Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming

Silicon (Si) exports from terrestrial to marine systems can dictate phytoplankton species composition in Arctic coastal waters. Diatoms are often the dominant autotroph in Arctic waters, making Si an important control on Arctic marine primary productivity. Yet, even as Arctic regions are among the f...

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Main Author: Carey, Joanna
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2020
Subjects:
Online Access:https://doi.org/10.5061/dryad.7sqv9s4pp
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spelling ftzenodo:oai:zenodo.org:4960351 2024-09-15T18:29:54+00:00 Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming Carey, Joanna 2020-02-20 https://doi.org/10.5061/dryad.7sqv9s4pp unknown Zenodo https://doi.org/10.1029/2019gb006308 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.7sqv9s4pp oai:zenodo.org:4960351 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode biogenic silica dissolved silica Permafrost info:eu-repo/semantics/other 2020 ftzenodo https://doi.org/10.5061/dryad.7sqv9s4pp10.1029/2019gb006308 2024-07-26T19:23:04Z Silicon (Si) exports from terrestrial to marine systems can dictate phytoplankton species composition in Arctic coastal waters. Diatoms are often the dominant autotroph in Arctic waters, making Si an important control on Arctic marine primary productivity. Yet, even as Arctic regions are among the fastest warming on Earth, we lack baseline knowledge on the magnitudes and controls of Arctic river Si exports. To address uncertainties in current and future Si behavior, we used a combination of field data and modeling to quantify daily yields of dissolved Si (DSi) and biogenic Si (BSi) from a 400 km space‐for‐time latitudinal gradient of seven basins across the boreal‐Arctic transition in Alaska (USA) over the course of two years (2015‐2016). Mean annual DSi concentrations (33‐149 μM) and yields (13‐49 kmol km ‐2 yr ‐1 ) were significantly and positively correlated with mean basin active layer depth, indicating that permafrost thaw will likely increase DSi fluxes to Arctic coastal waters. Conversely, BSi concentrations (7‐16 μM) and yields (2.6‐4.5 kmol km ‐2 yr ‐1 ) were more uniform across the seven basins, indicating that warming may not substantially alter BSi loads to coastal systems in the near future. Our data also indicate that climatic warming will advance the timing of Si delivery to coastal waters in the spring, although the ratios of Si to nitrogen in Arctic river exports will likely remain steady. These results highlight the important role of basin hydrology, largely driven by permafrost extent, as a key driver of Si exchange at the land‐sea interface in the Arctic. Data includes concentration (units in micromolar, also indicated in spreadsheet) and flow data (area-normalized water yields in cubic meters per hour per square kilometer). Any missing cells or 'NA's means that no data available for that sample. Funding provided by: National Science Foundation Crossref Funder Registry ID: http://dx.doi.org/10.13039/100000001 Award Number: 1451527 Other/Unknown Material permafrost Phytoplankton Alaska Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic biogenic silica
dissolved silica
Permafrost
spellingShingle biogenic silica
dissolved silica
Permafrost
Carey, Joanna
Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming
topic_facet biogenic silica
dissolved silica
Permafrost
description Silicon (Si) exports from terrestrial to marine systems can dictate phytoplankton species composition in Arctic coastal waters. Diatoms are often the dominant autotroph in Arctic waters, making Si an important control on Arctic marine primary productivity. Yet, even as Arctic regions are among the fastest warming on Earth, we lack baseline knowledge on the magnitudes and controls of Arctic river Si exports. To address uncertainties in current and future Si behavior, we used a combination of field data and modeling to quantify daily yields of dissolved Si (DSi) and biogenic Si (BSi) from a 400 km space‐for‐time latitudinal gradient of seven basins across the boreal‐Arctic transition in Alaska (USA) over the course of two years (2015‐2016). Mean annual DSi concentrations (33‐149 μM) and yields (13‐49 kmol km ‐2 yr ‐1 ) were significantly and positively correlated with mean basin active layer depth, indicating that permafrost thaw will likely increase DSi fluxes to Arctic coastal waters. Conversely, BSi concentrations (7‐16 μM) and yields (2.6‐4.5 kmol km ‐2 yr ‐1 ) were more uniform across the seven basins, indicating that warming may not substantially alter BSi loads to coastal systems in the near future. Our data also indicate that climatic warming will advance the timing of Si delivery to coastal waters in the spring, although the ratios of Si to nitrogen in Arctic river exports will likely remain steady. These results highlight the important role of basin hydrology, largely driven by permafrost extent, as a key driver of Si exchange at the land‐sea interface in the Arctic. Data includes concentration (units in micromolar, also indicated in spreadsheet) and flow data (area-normalized water yields in cubic meters per hour per square kilometer). Any missing cells or 'NA's means that no data available for that sample. Funding provided by: National Science Foundation Crossref Funder Registry ID: http://dx.doi.org/10.13039/100000001 Award Number: 1451527
format Other/Unknown Material
author Carey, Joanna
author_facet Carey, Joanna
author_sort Carey, Joanna
title Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming
title_short Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming
title_full Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming
title_fullStr Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming
title_full_unstemmed Arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming
title_sort arctic river dissolved and biogenic silicon exports - current conditions and future changes with warming
publisher Zenodo
publishDate 2020
url https://doi.org/10.5061/dryad.7sqv9s4pp
genre permafrost
Phytoplankton
Alaska
genre_facet permafrost
Phytoplankton
Alaska
op_relation https://doi.org/10.1029/2019gb006308
https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.7sqv9s4pp
oai:zenodo.org:4960351
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.7sqv9s4pp10.1029/2019gb006308
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