Nitrogen in past marine environments
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Increases in water-column denitrification under extremely low oxygen concentrations fractionate nitrogen isotopes in nitrate toward heavier δ15N values by up to 20‰.
“Increases in watercolumn denitrification under extremely low oxygen concentrations will fractionate N isotopes in nitrate towards heavier δ 15 N values by up to 20 ‰ (e.g., Galbraith et al., 2008).”
From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Galbraith et al., 2008
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- Authors
- Galbraith, E. D., Sigman, D. M., Robinson, R. S., & Pedersen, T. F.
- Venue
- Nitrogen in the Marine Environment
- Publisher
- Elsevier
- Published
- 2008
- Pages
- 1497-1535
- OpenAlex
- W2484519305
- Cited by
- 67
- References
- 199
- Citations by year
- 2026: 1 · 2025: 5 · 2024: 1 · 2023: 5 · 2022: 5 · 2021: 8 · 2020: 3 · 2019: 6 · 2018: 8 · 2017: 1 · 2016: 4 · 2015: 8 · 2014: 2 · 2013: 3 · 2012: 1
- FWCI
- 4.57
- Type
- book chapter
- Language
- en
- Open access
- Licence
- cc-by
- Locations
- Elsevier eBooks (publishedVersion)
- Journal of Media Literacy Education (submittedVersion, cc-by)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- marine nitrogen cycle, fixed nitrogen, glacial-interglacial cycles, marine sediment, ice cores, nitrogen residence time, paleoceanography
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