Western CEDAR - Scholars Week: What was wildfire activity like in Bellingham 56 million years ago?
 

What was wildfire activity like in Bellingham 56 million years ago?

Research Mentor(s)

Camilo Ponton

Description

Wildfire regimes are expected to change, with wildfires increasing in frequency and severity as climate changes in the Pacific Northwest (Halofsky et al., 2020). To better understand the effect of warming climate on wildfires, I propose to reconstruct a paleo-wildfire regime during the Paleocene-Eocene, a period of past global warming. The Chuckanut Formation is a late Paleocene to late Eocene sedimentary deposit with a robust paleobotanical record (Breedlovestrout et al., 2013) showing the existence of subtropical forests in northwest Washington. Polycyclic aromatic hydrocarbons (PAHs) are molecules produced during incomplete combustion of biomass that readily preserve in the sedimentary record (Lima et al., 2005) and are used to reconstruct past wildfires. I expect to see an increase in PAHs in the Paleocene compared to the late Eocene, because warmer climate and denser forests would provide ample fuel to burn and increase the severity and frequency of wildfires.

Document Type

Event

Start Date

May 2022

End Date

May 2022

Location

SMATE Library (Bellingham, Wash.)

Department

Geology

Genre/Form

student projects; posters

Type

Image

Rights

Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this document for commercial purposes, or for financial gain, shall not be allowed without the author’s written permission.

Language

English

Format

application/pdf

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May 19th, 9:00 AM May 19th, 12:00 PM

What was wildfire activity like in Bellingham 56 million years ago?

SMATE Library (Bellingham, Wash.)

Wildfire regimes are expected to change, with wildfires increasing in frequency and severity as climate changes in the Pacific Northwest (Halofsky et al., 2020). To better understand the effect of warming climate on wildfires, I propose to reconstruct a paleo-wildfire regime during the Paleocene-Eocene, a period of past global warming. The Chuckanut Formation is a late Paleocene to late Eocene sedimentary deposit with a robust paleobotanical record (Breedlovestrout et al., 2013) showing the existence of subtropical forests in northwest Washington. Polycyclic aromatic hydrocarbons (PAHs) are molecules produced during incomplete combustion of biomass that readily preserve in the sedimentary record (Lima et al., 2005) and are used to reconstruct past wildfires. I expect to see an increase in PAHs in the Paleocene compared to the late Eocene, because warmer climate and denser forests would provide ample fuel to burn and increase the severity and frequency of wildfires.