When it comes to climate change, relationships are everything. That’s a key takeaway of a new UO study that examines the interaction between plants, atmospheric carbon dioxide and rising water levels in the Mississippi River.
Published recently in the Geological Society of America’s journal GSA Today, the study compared historical atmospheric carbon data against observations of herbarium leaf specimens to quantify the relationship between rising carbon levels and increasingly catastrophic floods in the American Midwest.
Using data covering more than two centuries, researchers demonstrated that as carbon levels in the atmosphere have risen due to the burning of fossil fuels, the ability of plants to absorb water from the air has decreased. That means more rainfall makes its way into rivers and streams, adding to their potential for damaging floods.
Co-authored by UO Museum of Natural and Cultural History geologist Greg Retallack and earth sciences graduate student Gisele Conde, the study focused on Ginkgo biloba leaf specimens representing a time span of just over 260 years.
The team examined the leaves’ stomata, tiny pores that deciduous plants use to take up carbon dioxide from the atmosphere. In low-carbon environments, plants increase the density of stomata so they can take in enough carbon dioxide for photosynthesis, but they need relatively few stomata in carbon-rich environments.
“Variations in stomatal density, which we observed using microscopic imaging, reflect corresponding changes in atmospheric carbon over the 264-year span,” said Retallack, director of the museum’s Condon Fossil Collection and a professor of earth sciences.
Stomatal density also governs the degree of transpiration, the process by which plants absorb water and give off water vapor; the fewer the stomata, the lower the transpiration potential. In the leaf specimens under examination, the researchers observed an overall decline in stomatal density and transpiration