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Based on measurements of bulk density of fine textured horizons 1. Here we focus on the aquifer within the Moccasin strath terrace Fig. The shallow aquifers and streams emerging from them are well-suited to research on variation in the controls on denitrification because the terrace has well-defined hydrologic boundaries, and soils across the terrace are of varying thicknesses and textures that dictate a range of water storage and biogeochemical conditions Sigler et al.
Location and character of the Judith River Watershed JRW and Moccasin terrace in the context of: A the location of the study area within the United States, the northern Great Plains green shaded area , and the Mississippi Atchafalaya River Basin gray outline ; B the locations of the Moccasin terrace and towns nearest to the study fields where lysimeters and rain water samplers were installed; C land use on the Moccasin terrace for the growing season USDA ; and D soil series, catchments black outlines , and stream sample sites blue symbols , non-riparian groundwater sample sites brown symbols , and riparian groundwater sample sites green symbols on the Moccasin terrace.
Symbol shapes match those of Sigler et al. Lysimeters were installed near the bottom of the fine textured soil horizons, with nine in soils with relatively thin fine-textured zones 40—80 cm; shallow and nine in soils with relatively thick fine-textured zones 80— cm; deep. Lysimeters were visited approximately every two weeks during periods with sufficient soil water to produce samples between and Groundwater and surface water sampling between and included two wells, five springs, and three stream sites distributed across the Moccasin terrace Fig.
The terrace aquifer, which is isolated from riparian influence due to stream incision, was assessed using upland wells. Springs are located both adjacent to and within riparian areas and represent a range of influence from the riparian environment, determined by geomorphic context at the spring orifice. Major ions in soil water, groundwater, and stream samples for the four-year sample period — were characterized previously Sigler et al. Nitrate isotope analyses were conducted at Woods Hole Oceanographic Institution, using the denitrifier method Sigman et al.
Precipitation samples were collected between and during these rain-dominated months at three study fields Fig. A composite sample of snow was collected from the snowpack near Field B and near Field C on 30 March A working local groundwater standard included after every fourth sample across eight runs had a standard deviation from the mean of 0. Isotopic signals of denitrification The N isotopic composition of nitrogenous compounds is subject to fractionation during transformations within the N cycle Kendall et al.
The expected influence of oxygen and DOC concentrations on denitrification were explored as corroborating lines of evidence. Although a measurement of low DO indicates conditions immediately upgradient from the sample site were conducive for denitrification, high DO at a sample site does not preclude the possibility that low DO conditions facilitated denitrification further upgradient, followed by reoxygenation. Similarly, while high DOC at a sample site indicates electron donors may have been present for denitrification locally or immediately upgradient, low DOC does not preclude the possibility that DOC was available upgradient and was removed by respiration and denitrification.
Hence, we interpret the DO and DOC relationships independently as separate lines of evidence for denitrification but do not distinguish relative control between these two drivers. Collectively, these regression statistics provide simple metrics for assessing confidence in interpretation of an observed isotopic effect consistent with denitrification.
Estimating fallow soil denitrification rates Summer fallow land use provides periods of minimal plant uptake that allow a unique opportunity to assess the net effects of nitrification and denitrification on Nr in soil. We use a stochastic Monte Carlo approach to explore the ranges in magnitude of soil denitrification during fallow periods that may be expected to balance the effects of nitrification. Total denitrification Nden,T over the period of interest is a function Eq.
The steady state results from the assumption that inputs occur at a constant rate with a constant isotopic value infinite source pool here is SON , and the assumption that the isotopic fractionation effects of nitrification more specifically, ammonification plus nitrification and denitrification are constant. Now, giant clams are also threatened by rapid environmental change from both a suite of local and regional scale stressors and global change, including climate change, global warming, marine heatwaves and ocean acidification.
The interplay between local- to regional-scale and global-scale drivers is likely to cause an array of lethal and sub-lethal effects on giant clams, potentially limiting their depth distribution on coral reefs and decreasing suitable habitat area within natural ranges of species. Global change stressors, pervasive both in unprotected and protected areas, threaten to diminish conservation efforts to date. International efforts urgently need to reduce carbon dioxide emissions to avoid lethal and sub-lethal effects of global change on giant clams.
Meanwhile, knowledge of giant clam physiological and ecological responses to local—regional and global stressors could play a critical role in conservation strategies of these threatened species through rapid environmental change.
Further work on how biological responses translate into habitat requirements as global change progresses, selective breeding for resilience, the capacity for rapid adaptive responses of the giant clam holobiont and valuing tourism potential, including recognizing giant clams as a flagship species for coral reefs, may help improve the prospects of these charismatic megafauna over the coming decades.
Climate change, causing global climate destabilization, is being realized through increases in temperature, heatwaves and associated phenomena, such as ocean acidification—where carbon dioxide CO2 reacts with seawater lowering the pH of the oceans. Global change has accelerated rapidly, particularly in the past 50 years, and we are tracking the worst-case emissions scenario—the business-as-usual Representative Concentration Pathway RCP 8.
This recent epoch of change is causing major ecosystem losses and a biodiversity crisis on Earth, with many species threatened or lost already in the sixth mass extinction. We are inevitably losing species before they can be described, let alone understood. Rapid global change in the marine realm has contributed to consecutive global ocean heating events in the past decade Bureau of Meteorology,
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