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Updated: Aug 15, 2026

Reconstructing Terrestrial Paleoclimate and Paleoecology with Fossil Leaves Using Digital Leaf Physiognomy and Leaf Mass Per Area
Published on: October 25, 2024
Forest canopy decline under elevated CO2 during the Paleocene-Eocene Thermal Maximum
Regan E Dunn1,2, Marieke Dechesne3, Brady Z Foreman4
1Samuel Oschin Global Center for Ice Age Research, La Brea Tar Pits, Natural History Museum of Los Angeles County, Los Angeles, CA, USA.
Rapid global warming caused forest canopies to open and vegetation to shift dramatically during the Paleocene-Eocene Thermal Maximum (PETM). These ancient climate shifts offer insights into modern forest ecosystem responses to warming.
Area of Science:
- Paleoclimatology
- Ecology
- Paleobotany
Background:
- Anthropogenic warming impacts on forest ecosystems remain uncertain.
- The Paleocene-Eocene Thermal Maximum (PETM) serves as a valuable analog for rapid global warming events.
- Understanding past ecosystem responses can inform predictions of future climate change impacts.
Purpose of the Study:
- To reconstruct forest canopy density and composition changes during the PETM.
- To assess the impact of abrupt warming and carbon increase on vegetation.
- To investigate the relationship between plant community shifts and landscape stability.
Main Methods:
- Developed a proxy to quantify leaf area index (LAI) from palynomorph data.
- Analyzed palynomorphs to assess shifts in floral composition.
- Integrated Wyoming data with regional paleoclimate and paleoecological records.
Main Results:
- Forest canopies abruptly opened at the onset of PETM warming.
- Increased landscape erosion was observed.
- Vegetation shifted from broad-leaved angiosperms to fern- and palm-dominated ecosystems.
Conclusions:
- Continental-scale plant community shifts can lead to landscape destabilization.
- These vegetation changes have implications for long-term climate feedbacks.
- Past warming events provide crucial data for understanding current and future forest ecosystem dynamics.
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