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Isotopic heterogeneity and cycling of organic nitrogen in the oligotrophic ocean
Author(s) -
Meador T. B.,
Aluwihare L. I.,
Mahaffey C.
Publication year - 2007
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.2007.52.3.0934
Subject(s) - photic zone , diazotroph , nitrogen fixation , nitrogen , sink (geography) , cycling , nitrogen cycle , environmental chemistry , organic matter , isotopes of nitrogen , heterotroph , isotopic signature , biology , chemistry , nutrient , bacteria , ecology , phytoplankton , stable isotope ratio , paleontology , history , physics , cartography , organic chemistry , archaeology , quantum mechanics , geography
We measured the nitrogen (N) isotopic composition (δ 15 N) of a large set (n = 38) of high‐molecular‐weight (HMW) dissolved organic nitrogen (DON) samples isolated from the tropical and subtropical North Atlantic and Pacific Oceans. The δ 15 N signature of surface HMW DON is relatively invariable in both oligotrophic basins (4.1 ± 0.6‰ in the Atlantic; 5.4 ± 0.8‰ in the Pacific) and shows little correlation with sources or concentrations of N supporting new production in the euphotic zone. While large variations in δ 15 N of bulk HMW DON are not apparent, δ 15 N of proteins isolated from sites with relatively high rates of N 2 fixation (>80 µmol N m −2 d −1 ) were consistently depleted in 15 N relative to bulk HMW DON and to proteins isolated from sites where N 2 fixation does not routinely occur. This small component of HMW DON appears to be cycling more rapidly than bulk HMW DON and may be indicative of fresh DON contributed by organisms in the surface ocean. Furthermore, δ 15 N of DNA extracted from the bacterial size fraction (0.2‐0.5 µm) revealed that free‐living bacteria may be an important sink for isotopically depleted N produced during N 2 fixation. We suggest that there exists a tight coupling between the production and uptake of DON contributed by diazotrophs (N 2 fixers) in regions where N 2 fixation provides a major input of new nitrogen.