A chemical analysis of sediment cores from the North Pacific Ocean show a consistent pairing of volcanic ash and hypoxia, a low ocean oxygen interval spanning thousands of years, during times of rapid climate warming at the end of the last ice age, new research shows.
A chemical analysis of sediment cores from the North Pacific Ocean show a consistent pairing of volcanic ash and hypoxia, a low ocean oxygen interval spanning thousands of years, during times of rapid climate warming at the end of the last ice age, new research shows.
Understanding the relationship between volcanic activity, hypoxia and ice melt due to warming temperatures during the last ice age, which ended about 18,000 years ago, raises important questions about what might occur as the planet warms today.
“It is unknown right now whether volcanic eruptions will increase as the climate warms,” said the study’s lead author, Jianghui Du of ETH Zurich in Switzerland, who conducted the research as a doctoral student at Oregon State University’s College of Earth, Ocean, and Atmospheric Sciences.
Read more at: Oregon State University
Photo Credit: Julius_Silver
