A Close Look at Dissolved Silica Dynamics in Disko Bay, West Greenland
Publication Date
1-1-2025
Document Type
Article
Publication Title
Global Biogeochemical Cycles
Volume
39
Issue
1
DOI
10.1029/2023GB008080
Abstract
Discharge of calved ice, runoff and mixing driven by subglacial discharge plumes likely have consequences for marine biogeochemistry in Disko Bay, which hosts the largest glacier in the northern hemisphere, Sermeq Kujalleq. Glacier retreat and increasing runoff may impact the marine silica cycle because glaciers deliver elevated concentrations of dissolved silica (dSi) compared to other macronutrients. However, the annual flux of dSi delivered to the ocean from the Greenland Ice Sheet is poorly constrained because of difficulties distinguishing the overlapping influence of different dSi sources. Here we constrain silica dynamics around Disko Bay, including the Ilulissat Icefjord and four other regions receiving glacier runoff with contrasting levels of productivity and turbidity. Both dissolved silica and Si* ([dSi]-[NOx−]) concentrations indicated conservative dynamics in two fjords with runoff from land-terminating glaciers, consistent with the results of mixing experiments. In three fjords with marine-terminating glaciers, macronutrient-salinity distributions were strongly affected by entrainment of nutrients in subglacial discharge plumes. Entrainment of dSi from saline waters explained 93 ± 51% of the dSi enrichment in the outflowing plume from Ilulissat Icefjord, whereas the direct contribution of freshwater to dSi in the plume was likely 0%–3%. Whilst not distinguished herein, other minor regional dSi sources include icebergs and dissolution of amorphous silica (aSi) in either pelagic or benthic environments. Our results suggest that runoff around Greenland is supplemented as a dSi source by minor fluxes of 0.25 ± 0.67 Gmol yr−1 dSi from icebergs and ∼1.9 Gmol year−1 from pelagic aSi dissolution.
Funding Number
42150610482
Funding Sponsor
National Natural Science Foundation of China
Keywords
glacier, Greenland, iceberg, nutrient, ocean, silica
Department
Moss Landing Marine Laboratories
Recommended Citation
Mark J. Hopwood, Dustin Carroll, Yuanyuan Gu, Xin Huang, Jana Krause, Stefano Cozzi, Carolina Cantoni, María Fernanda Gastelu Barcena, Shandy Carroll, and Arne Körtzinger. "A Close Look at Dissolved Silica Dynamics in Disko Bay, West Greenland" Global Biogeochemical Cycles (2025). https://doi.org/10.1029/2023GB008080
Comments
The final version of the article will be available on 1st July 2025 due to embargo policy