2021
DOI: 10.1029/2020gb006775
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Assessment of C, N, and Si Isotopes as Tracers of Past Ocean Nutrient and Carbon Cycling

Abstract: Review of oceanic distribution, controlling processes, and sedimentary archives of C, N, and Si isotopes • Late Quaternary C, N, and Si sedimentary isotope records demonstrate coupling between the biological pump and atmospheric pCO2 • Cenozoic C, N, and Si sedimentary isotope records indicate large-scale changes in nutrient sources, concentrations, and the carbon cycle ESSOAr |

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Cited by 9 publications
(3 citation statements)
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“…It is advisable to determine the δ 13 C values of Particulate Organic Matter (POM) from the region and/or the δ 15 N values of an organism with a known trophic position (e.g., δ 15 N value of a filter-feeder species that it is in the second trophic level). To overcome the necessity of analysing POM stable isotopic values, it is possible to use values obtained from previous studies, or studies that modelled isotopic variation around the world's oceans (Somes et al, 2010;Farmer et al, 2021;St John Glew et al, 2021). However, when using values from previous studies or when comparing values obtained in beaks collected in different periods, it is necessary to account for the temporal variation of isotopes in the environment.…”
Section: Stable Isotopesmentioning
confidence: 99%
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“…It is advisable to determine the δ 13 C values of Particulate Organic Matter (POM) from the region and/or the δ 15 N values of an organism with a known trophic position (e.g., δ 15 N value of a filter-feeder species that it is in the second trophic level). To overcome the necessity of analysing POM stable isotopic values, it is possible to use values obtained from previous studies, or studies that modelled isotopic variation around the world's oceans (Somes et al, 2010;Farmer et al, 2021;St John Glew et al, 2021). However, when using values from previous studies or when comparing values obtained in beaks collected in different periods, it is necessary to account for the temporal variation of isotopes in the environment.…”
Section: Stable Isotopesmentioning
confidence: 99%
“…However, when using values from previous studies or when comparing values obtained in beaks collected in different periods, it is necessary to account for the temporal variation of isotopes in the environment. To solve this, the obtained δ 13 C values need to be corrected considering the Suess effect when values span across decades or consider modelled past δ 13 C values (Farmer et al, 2021). For the δ 15 N, the use of values obtained by previous modelling studies is so far the best option (Somes et al, 2010;Farmer et al, 2021;Verwega et al, 2021).…”
Section: Stable Isotopesmentioning
confidence: 99%
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