California Current Ecosystem LTER

Nitrate Isotopes (CalCOFI Cruise)

Title
Nitrogen and oxygen stable isotopes of nitrate from CalCOFI lines 80 and 93 plus station 081.8 046.9. Collected on cruises from 2010 to 2016.

Abstract
Stable isotopes of nitrate were measured on CalCOFI cruises from 2010-2016 from lines 80 and 93 plus station 081.8 046.9. Samples were filtered directly from the CTD and then frozen until analysis. Samples collected from 2010-2012 were analyzed in the Sigman Lab at Princeton University. Samples collected from 2013-2016 were analyzed in the Wankel Lab at Woods Hole Oceanographic Insititution. Five samples from station 081.8 046.9 (the Santa Barbara Basin) were further analyzed for nitrogen isotopes of nitrite in the Wankel Lab.

Keywords
CTD, isotopes, nitrite, nitrogen, oceans, stable isotopes

LTER Data System Record
http://dx.doi.org/10.6073/pasta/6929b7004a5d947bb1beec0dadf37fad
Projects
California Current Ecosystem LTER

Creators
Aluwihare, Lihini (laluwihare@ucsd.edu)
White, Margot (margotw42@gmail.com)

Contact
CCE LTER Information Manager (ccelter.im@gmail.com)

Other Personnel
Dovel, Shonna sample collection
Wankel, Scott sample analysis
Rafter, Patrick sample analysis

Data

table Nitrate isotopes
Nitrogen and oxygen stable isotopes of nitrate
Rows: 1352
Columns: 23
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Methods


Sample collection
Samples were collected during CalCOFI cruises from 2010-2016. Samples for nitrate and nitrite isotopes were filtered through GF/F filters (0.7 mm pore size) directly from Niskin bottles mounted on a standard conductivity-temperature-depth rosette system (CTD), and frozen until analysis. 

Nitrate isotope analysis
Nitrogen and oxygen isotopes of NO3- were analyzed using the denitrifier method (Casciotti et al., 2002; Sigman et al., 2001). Samples from 2010-2012 were measured according to Rafter & Sigman 2016. Those from 2013-2015 were measured according to Buchwald et al. 2018. Briefly, sample N2O was purified using a customized purge and trap system and analyzed on a continuous flow IsoPrime 100 isotope ratio mass spectrometer (IRMS). NO2- concentrations greater than 2% of NO3-+NO2- were removed by addition of sulfamic acid prior to injection (Granger & Sigman, 2009). Corrections for drift, size and fractionation of O isotopes during bacterial conversion were carried out using NO3- reference materials USGS 32, USGS 34 and USGS 35 (McIlvin & Casciotti, 2011). Typical reproducibility for d15NNO3 and d18ONO3 measurements was ±0.2‰ and 0.4‰, respectively. Samples with less than 1 uM nitrate were not analyzed.

Nitrite isotope analysis
Nitrogen isotopes of NO2- were analyzed using the sodium azide method, in which NO2- is quantitatively converted to N2O by addition of an acetic acid buffered sodium azide solution (McIlvin & Altabet, 2005). Reported d15NNO2 values were normalized against internal nitrite isotope reference standards WILIS 10 (-1.7‰) and WILIS 11 (+57.1‰) (Wankel et al., 2017). Typical reproducibility for d15NNO2 is ±0.1‰.