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Nitrogen isotope effects in the assimilation of inorganic nitrogenous compounds by marine diatoms

Wada, Eitaro, Hattori, Akihiko·1978·Geomicrobiology Journal

Abstract

Nitrogen isotope fractionation in the assimilation of inorganic nitrogenous compounds was studied using marine diatoms (Phaeodactylum tricornutum and Chaetoceros sp.). The isotopic composition (δ15N) of the diatoms ranged from 7 to ‐18‰ relative to that of the nitrogen source, i.e., ammonium, nitrite, or nitrate. When the growth was light‐limited, the isotope fractionation in nitrate assimilation was inversely correlated with the growth rate. The highest fractionation factor of 1.016 was obtained when the growth rate was as low as 0.025 day‐1. Fractionation was negligible when the growth, rate was higher than 1 day‐1. A steady‐state kinetic model was applied to explain the isotope fractionation in nitrate assimilation. The nitrogen isotope fractionation primarily takes place at the step of N‐O bond breaking in nitrate reduction to nitrite. The extent of the isotope fractionation associated with the nitrate uptake is very small, and barely exceeds the limit of detection.

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Metadata

Authors
Wada, E., & Hattori, A.
Venue
Geomicrobiology Journal
Published
1978-01
Volume
1
Issue
1
Pages
85-101
ISSN
  • 0149-0451 (ISSN-L)
  • 1521-0529
OpenAlex
W2048227697
Cited by
320
References
16
FWCI
2.31
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Nitrogen isotope effects in the assimilation of inorganic nitrogenous compounds by marine diatoms. https://app.cochat.ai/papers/10.1080/01490457809377725
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Wada, E., & Hattori, A. (1978). Nitrogen isotope effects in the assimilation of inorganic nitrogenous compounds by marine diatoms. Geomicrobiology Journal. https://doi.org/10.1080/01490457809377725

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