Arctic sea ice algae differ markedly from phytoplankton in their ecophysiological characteristics

Author(s):  
AC Kvernvik ◽  
CJM Hoppe ◽  
M Greenacre ◽  
S Verbiest ◽  
JM Wiktor ◽  
...  
2016 ◽  
Vol 98 ◽  
pp. 82-97 ◽  
Author(s):  
Jean-François Rontani ◽  
Simon T. Belt ◽  
Thomas A. Brown ◽  
Rémi Amiraux ◽  
Michel Gosselin ◽  
...  

2017 ◽  
Vol 585 ◽  
pp. 49-69 ◽  
Author(s):  
V Galindo ◽  
M Gosselin ◽  
J Lavaud ◽  
CJ Mundy ◽  
B Else ◽  
...  

2020 ◽  
Vol 648 ◽  
pp. 95-110 ◽  
Author(s):  
LC Lund-Hansen ◽  
I Hawes ◽  
K Hancke ◽  
N Salmansen ◽  
JR Nielsen ◽  
...  

Ice algae are key contributors to primary production and carbon fixation in the Arctic, and light availability is assumed to limit their growth and productivity. We investigated photo-physiological responses in sea ice algae to increased irradiance during a spring bloom in West Greenland. During a 14 d field experiment, light transmittance through sea ice was manipulated to provide 3 under-ice irradiance regimes: low (0.04), medium (0.08), and high (0.16) transmittances. Chlorophyll a decreased with elevated light availability relative to the control. Maximum dark-adapted photosynthetic efficiency (ΦPSII_max) showed an initially healthy and productive ice algae community (ΦPSII_max > 0.6), with ΦPSII_max decreasing markedly under high-light treatments. This was accompanied by a decrease in the light utilization coefficient (α) and photosynthetic capacity (maximum relative electron transfer rate), and a decrease in the ratio of mono- to polyunsaturated fatty acids. This was partly explained by a corresponding increase of photoprotective pigments (diadinoxanthin and diatoxanthin), and a development of mycosporine-like amino acids as identified from a distinctive spectral absorption peak at 360 nm. After 14 d, in situ fluorescence imaging revealed significant differences in ΦPSII_max between treatments of dark-adapted cells (i.e. those sampled before sunrise and after sunset), during diel cycles, with clear chronic photoinhibition in high and medium treatments. Data demonstrate the high sensitivity of spring-blooming Arctic sea ice algae to elevated irradiance caused by loss of snow cover. The predicted loss of snow cover on landfast ice will negatively impact ice algae, their potential primary production, and nutritional quality for higher trophic levels.


ARCTIC ◽  
2020 ◽  
Vol 73 (1) ◽  
pp. 114-117
Author(s):  
Spencer Apollonio

Arctic sea ice algae produce extracellular organic products, which, as bioconditioners of seawater, may stimulate early summer growth of pelagic, under-sea-ice phytoplankton in low light and low temperature conditions. Sea ice algae are inhibited or decline in numbers if prematurely exposed to high light conditions, thereby reducing their ability to produce bioconditioners. As climate change creates an early reduction or removal of snow and sea ice cover, the result may be a decrease in primary phytoplankton production.


2017 ◽  
Vol 122 (9) ◽  
pp. 7466-7487 ◽  
Author(s):  
Giulia Castellani ◽  
Martin Losch ◽  
Benjamin A. Lange ◽  
Hauke Flores

2017 ◽  
Vol 122 (6) ◽  
pp. 1486-1505 ◽  
Author(s):  
Hanna M. Kauko ◽  
Torbjørn Taskjelle ◽  
Philipp Assmy ◽  
Alexey K. Pavlov ◽  
C. J. Mundy ◽  
...  

Water ◽  
2019 ◽  
Vol 11 (5) ◽  
pp. 926
Author(s):  
Guiju Li ◽  
Huixiang Xie ◽  
Guisheng Song ◽  
Michel Gosselin

Chromophoric dissolved organic matter (CDOM) is highly enriched in bottom sea ice in the Arctic during ice algal blooms, giving rise to multifaceted ecological implications in both the sea ice and the underlying seawater. We conducted laboratory culture incubations to assess the potential role of ice algae in the accumulation of CDOM in Arctic sea ice. Non-axenic monocultures of Attheya septentrionalis and Nitzschia frigida and a natural ice algal assemblage (NIAA) were grown at 4 °C in an f/2 medium under cool white fluorescent light. Culture samples were collected several days apart throughout the exponential, stationary, and senescent phases, and analyzed for CDOM absorbance, chlorophyll a, and bacterial cell abundance. The cultures displayed apparent specific growth rates of algal and bacterial cells comparable to those in the field. Accumulations of CDOM were observed in all cultures during the time-course incubations, with the senescent phase showing the largest accumulations and the highest production rates. The senescent-phase production rate for NIAA was ~40% higher than that for A. septentrionalis. The chlorophyll a-normalized CDOM production rates in the cultures are comparable to those reported for Arctic first-year sea ice. The absorption spectra of CDOM in the cultures exhibited characteristic short-ultraviolet shoulders similar to those previously identified in sea ice. This study demonstrates that ice algal-derived CDOM can account for the springtime accumulation of CDOM in Arctic sea ice.


2016 ◽  
Vol 51 (3) ◽  
pp. 387-396 ◽  
Author(s):  
Ho Jung Song ◽  
Jae Hyung Lee ◽  
Gawn Woo Kim ◽  
So Hyun Ahn ◽  
Houng-Min Joo ◽  
...  

1973 ◽  
Vol 30 (6) ◽  
pp. 835-838 ◽  
Author(s):  
R. C. Clasby ◽  
Rita Horner ◽  
Vera Alexander

With the use of SCUBA diving and a new 14C incubation chamber, the rates of carbon fixation by the algal community that lives within the undersurface of sea ice have been measured. Rates of primary productivity ranged from 7.67-mg C/m2∙hr near the peak of the bloom to a low of 0.30-mg C/m2∙hr just prior to the thaw period.


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