Amazon Basin Climate and Fire

The massive scale of the Amazon rainforest as a carbon sink gives it a significant influence on the global carbon cycle. However, droughts and fire, resulting partially from deforestation and fragmentation and partially from global climate patterns threaten to create a “dieback” scenario where the forest no longer functions as a carbon sink.

The climatic history of the Amazon basin is relevant to understand the effects of climate on forest distribution and composition. South America originally formed part of the Gondwanaland supercontinent, connected with Africa and Antarctica. Just 2 million years ago, in recent geologic time, the Isthmus of Panama closed to connect the Americas (explaining part of the distinction in North American and South American flora and fauna). Tropical Amazon forest may have existed as early as the late Cretaceous (100-66 mya). Some propose that dinosaurs may have modified the landscape, and that extensive humid forest did not exist until the dinosaurs were replaced by smaller fauna and a greater percentage of frugivore seed dispersers, closer to the Eocene (56-34 mya). Global warming during the Eocene, combined with the formation of the Andes Mountains, created a maximum period of rainforest formation, resulting in speciation of many rainforest plants.  Although rainforests contracted from parts of southern South America, humid forest remained expansive throughout the Amazon basin into the Pliocene (5-2 mya). Climate fluctuations during the last million years in the Pleistocene caused periodic ebb and flow of humid forest and dry savanna. The Amazon refugia theory has been proposed to explain the area’s high biodiversity, where expansive savannas concentrated rainforest species into small areas, leading to speciation. Although today most agree that savannas were small in extent, some studies discover evidence of extensive savanna as recent as 2,000 years before the present. 

After European colonization, it is likely that indigenous population crashes resulted in increased forest growth, perpetuating the virgin forest myth of the Amazon rainforest (see more- history of human settlement). In recent decades, however, deforestation and land use change threaten to disrupt the ecological balance of the Amazon forest as a whole. The Amazon dieback theory is a scenario where water stress, increased temperature, and other extreme climatic events cause tree death throughout the Amazon basin and a further increase in global carbon emissions. Fire and forest fragmentation could further exacerbate the Amazon die-back, as can dry conditions, as Amazon forests are vulnerable to drought. A study in Science (2009) found that the 2005 drought had a significantly negative impact on biomass growth, massively reducing the Amazon rainforest’s potential as a carbon sink. Areas particularly vulnerable to dieback are the seasonal forests of the southeast Amazon around the Brazilian state of Mato Grosso. In this area, a recent study discovered marked increases in fire which burned 5-12% of southeastern Amazon forest, resulting in significant ecological consequences. In other areas of the Amazon basin, selective logging is found to increase fire risk; regeneration is often impeded by lianas.

Early predictions forecasted grave scenarios for Amazon deforestation and subsequent dieback by the middle of the 21st century. However, recent studies have found that rainforests may be more resilient to drought and changing climate, and may continue to store carbon longer. Regardless, reducing deforestation and large fires will maintain carbon stocks and help in global climate regulation, a principle argument behind REDD+ conservation programs. In the Amazon basin, many groups now focus on climate adaption, or making forests and forest communities resilient to effects such as drought and flood. Many of these programs encourage food security and local production, increasing crop diversity, and agroforestry.   


Sources:

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Cox, P. M., Betts, R. A., Jones, C. D., Spall, S. A., & Totterdell, I. J. (2000). Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Nature408(6809), 184-187.

Denevan, W. M. (1992). The pristine myth: the landscape of the Americas in 1492. Annals of the Association of American Geographers, 82(3), 369-385.

Doyle, A. (2014, July 7). Amazon rainforest grew after climate change 2,000 years ago study. Reuters. Retrieved from: http://uk.reuters.com/article/2014/07/07/environment-amazon-idUKL6N0PI5L320140707

Fu, R., Yin, L., Li, W., Arias, P. A., Dickinson, R. E., Huang, L., … & Myneni, R. B. (2013). Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection. Proceedings of the National Academy of Sciences110(45), 18110-18115.

Gerwing, J. J. (2002). Degradation of forests through logging and fire in the eastern Brazilian Amazon. Forest ecology and management157(1), 131-141.

Heffernan, O. (2013, March 10).Tropical forests unexpectedly resilient to climate change. Nature. Retrieved from: http://www.nature.com/news/tropical-forests-unexpectedly-resilient-to-climate-change-1.12570

Maslin, M., Malhi, Y., Phillips, O., & Cowling, S. (2005). New views on an old forest: assessing the longevity, resilience and future of the Amazon rainforest. Transactions of the Institute of British Geographers30(4), 477-499.

Nepstad, D. C., Stickler, C. M., Soares-Filho, B., & Merry, F. (2008). Interactions among Amazon land use, forests and climate: prospects for a near-term forest tipping point. Philosophical Transactions of the Royal Society B: Biological Sciences, 363(1498), 1737-1746.

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Region: 
Amazon