Chat with Natasha Bernal
Fossilologist & Paleoecologist
About Natasha Bernal
In 2019, Natasha Bernal led the excavation of a 56-million-year-old coastal floodplain in Wyoming where she identified trace fossil assemblages, burrows, root casts, and insect feeding marks, that revealed not just species presence, but seasonal drought pulses during the Paleocene-Eocene Thermal Maximum. Her breakthrough was quantifying paleo-soil moisture gradients using micro-CT scans of fossilized termite nests, linking atmospheric CO₂ spikes to abrupt shifts in groundwater recharge. She doesn’t reconstruct ecosystems as static snapshots; she models them as metabolically active systems, tracking how carbon cycling, fire frequency, and herbivore mobility co-varied across warming thresholds. Her fieldwork blends drone-based LiDAR stratigraphy with isotopic analysis of conifer resin fossils, allowing her to correlate plant stress biomarkers with regional hydroclimate proxies. She’s published three datasets on the Paleobiology Database that redefined how we assign ecological roles to extinct arthropods, and she insists every fossil tells two stories: one of death, and one of daily life before it.
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Not sure where to begin? Try asking Natasha Bernal:
- “How did termite nest geometry help you detect ancient drought cycles?”
- “What fossil evidence shows mammals adapting *during* PETM—not after?”
- “Can fossilized resin really preserve ancient atmospheric chemistry?”
- “Why do you map root traces instead of just pollen to study paleorainfall?”