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The Andes Biodiversity and Ecosystems Research Group (ABERG)
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 L. 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, Peru Jet Propulsion Laboratory, NASA
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Talk structure Study region Plant diversity and distributions
Ecosystem productivity Heterotrophic processes Plant distribution change Tree line studies
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Kosñipata Valley and adjoining Amazon lowlands
Andes Biodiversity and Ecosystem Research Group:
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200m 2000m 1250m 2250m 1750m 1000m 1500m 2500m 2750m Show transect of plots 3000m 3250m 3450m
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26.4oC 15.3oC 21oC 14.8oC 16.7oC 22.1oC 19oC 13.3oC 11.9oC 10.5oC
Malhi, Y. et al (2010) Elevation gradients in the tropics: laboratories for ecosystem ecology and global change research, Global Change Biology, 16, 12,
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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, 6
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Talk structure Study region Plant diversity and distributions
Ecosystem productivity Heterotrophic processes Plant distribution change Tree line studies
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Temperature and rainfall gradients
1 ha plots Trees 10cm dbh >60 ha
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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
Elevation (m) Tree species ranking
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Talk structure Study region Plant diversity and distributions
Ecosystem productivity Heterotrophic processes Plant distribution change Tree line studies
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gem.tropicalforests.ox.ac.uk Measuring Tropical Forest Carbon Allocation and Cycling: A RAINFOR-GEM Field Manual for Intensive Census Plots (v2.2). Manual, Global Ecosystems Monitoring network,
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The carbon cycle of a forest at Tambopata. Peru
GPP= 36.15±3.97 NPPTotal = 15.14±0.83 NPPAG = 9.96±0.41 NPPBG = 5.18±0.72 NPP litterfall = 5.61±0.32 NPP herbivory = 0.76±0.05 R leaf =8.86±2.78 NPP branch turnover = 0.95±0.10 R stem = 5.85±2.50 D fine litterfall 5.61±0.32 NPP ACW= 2.64±0.24 R cwd R soil =12.98±0.82 D CWD 3.59±0.26 R coarseroot 1.23±0.62 R rhizosphere 5.07±0.86 NPP coarse roots = 0.51±0.05 NPP fine roots = 4.67±0.72 D root 5.18±0.72 R soilhet = 7.14±0.49 Malhi et al, Plant Ecology and Diversity, 2014
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GPP and NPP decline with elevation
but the transition is abrupt at around m asl (dry season cloud base)
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Canopy photosynthetic capacity and leaf area index do
not show a strong decline or abrupt transition with elevation Max photosynthesis under high light Leaf Area Index Once cloud immersion is factored out, autotrophic processes may have little dependence on mean temperature
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Talk structure Study region Plant diversity and distributions
Ecosystem productivity Heterotrophic processes Plant distribution change Tree line studies
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Exploring heterotrophic processes
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Translocation of root-free soil
Zimmermann et al. (2010)
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Large-scale leaf and wood translocation experiment
Salinas et al. (2011) New Phytologist
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Translocation experiments along the elevation gradient
Leaf litter 4725 litter bags Q10 = 3.06±0.28 (r2 = 0.97, p = 0.002) Salinas et al., New Phytologist, 2011 Fine wood litter 1575 litter bags Q10 = 4.0±0.56 (r2 = 0.95, p = 0.004) Salinas et al. In review.
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The sensitivity of heterotrophic decomposition is so high because
soil microbial and macrofaunal communities completely change at warmer temperatures Microbial biomass increases with elevation Increased dominance of fungi relative to bacteria at high elevation Termites are only abundant in the lowlands Palin et al. (2011) Biotropica Palin et al. (2001) Biotropica Whittaker et al. (2014) Journal of Ecology
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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 region Plant diversity and distributions
Ecosystem productivity Heterotrophic processes Plant distribution change Tree line studies
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Niches from collection data
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MIGRATION RATE (m yr-1) PLOT 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). Feeley et al JBioGeo 28
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Required migration rate for climate equilibrium
Perú: Costa Rica: Required migration rate for climate equilibrium MIGRATION RATE (m yr-1) +2.0m yr-1 (+0.6 – +3.6m yr-1) +2.0m yr-1 (+0.5 – +3.5m yr-1). Feeley, et al. 2013, Global Change Biology
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Talk structure Study region Plant diversity and distributions
Ecosystem productivity Heterotrophic processes Plant distribution change Tree 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 IKONOS satellite
imagery 2005
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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 Status Annualized migration rate (m y-1) Years to 2100 climate equilibrium (+5⁰C) Timberline Protected 0.24 3,750 Unprotected 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
DCA Axis 2
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Composition and Elevation (1 ha plots)
DCA Axis 1 Elevation (m)
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