<?xml version="1.0" encoding="UTF-8"?><!--*** Generated from internal PANGAEA metadata schema by dif.xslt ***--><DIF xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.4.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/">
<Entry_ID>PANGAEA_986850</Entry_ID>
<Entry_Title>Nitrate concentration and nitrate stable isotopic signatures in seawater in the Labrador Sea in spring 2022</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Dempsey, Britton; Kam, Kitty; Rondón, Anadiuska N; Wallace, Douglas WR; Buchwald, Carolyn</Dataset_Creator>
<Dataset_Title>Nitrate concentration and nitrate stable isotopic signatures in seawater in the Labrador Sea in spring 2022</Dataset_Title>
<Dataset_Release_Date>2026-02-12</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.986850</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Carolyn</First_Name>
<Last_Name>Buchwald</Last_Name>
</Personnel>
<Personnel>
<Role>Investigator</Role>
<First_Name>Douglas WR</First_Name>
<Last_Name>Wallace</Last_Name>
<Email>douglas.wallace@dal.ca</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>Event label</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Latitude of event</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Longitude of event</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Date/Time of event</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>DEPTH, water</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Nitrate</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>δ15N, nitrate</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>δ15N, nitrate, standard deviation</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>δ18O, nitrate</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>δ18O, nitrate, standard deviation</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>CE22009</Keyword>
<Keyword>CE22009_11_Day</Keyword>
<Keyword>CE22009_12_Day</Keyword>
<Keyword>CE22009_4_Day</Keyword>
<Keyword>CE22009_6_Day</Keyword>
<Keyword>CE22009_8_Day</Keyword>
<Keyword>CE22009_9_Day</Keyword>
<Keyword>CTD_cast_11</Keyword>
<Keyword>CTD_cast_14</Keyword>
<Keyword>CTD_cast_17</Keyword>
<Keyword>CTD_cast_21</Keyword>
<Keyword>CTD_cast_25</Keyword>
<Keyword>CTD_cast_8</Keyword>
<Keyword>CTD/Rosette</Keyword>
<Keyword>Labrador Sea</Keyword>
<Keyword>nitrate concentration in sea water</Keyword>
<Keyword>stable nitrogen isotope (δ15N)</Keyword>
<Sensor_Name>
<Long_Name>Automated wet chemistry analyzer, SKALAR, SAN++</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Denitrifier method (McIlvin and Casciotti, 2011); measured with an isotope ratio mass spectrometer (IRMS), Thermo delta V</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>Celtic Explorer</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>2022-05-20</Start_Date>
<Stop_Date>2022-05-25</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>58.4833</Southernmost_Latitude>
<Northernmost_Latitude>58.8167</Northernmost_Latitude>
<Westernmost_Longitude>-49.61009999999999</Westernmost_Longitude>
<Easternmost_Longitude>-49.110000000000014</Easternmost_Longitude>
<Minimum_Depth>5.0 m (DEPTH, water)</Minimum_Depth>
<Maximum_Depth>2000.0 m (DEPTH, water)</Maximum_Depth>
</Spatial_Coverage>
<Access_Constraints>unrestricted</Access_Constraints>
<Use_Constraints>CC-BY-4.0: Creative Commons Attribution 4.0 International</Use_Constraints>
<Data_Set_Language>English</Data_Set_Language>
<Data_Center>
<Data_Center_Name>
<Short_Name>PANGAEA</Short_Name>
<Long_Name>Data Publisher for Earth &amp; Environmental Science</Long_Name>
</Data_Center_Name>
<Data_Center_URL>https://www.pangaea.de/</Data_Center_URL>
<Personnel>
<Role>Data Center Contact</Role>
<First_Name>Michael</First_Name>
<Last_Name>Diepenbroek</Last_Name>
<Email>info@pangaea.de</Email>
<Contact_Address>
<Address>Leobener Str.</Address>
<City>Bremen</City>
<Province_or_State>Bremen</Province_or_State>
<Postal_Code>28359</Postal_Code>
<Country>Germany</Country>
</Contact_Address>
</Personnel>
</Data_Center>
<Distribution>
<Distribution_Media>online</Distribution_Media>
<Distribution_Size>345 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Reference>Granger, Julie; Sigman, Daniel M (2009): Removal of nitrite with sulfamic acid for nitrate N and O isotope analysis with the denitrifier method. Rapid Communications in Mass Spectrometry, 23(23), 3753-3762, https://doi.org/10.1002/rcm.4307</Reference>
<Reference>McIlvin, Matthew R; Casciotti, Karen L (2011): Technical Updates to the Bacterial Method for Nitrate Isotopic Analyses. Analytical Chemistry, 83(5), 1850-1856, https://doi.org/10.1021/ac1028984</Reference>
<Summary>Seawater was collected for nitrate concentration and stable isotopic analyses between May 20th and May 25th, 2022 aboard RV Celtic Explorer in an area between 58 - 59 degrees N and 49 - 50 degrees W. Nitrate concentration samples were collected from the Niskin unfiltered into 15ml centrifuge tubes and immediately frozen at -20 degrees C. After the survey, these samples were then thawed to room temperature and analyzed using standard colorimetric protocols coupled with a continuous flow nutrient analyzer at the Canada Excellence Research Chairs (CERC) laboratory at Dalhousie University. Sampling for nitrate stable isotopic measurements was conducted by filtering seawater directly from the Niskin-rosette using 0.22 µm polyethersulfone (PES) syringe filters (VWR Cat. no. 76479-018) and collected into 60 mL HDPE bottles, which were then immediately frozen upright at -20 degrees C. Isotopic analyses were prepared in duplicate using the denitrifier method (McIlvin and Casciotti, 2011; doi:10.1021/ac1028984), and analyzed using isotope ratio mass spectrometery (IRMS) on a Thermo Delta V located in the Canada Excellence Research Chairs (CERC) laboratory at Dalhousie University. Samples with detectable nitrite (&gt;0.1 µmol/l) concentrations were first treated with sulfamic acid to remove potential interference on the 15N-NO3 pool as the denitrifier method does not discriminate between nitrate or nitrite (Granger and Sigman, 2009; doi:10.1002/rcm.4307). Isotopic analyses were referenced against USGS32, USGS34, and IAEA-NO3 reference materials. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.986850"!</Summary>
<Related_URL>
<URL>http://oceanography.dal.ca/person/Wallace_Douglas.html</URL>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1002/rcm.4307</URL>
<Description>Removal of nitrite with sulfamic acid for nitrate N and O isotope analysis with the denitrifier method</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1021/ac1028984</URL>
<Description>Technical Updates to the Bacterial Method for Nitrate Isotopic Analyses</Description>
</Related_URL>
<Related_URL>
<URL>https://download.pangaea.de/reference/134405/attachments/nwa-bcp_cruise_report_CE22009.pdf</URL>
<Description>CE22009</Description>
</Related_URL>
<Related_URL>
<URL>https://www.marine.ie/site-area/infrastructure-facilities/research-vessels/celtic-explorer</URL>
<Description>Celtic Explorer</Description>
</Related_URL>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2026-02-12</DIF_Creation_Date>
<Last_DIF_Revision_Date>2026-02-13</Last_DIF_Revision_Date>
</DIF>
