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Dr. Bertrand BoekenDry Rangeland Ecology and Management LabThe Wyler Dept. of Dryland AgricultureJacob Blaustein Institute for Desert ResearchBen-Gurion University of the NegevSede Boqer Campus 84990 Israel
Ben-Gurion University of the Negev
Plant responses to climate change in the Negev
© BBoeken 2010
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Plant responses to climate change
in the Negev
• Possible changes in climate
– CO2, Temperatures, Rainfall
• Effects on Negev plants
– Individuals plants
– Populations
– Spatial distributions
– Plant communities
– Patterns of vegetation
• Consequences for landscape structure
and land degradation (desertification)
3
Changes in climate
• Greenhouse gases
– Global increase of atmospheric
CO2 and CH4 concentrations
– Causes global warming
• Regional temperature change
– Higher averages, minima and/or maxima?
– At higher latitudes (N) higher winter minimum temperatures
observed
– Uncertain what happens in the Negev
(after last year’s frost, the average is lower anyway!)
4
Changes in rainfall in the Negev
More, same or less total rainfall per
year?
– Lower mean in the last decades:
~150mm/yr, vs. 200mm/yr (long-term)
– Possibly greater variance
– Higher frequency of drought years
with ≤ 50% long-term mean)
Probable changes in distribution of
rainfall during the rainy season
– Higher intensity of rain events
– Longer droughts between rain events
Total annual rainfall in Park Shaked
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50
100
150
200
250
300
19
92
19
94
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96
19
98
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00
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02
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06
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20
10
Rain
fall
(mm
)
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Effects on individual plants• Higher temperatures
– Increased growth during the rainy seasonBiochemical processes increase with temperature
– Earlier seed germinationIn species with low-temperature inhibition of germination
– Fewer seeds germinateIn species that require low temperature
– Earlier flowering
In species without strict day-length response
– A-synchrony with pollinatorsIf insects have different developmental temperature
response
• Higher CO2– Increased growthPhotosynthesis assimilates CO2 to produce sugars,
used for growth
– Lower water lossFewer stomates open
Temperature
Gro
wth
or
ger
min
ati
on
ra
te
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• Heavier rainfall
– Not just more growth
– But more damage
– Greater variability of soil moisture
Indirect effect: more runoff, erosion, and
local accumulation
Sources of runoff become drier,
sinks become fewer but wetter
• Longer droughts
– Shorter growing season
– Less growth
– More mortality
– Less reproduction
– Less germination
Effects of rainfall changes
Less
water in
source More water
in sink
Runoff
Infiltration
Time
So
il m
ois
ture
Current vs
Expected
Drought period
Rain intensity
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• Changes in temperature, rainfall intensity and drought
have different positive or negative effects on vital rates
1. Seed survival and germination
2. Seedling establishment and survival
3. Juvenile growth and survival
4. Growth, maturation and flowering
5. Adult survival
6. Seed production (fecundity)
7. Seed dispersal
(6 x 7 x 1). Reproductive success (fertility)
• Effects vary a lot between
– Species
– Life forms (annuals, shrubs)
– Environments (exposed or shaded patches)
• Net result is population growth and expansion, or decrease and extinction
• No single prediction of climate change effects
Effects on populations
Plant life-cycle (polycarpic perennial)
Z
S
1
2 4
7
J A
5
6
3
8
Effects on species• Annuals
– Fast-growing dominants may decrease
Need ample water
Dominant grasses: No seed dormancy,
germination of new seeds every year
– Slower-growing species may increase
Need less water
Have dormant seed bank
Will be less suppressed by dominants
– Species requiring good sites (runoff sinks, more water, shade)
May have fewer good sites, but increase there
• Shrubs
– Lower seedling establishment in open sites
Due to increased runoff – greater risk of washing away
– Fewer survivors may grow better
Due to increased soil moisture in sinks
Stipa capensis
Noaea mucronata and Atractylis serratuloides
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Community consequences• Changes in competitive relations (among annuals and among shrubs)
– Dominants may become sparser
– Some minor species may become dominant
Currently suppressed by low temperature or by dominants
Or by low soil moisture in good sites
• Invasion of new species
– Species from harsher (dry, hot)
environments (further south or east)
Most likely dominants
Currently absent due to local conditions and exclusion
Unknown how they perform –
growth, litter, soil, patch formation (shrubs)
• Herbivores and their predators,
and pathogens of plants and animals
– May locally decrease of increase
– New ones may invade
Hamada scoparia
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Spatial distributions
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• Geographical distributions will change
– By local extinction of existing populations
– By colonization of unoccupied areas (invasion)
• Ranges can move along the aridity gradient
– Species can colonize locations where they were
absent
due to lower temperatures or competitive exclusion
– Or in wetter sink patches
• Distributions can become very restricted
– If extinction >> colonization
as colonization is inhibited by the physical impacts of
climate change (strong runoff, erosion)
11
Landscape structure• Shrubs form sink patches
– Landscape modulation
• By patch and pattern formation
– Transition of open (crusted) matrix
to dense shrub patch with soil mound
• Captures runoff water, soil and OM
• Seed capture, retention
• High productivity • Shrub patches are hot-spots for species richness
– Dense annual vegetation
• Under or around shrub canopy
– High annual species richness
– Shelter and food for herbivores and
granivores
Shrub seedling
Shrub patch
12
Landscape structure• Spatial heterogeneity is essential for retaining water
– Sinks for resources (runoff, soil, nutrients and OM)
– With lower shrub density, more erosion and resource
loss down slopes and out of the watershed
• Depends on survival and establishment of current
shrub species
– Better growth and survival, or
– Slower patch formation by shrubs as erosion
increases, and
• Failure of shrub seedling establishment
– positive feedback: the fewer shrubs, the fewer new
shrubs
• Not easily replaced by new shrub species
– Establishment may fail
– They may be worse patch formers
13
Landscape changes• Shrub cover may decrease
– In shrub species that are sensitive to drought
– And if their patches are easily eroded
As in Atractylis and Noaea mucronata (at 150-250
mm/yr)
– Where annuals stabilize the shrub mound
• Or shrub cover may increase
– In species that capture runoff water efficiently
As in Sarcopoterium spinosum (at 250-400 mm/yr)
– But with negative effects on annuals
– If the annuals grow around shrubs
– And shrub patches merge
14
Land degradation
• Current cause for degradation =
Livestock grazing
– Herbivory
• Annual plant removal
• Exposure of mounds
– Trampling of shrub mounds
• Dissipation of mounds
• Erosion and loss of material
Runoff
Rain• Reduction of patch density and size
– Fewer sinks for runoff
– Fewer hot-spots for herbaceous vegetation
– More runoff
• Resource loss
• High energy
• Erosion
– Positive feedback
• Low shrub establishment
• Restoration necessary
15
Summary
• Higher CO2 and temperature
– Positive and negative effects on all biota
• Possibly increased rain intensity and drought
– Greater annual fluctuations
– Greater spatial variation in soil moisture
– More runoff: resource loss and erosion
– Fewer but wetter sink patches
• Landscape changes
– Lower heterogeneity
– Increase or reduction of shrub patch (sinks)
– Increased runoff, resource loss, erosion
• Land degradation
– Especially in combination with livestock grazing
– Restoration / rehabilitation / reclamation
• Many possible effects on plants– On recruitment, growth, survival and
reproduction
• Variable population responses– Local or regional species extinctions
• Shifts in spatial distributions– Reduction/expansion,
colonization/invasion
• Community changes – Dominance, species diversity