Effects of increase glacier discharge on phytoplankton bloom dynamics and pelagic geochemistry in a high Arctic fjord. (December 2017)

• Record Type: Journal Article
• Authors: Calleja, Maria Ll.; Kerhervé, P.; Bourgeois, S.; Kędra, M.; Leynaert, A.; Devred, E.; Babin, M.; Morata, N.
• Is Part Of: Progress in oceanography. Volume 159(2017:Dec.)
• Page Start: 195
• Page End: 210
• Publication Date: 2017-12
• Subjects: Arctic -- Fjords -- Glaciers -- Organic matter -- Diatom bloom -- Carbon and nitrogen stable isotopes; Norway -- Svalbard -- Spitsbergen -- Kongsfjorden; Oceanography -- Periodicals; 551.4605
• DOI: 10.1016/j.pocean.2017.07.005
• Languages: English
• ISSNs: 0079-6611

Abstract

Highlights: Glacier retreat is affecting the ecosystem dynamics of high arctic fjords. Seasonal and spatial environmental changes of Kongsfjorden were examined during 2012. The bloom dynamics and changes in the pelagic geochemistry were evaluated. A singular and strong diatom bloom was observed in May at the fjord glacier front. Isotopic data revealed very depleted organic material during high melting seasons. Abstract: Arctic fjords experience extremely pronounced seasonal variability and spatial heterogeneity associated with changes in ice cover, glacial retreat and the intrusion of continental shelf's adjacent water masses. Global warming intensifies natural environmental variability on these important systems, yet the regional and global effects of these processes are still poorly understood. In the present study, we examine seasonal and spatial variability in Kongsfjorden, on the western coast of Spitsbergen, Svalbard. We report hydrological, biological, and biogeochemical data collected during spring, summer, and fall 2012. Our results show a strong phytoplankton bloom with the highest chlorophyll a (Chl a ) levels ever reported in this area, peaking 15.5 µg/L during late May and completely dominated by large diatoms at the inner fjord, that may sustain both pelagic and benthic production under weakly stratified conditions at the glacier front. A progressively stronger stratification of the water column during summer and fall was shaped by the intrusion of warm Atlantic water (T > 3 °C and Sal > 34.65) into the fjord at around 100 m depth, and by turbid freshwater plumes (T < 1 °C and Sal < 34.65) at the surface due to glacier meltwater input. Biopolymeric carbon fractions and isotopic signatures of the particulate organic material (POM) revealed very fresh and labile material produced during the spring bloom ( 13 C enriched, with values up to −22.7‰ at the highest Chl a peak, and high in carbohydrates and proteins content – up to 167 and 148 µg/L, respectively-), and a clear and strong continental signature of the POM present during late summer and fall ( 13 C depleted, with values averaging −26.5‰, and high in lipid content – up to 92 µg/L-) when freshwater melting is accentuated. Our data evidence the importance of combining both physical (i.e. water mass dominance) and geochemical (i.e. characteristics of material released by glacier runoff) data in order to understand the timing, intensity and characteristics of the phytoplankton bloom in Kongsfjorden, a continuously changing system due to sustained warming. In a scenario where glacial retreat is predicted to increase the impacts of meltwater discharge and associated delivery of organic and inorganic material to the surrounding waters, special attention is required in order to predict the consequences for Arctic fjords and adjacent shelf ecosystems.