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            <gco:CharacterString>Cite this dataset as: Mulholland, M., Chappell, P. D. (2024) Nitrogen fixation incubation data from cruise TN368 in July 2019 for SPIROPA project. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-05-23 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/928568 [access date]</gco:CharacterString>
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        <gco:CharacterString>after Selden et al. 2024 JGR Table S1 Dataset Description: &amp;lt;p&amp;gt;This nitrogen fixation incubation data&amp;amp;nbsp;is a supplement to BCO-DMO dataset&amp;amp;nbsp;https://www.bco-dmo.org/dataset/927927, which is&amp;amp;nbsp;hydrographic, nutrient, and mean nitrogen fixation rate data from the SPIROPA project's third cruise.&amp;amp;nbsp; Bottle data from the TN368 cruise (Chief Sci McGillicuddy) can be viewed here:&amp;amp;nbsp;https://www.bco-dmo.org/dataset/849340.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Glossary of terms:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
A = Atom-% enrichment&amp;lt;br /&amp;gt;
APN = Atom-% enrichment of the particulate nitrogen pool&amp;lt;br /&amp;gt;
BDL = Below detection limit&amp;lt;br /&amp;gt;
DNQ = Detectable but not quantifiable&amp;lt;br /&amp;gt;
LOD = Limit of detection&amp;lt;br /&amp;gt;
LOQ = Limit of quantification&amp;lt;br /&amp;gt;
N2 = Nitrogen gas&amp;lt;br /&amp;gt;
PETG = Polyethylene Terephthalate Glycol&amp;lt;br /&amp;gt;
PN = Particulate nitrogen&amp;lt;br /&amp;gt;
NFR = Nitrogen fixation rate&amp;lt;br /&amp;gt;
SUR = Specific uptake rate&amp;lt;br /&amp;gt;
t0 = time initial&amp;lt;br /&amp;gt;
tf = time final&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;div class=&amp;quot;field&amp;quot; id=&amp;quot;form_location&amp;quot;&amp;gt;
&amp;lt;p&amp;gt;Nitrogen fixation rates and hydrographic data were measured in July 2019 in&amp;amp;nbsp;conjunction with the SPIROPA (Shelfbreak Productivity Interdisciplinary Research Operation at the Pioneer Array)&amp;amp;nbsp;project cruises (Chief Scientist Dr. Dennis McGillicuddy).&amp;amp;nbsp;This case study was conducted at the Mid-Atlantic Bight shelfbreak front to the south of Massachusetts, USA to examine whether significant N2 fixation occurs in the continental shelf region. On July 5th, 2019, the&amp;amp;nbsp;vessel R/V Thomas G. Thompson (cruise TN368) departed Woods Hole, MA and performed multiple transects in the&amp;amp;nbsp;area of 70 to 71 degrees West longitude and 39 to 40.5 degrees North latitude. Sampling was restricted to waters above the 0.1% light level.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Water was collected in 10L Niskin bottles on a 24-bottle rosette.&amp;amp;nbsp;Vertical conductivity, temperature, and depth profiles were measured&amp;amp;nbsp;concurrently using a Sea-Bird 911+ CTD profiler. Samples to determine nitrate, phosphate, and silicate concentrations were filtered (0.4 um, polycarbonate) directly from the Niskin bottles into acid-washed polyethylene bottles and stored&amp;amp;nbsp;frozen until analysis via standard colorimetric methods at the WHOI Nutrient Analytical Facility using a SEAL Analytical AA3 HR discrete chemistry analyzer. Detection limits for nitrate, phosphate, and silicate methods were 0.040, 0.030 and 0.009 μM, respectively.&amp;lt;/p&amp;gt;

&amp;lt;div&amp;gt;
&amp;lt;p&amp;gt;This dataset presents the full incubation result&amp;amp;nbsp;with all replicates. The associated environmental (hydrographic) data is presented in a separate dataset&amp;amp;nbsp;along with the mean uptake and fixation rates. Please refer to BCO-DMO dataset&amp;amp;nbsp;https://www.bco-dmo.org/dataset/927927&amp;lt;/p&amp;gt;
&amp;lt;/div&amp;gt;

&amp;lt;p&amp;gt;Nitrogen fixation rate measurements (NFR) were quantified on repeat cross-frontal transects using the&amp;amp;nbsp;&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;amp;nbsp;bubble release technique (Chang et al., 2019; Klawonn et al., 2015), which is a variant of the &amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; tracer method (Montoya et al., 1996) which accounts for the slow dissolution time of N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; gas (White et al., 2020).&amp;amp;nbsp; The particular approach used for this study have been described in Selden et al. (2019), Selden, Chappell, et al. (2021), and Selden, Mulholland, et al. (2021). To measure&amp;amp;nbsp;&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;amp;nbsp;uptake, triplicate PETG bottles (0.5-2 L) were rinsed with whole water then filled, ensuring that no bubbles remained. Using a gas tight syringe (VICI Precision Sampling),&amp;amp;nbsp;&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;amp;nbsp;gas (~99%, Cambridge Isotope Laboratories) was added through a flexible silicon septa. Samples were gently rocked for 15 min as described by Selden et al. (2019). Any remaining bubble was subsequently removed to ensure constant isotopic enrichment over the incubation period, and bottles were incubated on-deck for approximately 24 hours. As the vessel moved across the front, a large temperature gradient was encountered (from 16°C&amp;amp;nbsp;to 26°C).&amp;amp;nbsp;To avoid temperature-shocking the samples during transit, we maintained three on-deck incubators that recirculated water through aquaria chillers (MC-1/10HP, AquaEuroUSA) housed in custom casings (built from King Starboard plastic sheet) for protection and maintained approximate temperature conditions for shelf, frontal, and offshore waters, respectively.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;At the end of the incubation period, a 6 milliliter sample aliquot was collected from each bottle and transferred to a helium-purged Exetainer&amp;lt;sup&amp;gt;TM&amp;lt;/sup&amp;gt;&amp;amp;nbsp;containing 50 μl zinc chloride (50% w/v). These samples were stored at room temperature and upside-down in 15 ml Falcon&amp;lt;sup&amp;gt;TM&amp;lt;/sup&amp;gt;&amp;amp;nbsp;tubes, submerged in ultrapure water, until analysis at the UC Davis Stable Isotope Facility. The remaining incubation volume was then filtered for initial particulate nitrogen (PN) samples. Initial and final PN isotopic composition and concentration were analyzed at Old Dominion University on a Europa 20/20 isotope ratio mass spectrometer with an automated N and carbon preparation module. Low mass samples (&amp;amp;lt;10 µg N) were excluded from downstream analysis as IRMS response can become non-linear at low mass (White et al., 2020).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;S&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0); font-family:helvetica,arial,sans-serif; font-size:14.4px&amp;quot;&amp;gt;pecific uptake rates were calculated following Montoya et al. (1996), with equations detailed below.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/748850.rdf" xlink:title="OCE-1657803" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1657803 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1657803</gmx:Anchor>
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            <gmx:Anchor xlink:href="http://orcid.org/0000-0001-5212-6228" xlink:title="ORCID" xlink:actuate="onRequest">Phoebe Dreux Chappell</gmx:Anchor>
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&lt;p&gt;The continental shelf break of the Middle Atlantic Bight supports a productive and diverse ecosystem. Current paradigms suggest that this productivity is driven by several upwelling mechanisms at the shelf break front. This upwelling supplies nutrients that stimulate primary production by phytoplankton, which in turn leads to enhanced production at higher trophic levels. Although local enhancement of phytoplankton biomass has been observed in some circumstances, such a feature is curiously absent from time-averaged measurements, both from satellites and shipboard sampling. Why would there not be a mean enhancement in phytoplankton biomass as a result of the upwelling? One hypothesis is that grazing by zooplankton prevents accumulation of biomass on seasonal and longer time scales, transferring the excess production to higher trophic levels and thereby contributing to the overall productivity of the ecosystem. However, another possibility is that the net impact of these highly intermittent processes is not adequately represented in long-term means of the observations, because of the relatively low resolution of the in-water measurements and the fact that the frontal enhancement can take place below the depth observable by satellite. The deployment of the Ocean Observatories Initiative (OOI) Pioneer Array south of New England has provided a unique opportunity to test these hypotheses. The combination of moored instrumentation and autonomous underwater vehicles will facilitate observations of the frontal system with unprecedented spatial and temporal resolution. This will provide an ideal four-dimensional (space-time) context in which to conduct a detailed study of frontal dynamics and plankton communities needed to examine mechanisms controlling phytoplankton populations in this frontal system. This project will also: (1) promote teaching, training and learning via participation of graduate and undergraduate students in the research , (2) provide a broad dissemination of information by means of outreach in public forums, printed media, and a video documentary of the field work, and (3) contribute to improving societal well-being and increased economic competitiveness by providing the knowledge needed for science-based stewardship of coastal ecosystems, with particular emphasis on connecting with the fishing industry through the Commercial Fisheries Research Foundation.&lt;/p&gt;
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	Name: spl_id
	Units: dimensionless
	Description: &lt;p&gt;Unique identifier for individual N2 uptake incubation bottles; meant for internal lab use (may be of value to anyone who wishes to discuss specific samples with corresponding authors)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929506.rdf
	Name: collection_date_EST
	Units: dimensionless
	Description: &lt;p&gt;Datetime of sample collection in eastern standard time (EST)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929507.rdf
	Name: latitude
	Units: decimal degrees
	Description: &lt;p&gt;Latitude of sampling site&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929508.rdf
	Name: longitude
	Units: decimal degrees
	Description: &lt;p&gt;Longitude of sampling site&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929509.rdf
	Name: cruise
	Units: dimensionless
	Description: &lt;p&gt;Cruise identification&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929510.rdf
	Name: cast
	Units: dimensionless
	Description: &lt;p&gt;Cast identifier for cruise TN368 on R/V T.G. Thompson&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929511.rdf
	Name: z_m
	Units: meters (m)
	Description: &lt;p&gt;Depth of sample collection&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929512.rdf
	Name: time_hr
	Units: hours
	Description: &lt;p&gt;Duration of incubation&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929513.rdf
	Name: vol_L
	Units: liters (L)
	Description: &lt;p&gt;Incubation volume&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929514.rdf
	Name: apn_tf
	Units: atom percent
	Description: &lt;p&gt;Atom% 15N enrichment at final time point (i.e., at time equals incubation duration)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929515.rdf
	Name: pn_uM_tf
	Units: micromoles nitrogen per liter (umol N2/L)
	Description: &lt;p&gt;Particulate nitrogen concentration at final time point&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929516.rdf
	Name: pnpc_flag
	Units: dimensionless
	Description: &lt;p&gt;Flag indicating whether an independent sample was available to determine particulate nitrogen concentration at the time of sample collection; &amp;quot;NO_SPL&amp;quot; indicates that no sample was available; &amp;quot;INSUFFICIENT_N_MASS&amp;quot; indicates that the sample collected for initial PN determination did not have sufficient mass (&amp;gt;10 ug N) to allow for robust isotopic analysis&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929517.rdf
	Name: apn_t0
	Units: atom percent
	Description: &lt;p&gt;Atom% 15N enrichment at initial time point&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929518.rdf
	Name: pn_uM_t0
	Units: micromoles nitrogen per liter (umol N2/L)
	Description: &lt;p&gt;Particulate nitrogen concentration at initial time point&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929519.rdf
	Name: an2_flag
	Units: dimensionless
	Description: &lt;p&gt;Flag indicating whether a subsample to directly determine 15N enrichment of the N2 pool in the specific incubation bottle was analyzed; &amp;quot;NO_AN2_SPL_RUN&amp;quot; indicates that the sample was lost, damaged, or otherwise unable to be analyzed&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929520.rdf
	Name: an2
	Units: atom percent
	Description: &lt;p&gt;Atom% 15N enrichment of N2 pool in incubation bottle; subsampled at final time point&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929521.rdf
	Name: mindetdiff
	Units: atom percent
	Description: &lt;p&gt;The minimum detectable difference between the atom% enrichment at the initial and final time points of the incubation; calculated as 3 times the standard deviation of 7 replicate 12.5 ug N standards (sulfanilimide)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929522.rdf
	Name: apn_t0_flag
	Units: dimensionless
	Description: &lt;p&gt;Flag indicates where the atom% 15N enrichment of the N2 pool came from; &amp;quot;MEAN_APNT0_USED_IN_CALC&amp;quot; indicates that the mean atom% enrichment achieved across experiments was used to calculate a rate; no flag indicates that a direct measurement was available and used&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929523.rdf
	Name: mass_flag
	Units: dimensionless
	Description: &lt;p&gt;Flag indicates where the particulate nitrogen concentration used to calculate a N2 fixation rate came from; &amp;quot;Tf_MASS_USED&amp;quot; indicates that no data was available for the initial time point to calculate an average across the incubation, and concentration was instead assumed constant across the incubation (and the final time point concentration value was used); no value indicates that the average across the incubation period was used&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929524.rdf
	Name: pn_uM_used
	Units: micromoles nitrogen per liter (umol N2/L/day)
	Description: &lt;p&gt;The actual value for particulate nitrogen concentration used to calculate N2 fixation rate; where concentrations were available at both initial and final time points, the average was used&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929525.rdf
	Name: sur
	Units: per day
	Description: &lt;p&gt;Specific N2 uptake rate&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929526.rdf
	Name: nfr
	Units: nanomoles nitrogen per liter per day (nmol N2/L/day)
	Description: &lt;p&gt;N2 fixation rate&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929527.rdf
	Name: lod
	Units: nanomoles nitrogen per liter per day (nmol N2/L/day)
	Description: &lt;p&gt;Limit of detection for N2 fixation rate at given sampling location&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929528.rdf
	Name: loq
	Units: nanomoles nitrogen per liter per day (nmol N2/L/day)
	Description: &lt;p&gt;Limit of quantification for N2 fixation rate for given incubation experiment&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929529.rdf
	Name: lod_sur
	Units: per day
	Description: &lt;p&gt;Limit of detection for specific N2 uptake rate for given incubation experiment&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929530.rdf
	Name: loq_sur
	Units: per day
	Description: &lt;p&gt;Limit of quantification for specific N2 uptake rate for given incubation experiment&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929531.rdf
	Name: det_flag
	Units: dimensionless
	Description: &lt;p&gt;flag indicates whether N2 uptake was detectable and/or quantifiable; &amp;quot;BDL&amp;quot; indicates that it was below the detection limit; &amp;quot;DNQ&amp;quot; indicates that it was detectable but not quantifiable&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929532.rdf
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	Units: unitless
	Description: &lt;p&gt;Datetime of sampling in UTC (if original datetimes were EST or GMT-5)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/929533.rdf
	Name: ISO_DateTime_UTC_if_EDT
	Units: unitless
	Description: &lt;p&gt;Datetime of sampling in UTC (if original datetimes were actually EDT or GMT-4)&lt;/p&gt; 
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&amp;lt;p&amp;gt;Nitrogen fixation rates and hydrographic data were measured in July 2019 in&amp;amp;nbsp;conjunction with the SPIROPA (Shelfbreak Productivity Interdisciplinary Research Operation at the Pioneer Array)&amp;amp;nbsp;project cruises (Chief Scientist Dr. Dennis McGillicuddy).&amp;amp;nbsp;This case study was conducted at the Mid-Atlantic Bight shelfbreak front to the south of Massachusetts, USA to examine whether significant N2 fixation occurs in the continental shelf region. On July 5th, 2019, the&amp;amp;nbsp;vessel R/V Thomas G. Thompson (cruise TN368) departed Woods Hole, MA and performed multiple transects in the&amp;amp;nbsp;area of 70 to 71 degrees West longitude and 39 to 40.5 degrees North latitude. Sampling was restricted to waters above the 0.1% light level.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Water was collected in 10L Niskin bottles on a 24-bottle rosette.&amp;amp;nbsp;Vertical conductivity, temperature, and depth profiles were measured&amp;amp;nbsp;concurrently using a Sea-Bird 911+ CTD profiler. Samples to determine nitrate, phosphate, and silicate concentrations were filtered (0.4 um, polycarbonate) directly from the Niskin bottles into acid-washed polyethylene bottles and stored&amp;amp;nbsp;frozen until analysis via standard colorimetric methods at the WHOI Nutrient Analytical Facility using a SEAL Analytical AA3 HR discrete chemistry analyzer. Detection limits for nitrate, phosphate, and silicate methods were 0.040, 0.030 and 0.009 μM, respectively.&amp;lt;/p&amp;gt;

&amp;lt;div&amp;gt;
&amp;lt;p&amp;gt;This dataset presents the full incubation result&amp;amp;nbsp;with all replicates. The associated environmental (hydrographic) data is presented in a separate dataset&amp;amp;nbsp;along with the mean uptake and fixation rates. Please refer to BCO-DMO dataset&amp;amp;nbsp;https://www.bco-dmo.org/dataset/927927&amp;lt;/p&amp;gt;
&amp;lt;/div&amp;gt;

&amp;lt;p&amp;gt;Nitrogen fixation rate measurements (NFR) were quantified on repeat cross-frontal transects using the&amp;amp;nbsp;&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;amp;nbsp;bubble release technique (Chang et al., 2019; Klawonn et al., 2015), which is a variant of the &amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; tracer method (Montoya et al., 1996) which accounts for the slow dissolution time of N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; gas (White et al., 2020).&amp;amp;nbsp; The particular approach used for this study have been described in Selden et al. (2019), Selden, Chappell, et al. (2021), and Selden, Mulholland, et al. (2021). To measure&amp;amp;nbsp;&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;amp;nbsp;uptake, triplicate PETG bottles (0.5-2 L) were rinsed with whole water then filled, ensuring that no bubbles remained. Using a gas tight syringe (VICI Precision Sampling),&amp;amp;nbsp;&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;amp;nbsp;gas (~99%, Cambridge Isotope Laboratories) was added through a flexible silicon septa. Samples were gently rocked for 15 min as described by Selden et al. (2019). Any remaining bubble was subsequently removed to ensure constant isotopic enrichment over the incubation period, and bottles were incubated on-deck for approximately 24 hours. As the vessel moved across the front, a large temperature gradient was encountered (from 16°C&amp;amp;nbsp;to 26°C).&amp;amp;nbsp;To avoid temperature-shocking the samples during transit, we maintained three on-deck incubators that recirculated water through aquaria chillers (MC-1/10HP, AquaEuroUSA) housed in custom casings (built from King Starboard plastic sheet) for protection and maintained approximate temperature conditions for shelf, frontal, and offshore waters, respectively.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;At the end of the incubation period, a 6 milliliter sample aliquot was collected from each bottle and transferred to a helium-purged Exetainer&amp;lt;sup&amp;gt;TM&amp;lt;/sup&amp;gt;&amp;amp;nbsp;containing 50 μl zinc chloride (50% w/v). These samples were stored at room temperature and upside-down in 15 ml Falcon&amp;lt;sup&amp;gt;TM&amp;lt;/sup&amp;gt;&amp;amp;nbsp;tubes, submerged in ultrapure water, until analysis at the UC Davis Stable Isotope Facility. The remaining incubation volume was then filtered for initial particulate nitrogen (PN) samples. Initial and final PN isotopic composition and concentration were analyzed at Old Dominion University on a Europa 20/20 isotope ratio mass spectrometer with an automated N and carbon preparation module. Low mass samples (&amp;amp;lt;10 µg N) were excluded from downstream analysis as IRMS response can become non-linear at low mass (White et al., 2020).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;S&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0); font-family:helvetica,arial,sans-serif; font-size:14.4px&amp;quot;&amp;gt;pecific uptake rates were calculated following Montoya et al. (1996), with equations detailed below.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;
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                <gco:CharacterString>&amp;lt;p&amp;gt;Specific N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; uptake rates (SUR) were calculated following Montoya et al. (1996):&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Equation 1:&amp;amp;nbsp; &amp;amp;nbsp; &amp;amp;nbsp; &amp;amp;nbsp;SUR = (APN_tf - APN_t0) / (AN2 - APN_t0) ] x (1/time)&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
where A represents the atom-% enrichment of the initial (t=0) or final (t=f) particulate nitrogen (PN)&amp;amp;nbsp;pool, or the nitrogen (N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;) pool. Across all experiments, AN2 averaged 3.89 ± 2.0%. Experiments with &amp;amp;lt;1% enrichment were excluded from downstream analysis. The specific uptake rate represents the relative contribution of diazotroph-derived N to PN turnover within a given sample. Absolute N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; fixation rates (NFR) were calculated as:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Equation 2:&amp;amp;nbsp; &amp;amp;nbsp; &amp;amp;nbsp; &amp;amp;nbsp;NFR = SUR x [PN]&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
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