Cited by 34Fire effects on ecosystemsPlant Water Relations and Carbon DynamicsEcosystem dynamics and resilience

The resilience of Amazon tree cover to past and present drying

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Kukla, Tyler, Ahlström, Anders, Maezumi, S. Yoshi, Chevalier, Manuel, Lu, Zhengyao, Winnick, Matthew J., Chamberlain, C. Page·2021·Global and Planetary Change

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Crossref · 10.1016/j.gloplacha.2021.103520

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  • Past drought periods also coincided with cooler temperatures, which probably reduced water demand by trees.

    “However, these periods also coincided with cooler temperatures20,21, which probably reduced water demand by trees30.”

    From Critical transitions in the Amazon forest system (2024) · cites this paper as [21]

    Citation 30 is attached to the suggestion that cooler temperatures reduced trees’ water demand; the preceding citations support the timing of cooler temperatures. The Introduction discusses mid-Holocene drying and tree-cover resilience, but the passages retrieved for cooler temperatures, water demand, and evapotranspiration do not address that proposed effect. (LLM, conf=0.72)

    Experimental — accuracy not yet measured
  • During the Last Glacial Maximum and mid-Holocene, forests persisted even when humans were already present in the landscape.

    “More recently, during the drier and cooler conditions of the Last Glacial Maximum20 (LGM) (around 21,000 years ago) and of the mid-Holocene epoch21 (around 6,000 years ago), forests persisted even when humans were already present in the landscape22.”

    From Critical transitions in the Amazon forest system (2024) · cites this paper as [21]

    The Introduction (p. 2) says the paper examines central and western Amazon tree cover under drier mid-Holocene conditions, but the passages available do not establish that forests persisted while humans were present. Searches for human presence, anthropogenic activity, forest persistence, and the Last Glacial Maximum found no passage addressing that conjunction. (LLM, conf=0.70)

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Authors
Kukla, T., Ahlström, A., Maezumi, S. Y., Chevalier, M., Lu, Z., Winnick, M. J., & Chamberlain, C. P.
Affiliations
  • Stanford University (US)
  • Lund University (SE)
  • University of Amsterdam (NL)
  • University of Bonn (DE)
  • University of Massachusetts Amherst (US)
Corresponding author
Kukla, Tyler
Venue
Global and Planetary Change
Publisher
Elsevier BV
Published
2021-07
Volume
202
Pages
103520
ISSN
0921-8181 (ISSN-L)
OpenAlex
W3162199618
Cited by
34
References
4
Citations by year
2026: 1 · 2025: 3 · 2024: 8 · 2023: 12 · 2022: 9 · 2021: 1
FWCI
2.96
Type
journal article
Language
en
Open access
Locations
  • Global and Planetary Change (acceptedVersion)
  • Zenodo (CERN European Organization for Nuclear Research) (submittedVersion, cc-by)
  • Lund University Publications (Lund University) (submittedVersion)
Funders
European Commission
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Fire effects on ecosystems
  • Physical Sciences › Environmental Science › Global and Planetary Change › Plant Water Relations and Carbon Dynamics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Ecosystem dynamics and resilience
Keywords
aridification, drought resilience, vegetation-climate feedback, mid-Holocene, fire, deforestation, grassland encroachment, pollen, charcoal, speleothem oxygen isotopes, LPJ-GUESS, future precipitation projections, anthropogenic land use

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