Toggle Main Menu Toggle Search

Open Access padlockePrints

Nitrogen fixation rates diagnosed from diurnal changes in elemental stoichiometry

Lookup NU author(s): Professor Sam Wilson

Downloads


Licence

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License (CC BY-NC 4.0).


Abstract

© 2018 The Authors. Limnology and Oceanography published by Wiley Periodicals, Inc. on behalf of Association for the Sciences of Limnology and Oceanography. The carbon, nitrogen, and phosphorus (C, N, and P, respectively) composition and elemental ratios were measured in the 20–200 μm size fraction during July 2015 in the surface waters of an anticyclonic eddy encountered north of Hawaii in the oligotrophic North Pacific Subtropical Gyre. The observed particulate N : P ratio fluctuated by approximately a factor of two over the diel cycle. We present a simple mathematical argument connecting this change to a rate of biological nitrogen fixation, and calculate the nitrogen fixation rate to be ≥ 13 nmol L−1 d−1 for this size class. This value is higher than simultaneous bottle-incubation based rates measured with isotopic tracers, yet is consistent with historic rate measurements from the region. As confirmation of our methods, diurnal changes in C : N : P of laboratory cultures of the diazotrophic genus Trichodesmium were measured. In the laboratory, we show that estimates of nitrogen fixation from stoichiometric time series are equivalent to those derived directly from mass balance. The disparity between nitrogen fixation rates derived from tracer measurements and particulate stoichiometry in the field suggests that large diazotrophs may be underestimated in small volume (∼ 4 L) bottle incubations as a result of either spatial heterogeneity or vertical migration of large cells. Otherwise, processes other than diazotrophy must cause the observed changes in stoichiometry. This approach represents a novel and scalable means of quantifying in situ nitrogen fixation rates from diurnal changes in size-fractionated stoichiometry. We also infer carbon fixation, growth rates, and phosphorus uptake in the 20–200 μm size class.


Publication metadata

Author(s): Follett CL, White AE, Wilson ST, Follows MJ

Publication type: Article

Publication status: Published

Journal: Limnology and Oceanography

Year: 2018

Volume: 63

Issue: 5

Pages: 1911-1923

Print publication date: 01/09/2018

Online publication date: 26/04/2018

Acceptance date: 14/03/2018

Date deposited: 16/12/2021

ISSN (print): 0024-3590

Publisher: Wiley-Blackwell

URL: https://doi.org/10.1002/lno.10815

DOI: 10.1002/lno.10815


Altmetrics

Altmetrics provided by Altmetric


Funding

Funder referenceFunder name
329108
3778
553242
3794

Share