Pleistocene fragmentation of Amazon species’ ranges · Haffer, J. 1969. Speciation in Amazonian...
Transcript of Pleistocene fragmentation of Amazon species’ ranges · Haffer, J. 1969. Speciation in Amazonian...
Bonaccorso et al. 2006. Diversity Distrib. 12: 157-164.
Pleistocene fragmentation of AmazonPleistocene fragmentation of Amazonspeciesspecies’’ rangesranges
Photo: University of KansasPhoto: University of Kansas
HafferHaffer, J. 1969. Speciation in Amazonian forest birds., J. 1969. Speciation in Amazonian forest birds.HafferHaffer, J. 1997. Alternate models of vertebrate speciation., J. 1997. Alternate models of vertebrate speciation.
THE REFUGIA HIPOTHESIS
Speciation in the Amazon had been produced by cycles of Speciation in the Amazon had been produced by cycles of
expansion and contraction of forest environments during the expansion and contraction of forest environments during the
PleistocenePleistocene
During glacial periods, reduced temperature and humidity in the During glacial periods, reduced temperature and humidity in the
lowlands of South America left relatively small lowlands of South America left relatively small ““islandsislands”” of of
tropical rainforests surrounded by xeric habitatstropical rainforests surrounded by xeric habitats
Spatial disjunctions and isolation of populationsSpatial disjunctions and isolation of populations
HafferHaffer, J. 1969. Speciation in Amazonian forest birds., J. 1969. Speciation in Amazonian forest birds.
NAPONAPO
INAMBARIINAMBARI
IMERIIMERI
GUIANAGUIANA
BELÉMBELÉM
RONDÔNIARONDÔNIA
Haffer’sHaffer’s RefugiaRefugia
HafferHaffer & & Prance’sPrance’s RefugiaRefugia
Haffer & Prance, 2002.
Latter Pleistocene changes evidence Latter Pleistocene changes evidence for savanna expansionfor savanna expansion
Colinvaux et al. (1996, 2000, 2001)
Hoorn, C. (1997)
PalynologicalPalynological EvidenceEvidence
“Western Amazon was forested in the “Western Amazon was forested in the Pleistocene as it is now”Pleistocene as it is now”
““PalynologicalPalynological data give no indication of data give no indication of major major vegetationalvegetational changes in the drainage changes in the drainage basin” (of the Amazon)basin” (of the Amazon)(Amazon Fan)(Amazon Fan)
(“(“LagoLago PataPata”, site in north”, site in north--western western Amazon)Amazon)
Pollen evidencesPollen evidences
“All available Amazonian pollen data, without “All available Amazonian pollen data, without exception and including new data, imply biome exception and including new data, imply biome stability: no pollen data suggest increased stability: no pollen data suggest increased coverage of savanna in glacial times”coverage of savanna in glacial times”
ObjectiveObjective
To study how changes in climatic conditions during
the Last Glacial Maximum** might have affected the
patterns of distribution of Amazonian forest and
savanna species, using ecological niche modeling
****refers to the time of maximum extent of the refers to the time of maximum extent of the ice sheetsice sheets during the last during the last glaciationglaciation, , approximately 21 thousand years ago.approximately 21 thousand years ago.
Predictions:Predictions:
Testing Testing Haffer’sHaffer’s HipothesisHipothesis
Reduction and fragmentation Reduction and fragmentation in the potential distributions of forest speciesin the potential distributions of forest species
Expansion in the potential distributions of Expansion in the potential distributions of savanna speciessavanna species
Collection locality dataCollection locality data
Ecological dataEcological data
Distributional Distributional prediction in the presentprediction in the present
Projection to past scenarioProjection to past scenario
Ecological Niche Modeling: GARPEcological Niche Modeling: GARP
GARPGARPGenetic Genetic Algorithm of Algorithm of RuleRule--set set PredictionPrediction
AspectAspectSlopeSlopeTopographic IndexTopographic Index
3Paleoclimate Modeling Intercomparison Project (http://www-lsce.cea.fr/pmip/)
1US Geological Survey (http://edcdaac.usgs.gov/gtopo30/hydro/)
21,000 Years Ago21,000 Years Ago33
Topographic LayersTopographic Layers11
Hadley Centre for Climate Hadley Centre for Climate Prediction and ResearchPrediction and ResearchCanadian CenterCanadian Center
Environmental data SetEnvironmental data Set
Climatic LayersClimatic Layers TemperatureTemperaturePrecipitationPrecipitation
PresentPresent22
2Intergovernmental Panel on Climate Change (http://www.ipcc.ch)
AutomolusAutomolus infuscatusinfuscatusCampephilusCampephilus rubricollisrubricollisFormicariusFormicarius colmacolmaPhylidorPhylidor pyrrhodespyrrhodesPipraPipra coronatacoronataTangaraTangara mexicanamexicanaRauvolfiaRauvolfia paraensisparaensisR. R. polyphyllapolyphyllaR. R. spruceisprucei
Forest speciesForest species
Species distributionSpecies distribution
AtheneAthene cuniculariacuniculariaSublegatusSublegatus modestusmodestusAmmodramusAmmodramus humeralishumeralisEmberizoidesEmberizoides herbicolaherbicolaSporophilaSporophila plumbeaplumbeaRauvolfiaRauvolfia weddellianaweddellianaR. R. ligustrinaligustrinaCuratellaCuratella americanaamericana
Savanna speciesSavanna species
Species distributionSpecies distribution
Results and DiscussionResults and Discussion
LastLast Glacial Glacial MaximumMaximum
CoincidentCoincident mapmap for for forestforest speciesspecies
• Potential distribution of forest species contracted and fragmented during the last glacial maximum
• Potential distribution of savanna species expanded during the same period, but all data aren’t conclusive
• Contraction of potential distributions of forest species may have created places that retained suitable habitat during the last Glaciation
Results and DiscussionResults and Discussion
Haffer’sHaffer’s RefugiaRefugia??
Potential Distribution Potential Distribution 21000 Years Ago21000 Years Ago
Forest: All Species Forest: All Species Hadley and CanadianHadley and Canadian Modified from Modified from HafferHaffer (1969) and (1969) and BonaccorsoBonaccorso (2006).(2006).
NAPONAPO
IMERIIMERIGUIANAGUIANA
BELEMBELEM
RONDONIARONDONIAINAMBARIINAMBARI
To think about…To think about…
• Contraction of potential distributions of forest species may have created places that retained suitable habitat during the last Glaciation. But, were these changes strong enough to produce speciation in the Amazon Basin?
• Are the ecological niches conservatism over evolutionary time periods?