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Biophysical interactions of
bacteria with the soil environment.
The microbial community ecology
of the processes important to ecosystem Nand C cycling.
Mechanisms of plant-microbial interaction (outside of the
relatively well-defined symbioses).
Biophysical ecology of
microbial degradation of pollutants.
Microbial processing of plant
carbon to yield humic substances.
Plant-microbial C and N interactions in the rhizosphere.
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Family Photos:
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Blodgett
2006
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Puerto
Rico 2006
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People
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Telephone
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email
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Steve Blazewicz
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510-642-6847
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sjb@nature.berkeley.edu
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Damon Bradbury
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510-643-2402
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bradbury@nature.berkeley.edu
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Rebecca Daly
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510-642-6847
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rdaly@berkeley.edu
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Laura Dane
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510-642-2402
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ldane@nature.berkeley.edu
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Eric Dubinsky
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510-642-6847
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dubinsky@nature.berkeley.edu
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Dara Goodheart
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510-642-6847
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goodheartd@berkeley.edu
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Mary
Firestone
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510-642-3677
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mkfstone@nature.berkeley.edu
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Don
Herman
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510-642-6847
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skyhawk@nature.berkeley.edu
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Marissa Lafler
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510-643-2402
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mlafler@gmail.com
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Erin Nuccio
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510-642-6847
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enuccio@berkeley.edu
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Sarah Placella
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510-643-2402
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placella@nature.berkeley.edu
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The research interests of our soil
microbial ecology group include:
Biophysical
interactions of bacteria with the soil environment. We
want to understand how the physical characteristics of the solid
matrix determine growth and activity of soil microbes and how
indigenous microbes alter the characteristics of their
microhabitats in soil. In the past several years we have
focused on soil water relations, biofilms, and physical transport
processes controlling the supply of substrates and nutrients to
microbes.
The
microbial community ecology of the processes important to
ecosystem N and C cycling. We want to know whether
the structure of soil microbial communities control N or C
transformations such as nitrification, denitrification,
mineralization of organic compounds, and production / consumption
of atmoshperically reactive trace gases. How does microbial
community structure vary among soils and how do differences in
microbial community structure translate into differences in soil
processes?
Mechanisms of
plant-microbial interaction (outside of the relatively
well-defined symbioses). The interactions of plant
roots with soil microorganisms are spatially and temporally
complex; however, it is becoming increasingly apparent that these
interactions are fundamental to soil carbon dynamics and the
availability of inorganic and organic N to plants.
Current
research projects conducted by our group include:
Biophysical
ecology of microbial degradation of pollutants. We
are currently investigating the mechanisms through which soil
desiccation controls bacterial utilization of organic carbon
compounds. The water characteristics of soil control the
availability of gas-phase constituents to bacteria as well as
directly impacting the physiology of the organisms. We are
looking at the diffusional availability of a variety of organic
compounds to bacteria encased in exopolysaccharide habitats. The
physical effects on substrate availability and the effects on
cellular physiology combine to produce a range of water potential
in soil optimized for bacterial degradation of pollutant
compounds. this type of information may be of value in
managing soil systems to promote biodegradation of pollutant
compounds.
Microbial processing
of plant carbon to yield humic substances. The
metabolic characteristics of the microbial community and the
cellular composition (wall components, extracellular components)
may have the potential to determine the rate and dominance of
different carbon stabilization pathways. In this research
we ask whether soil microbial communities vary in their carbon
processing characteristics. We are assessing microbial
functional and taxonomic diversity, investigating community
control over carbon partitioning, and quantifying the
contribution of microbial cell walls to stable carbon. This
work incorporates aspects of humus chemistry, soil
microbilogy and ecosystem ecology to address the role that
microorganisms and microbial diversity play in ecosystem
functioning. Ultimately, this work may have implications
for regional carbon cycling models, and for predicting response
of soil carbon pools to environmental and land-use change.
Plant-microbial C and N
interactions in the rhizosphere. We are determining
the processes and spatial and temporal patterning by which roots
alter mineralization of C and N in the rhizosphere. We are
also attempting to understand the mechanisms involved in
mineralization of the N from microbial biomass and whether the
root zone is an active area of N mineralization and hence an
important source of N for soil microbes and plant roots. these
questions about plant-microbial interactions are fundamental to C-
and N-cycling and potentially determine ecosystem response to the
changing environment.
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Emeriti
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can be reached at:
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Teri
Balser
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teribalser@yahoo.com
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Jeff Bird
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Jbird@qc.cuny.edu
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Eoin Brodie
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ELBrodie@lbl.gov
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Kristen DeAngelis
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KDeAngelis@lbl.gov
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Claire Eustace
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claire_eustace2004@yahoo.com
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Val Eviner
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EvinerV@ecostudies.org
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Charles H. Jaeger III
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jaeger@arches.uga.edu
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Christine
Hawkes
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chawkes_at_mail_dot_utexas_dot_edu
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Trish Holden
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holden@eos.crseo.ucsb.edu
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Jason Jaeger
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jaeger@arches.uga.edu
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Kristine Johnson
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kristinekjohnson@hotmail.com
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Evaly Long
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evaly.long@gmail.com
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Ryan Miya
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ryanmiya@hotmail.com
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Jennifer Pett-Ridge
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pettridge2@llnl.gov
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Egbert
Schwartz
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Egbert.schwartz@nau.edu
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Tia Shimada
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tiaakemi@gmail.com
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Pam Templer
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ptempler@bu.edu
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Andy Thompson
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awt@nature.berkeley.edu
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Mark Waldrop
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mwaldrop@usgs.gov
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Our mailing address is:
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Our shipping address is:
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ESPM - Ecosystem Sciences
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ESPM – Ecosystem Sciences
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137 Mulford Hall
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54 Mulford Hall
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University of California
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University of California
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Berkeley, CA 94720-3114
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Berkeley, CA 94720
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Last updated: January 29, 2008
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