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Transcript
The hidden half of ecosystem responses to climate change: what
happens belowground?
PI: Christine V. Hawkes, University of Texas at Austin
Our goal is to understand how soils and soil microorganisms will respond to climate
change and how these responses will feedback to ecosystem carbon cycling.
Saprophytic fungi responsible for decomposition and mycorrhizal fungi that transfer
carbon from above- to belowground are likely to be the dominant biotic drivers behind
the amount of soil carbon released to the atmosphere. Both types of fungi can respond
to climate independently of plants and thus represent a large unknown in ecosystem
responses to altered precipitation and temperature. A broad evaluation of climate
change effects on soil fungi is integral to predicting future soil carbon storage and loss
and may facilitate mitigation strategies.
We will ask three key questions:
(1) How do roots and fungi respond to predicted changes in precipitation?
(2) How do belowground responses to climate change affect soil carbon balance?
(3) Are mycorrhizal fungi adapted to local climatic conditions such that fungal
communities could be manipulated to facilitate carbon storage under projected
climate scenarios?
To do this, we will use three approaches:
(1) Determine functional responses of plant roots and soil fungi to altered
precipitation with field manipulation of precipitation at the community level;
(2) Determine response mechanisms and identify target fungi with greenhouse
manipulation of precipitation at the species level;
(3) Use experimental data to parameterize predictive models of ecosystem response
to climate change.
The field experiment will be set up at the UT Ladybird Johnson Wildflower Center in
Austin, TX. We will use six different precipitation manipulations ranging from historical
mean annual precipitation for the region to predicted severe drought (2 SD away from
the historical mean). This research will provide the information needed to quantitatively
assess how belowground responses, particularly soil fungal responses, will alter soil
carbon cycling under projected future climate scenarios. Ultimately, we hope this work
will lead to the development of simple strategies for manipulating fungi to increase
carbon sequestration in soil, such as ‘high sequestration’ fungal amendments.
Right: Experimental shelters in late Aug 2009,
with grasses transplanted one week prior.
Below: Ground-eye view of plots with grasses in
early Sept 2009, two weeks after planting.
Irrigation poles are visible at the corners of each
plot.
Below right: View of one plot with four subplots
representing two plant communities (tallgrass,
shortgrass) and two soil treatments (clay, clay
plus sand).