Detrital input sustains diatom production off a glaciated Arctic coast
Ng, Hong Chin; Hendry, Katharine R. ORCID: https://orcid.org/0000-0002-0790-5895; Ward, Rachael; Woodward, E.M.S.; Leng, Melanie J. ORCID: https://orcid.org/0000-0003-1115-5166; Pickering, Rebecca A.; Krause, Jeffrey W.. 2024 Detrital input sustains diatom production off a glaciated Arctic coast. Geophysical Research Letters, 51 (12), e2024GL108324. 11, pp. https://doi.org/10.1029/2024GL108324
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© 2024. The Author(s). Geophysical Research Letters - 2024 - Ng - Detrital Input Sustains Diatom Production off a Glaciated Arctic Coast.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (1MB) | Preview |
Abstract/Summary
In the Arctic and subarctic oceans, the relatively low supply of silicon (compared to other nutrients) can make it limiting for the growth of diatoms, a fundamental building block of the oceanic food web. Glaciers release large quantities of dissolved silicon and dissolvable solid amorphous silica phases into high-latitude estuaries (fjords), but the role of these glacially-derived silica phases in sustaining diatom growth in the coastal and open-water sectors remains unknown. Here we show how stable and radiogenic silicon isotopes can be used together to address this question, using southwest Greenland as a case study. This study finds enhanced levels of detrital (i.e., mineral) amorphous silica, likely glacially-sourced, sustaining a large portion of diatom growth observed off the coast, revealing how the phytoplankton community can function during high-meltwater periods.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | https://doi.org/10.1029/2024GL108324 |
ISSN: | 0094-8276 |
Additional Keywords: | Arctic coast, nutrient cycling, glacial weathering products, isotope application, Polar marine ecosystems |
Date made live: | 13 Jun 2024 11:07 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/534355 |
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