Contributors | Affiliation | Role |
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Casciotti, Karen L. | Stanford University | Principal Investigator |
Rauch, Shannon | Woods Hole Oceanographic Institution (WHOI BCO-DMO) | BCO-DMO Data Manager |
Nitrate, nitrite, and nitrous oxide isotope measurements from the Eastern Tropical South Pacific ocean (NBP13-05). The data in this dataset were published in Peters et al. (2018) and Casciotti et al. (2018).
Samples were collected from a standard Niskin bottle rosette.
Nitrate isotope analyses were conducted by denitrifier method (Sigman et al., 2001; Casciotti et al., 2002) with updates (McIlviin and Casciotti, 2011). Nitrite was removed from samples containing more than 0.1 uM nitrite, using sulfuric acid (Granger and Sigman, 2009). Standards include USGS32, USGS34, and USGS35.
Nitrite isotope analyses were conducted by azide method (McIlvin and Altabet, 2005). Standards include N23, N7373, and N10219.
Nitrous oxide isotope analyses were conducted as described in McIlvin and Casciotti, 2010. N2O isotope measurements were calibrated against a laboratory N2O working gas.
The water mass analysis for the oxygen deficient zone waters was conducted as described in Peters et al., 2018, Deep Sea Research II, Estimating fixed nitrogen loss and associated isotope effects using concentration and isotope measurements of NO3-, NO2-, and N2 from the Eastern Tropical South Pacific oxygen deficient zone.
File |
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ETSP_NBP13-05.csv (Comma Separated Values (.csv), 126.91 KB) MD5:d1c9102c3a7f7b5fa0f1c9dc849c9d0a Primary data file for dataset ID 744679 |
Parameter | Description | Units |
CTD_cast | cast identifier from cruise | unitless |
STN | station identifier from cruise | unitless |
date | date; formatted as yyyy-mm-dd | unitless |
DEPTH | sample depth | meters |
PRESSURE | pressure | decibars |
latitude | latitude of sampling | degrees North |
longitude | longitude of sampling | degrees East |
TEMPERATURE | temperature | degrees C |
SALINITY | salinity | PSU |
SIGMA_THETA | sigma-theta | kg/m3 |
SBE_OXYGEN | oxygen measured by SBE | umol/kg |
O2_SAT_mL_L | oxygen saturation in milliters per liter | ml/L |
O2_SAT_umol_kg | oxygen saturation in micromoles per kilogram | umol/kg |
AOU | apparent oxygen utilization | umol/kg |
NO3_sample_IDs | internal reference number for sample | unitless |
sulfamic_treated | An asterisk indicates a sample was treated with sulfamic acid to remove nitrite prior to nitrate isotopic analysis | unitless |
d15N_NO3 | delta 15N of nitrate | per mil vs. N2 |
d15N_NO3_sd | standard deviation of d15N_NO3 | per mil |
d18O_NO3 | delta 18O of nitrate | per mil vs. VSMOW |
d18O_NO3_sd | standard deviation of d18O_NO3 | per mil |
d15N_NO2 | delta 15N of nitrite | per mil vs. N2 |
d15N_NO2_sd | standard deviation of d15N_NO2 | per mil |
d18O_NO2 | d18O of nitrite | per mil vs. VSMOW |
d18O_NO2_sd | standard deviation of d18O_NO2 | per mil |
N2O_sample_ID_1 | internal reference number for sample (replicate 1 of 2) | unitless |
N2O_sample_ID_2 | internal reference number for sample (replicate 2 of 2) | unitless |
N2O_conc | N2O concentration | nM |
N2O_conc_sd | standard deviation of N2O_conc | nM |
N2O_SP | N2O site preference | per mil |
N2O_SP_sd | standard deviation of N2O_SP | per mil |
d15N_N2O | delta 15N of N2O | per mil vs. N2 |
d15N_N2O_sd | standard deviation of d15N_N2O | per mil |
d18O_N2O | delta 18O of N2O | per mil vs. VSMOW |
d18O_N2O_sd | standard deviation of d18O_N2O | per mil |
d15Na | delta 15N of N2O-alpha | per mil vs. N2 |
d15Na_sd | standard deviation of d15Na | per mil |
d15Nb | delta 15N of N2O-beta | per mil vs. N2 |
d15Nb_sd | standard deviation of d15Nb | per mil |
Kelvin | Temperature in Kelvin | K |
ln_Ko | natural logarithm of Ko, the solubility of N2O in seawater as per Weiss and Price, 1980 | unitless |
Ko | solubility of N2O in seawater, as per Weiss and Price, 1980 | mol N2O/kg/atm |
N2O_sat_mol_kg | concentration of N2O at equilibrium with atmosphere at in situ temperature and salinity | mol N2O/kg |
N2O_sat_nmol_L | concentration of N2O at equilibrium with atmosphere at in situ temperature and salinity, converted to nmol/L | nmol N2O/L |
delta_N2O | N2O supersaturation, deltaN2O = [N2O]obs - [N2O]sat | nmol N2O/L |
ESPIW | % Eastern South Pacific Intermediate Water, as per Peters et al., 2018 Deep Sea Research II | % |
ESSW | % Equatorial Subsurface Water, as per Peters et al., 2018 Deep Sea Research II | % |
Dataset-specific Instrument Name | ThermoFinnigan DeltaPLUS XP |
Generic Instrument Name | Isotope-ratio Mass Spectrometer |
Dataset-specific Description | All isotopic measurements were made on a ThermoFinnigan DeltaPLUS XP isotope ratio mass spectrometer. |
Generic Instrument Description | The Isotope-ratio Mass Spectrometer is a particular type of mass spectrometer used to measure the relative abundance of isotopes in a given sample (e.g. VG Prism II Isotope Ratio Mass-Spectrometer). |
Website | |
Platform | RVIB Nathaniel B. Palmer |
Start Date | 2013-06-24 |
End Date | 2013-07-27 |
Description | Additional cruise information is available at:
http://www.marine-geo.org/link/entry.php?id=NBP1305 and https://gcmd.nasa.gov/KeywordSearch/Metadata.do?EntryId=NBP1305 |
The eastern tropical South Pacific (ETSP) is a hot spot for oceanic nitrogen cycling. This region of upwelling and high productivity fuels high rates of oxygen consumption below the mixed layer, nitrate regeneration from nitrification, and ultimately denitrification of nitrate to N2 gas. The climatically important trace gas nitrous oxide (N2O) also reaches extreme high concentrations in the oxycline and extreme low concentrations in the heart of the oxygen minimum zone (OMZ), indicating active cycling in this region. Despite many years of investigation, the mechanism of N2O production in this hot spot is ambiguous because of the potential overlap or coupling of nitrification and denitrification processes at low oxygen tensions.
The investigators employed novel stable isotopic techniques to identify processes involved with nitrous oxide production and consumption in the water column at multiple sites within the eastern tropical South Pacific. They also sought to map the natural distributions of nitrate, nitrite and nitrous oxide concentrations and isotopes at high spatial resolution in order to develop a dataset with which to constrain ocean models based on their rate measurements.
Incubation experiments were carried out at sea to quantify the rates of nitrification and N2O cycling in samples throughout the oxygen minimum zone. In addition, approximately 1000 samples were collected for nitrate and nitrite isotopic analysis and 500 samples for N2O isotopic analysis. The investigators worked closely with other researchers onboard to work towards developing the most coherent picture of nitrogen cycling in the eastern tropical Pacific to date.
Funding Source | Award |
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NSF Division of Ocean Sciences (NSF OCE) | |
NSF Division of Ocean Sciences (NSF OCE) |