Earth System & Paleoclimate Model

PETM 56M: Paleocene-Eocene Thermal Maximum & Modern Forest Dieback

Carbon-Climate Engine
Simulation Scenarios
4,500

Cumulative carbon released from methane clathrates, volcanic sills, or fossil combustion.

1.2

PETM averaged ~1-2 Pg C/yr; Modern anthropogenic rate is ~10-11 Pg C/yr (10x faster).

1.40

Megadrought frequency & precipitation flashiness driving soil moisture deficits.

+5.5°C

Equilibrium surface temperature response modulated by polar amplification.

⚠️
Vulnerable Transition
Mid-latitude humid forests shifting to dry deciduous scrubland.
Terrestrial Biome Distribution & Dieback Matrix -55.93 Ma (Hyperthermal Peak)
Global Mean: 24.5°C Live Biomass: 62%
Rainforest/Humid
Temperate Forest
Savanna / Scrub
Arid Steppe / Desert
Active Dieback / Wildfire
Polar Deciduous
Historical PETM Chronology Scrubber -55.930 Ma
-56.20 Ma (Pre-PETM) -55.93 Ma (Peak) -55.70 Ma (Recovery)
Live Telemetry & Proxies Real-time Flux
Global Surface Temp 26.8°C +5.8°C vs pre-industrial
Atmospheric pCO₂ 1,840 ppm Stomatal proxy match
Forest Canopy Cover 54.2% -45.8% biome loss
Soil Carbon Feedback +3.4 Pg/yr Heterotrophic release
Biomass Loss vs. Atmospheric CO₂ Trajectory
PETM Fossil Proxy vs. Modern Parallels
Proxy / Metric 56 Ma PETM Proxy 21st Century Parallels
Carbon Rate 1.0–2.0 Pg C / yr 10.5 Pg C / yr (5–10×)
Tropical Biome Bighorn Basin & Neotropics flora shift to scrub Amazon savannization risk >2.5°C
High Latitudes Metasequoia swamps in Arctic (75°N) Boreal wildfire + permafrost thaw
Recovery Window ~100,000–150,000 yrs Deep millennial ocean/rock sink