Initial DOM properties ( t 0 ) and changes (diff) after 12 days of incubation under natural sunlight (per cent differences given in parentheses), including dissolved organic carbon (DOC), absorption coefficient of CDOM at 320 nm ( a 320 ), SUVA index ( A 254 /DOC), CDOM absorption slope at 290 nm ( S 290 ), and four PARAFAC components extracted from EEMs of fluorescence (C1–C4, and the sum C1–C4, given in Raman units, RU)

• Main Authors: Laurion, Isabelle, Mladenov, Natalie
• Format: Dataset
• Language: unknown
• Published: IOP Publishing 2013
• Subjects: Environmental Science; Arctic; Canada; Ice; permafrost; wedge*
• Online Access: https://dx.doi.org/10.6084/m9.figshare.1011780.v1; https://iop.figshare.com/articles/dataset/___Initial_DOM_properties_em_t_em_sub_0_sub_and_changes_diff_after_12_days_of_incubation_under_natur/1011780/1

Table 1. Initial DOM properties ( t 0 ) and changes (diff) after 12 days of incubation under natural sunlight (per cent differences given in parentheses), including dissolved organic carbon (DOC), absorption coefficient of CDOM at 320 nm ( a 320 ), SUVA index ( A 254 /DOC), CDOM absorption slope at 290 nm ( S 290 ), and four PARAFAC components extracted from EEMs of fluorescence (C1–C4, and the sum C1–C4, given in Raman units, RU). Significant treatment effect (ANOVA) is given in bold. Abstract The abundant thaw lakes and ponds in the circumarctic receive a new pool of organic carbon as permafrost peat soils degrade, which can be exposed to significant irradiance that potentially increases as climate warms and ice cover shortens. Exposure to sunlight is known to accelerate the transformation of dissolved organic matter (DOM) into molecules that can be more readily used by microbes. We sampled the water from two common classes of ponds found in the ice-wedge system of continuous permafrost regions of Canada, polygonal and runnel ponds, and followed the transformation of DOM over 12 days by looking at dissolved organic carbon (DOC) concentration and DOM absorption and fluorescence properties. The results indicate a relatively fast decay of color (3.4 and 1.6% loss d −1 of absorption at 320 nm for the polygonal and runnel pond, respectively) and fluorescence (6.1 and 8.3% loss d −1 of total fluorescent components, respectively) at the pond surface, faster in the case of humic-like components, but insignificant losses of DOC over the observed period. This result indicates that direct DOM mineralization (photochemical production of CO 2 ) is apparently minor in thaw ponds compared to the photochemical transformation of DOM into less chromophoric and likely more labile molecules with a greater potential for microbial mineralization. Therefore, DOM photolysis in arctic thaw ponds can be considered as a catalytic mechanism, accelerating the microbial turnover of mobilized organic matter from thawing permafrost and the production of greenhouse gases, especially in the most shallow ponds. Under a warming climate, this mechanism will intensify as summers lengthen.