Shaenandhoa García-Rangel Juan Papadakis Edgard Yerena Departamento de Estudios Ambientales, Universidad Simón Bolívar Venezuela 20 th International Conference.

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Presentation transcript:

Shaenandhoa García-Rangel Juan Papadakis Edgard Yerena Departamento de Estudios Ambientales, Universidad Simón Bolívar Venezuela 20 th International Conference on Bear Research and Management, Ottawa – Canada 2011 Climate change: A threat for the Andean bear?

Topics The Latin-American context to global warming. The Andes mountain range The Andean bear Climate change – Andean-bear project Objectives Methods Preliminary results Limitations and future directions

The Latin-American context In Latin America, climate impacts are very significant and expected to irreversibly affect key ecosystems and the services these provide. (Vergara 2007) In 2005, over 80% of coral reefs across the Caribbean basin suffered bleaching as a consequence of heat stress. Risk of coastal flooding and salinization. Increase in sea-level rise across the South Atlantic Coast. Hurricanes trends have intensified. Costs of impacts > 2 times since of 10 most active years have been recorded since Changes in precipitation and temperature patterns. Amazonian drought of 2005 and the prospect of Amazonian dieback. Critical role in precipitation patterns across South America. (GEOLAC 2010, Vergara, 2007)

The Latin-American context Human-pop. growth > mean Exploitation of natural resources Total GHG contribution: 11.78% Net forest loss > 0.5% yearly (Eclac, 2009, Geolac 2010, FAO 2005 )

The Latin-American context THE ANDES MOUNTAIN RANGE Global circulation models Rapid Glacier Retreat Troposphere warming Shift in the freezing point isotherm Temperature increases > lowlands Change the ecology of the Andes (Vergara, 2007) Cotopaxi Glacier, Ecuador 30% decrease % decrease (UNEP, Cathalac;Vergara 2007)

The Latin-American context THE ANDES MOUNTAIN RANGE Global circulation models Rapid Glacier Retreat Troposphere warming. Shift in the freezing point isotherm. Vulnerability of high-mountain ecosystems Water cycle disruptions. Disappearance of high-altitude water bodies. Increase occurrence of fires. Temperature increases > lowlands Change the ecology of the Andes (Vergara, 2007) (Palminteri et al. 2001, Vergara 2007)

The Latin-American context THE ANDES MOUNTAIN RANGE Global circulation models Rapid Glacier Retreat Vulnerability of high-mountain ecosystems Temperature increases > lowlands Change the ecology of the Andes (Vergara, 2007) (Palminteri et al. 2001, Vergara 2007) Reduction of water supplies for food production and urban areas Limitations in hydroelectric power generation Highest concentration of human population High deforestation rates

The Latin-American context VULNERABLE

Climate change – Andean-bear project THE ANDEAN BEAR VULNERABLE (Goldstein et al. 2008) Carnivore in SA moving faster towards extinction (Cardillo et al. 2004) Population trends Habitat loss 2-4% a year High levels of fragmentation (Goldstein et al. 2008)

Climate change – Andean-bear project OBJECTIVES To evaluate the impact of global warming on the Andean bear across the Northern Andes. To compare the impact of global warming and land-cover change on the Andean bear across the Northern Andes. To evaluate the role of protected areas to secure Andean-bear habitat in the future. PRELIMINARY RESULTS ANALYSIS LIMITATIONS FUTHER QUESTIONS RISEN (Rodriguez et al. 2003)

Climate change – Andean-bear project METHODS Species Distribution Models (SDMs) for different scenarios Changes in Andean-bear habitat suitability 1)Species presence data (1844 ~ 2004): 544 records. GBIF ( ) : 33 records. Yerena (1994): 108 records. Sánchez-Mercado (2008): 404 records.

Climate change – Andean-bear project METHODS 1)Species presence data (1844 ~ 2004): 544 records.

METHODS 1)Species presence data (1844 ~ 2004): 544 records. (ArcGIS 9.3) 2) Independent variables WorldClim ( Average conditions: Today Model: CCCMA, scenario B2. Year = 2050 (Flato et al. 2000) Climate change – Andean-bear project Temp. max and min. Precipitation Elevation

METHODS WorldClim ( Model: CCCMA, scenario B2. Year = 2050 (Flato et al. 2000) Climate change – Andean-bear project

METHODS 1)Species presence data (1844 ~ 2004): 544 records. 2) Independent variables WorldClim ( Average conditions: Today Model: CCCMA, scenario B2. Year = 2050 (Flato et al. 2000) DMSP-OLS Nighttime Lights Time Series V and 2009 models. GBIF ( Food resources according to Figueroa and Stucchi (2009) Climate change – Andean-bear project Temp. max and min. Precipitation Elevation Families: 5 Genera: ~10 Species: 18

METHODS 1)Species presence data (1844 ~ 2004): 544 records. 2) Independent variables 3)SDMs Climate change – Andean-bear project Maximum Entropy Method (Phillips et al. 2006) Scale: 30 arc-seconds (~1 km). Maxent Versión 3.3.3e, HPTQ. Jack-knifing procedure for variable importance. AUC measure for model evaluation. 15% testing dataset. “Maximum test sensitivity plus specificity” threshold for output. Today Climate Climate + Food resources Climate + Nightlights Climate + Food resources + Nightlights Future Climate Climate + Food resources ArcGIS 9.3

RESULTS Climate change – Andean-bear project

RESULTS Model: Climate Model: Climate + Food resources Climate change – Andean-bear project Today Future Today Future

RESULTS Food resources are important modulators of Andean-bear’s habitat suitability. Model: Climate + Food Resources Today Future Variable contribution: 42.8% Variable contribution: 36.8% Climate change – Andean-bear project

RESULTS Today 2050 Climate change – Andean-bear project

RESULTS Today 2050

DISCUSSION Climate change – Andean-bear project DISCUSSION 1.Preliminary results show that climate change do not seem to pose a major threat to Andean bears in the middle-term (2050). Land-cover change and human-population growth are known threats to the species, and so they must be incorporated in any assessment regarding climate change. 2. Models show potential Andean-bear habitat suitability. Areas are considerably overestimated but relative variations could be indicators of future scenarios. No historic barriers or restriction due to human developments are incorporated. We require information on land-cover change to be able to draw guidelines for conservation.

DISCUSSION 3. Changes in the distribution of food resources could open new spaces to the Andean bear. Species overlap remains within the Northern Andes. Andean bears are constrain to the limits of the Northern Andes by some unidentified factor (Temperature?, food resources?). Climate change – Andean-bear project

WHAT’S NEXT? 1. To increase coverage and time-span of Andean-bear present points. 2. To explore differential weighting of food resources and the inclusion of other species. 3. To incorporate land-cover change projections. 4. To evaluate prediction behavior with CSIRO and HADCM3 climatic models and other scenarios available. 5. To evaluate the role of protected areas to secure Andean-bear habitat. Climate change – Andean-bear project

Dr Chris Servheen. Dr Martyn Obbard. Dr Ada Sánchez-Mercado. Érika Pedraza. Bear Specialist Group. Laboratorio de Sensores Remotos y Análisis Geoespacial. ESRI Conservation Program. Acknowledgements Universidad Simón Bolívar

Thank you!

RESULTS Climate change – Andean-bear project