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Climate Change, Disease, and Amphibian Declines. by Jason R. Rohr. University of South Florida Department of Biology, SCA 110 4202 E. Fowler Ave. Tampa, FL 33620 jasonrohr@gmail.com. Climate Change, Amphibian Declines, and Bd.
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Climate Change, Disease, and Amphibian Declines by Jason R. Rohr University of South Florida Department of Biology, SCA 110 4202 E. Fowler Ave. Tampa, FL 33620 jasonrohr@gmail.com
Climate Change, Amphibian Declines, and Bd Also evidence that Bd-related declines are linked to climate change (Pounds et al. 2006, Bosch et al. 2006)
Outline for Talk Does global climate change affect worldwide amphibian declines associated with chytrid fungal infections?
71 of 113 spp. presumed extinct, many of which were ostensibly caused by chytridiomycosis from La Marca et al. 2005. Biotropica
Climate, Bd, and Conservation Planning • If we understand the climatic factors that accelerate Bd spread, increase host susceptibility, or elevate pathogen virulence, we can identify present and future geographic locations that might have amphibians at risk of Bd-related declines • Hence, we can better target areas that warrant monitoring and remediation
Tenuous Links Between Climate and Amphibian Declines • Most of the evidence supporting climate change as a factor in Bd-related amphibian extinctions comes from a positive, but temporally confounded, multi-decade correlation between air temperature and extinctions in the toad genus Atelopus Rohr et al. 2008 PNAS
Need to Conduct Detrended Analyses? • If there is a true relationship between climate and Bd-related extinctions, fluctuations around temporal trends in temperature and extinctions should also positively correlate • There would many fewer non-causal explanations for this correlation than the multidecadal relationship between declines and temperature
Objectives Use the Atelopus database to simult-aneously test various climate-related hypotheses for amphibian declines, controlling for multidecadal correlations and the intrinsic spatiotemporal spread of Bd
ENSO: El Niño-Southern Oscillation • Commonly referred to as simply El Niño is a global coupled ocean-atmosphere phenomenon • The Pacific ocean signatures, El Niño (warm and wet) and La Niña (cool and dry) are important temperature fluctuations in surface waters of the tropical Eastern Pacific Ocean • The atmospheric signature, the Southern Oscillation (SO) reflects the monthly or seasonal fluctuations in the air pressure • Effects of El Niño in South America are direct and stronger than in North America
Proximal Hypotheses for Enigmatic/Bd-related Declines • Spatiotemporal spread hypothesis:declines are caused by the introduction and spread of Bd, independent of climate (Bell et al. 2004, Lips et al. 2006) • Climate-based hypotheses: • Chytrid-thermal-optimum hypothesis:Increased cloud cover, due to warmer oceanic temperatures, leads to temperature convergence on the optimum temperature for growth of Bd (Pounds et al. 2006, Bosch et al. 2006) • Mean-climate hypothesis: changes in mean temp. and/or moisture conditions affect the distributions of amphibians (Whitfield et al. 2007, Buckley & Jetz 2007) • Climate-variability hypothesis: temporal variability in temp. cause suboptimal host immunity facilitating declines (Raffel, Rohr, et al. 2006)
Climate-Variability Hypothesis Ectotherms: *seasonal changes in body temperature*
Climate Variability Hypothesis • Hypothesis: unpredictable temperature shifts, which are increasing with GCC, benefit pathogens more than hosts. • faster metabolisms of parasites should allow them to acclimate more quickly to unpredictable temperature shifts, especially for ectothermic hosts • parasites have fewer cells and processes to adjust and generally withstand greater temperature extremes than hosts (Portner 2002) • owing to their shorter generation times, parasites should evolve more quickly than hosts to changes in climate
Climate Variability Hypothesis • The categorically faster metabolisms, smaller size, and greater reproductive capabilities of parasites than hosts provides a general hypothesis for how global climate change will affect disease risk– unpredictable climate variability should increase disease.
Is there Spatiotemporal Spread of Atelopus Extinctions? Rohr et al. 2008 PNAS
Atelopus Extinctions Through Time Best fit curve Rohr et al. 2008 PNAS
How we controlled for the likely epidemic spread of the pathogen
El Niño Years? La Niña Years?
Ultimate Hypothesis: ENSO Rohr and Raffel 2010 PNAS
Must Control for Intrinsic Dynamics to Detect Extrinsic Factors! • No significant ENSO signature if we don’t control for probable epidemic spread • Hence, the availability of susceptible hosts appears the primary factor influencing epidemic spread followed secondarily by climate
But What is the Proximate Explanation? What is it about El Nino years that is associated with amphibian extinctions?
Proximal Hypotheses for Enigmatic/Bd-related Declines • Spatiotemporal spread hypothesis: declines are caused by the introduction and spread of Bd, independent of climate (Bell et al. 2004, Lips et al. 2006) • Climate-based hypotheses: • Chytrid-thermal-optimum hypothesis:Increased cloud cover, due to warmer oceanic temperatures, leads to temperature convergence on the optimum temperature for growth of Bd (Pounds et al. 2006, Bosch et al. 2006) • Mean-climate hypothesis: changes in mean temp. and/or moisture conditions affect the distributions of amphibians (Whitfield et al. 2007, Buckley & Jetz 2007) • Climate-variability hypothesis: temporal variability in temp. cause suboptimal host immunity facilitating declines (Raffel, Rohr, et al. 2006)
Regional Predictorstested w/ and w/o a one year lag Mean absolute value of monthly differences (AVMD) in temp. Cloud cover x temp. (Pounds et al. 2006) Cloud cover (Pounds et al. 2006) Temperature-dependent Bd growth (Pounds et al. 2006) Precip. x temp. (Whitfield et al. 2007) Diurnal temp. range (DTR) Frost freq. Precip. Temp. Temp. max. Temp. min. Vapor press. Wet day freq.
Results of Best Subset Model Selection results are similar using AIC
Can Monthly Temperature Variability Explain Atelopus Extinctions? Rohr and Raffel 2010 PNAS
Amphibian extinctions have often occurred in warmer years, at higher elevations, and during cooler seasons.Are monthly and daily variability in temperature also greater at these times and locations?
Do Warmer Years Have Greater Variability in Temperature? Rohr and Raffel 2010 PNAS
Do Cooler Months Have Greater Variability in Temp.? Rohr and Raffel 2010 PNAS
DTR 2 R = 0.633 P <0.001 P <0.001 0.675 0.694 Lag amphibian extinctions P = 0.044 El Niño 3.4 - 0.4 66 2 R = 0.674 P =0.002 P <0.001 0.67 3 0.868 AVMD anomalies 2 R = 0.567 Results of Path Analysis Rohr and Raffel 2010 PNAS
Experimental Test • Acclimated Cuban tree frogs to 15 or 25⁰ C for four weeks • Challenged with Bd at start of week five • Quantified survival and pathogen loads 15⁰C 15⁰C 25⁰C 25⁰C
Does Temperature Variability Increase Bd Loads on Frogs? Bd load: Bd-induced mortality: Temperature shifts increased Bd loads and Bd-induced mortality Raffel et al. in press Nature Climate Change
Summary • Availability of susceptible hosts appears to be the primary factor influencing the spread of Bd • There is a strong ENSO signature to extinctions after controlling for epidemic spread • Both field patterns of extinctions and manipulative experiments support the climate-variability hypothesis for amphibian extinctions
ConclusionsTemperature, temperature variability, and Central Pacific El Niño events are increasing in tropical and subtropical regions because of climate change; thus, global climate change might be contributing to enigmatic amphibian declines, by increasing disease risk
ConclusionsElevated temperature variability might represent a common, but under-appreciated, link between climate change and both disease and biodiversity losses and might offer a general mechanism for why disease would increase with GCC.
Preparación de modelos • Molde de Látex a partir de un espécimen de colección. • Obtención de modelos de agar.
Día SECO - SOL (2 modelos) SECO - SOMBRA (2 modelos) Noche HÚMEDO - SOMBRA (2 modelos) HÚMEDO -SOL (2 modelos) Experimento de campo • 4 condiciones experimentales (factorial).
Experimento de campo • Modelos conectados a data loggers. • Reemplazo de modelos cada 3-4 hr. SECO SOL SECO SOMBRA HÚMEDO SOL HÚMEDO SOMBRA
T operativa y Pérdida de agua sombra húmedo sol seco Del Puerto Canyon; 12 march 2012; nublado; Annaxyrus boreas model
T ambiental y Pérdida de agua sol seco Tª sol sombra seco sol húmedo sombra húmedo Tª sombra Los Baños Cistern; 5 march 2012; soleado; metamórficos