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Many ecosystem services provided by wetlands decline if they are managed for agricultural use. Ecological restoration of retired agricultural lands can restore these ecosystem services, yet practitioners require information on where restoration is possible and most likely to succeed. We report trends in the Massachusetts cranberry industry which suggest that cranberry farms located in riparian fens are well suited for ecological restoration that enhance their characteristics and functions as wetlands. We created a classification scheme for cranberry farms based on their: (1) crop status; (2) renovation status; (3) cultivar type; and (4) hydrologic type for the Wareham River watershed in southeastern Massachusetts. We ranked farms for their priority for restoration and extrapolated our results to the total cranberry acreage of Massachusetts. The occurrence of low‐yielding native cranberry cultivars in all riparian farms (i.e. those with a direct hydrological connection to an adjacent river or stream), combined with our finding that 100% of the area of the highest‐yielding new cultivars were planted in newly renovated but non‐riparian farms suggest that riparian farms are not targets for investment but instead have a high likelihood of retirement. We found that 20% of farm area in this watershed had riparian hydrology, a proportion suggesting the existence of over 1,000 ha of high‐priority farms for restoration statewide. Restoration of these stream‐adjacent riparian farms can provide an exit strategy for some cranberry growers, ease economic pressures on remaining growers, and develop wetlands able to provide ecosystem services such as habitat provision, nitrogen removal, and recreation. [ABSTRACT FROM AUTHOR]

Urea‐N is a component of bioavailable dissolved organic nitrogen (DON) that contributes to coastal eutrophication. In this study, we assessed urea‐N in baseflow across land cover gradients and seasons in the Manokin River Basin on the Delmarva Peninsula. From March 2010 to June 2011, we conducted monthly sampling of 11 streams (4 tidal and 7 nontidal), 2 wastewater treatment plants, an agricultural drainage ditch, and groundwater underlying a cropped field. At each site, we measured urea‐N, DON, dissolved organic carbon (DOC), total dissolved nitrogen (TDN), NO3−‐N, and NH4+‐N. In general, urea‐N comprised between 1% and 6% of TDN, with the highest urea‐N levels in drainage ditches (0.054 mg N/L) and wetland‐dominated streams (0.035–0.045 mg N/L). While urea‐N did not vary seasonally in tidal rivers, nontidal streams saw distinct urea‐N peaks in summer (0.038 mg N/L) that occurred several months after cropland fertilization in spring. Notably, the proportion of wetlands explained 78% of the variance in baseflow urea‐N levels across the Manokin watershed. In wetland‐dominated basins, we found urea‐N was positively related to water temperature and negatively related to DOC:DON ratios, indicating short‐term urea‐N dynamics at baseflow were more likely influenced by instream and wetland‐driven processes than by recent agricultural urea‐N inputs. Findings demonstrate important controls of wetlands on baseflow urea‐N concentrations in mixed land‐use basins. Research Impact Statement: The proportion of wetlands in a Coastal Plain river system was a key determinant of baseflow urea‐N concentrations in nontidal streams and tidal rivers. [ABSTRACT FROM AUTHOR]

Abstract: Previous work suggests that δ18O values of human hair can be used to constrain the region-of-origin of unknown individuals, but robust assessments of uncertainties in this method are lacking. Here we assess one source of uncertainty – temporal variation in the δ18O value of drinking water – using a monthly tap water survey of δ18O to develop geospatial models (i.e., maps) of the intra-annual variation (seasonality) in tap water δ18O for the contiguous USA. Temporal variation in tap water δ18O was correlated with water-supply type, and was related to geographic patterns of precipitation δ18O seasonality and water residence time. The maps were applied in a Bayesian framework to identify the geographic origin of an unidentified woman found in Utah, based on measured δ18O of scalp hair. The results are robust in specifying parts of the western USA as the most likely region-of-origin. Incorporation of tap water δ18O seasonality in the analysis reduces the precision of geographic assignments, but other sources of uncertainty (e.g., spatial interpolation uncertainty) have an equal or larger effect. [Copyright &y& Elsevier]