Florida State University scientists have uncovered answers to a conundrum in Earth’s history: Why did marine life experience an extraordinary boom millions of years ago?
Scientists have long been puzzled about what triggered this explosion of life and a remarkable increase in the diversity of marine species during the Ordovician Period roughly 487 to 443 million years ago. A new study led by FSU Associate Professor of Geology Seth Young and postdoctoral fellow Anders Lindskog has provided insights into this ancient ecological transformation and the role oxygen played in it. Their study was published in Nature Geoscience.
To unravel the ancient mystery, Lindskog and Young embarked on a mission with colleagues at FSU and Lund University in Sweden to understand the environmental conditions, particularly the oxygen levels in the ancient seas, of the Ordovician Period. Oxygen is essential for the development of higher organisms, so it’s a key player in the evolution of marine life.
“By better understanding the backdrop to these changes, we can better understand the mechanisms that drive large-scale and long-term evolution — basically, how life became what it is today,” said Lindskog, who is now at Lund University.