Research by a University of Oklahoma scientist could lead to novel way to fight climate change. It has to do with dust.
Dr. Gerilyn Soreghan and a team of researchers from the University of California Riverside, Florida State University, University of Leeds, Hampton University, and Cornell University have been looking at some really old, iron-rich dust deposits. Like 300-million year old dust from the late Paleozoic period.
Dr. Soreghan says Earth’s atmosphere was as dusty as it has ever been 300 million years ago. She says it’s important to study those dust deposits because of the impact they had back then on Earth’s climate.
Here’s why: dust carries iron- iron is a fertilizer for plants- plants use photosynthesis-photosynthesis removes carbon from the atmosphere and replaces it with oxygen.
Dr. Soreghan says deep-time dust contained a lot of iron which means it “…should have even larger consequences for burial of carbon.” As for the modern day, there’s talk of iron fertilization as a geoengineering scheme to control the amount of carbon in the atmosphere.
Dr. Soreghan says her study on deep-time events shines a light on how those types of geoengineering endeavors may work in the present day but, she says, more research is needed.
You can read more on the study in this brief write-up by Dr. Soreghan or here where the Geological Society of America has published an article. The National Science Foundation and American Chemical Society funded the research.