Carbon and nutrient cycling in Antarctic landfast sea ice from winter to summer

Jones, Elizabeth M.; Henley, Sian F.; van Leeuwe, Maria A.; Stefels, Jacqueline; Meredith, Michael P. ORCID: https://orcid.org/0000-0002-7342-7756; Fenton, Mairi; Venables, Hugh J. ORCID: https://orcid.org/0000-0002-6445-8462. 2023 Carbon and nutrient cycling in Antarctic landfast sea ice from winter to summer. Limnology and Oceanography, 68 (1). 208-231. https://doi.org/10.1002/lno.12260

Before downloading, please read NORA policies.

Preview

Text (Open Access)
© 2022 The Authors. Limnology and Oceanography published by Wiley Periodicals LLC on behalf of Association for the Sciences of Limnology and Oceanography.
Limnology Oceanography - 2022 - Jones - Carbon and nutrient cycling in Antarctic landfast sea ice from winter to summer.pdf - Published Version
Available under License Creative Commons Attribution 4.0.
Download (6MB) | Preview

Official URL: https://aslopubs.onlinelibrary.wiley.com/doi/10.10...

Abstract/Summary

Seasonal cycling in carbon, alkalinity, and nutrients in landfast sea ice in Hangar Cove, Adelaide Island, West Antarctic Peninsula, were investigated during winter, spring, and summer 2014–2015. Temporal dynamics were driven by changes in the ice-sea physicochemical conditions, ice-algal community composition, and organic matter production. Winter sea ice was enriched with dissolved inorganic carbon (DIC) and inorganic nutrients from organic matter remineralization. Variations in alkalinity (Alk) and DIC indicated that abiotic calcium carbonate (ikaite) precipitation had taken place. Relative to other nutrients, low phosphate (PO4) concentrations potentially resulted from co-precipitation with ikaite. Seawater flooding and meltwater induced variability in the physical and biogeochemical properties in the upper ice in spring where nutrient resupply supported haptophyte productivity and increased particulate organic carbon (POC) in the interstitial layer. Rapid nitrate (NO3) and DIC (< 165 μmol kg−1) uptake occurred alongside substantial build-up of algal biomass (746 μg chlorophyll a L−1) and POC (6191 μmol L−1) during summer. Silicic acid drawdown followed NO3 depletion by approximately 1 month with a shift to diatom-dominated communities. Accumulation of PO4 in the lower ice layers in summer likely resulted from PO4 released during ikaite dissolution in the presence of biofilms. Increased Alk : DIC ratios in the lower ice and under-ice water suggested that ikaite dissolution buffered against meltwater dilution and enhanced the potential for atmospheric CO2 uptake. This study revealed strong seasonality in carbon and nutrient cycling in landfast sea ice and showed the importance of sea ice in biogeochemical cycling in seasonally ice-covered waters around Antarctica.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1002/lno.12260
ISSN:	0024-3590
Date made live:	15 Nov 2022 12:11 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/533550

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1002/lno.12260

ISSN:

0024-3590

Date made live:

15 Nov 2022 12:11 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/533550