Seawater samples were obtained during the R/V Atlantis (AT15-61) and R/V Melville (MV1104) cruises from January to February 2010 and March to April 2011. Water samples were collected at discrete depths using Niskin bottle type rosette samplers equipped with either 24 bottles (10L) or 12 bottles (20L), and an SBE9plus conductivity-temperature-depth (CTD) sensor package (SeaBird Electronics, Bellevue, WA).
The d15N and d18O of NO3- was determined using the "denitrifier" method (Casciotti et al., 2002; Sigman et al., 2001) with updated techniques (McIlvin & Casciotti, 2011). Samples were treated with sulfamic acid to remove NO2-, if present (Granger & Sigman, 2009).
The d15N and d18O of NO2- was determined using the chemical reduction of NO2- to nitrous oxide (N2O) using the "azide method" (McIlvin & Altabet, 2005).
Samples were collected on the R/V Atlantis in January through February 2010, and the R/V Melville in March through April 2011 between 10° and 20° South and between 80° and 100° West, with station locations and sample depths, salinities, sigma theta, oxygen concentrations values, etc. reported in the 'ETSP N2O' dataset. Water column samples were collected by Niskin bottles deployed on a rosette equipped with conductivity-temperature-depth (CTD) sensors. All samples were collected into sample-rinsed HDPE bottles and passed through a 0.2 micrometer (um) filter before collection, and were stored at -20° Celsius until analysis on land.