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Non-uniform tropical forest responses to the ‘Columbian Exchange’ in the Neotropics and Asia-Pacific

MPS-Authors
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Hamilton,  Rebecca
isoTROPIC, Max Planck Institute for the Science of Human History, Max Planck Society;

/persons/resource/persons247353

Wolfhagen,  Jesse
Archaeology, Max Planck Institute for the Science of Human History, Max Planck Society;

/persons/resource/persons208838

Amano,  Noel
Archaeology, Max Planck Institute for the Science of Human History, Max Planck Society;

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Boivin,  Nicole
Archaeology, Max Planck Institute for the Science of Human History, Max Planck Society;

/persons/resource/persons249504

Findley,  David Max
isoTROPIC, Max Planck Institute for the Science of Human History, Max Planck Society;

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Roberts,  Patrick
isoTROPIC, Max Planck Institute for the Science of Human History, Max Planck Society;

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Citation

Hamilton, R., Wolfhagen, J., Amano, N., Boivin, N., Findley, D. M., Iriarte, J., et al. (2021). Non-uniform tropical forest responses to the ‘Columbian Exchange’ in the Neotropics and Asia-Pacific. Nature Ecology & Evolution, s41559-021-01474-4. doi:10.1038/s41559-021-01474-4.


Cite as: https://hdl.handle.net/21.11116/0000-0008-BCCE-D
Abstract
It has been suggested that Iberian arrival in the Americas in 1492 and subsequent dramatic depopulation led to forest regrowth that had global impacts on atmospheric CO2 concentrations and surface temperatures. Despite tropical forests representing the most important terrestrial carbon stock globally, systematic examination of historical afforestation in these habitats in the Neotropics is lacking. Additionally, there has been no assessment of similar depopulation–afforestation dynamics in other parts of the global tropics that were incorporated into the Spanish Empire. Here, we compile and semi-quantitatively analyse pollen records from the regions claimed by the Spanish in the Atlantic and Pacific to provide pan-tropical insights into European colonial impacts on forest dynamics. Our results suggest that periods of afforestation over the past millennium varied across space and time and depended on social, economic and biogeographic contexts. We argue that this reveals the unequal and divergent origins of the Anthropocene as a socio-political and biophysical process, highlighting the need for higher-resolution, targeted analyses to fully elucidate pre-colonial and colonial era human–tropical landscape interactions.