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Brent G. Pautler

Researcher at University of Toronto

Publications -  21
Citations -  494

Brent G. Pautler is an academic researcher from University of Toronto. The author has contributed to research in topics: Arctic & Climate change. The author has an hindex of 11, co-authored 20 publications receiving 432 citations. Previous affiliations of Brent G. Pautler include Advanced Chemistry Development & University of Guelph.

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Arctic Permafrost Active Layer Detachments Stimulate Microbial Activity and Degradation of Soil Organic Matter

TL;DR: It is indicated that ALDs may amplify climate change due to the release of labile SOM substrates from thawing High Arctic permafrost.
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Molecular characterization of dissolved organic matter in glacial ice: coupling natural abundance 1H NMR and fluorescence spectroscopy.

TL;DR: This study suggests that the bulk of the dissolved organic matter from these glaciers is a mixture of biologically labile molecules derived from microbes.
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Evidence for the enhanced lability of dissolved organic matter following permafrost slope disturbance in the Canadian High Arctic

TL;DR: In this article, passive samplers were placed throughout paired High Arctic watersheds during the duration of the 2008 spring flush in Nunavut, Canada and were analyzed for structural and spectral characteristics via NMR and fluorescence spectroscopy as well as vulnerability to degradation with simulated solar exposure.
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Synthesis and surface control of colloidal Cr3+-doped SnO2 transparent magnetic semiconductor nanocrystals.

TL;DR: The synthesis of colloidal Cr(3+)-doped SnO(2) nanocrystals prepared under mild conditions via a hydrolysis method is described and it is shown by means of nanocrystal surface ligand exchange that even under mild reaction conditions a significant fraction of the dopant ions reside on the Nanocrystal surfaces.
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Detection and structural identification of dissolved organic matter in Antarctic glacial ice at natural abundance by SPR-W5-WATERGATE 1H NMR spectroscopy.

TL;DR: The detection of free amino acid and amino sugar monomer components of peptidoglycan within the ice suggests that Antarctic glacial DOM likely originates from in situ microbial activity, which may result in a flux of nutrients into adjacent ecosystems.