Heavy metal contamination in mangrove habitats of Singapore
Heavy metal contamination in mangrove habitats of Singapore
复制标题
DOI:
10.1016/j.marpolbul.2005.09.008
复制
发表时间:
2005-12-01
影响因子:
5.8
通讯作者:
Obbard, JP
中科院分区:
文献类型:
--
作者:
Cuong, DT;Bayen, S;Obbard, JP
Mangroves represent a critical ecological habitat to a diverse range of marine fauna and serve as a wintering site for a wide variety of migratory birds, but are highly endangered in Southeast Asia due to direct exploitation and disturbance. In Singapore, mangroves comprised around 13% of the total land area in 1820, but coverage is now less than 5%(Ng and Sivasothi, 1999). Mangroves are at risk from environmental pollutants, especially heavy metals that are associated with a diverse range of anthropogenic activities including shipping, dredging, and urban wastewater discharges. The accumulation of heavy metals in mangrove sediments has been reported for a number of countries including Australia, Hong Kong and Brazil (Harbison, 1986; Tam and Wong, 1995a, b, 1996; Lacerda et al., 1991; Machado et al., 2002a, b). Although there have been investigations on the levels of heavy metals in the coastal marine sediments of Singapore (Goh and Chou, 1997; Wood et al., 1997; Nayar et al., 2004), heavy metal data for local mangrove habitats are lacking. The objectives of this study were:(i) to determine the levels of heavy metals in representative mangrove habitats of Singapore;(ii) to compare levels between two mangrove habitats that are on opposite sides of a land-linked causeway between Singapore and Malaysia; and (iii) to evaluate contamination in the context of similar data reported from other countries. The data from this study is of use with respect to our understanding of the fate and impact of pollutants in mangrove systems, as well as the conservation of remaining mangrove habitats in Singapore. Samples were collected within a one-week period in April 2004 at two mangrove sites in Singapore ie Sungei Buloh and Sungei Khatib Bongsu (Fig. 1). These sites are located on opposite sides of a land-linked causeway between Singapore and Malaysia in the Straits of Johore. The causeway represents a physical barrier to marine hydrodynamics around SingaporeÕs northern coast, where there is no exchange of seawater across the causeway. The S. Buloh mangrove has been used in the past as a site for prawn aquaculture before being declared a protected nature reserve in 1989. S. Khatib Bongsu is not a protected site. Mangrove samples included the sea surface microlayer (SML) and subsurface water, sediments and biota. Levels of As, Cd, Cr, Cu, Ni, Pb and Zn were measured in all samples (except for As in sediments and Cr in biota). Two subsurface seawater (depth 40 cm, 2 l) and SML samples (2 l) were collected at the S. Buloh and S. Khatib Bongsu mangroves, respectively. SML samples were collected using the glass plate method (Harvey and Burzell, 1972; Carlson, 1982 and Zhang et al., 2003). A glass plate (30· 30· 0.5 cm) was dipped vertically through the water surface and withdrawn at a speed of about 5–6 cm/s. The attached water on both sides of the glass plate was wiped off into a sample bottle using a rubber blade, and then thoroughly rinsed with the water being collected. The thickness of the SML collected was determined by division of the volume collected with each plate dip by the surface area of the plate. In this study, the sampling thickness of the SML was around 40–60 μm. The definition and