Fritsen, Christian H; Wirthlin, Eric D; Momberg, Diane K; Lewis, Michael J; Ackley, Stephen F (2011): (Table 1) Chlorophyll a content and microalgae abundance and biovolume in pack ice in the Bellingshausen Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.810069,

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Supplement to: Fritsen, CH et al. (2011): Bio-optical properties of Antarctic pack ice in the early austral spring. Deep Sea Research Part II: Topical Studies in Oceanography, 58(9-10), 1052-1061, https://doi.org/10.1016/j.dsr2.2010.10.028

Pack ice in the Bellingshausen Sea contained moderate to high stocks of microalgal biomass (3-10 mg Chl a/m**2) spanning the range of general sea-ice microalgal microhabitats (e.g., bottom, interior and surface) during the International Polar Year (IPY) Sea Ice Mass Balance in the Antarctic (SIMBA) studies. Measurements of irradiance above and beneath the ice as well as optical properties of the microalgae therein demonstrated that absorption of photosynthetically active radiation (PAR) by particulates (microalgae and detritus) had a substantial influence on attenuation of PAR and irradiance transmission in areas with moderate snow covers (0.2-0.3 m) and more moderate effects in areas with low snow cover. Particulates contributed an estimated 25 to 90% of the attenuation coefficients for the first-year sea ice at wavelengths less than 500 nm. Strong ultraviolet radiation (UVR) absorption by particulates was prevalent in the ice habitats where solar radiation was highest - with absorption coefficients by ice algae often being as large as that of the sea ice. Strong UVR-absorption features were associated with an abundance of dinoflagellates and a general lack of diatoms - perhaps suggesting UVR may be influencing the structure of some parts of the sea-ice microbial communities in the pack ice during spring. We also evaluated the time-varying changes in the spectra of under-ice irradiances in the austral spring and showed dynamics associated with changes that could be attributed to coupled changes in the ice thickness (mass balance) and microalgal biomass. All results are indicative of radiation-induced changes in the absorption properties of the pack ice and highlight the non-linear, time-varying, biophysical interactions operating within the Antarctic pack ice ecosystem.

Weighted average Chl a concentration was originally given in mg/m**3 and was converted into µg/cm**3 by dividing by 1000. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150