Ge N0

Ms. Ge N0


Research Focus & Metrics

Academic Career Length

14Years (2013-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 November 2017 in Applied Soil Ecology
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Journal Article
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ABAdnane Bargaz
Adnane Bargaz
GNGe N0
Ge N0
RFRoberta Fulthorpe
Roberta Fulthorpe
GCGeorg Carlsson
Georg Carlsson
JFJessie R. Furze
Jessie R. Furze
MIMarney E. Isaac
Marney E. Isaac

9 July 2014 in GCB Bioenergy
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Journal Article
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TSTara E. Sackett
Tara E. Sackett
NBNathan Basiliko
Nathan Basiliko
GNGe N0
Ge N0
CWCarolyn Winsborough
Carolyn Winsborough
JSJonathan Schurman
Jonathan Schurman
Sean ThomasSean Thomas
Sean Thomas

9 April 2015 in Biology and Fertility of Soils
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Journal Article
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GNGe N0
Ge N0
NBNathan Basiliko
Nathan Basiliko
RFRoberta Fulthorpe
Roberta Fulthorpe
TSTara E. Sackett
Tara E. Sackett
STSean C. Thomas
Sean C. Thomas

5 January 2023 in Nature Geoscience
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Journal Article
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GNGe N0
Ge N0
ASAlexander J. Smith
Alexander J. Smith
MKMatthew Kirwan
Matthew Kirwan
RRRoy L. Rich
Roy L. Rich
JMJ. Patrick Megonigal
J. Patrick Megonigal

7 October 2019 in Proceedings of the National Academy of Sciences
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GNGe N0
Ge N0
MKMatthew L. Kirwan
Matthew L. Kirwan
RRRoy L. Rich
Roy L. Rich
JMJ. Patrick Megonigal
J. Patrick Megonigal
Significance: Interactions between nutrient supply and plant demand dictate key terrestrial ecosystem feedbacks to global climate change. We investigated these responses in a marsh ecosystem and found that plants and soils respond to warming at different temperatures. Modest warming caused plant demand for nitrogen (N) to outpace the soil N supply, while more extreme warming caused the N supply to outpace plant N demand. These responses changed when elevated CO2was added to the warming treatments. Globally, terrestrial plant N demand has exceeded soil N supply in unfertilized ecosystems over the past century; our results reveal that this imbalance is driven primarily by elevated CO2and forecast that N supply will likely increase over plant demand as warming exceeds 2 °C.

11 December 2013 in Journal of Geophysical Research: Biogeosciences
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Journal Article
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GNGe N0
Ge N0
RVRuth K. Varner
Ruth K. Varner
JBJill L. Bubier
Jill L. Bubier
SFSteve Frolking
Steve Frolking
[1] Peatlands are a large natural source of atmospheric methane (CH4), and the sedge Carex rostrata plays a critical role in the production, oxidation, and transport of CH4 in these systems. This 4 year clipping experiment examined the changes in CH4 emissions from a temperate peatland after removing all aboveground C. rostrata biomass. Methane fluxes, dissolved CH4, and environmental variables were measured during spring, summer, and fall from 2008 to 2011. Clipping and removing the C. rostrata leaves and stems caused an immediate decrease in CH4 emissions that persisted over 4 years of this study. There was a strong seasonal trend in CH4 flux, with the largest treatment effects occurring during the fall months when the sedges were senescing. As expected, there was a strong positive correlation between C. rostrata green-leaf area and CH4 flux, implying that the presence of C. rostrata increases CH4 emissions from this peatland. Large interannual variability in vegetation distribution and biomass, water table depth, and temperature was observed in this study, indicating the importance of multiyear studies for understanding the interactions among these factors to determine how they could be incorporated into biogeochemical models to predict CH4 emissions under changing environmental conditions.