at Laguna Pirhuacocha. There, a correlation between As and the redox-sensitive element manganese (Mn) suggests that the sedimentary As burden is undergoing diagenetic migration towards the sediment-water interface. This mobility has contributed to surface sediment As concentrations in excess of 1100 mu g g(-1). The results presented here chronicle a rapidly changing Andean environment, and highlight a need for future research in the rate and magnitude of atmospheric metal pollution. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:262 / 272
页数:11
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