Arctic River Dissolved and Biogenic Silicon Exports—Current Conditions and Future Changes With Warming. Issue 3 (28th February 2020)

• Record Type: Journal Article
• Authors: Carey, Joanna C.; Gewirtzman, Jonathan; Johnston, Sarah Ellen; Kurtz, Andrew; Tang, Jianwu; Vieillard, Amanda M.; Spencer, Robert G. M.
• Is Part Of: Global biogeochemical cycles. Volume 34:Issue 3(2020:Mar.)
• Page Start: no
• Page End: no
• Publication Date: 2020-02-28
• Subjects: Arctic -- rivers -- biogenic -- silica -- dissolved silica -- climate change -- permafrost; Biogeochemical cycles -- Periodicals; Electronic journals; 577.1405
• DOI: 10.1029/2019GB006308
• Languages: English
• ISSNs: 0886-6236

Abstract

Abstract: 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 (United States) over the course of 2 years (2015–2016). Mean annual DSi concentrations (33–149 μM) and yields (13–49 kmol km −2 year −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 year −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. Key Points: Increasing active layer depth is associated with significantly higher dissolved Si exports, while biogenic Si shows no such pattern Climatic warming is likely to increase dissolved, but not biogenic, Si exports from Alaskan Arctic rivers to coastal receiving waters Permafrost thaw, and associated shifts in hydrology, exert a larger control over Arctic Si exports, compared to shifting vegetation cover