Tracing the role of Arctic shelf processes in Si and N cycling and export through the Fram Strait: insights from combined silicon and nitrate isotopes

Nutrient cycles in the Arctic Ocean are being altered by changing hydrography, increasing riverine inputs, glacial melt and sea-ice loss due to climate change. In this study, combined isotopic measurements of dissolved nitrate ( δ 15 N-NO 3 and δ 18 O-NO 3 ) and silicic acid ( δ 30 Si(OH) 4 ) are us...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: M. C. F. Debyser, L. Pichevin, R. E. Tuerena, P. A. Dodd, A. Doncila, R. S. Ganeshram
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
Arctic
Arctic Ocean
Climate change
Fram Strait
Sea ice
Online Access:https://doi.org/10.5194/bg-19-5499-2022
https://doaj.org/article/35031836af68458ba8ce18409354cc23
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Summary:Nutrient cycles in the Arctic Ocean are being altered by changing hydrography, increasing riverine inputs, glacial melt and sea-ice loss due to climate change. In this study, combined isotopic measurements of dissolved nitrate ( δ 15 N-NO 3 and δ 18 O-NO 3 ) and silicic acid ( δ 30 Si(OH) 4 ) are used to understand the pathways that major nutrients follow through the Arctic Ocean. Atlantic waters were found to be isotopically lighter ( δ 30 Si(OH) <math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi/><mn mathvariant="normal">4</mn></msub><mo>=</mo><mo>+</mo></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="27pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="1a40839ccef088eeb629cb2b48ad95cd"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-19-5499-2022-ie00001.svg" width="27pt" height="10pt" src="bg-19-5499-2022-ie00001.png"/></svg:svg> 1.74 ‰) than their polar counterpart ( δ 30 Si(OH) <math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi/><mn mathvariant="normal">4</mn></msub><mo>=</mo><mo>+</mo></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="27pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="f65eb36be258f76aabb6be3a2cd3fb19"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-19-5499-2022-ie00002.svg" width="27pt" height="10pt" src="bg-19-5499-2022-ie00002.png"/></svg:svg> 1.85 ‰) owing to partial biological utilisation of dissolved Si (DSi) within the Arctic Ocean. Coupled partial benthic denitrification and nitrification on Eurasian Arctic shelves lead to the enrichment of δ 15 N-NO 3 and lighter δ 18 O-NO 3 in the polar surface waters ( δ 15 N-NO 3 = 5.44 ‰, δ 18 O-NO 3 ...

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