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            <gco:CharacterString>Cite this dataset as: Wilson, S. J., Song, B., Tobias, C., Anderson, I. C. (2024) In situ tracer injection experiment conducted with 15N-labeled ammonium in a shallow, sandy subterranean estuary in Gloucester Point, USA  in August 2019. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-01-15 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.917767.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Methods and Sampling: &amp;lt;p&amp;gt;These data were collected during August 2019 from a sandy subterranean estuary (STE) located in Gloucester Point, Virginia, USA. Porewater was collected from surface water and piezometers placed at 40, 50, and 60cm. Prior to the injection, porewater was collected from replicate 50cm piezometers and amended with 15N-labeled ammonium, sulfur hexaflouride, and bromide. The amended porewater was then reintroduced into the STE through the 50cm injection piezometers.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;After injection porewater was collected overtime from both the injection piezometers and other piezometers surrounding the injection well. At each time point, porewater was collected in serum bottles prepared with potassium hydroxide and were equlibrated by shaking before being run on a gas chromatograph with electron capture detection (GC-ECD, Shimadzu) in order to determine the sulfur hexaflouride concentration. Porewater was also collected for inorganic nutrients and ions, filtered with a 0.45 µm syringe filter (Whatman GE) and were frozen (-20 °C) until analysis.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/805733.rdf" xlink:title="OCE-1657801" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1657801 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1657801</gmx:Anchor>
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            <gmx:Anchor xlink:href="https://ror.org/04eeqc889" xlink:title="ROR ID" xlink:actuate="onRequest">Virginia Institute of Marine Science</gmx:Anchor>
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Nitrogen is an important nutrient that maintains high coastal ecosystem productivity. Yet excess nitrogen delivery can cause serious water quality deterioration including harmful algal blooms, fish kills, and oxygen free dead zones. Numerous nitrogen transformations regulate the balance between nitrogen delivery and nitrogen removal in coastal environments and the majority of these reactions occur in sediments where seawater passes through the subsurface and mixes with groundwater transported from uplands. This mixing zone, referred to as the subterranean estuary, is characterized by very different geochemistry than either the seawater above it or the groundwater below it. Thus, it has the potential to host a variety of unique reactions that affect nitrogen availability to the overlying water. Scientists from the College of William and Mary, Virginia Institute of Marine Science (VIMS), and the University of Connecticut (UConn) propose to examine the importance of a cryptic nitrogen cycle, a novel and potentially widespread nitrogen cycling process in the subterranean estuary. The cryptic nitrogen cycle comprises anoxic ammonium oxidation to nitrite (anoxic nitrification) coupled with anaerobic ammonium oxidation (anammox) or denitrification producing harmless dinitrogen gas. The proposed project represents highly transformative science because it has the potential to change the current paradigm detailing operation of the biogeochemical nitrogen cycle in anoxic environments. Occurrence of the cryptic nitrogen cycle would have broad implications for the nitrogen budget of terrestrial and groundwater systems and the coastal ocean. Characterization of the cryptic nitrogen cycle will allow us to better understand interactions among the nitrogen, metals, and sulfur cycles, and potential impacts of ongoing human modification of coastal environments. Educational contribution of this project focuses on graduate and undergraduate student training. Two graduate students at VIMS and UConn will receive interdisciplinary training in microbiology, molecular ecology, and biogeochemistry while several undergraduates recruited through the VIMS REU (Research Experience for Undergraduates) Program and the UConn marine science programs will also participate in the project. In addition, three summer undergraduate interns will be recruited from Hampton University, a historically Black college, and trained to enhance minority education and research in marine science. Public outreach will be achieved through popular venues such as VIMS Marine Science Day, and the VIMS After Hours Public Lecture Series at VIMS. Tobias at UConn also provides educational contributions and outreach efforts through the UConn Marine Scholars and Early College Experience programs and an exhibit at Mystic Aquarium.&lt;/p&gt;
&lt;p&gt;A cryptic nitrogen cycle is proposed as a new process coupling anoxic nitrification to microbial nitrogen removal pathways such as anammox and denitrification. Unlike anammox, which refers to the oxidation of ammonium by nitrite to form dinitrogen (N2) gas, anoxic nitrification occurs by oxidation of ammonium in the absence of oxygen using other common chemical oxidants such as metal oxides (namely, Fe and Mn) or sulfate, abundant in many marine and coastal systems. The thermodynamic favorability of these reactions relies on coupling nitrite formed via these oxidants with anammox or denitrification. Due to the coupling, nitrite will not accumulate or be measurable in anoxic marine systems. Thus, a cryptic N cycle responsible for nitrite production can occur as a novel N transforming process in anoxic environments, serve as a vital link to N2 production, and attenuate N loads discharging from a subterranean estuary (STE). Preliminary results from a STE in the York River Estuary located in Virginia showed substantial N2 production, representing removal of 50-75% of the fixed groundwater N, in ferruginous and sulfidic zones where neither nitrite nor nitrate were detectable. Stable isotope incubation experiments using the 15N tracer and molecular analysis of microbial communities suggest that coupled anoxic nitrification and anammox processes are the dominant N2 production pathways rather than canonical denitrification in the STE. Therefore, coupled anoxic nitrification-anammox in coastal groundwater may be a major unrecognized sink for fixed nitrogen at the land-sea interface. In addition to coastal groundwater, the cryptic N cycle has potential importance in anoxic zones and ocean basins. This proposal focuses on the STE because geochemical conditions there appear optimal for the proposed reactions to occur, and our preliminary data show strong evidence for a cryptic N cycle. The proposed work uses a combined geochemical, 15N isotope tracer and microbiological approach to evaluate environmental controls on the cryptic N cycle as well as to estimate its contribution to reduction of fixed N fluxes to the coastal ocean. Four approaches are proposed: (1) Field characterization of anoxic nitrification reactions and associated microbial communities in a subterranean estuary; (2) Laboratory incubation experiments to identify hotspots of the cryptic N cycle; (3) Controlled microcosm experiments to determine geochemical controls on anoxic nitrification; and (4) in situ assessment of anoxic nitrification to estimate the importance of the cryptic N cycle in a coastal aquifer.&lt;/p&gt;</gco:CharacterString>
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http://lod.bco-dmo.org/id/dataset-parameter/917818.rdf
	Name: Piezometer
	Units: unitless
	Description: &lt;p&gt;The ID of the piezometer that was sampled written as replicate cluster-injection site or trace site-depth in cm; (e.g., 1-I-50 is the first replicate cluster, injection site, 50cm depth)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917819.rdf
	Name: Sample_ID
	Units: unitless
	Description: &lt;p&gt;The ID of the piezometer that was sampled written as replicate cluster-injection site or trace site-depth in cm-timepoint; (e.g., 1-I-50-T1 is the first replicate cluster, injection site, 50cm depth, time point 1 )&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917820.rdf
	Name: Time_Point
	Units: unitless
	Description: &lt;p&gt;Injection experiment time point (BKGD, T0, T1, T2, etc). BKGD means background samples, so samples that were collected prior to the start of the injection.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917821.rdf
	Name: Date
	Units: unitless
	Description: &lt;p&gt;Date of sample collection&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917822.rdf
	Name: Time
	Units: unitless
	Description: &lt;p&gt;Time of sample collection&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917823.rdf
	Name: Hours_after_Injection
	Units: hours (hrs)
	Description: &lt;p&gt;Hours after injectate was introduced in the subsurface&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917824.rdf
	Name: Bromide_uM
	Units: micromoles per liter (uM)
	Description: &lt;p&gt;Bromide concentration in porewater in micromoles per liter (uM) measured by ion chromatograph&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917825.rdf
	Name: Chloride_mM
	Units: millimoles per liter (mM
	Description: &lt;p&gt;Chloride concentration in porewater in millimoles per liter (mM) measured by ion chromatograph&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917826.rdf
	Name: SF6_ppbv
	Units: parts per billion per volume (ppbv)
	Description: &lt;p&gt;Sulfur hexaflouride concentration in porewater in parts per billion per volume (ppbv) measured by gas chromatograph-electron capture detector&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917827.rdf
	Name: SF6_pM
	Units: picoMolar (pM)
	Description: &lt;p&gt;Sulfur hexaflouride concentration in porewater in picoMolar (pM) measured by gas chromatograph-electron capture detector&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917828.rdf
	Name: Nox_uM
	Units: micromoles per liter (uM)
	Description: &lt;p&gt;Nitrate + Nitrite concentration in porewater in micromoles per liter (uM) measured by a lachat autoanalyzer&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917829.rdf
	Name: NO2_uM
	Units: micromoles per liter (uM)
	Description: &lt;p&gt;Nitrite concentration in porewater in micromoles per liter (uM) measured by a lachat autoanalyzer&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917830.rdf
	Name: NH4_uM
	Units: micromoles per liter (uM)
	Description: &lt;p&gt;Ammonium concentration in porewater in micromoles per liter (uM) measured by a lachat autoanalyzer&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917831.rdf
	Name: True_d15N
	Units: parts per thousand (‰)
	Description: &lt;p&gt;Delta 15N measurement made by an isotope ratio mass spectrometer&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/917832.rdf
	Name: Mole_Fraction_Calc
	Units: unitless
	Description: &lt;p&gt;15N Mole Fraction calculated from the d15N value&lt;/p&gt; 
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