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Euphotic zone nitrification in the California Current Ecosystem

TitleEuphotic zone nitrification in the California Current Ecosystem
Publication TypeJournal Article
Year of Publication2019
AuthorsStephens B.M, Wankel S.D, Beman J.M, Rabines A.J, Allen A.E, Aluwihare LI
Date Published2019/11
Type of ArticleArticle; Early Access
ISBN Number0024-3590
Accession NumberWOS:000493036300001
Keywordsammonia; bacteria; carbon export; gravitational sinking; Marine & Freshwater Biology; monterey bay; nitrate; nitrifying archaea; nitrous-oxide; oceanography; oxidation-kinetics; oxidizing; oxygen isotopic composition; primary nitrite maximum

Nitrification, the microbial conversion of ammonium to nitrite then to nitrate, occurs throughout the oceanic water column, yet the environmental factors influencing the production of nitrate in the euphotic zone (EZ) remain unclear. In this study, the natural abundances of N and O isotopes (delta N-15 and delta O-18, respectively) in nitrate were used in an existing model framework to quantify nitrate contributed by EZ nitrification in the California Current Ecosystem (CCE) during two anomalously warm years. Model data estimated that between 6% and 36% of the EZ nitrate reservoirs were derived from the combined steps of nitrification within the EZ. The CCE data set found nitrification contributions to EZ nitrate to be positively correlated with nitrite concentrations (NO2-) at the depth of the primary nitrite maximum (PNM). Building on this correlation, EZ nitrification in the southern California Current was estimated to contribute on average 20% +/- 6% to EZ nitrate as inferred using the PNM NO2- of the long-term California Cooperative Oceanic Fisheries Investigation (CalCOFI) survey record. A multiple linear regression analysis of the CalCOFI PNM NO2- time series identified two conditions that led to positive deviations in NO2-. Enhanced PNM NO2-, and potentially enhanced EZ nitrification, may be linked to (1) reduced phytoplankton competition for ammonium (NH4+) and NO2- as interpreted from particulate organic carbon:chlorophyll ratios, and/or (2) to increased supply of NH4+ (and then NH4+ oxidation to NO2-) from the degradation of organic nitrogen as interpreted from particulate organic nitrogen concentrations.

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