variation of forest ecosystems with elevation: insights from a 3500 m elevation gradient in the...
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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
Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
Kosñipata Valley and adjoining Amazon lowlandsAndes Biodiversity and Ecosystem Research Group:
www.aberg.org
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
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
Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
0
1000
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7000
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0 1000 2000 3000 4000
Elevation (m)
Pre
cipit
atio
n (m
m y
r-1)
0
5
10
15
20
25
30
Mea
n A
nnual
Tem
per
ature
(deg
C)
Precipitation (mm yr-1)
Mean Annual Temperature(deg C)
>60 ha
1 ha plotsTrees 10cm dbh
Temperature and rainfall gradients
Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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
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
GPP and NPP decline with elevationbut the transition is abrupt at around 16-1700 m asl
(dry season cloud base)
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
Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
8.5oC 9.2oC10.5oC
11.9oC
13.3oC
15.3oC 14.8oC16.7oC
Exploring heterotrophic processes
19oC
21oC
22.1oC
26.4oC
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
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
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
Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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
RA
TIO
N R
AT
E (
m y
r-1)
Feeley et al. 2011 JBioGeo
-2
0
2
4
6
8
10
+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
RA
TIO
N R
AT
E (
m y
r-1)
Perú: Costa Rica:
Required migration rate for climate equilibrium
Talk structure
Study regionPlant diversity and distributionsEcosystem productivityHeterotrophic processesPlant distribution changeTree line studies
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
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
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
Axi
s 2