Abstract
Seagrass meadows and coral reefs along the coast of Saipan, a US commonwealth in the Northern Pacific, have been declining since the 1940s, possibly due to nutrient loading. This study investigated whether submarine groundwater discharge (SGD) contributes to nutrient loading and supports primary production on Saipan’s coast. SGD can be an important source of freshwater, nutrients, and other pollutants to coastal waters, especially in oceanic islands without well-developed stream systems. Ra and Rn isotopes were used as natural tracers of SGD. Nitrate, phosphate, and ammonium concentrations, ancillary water quality parameters, δ15N and δ18O of dissolved nitrate, and δ15N of primary producer tissue were measured. Our results pointed to discharge of low-salinity groundwater containing elevated concentrations of sewage-derived N at specific locations along Saipan’s coast. High SGD areas had lower salinity and pH, higher dissolved inorganic nitrogen concentrations, and elevated primary producer δ15N, indicative of sewage nitrogen inputs. We estimated that SGD could support 730–6400 and 3000–15,000 mol C d−1 of primary production in Tanapag and Garapan Lagoons, respectively, or up to approximately 60% of primary production in Garapan Lagoon. Efforts to improve water quality, reduce nutrient loading, and preserve coastal ecosystems must account for groundwater, since our results demonstrate that it is an important pathway of nitrogen delivery.
Highlights
Efforts to improve water quality, reduce nutrient loading, and preserve coastal ecosystems must account for groundwater, since our results demonstrate that it is an important pathway of nitrogen delivery
This study presents the first published data about submarine groundwater discharge (SGD), SGD-derived nutrient inputs, and nitrogen source tracking in Saipan
Salinities measured in all groundwater samples were consistently lower than in the adjacent coastal ocean (Figure 2)
Summary
Submarine groundwater discharge (SGD) is the flow of groundwater across the land-ocean interface into the ocean [1]. It includes groundwater originating from confined or unconfined aquifers and recirculated sea water. The mixing of saline ocean water and fresh groundwater can occur on tidal or seasonal scales [2], and SGD can occur either at the shoreline or offshore. Over the past 30 years, SGD has gained recognition as an important source of freshwater and nutrients into the coastal ocean, and Burnett et al [1] state that “almost all coastal zones are subject to such flow”. Numerous studies have demonstrated that SGD can provide subsidies of freshwater [3,4,5]
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