the andes biodiversity and ecosystems research group (aberg)
DESCRIPTION
Variation of forest ecosystems with elevation: insights from a 3500 m elevation gradient in the Andes. The Andes Biodiversity and Ecosystems Research Group (ABERG) Y. Malhi, M. Silman, P. Meir, K . Feeley , N. Salinas, S. Saatchi, M. Bird - PowerPoint PPT PresentationTRANSCRIPT
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Variation of forest ecosystems with elevation: insights from a 3500 m elevation gradient in the
Andes
The Andes Biodiversity and Ecosystems Research Group (ABERG)
Y. Malhi, M. Silman, P. Meir, K. Feeley, N. Salinas, S. Saatchi, M. BirdL. Aragao, C. Girardin, J. Fisher, T. Marthews, D. Metcalfe, J. Espejo, W. Farfan, K. Garcia, A. Nottingham, J. Whittaker, M. Zimmerman, K. Feeley, J. Rapp. J.
Lloyd, R. Guerreri, O. Atkin and many more
University of Oxford UK,Wake Forest University USA, University of Edinburgh UK,Univesidad San Antonio Abad ,Cuzco, Peru Pontoficia Universidad de Lima, PeruJet Propulsion Laboratory, NASA
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Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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Kosñipata Valley and adjoining Amazon lowlandsAndes Biodiversity and Ecosystem Research Group:
www.aberg.org
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3450m 3250m 3000m
2750m
2500m
2000m 2250m1750m
1500m
1250m
1000m
200m
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8.5oC 9.2oC10.5oC
11.9oC
13.3oC
15.3oC 14.8oC16.7oC
19oC
21oC
22.1oC
26.4oC
Malhi, Y. et al (2010) Elevation gradients in the tropics: laboratories for ecosystem ecology and global change research, Global Change Biology, 16, 12, 3171-3175
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Malhi, Y. et al (2010) Elevation gradients in the tropics: laboratories for ecosystem ecology and global change research, Global Change Biology, 16, 12, 3171-3175
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Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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0
1000
2000
3000
4000
5000
6000
7000
8000
0 1000 2000 3000 4000
Elevation (m)
Prec
ipita
tion
(mm
yr-1
)
0
5
10
15
20
25
30
Mea
n An
nual
Tem
pera
ture
(deg
C)
Precipitation (mm yr-1)Mean Annual Temperature(deg C)
>60 ha1 ha plotsTrees 10cm dbh
Temperature and rainfall gradients
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Tree Species Diversity
Lowland levels of diversity maintained to ~1700 m **
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Most species have narrow elevation ranges
Tree species ranking
Elev
ation
(m)
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Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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Measuring Tropical Forest Carbon Allocation and Cycling: A RAINFOR-GEM Field Manual for Intensive Census Plots (v2.2). Manual, Global Ecosystems Monitoring network,
gem.tropicalforests.ox.ac.uk
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GPP= 36.15±3.97 The carbon cycle of a forest at Tambopata. Peru
R leaf =8.86±2.78
R stem = 5.85±2.50
NPPTotal = 15.14±0.83
NPPAG = 9.96±0.41
NPPBG = 5.18±0.72
D fine litterfall
5.61±0.32
D CWD 3.59±0.26
R rhizosphere
5.07±0.86
R soil =12.98±0.82
D root
5.18±0.72
R soilhet = 7.14±0.49
NPP coarse roots = 0.51±0.05 NPP fine roots = 4.67±0.72
NPP ACW= 2.64±0.24
NPP litterfall = 5.61±0.32
NPP branch turnover = 0.95±0.10
NPP herbivory = 0.76±0.05
R cwd
R coarseroot
1.23±0.62
Malhi et al, Plant Ecology and Diversity, 2014
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GPP and NPP decline with elevationbut the transition is abrupt at around 16-1700 m asl
(dry season cloud base)
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Canopy photosynthetic capacity and leaf area index donot show a strong decline or abrupt transition with
elevationMax photosynthesis
under high light Leaf Area Index
Once cloud immersion is factored out, autotrophic processes may have little dependenceon mean temperature
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Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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8.5oC 9.2oC10.5oC
11.9oC
13.3oC
15.3oC 14.8oC16.7oC
Exploring heterotrophic processes
19oC
21oC
22.1oC
26.4oC
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Translocation of root-free soilZimmermann et al. (2010)
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Large-scale leaf and wood translocation experiment
Salinas et al. (2011) New Phytologist
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10 12 14 16 18 20 22 24 260
0.5
1
1.5
2
2.5
Annual mean soil temp. (°C)
k (x
10-
3 d-
1)
Leaf litter4725 litter bagsQ10 = 3.06±0.28(r2 = 0.97, p = 0.002)
Salinas et al.,New Phytologist, 2011
Fine wood litter1575 litter bagsQ10 = 4.0±0.56(r2 = 0.95, p = 0.004)
Salinas et al.In review.
Translocation experiments along the elevation gradient
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The sensitivity of heterotrophic decomposition is so high becausesoil microbial and macrofaunal communities completely change atwarmer temperatures
Microbial biomass increases with elevation
Increased dominance of fungi relative to bacteria at high elevation
Termites are only abundant in the lowlands
Whittaker et al. (2014) Journal of Ecology
Palin et al. (2011) Biotropica
Palin et al. (2001) Biotropica
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Implications under warming
Autotrophic processes may be very insensitive to temperature (within the range observed) because of acclimation and community turnover
Heterotrophic processes may be very sensitive to temperature because of community turnover
Hence warming would be expected to increase loss of carbon from soil more than it increases gain of carbon in tree biomass
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Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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Niches from collection data
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The mean plant community in most plots has been increasing over last 10 years by 2.0m yr-1 (+0.5 – +3.5m yr-1).
PLOT
MIG
RAT
ION
RAT
E (m
yr-
1)
Feeley et al. 2011 JBioGeo
-2
0
2
4
6
8
10
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+2.0m yr-1 (+0.5 – +3.5m yr-1). +2.0m yr-1 (+0.6 – +3.6m yr-1)
Feeley, et al. 2013, Global Change Biology
-2
0
2
4
6
8
10
-2
0
2
4
6
8
10
MIG
RAT
ION
RAT
E (m
yr-1
)Perú: Costa Rica:
Required migration rate for climate equilibrium
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Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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So tree species are shifting upslope.Is the forest biome also shifting?
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1963
2005
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1963
2005
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1963
2005
1963 US Air Force Recon aerial photography
IKONOSsatellite imagery
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Results: Andean timberline migration
• Across study area, ~80% of timberline did not change
• Upslope migration more likely in protected areas
• Upslope migration rates decreased with increasing elevation
• Overall migration rates far slower than required to maintain equilibrium with climate change
StatusAnnualized migration rate (m y-1)
Years to 2100 climate equilibrium (+5⁰C)
Timberline Timberline
Protected 0.24 3,750Unprotected 0.05 18,000
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The Grass Ceiling?
Ecotone migration rates are 12 to 110 times slower than the observed species migration rates in our valley
Protected areas help, but management may be needed interventions are needed to assist migration
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Large changes in composition with elevation
0 200 400 600 800 1000 1200 1400 1600 1800 20000
100
200
300
400
500
600
188.37962188.99268168.76875
225.52113
167.84694
453.13455
92.96796
0
209.59856183.77533
551.02478
413.05328
188.90228188.59557
191.03906194.22687184.69325
192.62175209.4856207.71837
189.28239
DCA Axis 1
DCA
Axis
2
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Composition and Elevation(1 ha plots)
DCA
Axis
1
Elevation (m)
0 500 1000 1500 2000 2500 3000 3500 4000-800
-600
-400
-200
0
200
400
600
800
1000
1200
1400