Eric Olson, Brandeis University
Biodiversity contributes significantly to our resilience and quality of life. Eric Olson addresses the presence of countless non-native species of plants and animals in our cities, how we can take steps to re-establish healthy ecological species relationships one yard at a time, and how our local climate can benefit.
Presented at the Urban and Suburban Carbon Farming to Reverse Global Warming conference at Harvard University on May 3, 2015, organized by Biodiversity for a Livable Climate.
www.bio4climate.org
2. Urbanization factoids
• At present, about 3–5% of global land area has been
converted to urban and developed land use (1)
• Urban areas in the United States increased by about
130% between 1960 and 2000 (1)
• Global urban areas could increase by about 1 million
square kilometers over the next 25 years (1)
• Within Massachusetts, 38% of the state is considered
urban according to US census classifications (2)
• Globally, the urban population in 2014 accounted for
54% of the total global population, up from 34% in 1960,
and continues to grow (3).
(1) Zhang et al. 2014. Multi-factor controls on terrestrial carbon dynamics in urbanized areas. Biogeosciences, 11, 7107–7124, 2014
(2) Rao et al. 2014. Atmospheric nitrogen inputs and losses along an urbanization gradient from Boston to Harvard Forest, MA.
BIOGEOCHEMISTRY 121: 229-245
(3) World Health Organization -- http://www.who.int/gho/urban_health/situation_trends/urban_population_growth_text/en/
3.
4. Carbon change over urban gradient
• Hyvonen et al. 2008. “N deposition can increase forest soil C sequestration
from 0.51 to 0.69 MgC/ha/yr”
• Jastrow et al. 2005 “reported that elevated CO2 concentration would
increase soil C sequestration by 0.19 MgC /ha/yr”
• Pouyat et al. 2002. “soil C content significantly increased in urban sites
compared with that in rural sites in New York red oak (Quercus rubra L.)
forests”
• Koerner and Klpatek. 2010. Soil C content significantly increased in urban
sites compared with that in rural sites in desert soils, Phoenix, AZ;
• Chen et al. 2013 Pine forests, urban to rural in S. China: found lower soil
carbon in urban vs rural sites. Why? Decrease in fine roots in urban areas.
And perhaps urban heat island effect speeding up decomposition.
ABIOTIC CHANGE? Role for invasives, locally?
5. “Ecosystems in urban areas usually contain a higher proportion of
exotic and naturalized plant and animal species than ecosystems in
rural areas....the effects of the presence of non-native species are
variable and complex. Changes in tree species composition can
change water and nutrient fluxed in the ecosystem through
differences in uptake and more subtly, through change in litter
quality and organic matter dynamics. Changes in soil fauna, such
as earthworms, many of which are non-native, can have important
effects on nutrient cycling and organic matter dynamics in forests
in urban areas and can buffer the effects of pollutants on soil
processes.”
Groffman, P., Pouyat, R., McDonnell, M. J., Pickett, S., and
Zipperer, W. C.: Carbon pools and trace gas fluxes in urban
forest soils, in: Advances in soil science: soil management and
greenhouse effect, edited by: Lai, R., Kimble, J., Levine, E., and
Stewart, B. A., CRC press, Boca Raton, 147, 1995.
6. Tamura M, Tharayil N. 2014. Plant litter
chemistry and microbial priming regulate
the accrual, composition and stability of
soil carbon in invaded ecosystems. New
Phytologist 203: 110–124.
Reviewed in thoughtful essay by Mathew E. Dornbush. 2014.
The myriad surprises of unwanted guests: invasive plants and
dynamic soil carbon pools. New Phytologist 203: 1–3
Tamura and Tharayil consider soil effects of two infamous
species : Kudzu and Japanese Knotweed
7. Trees and a structure swallowed by kudzu
Hall County, Georgia
9. “The discovery of Japanese knotweed on a person’s property can come as a
blow that completely undermines plans for the future.”
NEWSWEEK 2014. Japanese Knotweed: The Invasive Plant That Eats the
Value of Your Home
10.
11. Potential invader effects on carbon
• Increased fresh plant residues may increase
soil organic matter (SOM).
– Large amounts of low quality (low nutrient) litter
inhibits decomposer activity
– humifaction may increase. Increased supply of
litter may favor microbial activity that generates
hard-to-degrade (recalcitrant) forms of SOM
12. Potential invader effects on carbon
• Increased fresh plant residues may decrease
soil organic matter (SOM).
– “soil priming” may occur, whereby limits on
decomposer activity due to either lack of energy
(sugars) or nutrients (nitrogen) are lifted
– If invader provides high quality litter (as in case of
a nitrogen-fixing legume) may see enhanced
decomposer attack on existing SOM
13. Tamura M, Tharayil N. 2014. Plant litter chemistry and
microbial priming regulate the accrual, composition and
stability of soil carbon in invaded ecosystems. New Phytologist
203: 110–124.
RESULTS
JAPANESE KNOTWEED: “Compared with an adjacent
noninvaded old-field, P. cuspidatum-invaded soils exhibited a
26% increase in C, partially through selective preservation of
plant polymers.”
KUDZU: “Despite receiving a 22% higher litter input, P. lobata-
invaded Pinus stands exhibited a 28% decrease in soil C and a
twofold decrease in plant biomarkers, indicating microbial
priming of native soil C.”
14. Norway Maple, Ailanthus effects
Invasive trees Norway Maple (Acer platanoides)
and Tree of Heaven (Ailanthus altissima)
increase net nitrogen mineralization, net
nitrification, and soil nitrogen availability
compared to native tree species, including the
congener Sugar Maple (Acer saccharum)
(Gomez-Aparicio et al. 2008 Ecological Monographs).
Questions - How do non-legumes increase nitrogen activity?
Might these N effects “prime” soils, decreasing SOM?
15. Hypotheses
Compared to native species, successful invaders
may have thinner chlorophyll-enriched leaves
that are also lower in structural carbon
(characteristics that promote rapid growth).
Such characteristics would allow more rapid leaf
decomposition, “creating litter that contains a
higher concentration of nitrogen (higher litter
quality)”. (Rout and Callaway 2009)
16. Paradox of invasives
• But many invasives do not have these soil effects in
their native land.
• Could leaf traits have evolved in the new land?
Why might leaves become thinner in new
environment, with reduced allocation to cell walls?
Absence of specialized herbivores, reduced defense.
Reallocate nitrogen, carbon, to photosynthesis + seed
production.
A potential mechanism by which some invaders may
evolve leaves with traits that enhance nitrogen cycling
in the soil of invaded ecosystems.
17. Earthworms!
Worms come in different eco-types
• Anecic species feed on leaf litter (nightcrawler)
and create vertical burrows
• Epigeic species feed on leaf litter but live in
soil-litter interface, do not make burrows
• Endogeic species feed on soil (most common)
there are others…
18. ECOLOGY 94: 2827 2013
Opening Statement: “Exotic earthworm introductions
can alter above- and belowground properties of
temperate forests, but the net impacts on forest soil
carbon (C) dynamics are poorly understood. “
Note date. We have work to do!
Its complicated…Anecic, Epigeic, Endogeic
“What do you read, my lord?” “Worms, worms, worms”
19. ECOLOGY 94: 2827 2013
Mesocosm trials with three worm species
--- Lumbricus terrestris [anecic]
--- Aporrectodea trapezoides [endogeic]
--- Eisenia fetida [epigeic]
20. ECOLOGY 94: 2827 2013
RESULTS
1) Soil CO2 loss was 30% greater from the Endogeic x Epigeic
treatment than from controls (no earthworms) over the first 45
days
2) CO2 losses from monospecific treatments did not differ from
controls
3) Nightcrawlers pull leaf litter deeper into soil profile but….
4) Final soil C storage was slightly lower in earthworm combined
treatments. Increased C inputs deeper into soil were more than
offset by carbon losses across earthworm treatments.
21. Effects of exotic earthworms…
Depend on:
• Soil type
• Forest type
• Earthworm species
• Stage of worm invasion
23. URBANIZATION and Carbon Dynamics
1. Land use change. Rural land converted to
impervious surfaces, managed urban lawn,
urban forest
2. Land management change. Lawn (irrigation and
fertilization); urban forest management
(protection from logging and fire)
3. Local abiotic change: Urban heat island, local
CO2, O3, N all up, reduced solar radiation due to
air pollution and interactions
4. Global abiotic change: climate, elevated CO2
ABIOTIC CHANGE? Role for invasives, locally?
24. Source: Prof. Doug Tallamy, Chair, Dept. of Entomology and Wildlife Ecology, Univ. Deleware
Dramatically more
caterpillar biomass is
found on native vs
introduced plants.
Invasive plant impacts on carbon are complicated. But
invasives deserve to die for more clear cut reasons.