Document Type
Article
Publication Date
12-10-2019
Publication Title
Limnology and Oceanography
Volume
65
Issue
6
First Page
1217
Last Page
1234
Abstract
The standard model for aquatic ecosystems is to link hydrologic connectivity to dissolved organic carbon (DOC) concentration and dissolved organic matter (DOM) composition and, ultimately, reactivity. Studies across effective precipitation gradients have been suggested as models for predicting how carbon cycling will change in Arctic aquatic ecosystems with projected drying (i.e., reduced hydrologic connectivity). To evaluate links between DOM dynamics and hydrologic connectivity, 41 stream samples from Greenland were analyzed across an effective precipitation gradient for DOM optical properties and elemental composition using ultrahigh-resolution mass spectrometry. Sites with negative effective precipitation and decreased hydrologic connectivity exhibited elevated specific conductivity (SpC) and DOC concentrations as well as DOM composition indicative of decreased hydrologic connectivity, for example, lower aromaticity, assessed using carbon-specific UV absorbance at 254 nm, decreased relative abundances of polyphenolic and condensed aromatic compounds, and increased relative abundances of highly unsaturated and phenolic compounds. Allochthonous inputs decreased as the summer progressed as exhibited by decreases in aromatic compounds. A decrease in molecular richness and N-containing compounds coincided with the decrease in allochthonous inputs. DOC concentrations increased over the summer but more slowly than SpC, suggesting degradation processes outweighed combined evapoconcentration and production. The patterns in DOM composition suggest evapoconcentration and photodegradation are dominant controls. However, when hydrologic connectivity was high, regardless of effective precipitation, DOM reflected allochthonous sources such as snowmelt-fed wetlands. These results highlight the challenges of modeling carbon cycling in aquatic ecosystems across effective precipitation gradients, particularly those with strong seasonality and regional variability in hydrologic inputs.
Recommended Citation
Kllerman, Anne M.; Arellano, Ana; Podgorski, David C.; Martin, Ellen E.; Martin, Jonathan B.; Deuerling, Kelly M.; Bianchi, Thomas S.; and Spencer, Robert G. M., "Fundamental drivers of dissolved organic matter composition across an Arctic effective precipitation gradient" (2019). Geography and Geology Faculty Publications. 82.
https://digitalcommons.unomaha.edu/geoggeolfacpub/82
Comments
This is the accepted version of an article published by ASLO's Limnology and Oceanography on December 10, 2019 and can be accessed at https://doi.org/10.1002/lno.11385
This is the peer reviewed version of the following article: Kellerman AM, Arellano A, Podgorski DC, Martin EE, Martin JB, Deuerling KM, Bianchi TS, Spencer RGM (2019) Fundamental drivers of dissolved organic matter composition across an Arctic effective precipitation gradient. Limnology & Oceanography , which has been published in final form at [https://doi.org/10.1002/lno.11385]. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions.