Neogene origins and implied warmth tolerance of Amazon tree species
dc.contributor.author | Dick, Christopher W. | en_US |
dc.contributor.author | Lewis, Simon L. | en_US |
dc.contributor.author | Maslin, Mark | en_US |
dc.contributor.author | Bermingham, Eldredge | en_US |
dc.date.accessioned | 2013-02-12T19:01:00Z | |
dc.date.available | 2013-02-12T19:01:00Z | |
dc.date.issued | 2012-01 | en_US |
dc.identifier.citation | Dick, Christopher W.; Lewis, Simon L.; Maslin, Mark; Bermingham, Eldredge (2012). "Neogene origins and implied warmth tolerance of Amazon tree species." Ecology and Evolution 3(1): 162-169. <http://hdl.handle.net/2027.42/96354> | en_US |
dc.identifier.issn | 2045-7758 | en_US |
dc.identifier.issn | 2045-7758 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/96354 | |
dc.description.abstract | Tropical rain forest has been a persistent feature in South America for at least 55 million years. The future of the contemporary Amazon forest is uncertain, however, as the region is entering conditions with no past analogue, combining rapidly increasing air temperatures, high atmospheric carbon dioxide concentrations, possible extreme droughts, and extensive removal and modification by humans. Given the long‐term Cenozoic cooling trend, it is unknown whether Amazon forests can tolerate air temperature increases, with suggestions that lowland forests lack warm‐adapted taxa, leading to inevitable species losses. In response to this uncertainty, we posit a simple hypothesis: the older the age of a species prior to the Pleistocene, the warmer the climate it has previously survived, with Pliocene (2.6–5 Ma) and late‐Miocene (8–10 Ma) air temperature across Amazonia being similar to 2100 temperature projections under low and high carbon emission scenarios, respectively. Using comparative phylogeographic analyses, we show that 9 of 12 widespread Amazon tree species have Pliocene or earlier lineages (>2.6 Ma), with seven dating from the Miocene (>5.6 Ma) and three >8 Ma. The remarkably old age of these species suggest that Amazon forests passed through warmth similar to 2100 levels and that, in the absence of other major environmental changes, near‐term high temperature‐induced mass species extinction is unlikely. Our study provides evidence that widespread Amazon tree species originated in Neogene time frames, in which atmospheric warmth was similar to conditions expected in 2100 under IPCC projections. This implies a broader thermal tolerance of lowland tropical trees than is assumed by models that predict large‐scale Amazon forest dieback. | en_US |
dc.publisher | Univ. of Chicago Press | en_US |
dc.publisher | Wiley Periodicals, Inc. | en_US |
dc.subject.other | Molecular Clock | en_US |
dc.subject.other | Thermal Tolerance | en_US |
dc.subject.other | Tropical Trees | en_US |
dc.subject.other | Global Change | en_US |
dc.subject.other | Ecological Niche Models | en_US |
dc.subject.other | Comparative Phylogeography | en_US |
dc.subject.other | Amazon Forests | en_US |
dc.title | Neogene origins and implied warmth tolerance of Amazon tree species | en_US |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | en_US |
dc.subject.hlbsecondlevel | Ecology and Evolutionary Biology | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.identifier.pmid | 23404439 | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/96354/1/ece3441.pdf | |
dc.identifier.doi | 10.1002/ece3.441 | en_US |
dc.identifier.source | Ecology and Evolution | en_US |
dc.identifier.citedreference | Phillips, O., S. L. Lewis, T. R. Baker, K. J. Chao, and N. Higuchi. 2008. The changing Amazon forest. Philos. Trans. R. Soc. B‐Biol. Sci. 363: 1819 – 1827. | en_US |
dc.identifier.citedreference | IPCC. 2007. Summary for policy makers. Pp. 1 – 18 in S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller, eds. Climate change 2007: the physical science basis, contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge Univ. Press, Cambridge, UK. | en_US |
dc.identifier.citedreference | Jaramillo, C., D. Ochoa, L. Contreras, M. Pagani, H. Carvajal‐Ortiz, L. M. Pratt, et al. 2010. Effects of rapid global warming at the Paleocene‐Eocene boundary on neotropical vegetation. Science 330: 957 – 961. | en_US |
dc.identifier.citedreference | Jones, C., J. Lowe, S. Liddicoat, and R. Betts. 2009. Committed terrestrial ecosystem changes due to climate change. Nat. Geosci. 2: 484 – 487. | en_US |
dc.identifier.citedreference | Kay, K. M., J. B. Whitall, and S. A. Hodges. 2006. A survey of nuclear ribosomal internal transcribed spacer substitution rates across angiosperms: an approximate molecular clock with life history effects. BMC Evol. Biol. 6: 9 pp. | en_US |
dc.identifier.citedreference | Krause, G. H., K. Winter, B. Krause, P. Jahns, M. Garcia, J. Aranda, et al. 2010. High‐temperature tolerance of a tropical tree, Ficus insipida: methodological reassessment and climate change considerations. Funct. Plant Biol. 37: 890 – 900. | en_US |
dc.identifier.citedreference | Lewis, S. L., J. Lloyd, S. Sitch, E. T. A. Mitchard, and W. F. Laurance. 2009. Changing ecology of tropical forests: evidence and drivers. Annu. Rev. Ecol. Evol. Syst. 40: 529 – 549. | en_US |
dc.identifier.citedreference | Lewis, S. L., P. M. Brando, O. L. Phillips, G. M. F. van der Heijden, and D. Nepstad. 2011. The 2010 Amazon drought. Science 331: 554 – 554. | en_US |
dc.identifier.citedreference | Lloyd, J., and G. D. Farquhar. 2008. Effect of rising temperatures and [CO2] on the physiology of tropical forest trees. Philos. Trans. R. Soc. B‐Biol. Sci. 363: 1811 – 1817. | en_US |
dc.identifier.citedreference | Malhi, Y., J. T. Roberts, R. A. Betts, T. J. Killeen, W. H. Li, and C. A. Nobre. 2008. Climate change, deforestation, and the fate of the Amazon. Science 319: 169 – 172. | en_US |
dc.identifier.citedreference | Maslin, M., Y. Malhi, O. Phillips, and S. Cowling. 2005. New views on an old forest: assessing the longevity, resilience and future of the Amazon rainforest. Trans. Inst. Br. Geogr. 30: 477 – 499. | en_US |
dc.identifier.citedreference | Mayle, F. E., and M. J. Power. 2008. Impact of a drier Early‐Mid‐Holocene climate upon Amazonian forests. Philos. Trans. R. Soc. B. 363: 1829 – 1838. | en_US |
dc.identifier.citedreference | Morley, R. J. 2000. Origin and evolution of tropical rain forests. John Wiley & Sons Ltd, West Sussex. | en_US |
dc.identifier.citedreference | Poorter, L., L. Bongers, and F. Bongers. 2006. Architecture of 54 moist‐forest tree species: traits, trade‐offs, and functional groups. Ecology 87: 1289 – 1301. | en_US |
dc.identifier.citedreference | Rammig, A., T. Jupp, K. Thonicke, B. Tietjen, J. Heinke, S. Ostberg, et al. 2010. Estimating the risk of Amazonian forest dieback. New Phytol. 187: 694 – 706. | en_US |
dc.identifier.citedreference | Richardson, J. E., R. T. Pennington, T. D. Pennington, and P. M. Hollingsworth. 2001. Rapid diversification of a species‐rich genus of neotropical rain forest trees. Science 293: 2242 – 2245. | en_US |
dc.identifier.citedreference | Silva, S., C. Jaramillo, and M. L. Absy. 2010. Neogene palynology of the Solimões basin, Brazilian Amazonia. Palaeontographicaa 283: 1 – 67. | en_US |
dc.identifier.citedreference | Smith, S. A., and M. J. Donoghue. 2008. Rates of molecular evolution are linked to life history in flowering plants. Science 322: 86 – 89. | en_US |
dc.identifier.citedreference | Thomas, C. D., A. Cameron, R. E. Green, M. Bakkenes, L. J. Beaumont, and Y. C. Collingham, et al. 2004. Extinction risk from climate change. Nature 427: 145 – 148. | en_US |
dc.identifier.citedreference | Way, D. A., and R. Oren. 2010. Differential responses to changes in growth temperature between trees from different functional groups and biomes: a review and synthesis of data. Tree Physiol. 30: 669 – 688. | en_US |
dc.identifier.citedreference | Willis, K. J., R. M. Bailey, S. A. Bhagwat, and H. J. B. Birks. 2010. Biodiversity baselines, thresholds and resilience: testing predictions and assumptions using palaeoecological data. Trends Ecol. Evol. 25: 583 – 591. | en_US |
dc.identifier.citedreference | Yesson, C., S. J. Russell, T. Parrish, J. W. Dalling, and N. C. Garwood. 2004. Phylogenetic framework for Trema (Celtidaceae). Plant Syst. Evol. 248: 85 – 109. | en_US |
dc.identifier.citedreference | You, Y., M. Huber, R. D. Muller, C. J. Poulsen, and J. Ribbe. 2009. Simulation of the middle Miocene climate optimum. Geophys. Res. Lett. 36: 5 pp. | en_US |
dc.identifier.citedreference | Zachos, J., M. Pagani, L. Sloan, E. Thomas, and K. Billups. 2001. Trends, rhythms, and aberrations in global climate 65 Ma to present. Science 292: 686 – 693. | en_US |
dc.identifier.citedreference | Zachos, J. C., G. R. Dickens, and R. E. Zeebe. 2008. An early Cenozoic perspective on greenhouse warming and carbon‐cycle dynamics. Nature 451: 279 – 283. | en_US |
dc.identifier.citedreference | Botkin, D. B., H. Saxe, M. B. Araujo, R. Betts, R. H. W. Bradshaw, T. Cedhagen, et al. 2007. Forecasting the effects of global warming on biodiversity. Bioscience 57: 227 – 236. | en_US |
dc.identifier.citedreference | Brumfield, R. T., and A. P. Capparella. 1996. Historical diversification of birds in northwestern South America: a molecular perspective on the role of vicariant events. Evolution 50: 1607 – 1624. | en_US |
dc.identifier.citedreference | Clement, M., D. Posada, and K. A. Crandall. 2000. TCS: a computer program to estimate gene genealogies. Mol. Ecol. 9: 1657 – 1659. | en_US |
dc.identifier.citedreference | Coates, A. G., and J. A. Obando. 1996. The geologic evolution of the Central American isthmus. Pp. 21 – 56 in J. B. C. Jackson, A. F. Budd and A. G. Coates, eds. Evolution and environment in tropical America. Univ. of Chicago Press, Chicago. | en_US |
dc.identifier.citedreference | Colwell, R. K., G. Brehm, C. L. Cardelus, A. C. Gilman, and J. T. Longino. 2008. Global warming, elevational range shifts, and lowland biotic attrition in the wet tropics. Science 322: 258 – 261. | en_US |
dc.identifier.citedreference | Corlett, R. T. 2011. Impacts of warming on tropical lowland rainforests. Trends Ecol. Evol. 26: 606 – 613. | en_US |
dc.identifier.citedreference | Dick, C. W., and M. Heuertz. 2008. The complex biogeographic history of a widespread tropical tree species. Evolution 62: 2760 – 2774. | en_US |
dc.identifier.citedreference | Dick, C. W., K. Abdul‐Salim, and E. Bermingham. 2003. Molecular systematics reveals cryptic Tertiary diversification of a widespread tropical rainforest tree. Amer. Nat. 162: 691 – 703. | en_US |
dc.identifier.citedreference | Dick, C. W., R. Condit, and E. Bermingham. 2005. Biogeographic history and the high beta diversity of rainforest trees in Panama. Pp. 259 – 268 in R. Harmon, ed. The Rio chagres: a multidisciplinary profile of a tropical watershed. Springer Publishing Company, New York. | en_US |
dc.identifier.citedreference | Dick, C. W., E. Bermingham, M. R. Lemes, and R. Gribel. 2007. Extreme long‐distance dispersal of the lowland tropical rainforest tree Ceiba pentandra L. (Malvaceae) in Africa and the Neotropics. Mol. Ecol. 16: 3039 – 3049. | en_US |
dc.identifier.citedreference | Doughty, C. E., and M. L. Goulden. 2008. Are tropical forests near a high temperature threshold? J. Geophys. Res. Biogeosci. 113: 1 – 12. | en_US |
dc.identifier.citedreference | Drummond, A. J., and A. Rambaut. 2007. Bayesian evolutionary analysis by sampling trees. BMC Evol. Biol. 7: 214. | en_US |
dc.identifier.citedreference | Drummond, A. J., S. Y. W. Ho, M. J. Phillips, and A. Rambaut. 2006. Relaxed phylogenetics and dating with confidence. PLoS Biol. 4: e88. | en_US |
dc.identifier.citedreference | Feeley, K. J., and M. R. Silman. 2010. Biotic attrition from tropical forests correcting for truncated temperature niches. Glob. Change Biol. 16: 1830 – 1836. | en_US |
dc.identifier.citedreference | Galbraith, D., P. E. Levy, S. Sitch, C. Huntingford, P. Cox, M. Williams, et al. 2010. Multiple mechanisms of Amazonian forest biomass losses in three dynamic global vegetation models under climate change. New Phytol. 187: 647 – 665. | en_US |
dc.identifier.citedreference | Haywood, A. M., A. Ridgwell, D. J. Lunt, D. J. Hill, M. J. Pound, H. J. Dowsett, et al. 2011. Are there pre‐Quaternary geological analogues for a future greenhouse warming? Philos. Trans. R. Soc. Math. Phys. Eng. Sci. 369: 933 – 956. | en_US |
dc.identifier.citedreference | Helmens, K. F., and T. van der Hammen. 1994. The Pliocene and Quaternary of the high plain of Bogotá (Colombia): a history of tectonic uplift, basin development and climatic change. Quatern. Int. 21: 41 – 61. | en_US |
dc.identifier.citedreference | Hoorn, C., F. P. Wesselingh, H. ter Steege, M. A. Bermudez, A. Mora, J. Sevink, et al. 2010. Amazonia through time: andean uplift, climate change, landscape evolution, and biodiversity. Science 330: 927 – 931. | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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