The goal of this thesis was to characterize and quantify changes to Canadian Arctic organic matter (OM) induced by a physical disruption to the permafrost active layer by employing molecular-level techniques such as biomarker extraction and NMR to help elucidate its contribution to carbon turnover and global climate change. The initial biomarker characterization study determined that the extractable plant lipids were unaltered originating from the deposition of new vascular material or permafrost melt where a high alteration of lignin-derived OM was observed suggesting a long residence time in the ecosystem. Analysis of samples where there was a new and historical physical disruption to the permafrost landscape showed an initial increase i...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Organic carbon (OC) stored in Arctic permafrost represents one of Earth's largest and most vulnerabl...
Permafrost soils have accumulated vast stores of organic carbon recently estimated to be ~1600 Pg C....
This is an accepted manuscript of a published article.With increased warming in the Arctic, permafro...
The vast reservoir of organic matter (OM) locked up in Arctic permafrost may become vulnerable to de...
Soil organic carbon (SOC) in permafrost terrain is vulnerable to climate change. Perennially frozen ...
The Arctic is changing rapidly. Due to permafrost thaw processes, the permafrost carbon store is bec...
Organic matter (OM) in arctic permafrost ground contains about twice as much carbon (C) as is curren...
Climate change has severe impacts in the Arctic, where permafrost is thawing, glaciers are retreatin...
Permafrost organic matter is becoming increasingly mobilized by thaw with ongoing climate warming. T...
Climate change is predicted to be the most pronounced in high latitude ecosystems, however very litt...
Rapid warming and changing precipitation patterns in northern regions are alleviating temperature an...
Climate change induced permafrost thaw in the Arctic is mobilizing ancient dissolved organic carbon ...
Increased mineralization of the organic matter (OM) stored in permafrost is expected to constitute t...
With a warming Arctic, degradation of permafrost is expected to release organic and inorganic materi...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Organic carbon (OC) stored in Arctic permafrost represents one of Earth's largest and most vulnerabl...
Permafrost soils have accumulated vast stores of organic carbon recently estimated to be ~1600 Pg C....
This is an accepted manuscript of a published article.With increased warming in the Arctic, permafro...
The vast reservoir of organic matter (OM) locked up in Arctic permafrost may become vulnerable to de...
Soil organic carbon (SOC) in permafrost terrain is vulnerable to climate change. Perennially frozen ...
The Arctic is changing rapidly. Due to permafrost thaw processes, the permafrost carbon store is bec...
Organic matter (OM) in arctic permafrost ground contains about twice as much carbon (C) as is curren...
Climate change has severe impacts in the Arctic, where permafrost is thawing, glaciers are retreatin...
Permafrost organic matter is becoming increasingly mobilized by thaw with ongoing climate warming. T...
Climate change is predicted to be the most pronounced in high latitude ecosystems, however very litt...
Rapid warming and changing precipitation patterns in northern regions are alleviating temperature an...
Climate change induced permafrost thaw in the Arctic is mobilizing ancient dissolved organic carbon ...
Increased mineralization of the organic matter (OM) stored in permafrost is expected to constitute t...
With a warming Arctic, degradation of permafrost is expected to release organic and inorganic materi...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Organic carbon (OC) stored in Arctic permafrost represents one of Earth's largest and most vulnerabl...
Permafrost soils have accumulated vast stores of organic carbon recently estimated to be ~1600 Pg C....