Geochemical sourcing of runoff from a young volcanic watershed to an impacted coral reef in Pelekane Bay, Hawaii

被引:2
作者
Takesue, Renee K. [1 ]
Storlazzi, Curt D. [1 ]
机构
[1] US Geol Survey, Pacific Coastal & Marine Sci Ctr, 2885 Mission St, Santa Cruz, CA 95060 USA
关键词
Sediment provenance; Geochemical discrimination; Trace elements; Rare earth elements; Sediment traps; RARE-EARTH-ELEMENTS; GREAT-BARRIER-REEF; SEDIMENTARY PROCESSES; SUSPENDED-SEDIMENT; KOHALA VOLCANO; FRINGING-REEF; PUERTO-RICO; PROVENANCE; ISLAND; RIVER;
D O I
10.1016/j.scitotenv.2018.08.282
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Runoff of sediment and other contaminants from developed watersheds threatens coastal ecosystems and services. A sediment geochemical sourcing study was undertaken on a sediment-impacted coral reef flat to identify terrestrial sediment sources and how these changed over time. Geochemical signatures were identified for watershed soils that formed on Hawaiian basaltic and alkalic lavas using relatively immobile compatible (Ni, Sc) and incompatible (Nb, REE, Th) elements quantified by ICP-MS in total decompositions of the fine fraction of surface soils. Some soils also contained ash from late-erupting cinder cones that added alkalic geochemical signatures, resulting in distinctive mixed signatures near these geologic features. Sediment was collected in Pelekane Bay using sediment traps during winter 2010-2011 and a sediment core in order to geochemically source runoff entering the bay. Geochemical signatures in trapped sediment showed that runoff predominantly originated from the lower watershed along a highway corridor rather than from the upper watershed or areas with alkalic lavas. Soil in the highway corridor also contained Zn above levels of concern for aquatic organisms and anthropogenic Pb, indications that runoff control measures could reduce the exposure of the reef community to potentially toxic metals and other road-associated contaminants. The upper portion of a 60-yr long sediment record from Pelekane Bay was disturbed by tsunamigenic waves from the Tohoku earthquake, and the remainder was likely subject to mixing by winter waves that averaged out geochemical variations. On average, watershed regions with basaltic soils were the predominant source of runoff to the bay over the past GO years. By linking sediment runoff to geographic regions or features in watersheds, geochemical sourcing can provide insights that allow resource managers to direct runoff mitigation and soil conservation efforts to areas where they will be most effective. Published by Elsevier B.V.
引用
收藏
页码:353 / 363
页数:11
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