Nitrate, nitrite, and nitrous oxide isotope measurements from the Eastern Tropical South Pacific ocean collected on RVIB Nathaniel B. Palmer cruise NBP1305 from June to July 2013

Website: https://www.bco-dmo.org/dataset/744679
Data Type: Cruise Results
Version: 1
Version Date: 2018-08-28

Project
» Biogeochemistry of nitrous oxide cycling in the eastern tropical South Pacific (N2O Cycling)
ContributorsAffiliationRole
Casciotti, Karen L.Stanford UniversityPrincipal Investigator
Rauch, ShannonWoods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager

Abstract
Nitrate, nitrite, and nitrous oxide isotope measurements from the Eastern Tropical South Pacific ocean collected on RVIB Nathaniel B. Palmer cruise NBP1305 from June to July 2013. The data in this dataset were published in Peters et al. (2018) and Casciotti et al. (2018).


Coverage

Spatial Extent: N:-11.99976 E:-70.58334 S:-22.21654 W:-85.9989
Temporal Extent: 2013-06-27 - 2013-07-19

Dataset Description

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).


Methods & Sampling

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.


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Data Files

File
ETSP_NBP13-05.csv
(Comma Separated Values (.csv), 126.91 KB)
MD5:d1c9102c3a7f7b5fa0f1c9dc849c9d0a
Primary data file for dataset ID 744679

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Related Publications

Casciotti, K. L., Forbes, M., Vedamati, J., Peters, B., Martin, T., & Mordy, C. W. (2018). Nitrous oxide cycling in the Eastern Tropical South Pacific as inferred from isotopic and isotopomeric data. Deep Sea Research Part II: Topical Studies in Oceanography. doi:10.1016/j.dsr2.2018.07.014
Results
Peters, B., Horak, R., Devol, A., Fuchsman, C., Forbes, M., Mordy, C. W., & Casciotti, K. L. (2018). Estimating fixed nitrogen loss and associated isotope effects using concentration and isotope measurements of NO 3 – , NO 2 – , and N 2 from the Eastern Tropical South Pacific oxygen deficient zone. Deep Sea Research Part II: Topical Studies in Oceanography. doi:10.1016/j.dsr2.2018.02.011
Results

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Parameters

ParameterDescriptionUnits
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

%


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Instruments

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).


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Deployments

NBP1305

Website
Platform
RVIB Nathaniel B. Palmer
Start Date
2013-06-24
End Date
2013-07-27
Description


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Project Information

Biogeochemistry of nitrous oxide cycling in the eastern tropical South Pacific (N2O Cycling)

Coverage: Peruvian Oxygen Deficient Zone


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.



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Funding

Funding SourceAward
NSF Division of Ocean Sciences (NSF OCE)
NSF Division of Ocean Sciences (NSF OCE)

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