A new study led by University of Wisconsin Oshkosh geologist Timothy Paulsen and Michigan Tech geologist Chad Deering advances the understanding of the role that continents have played in the chemical evolution of Earth’s oceans, with implications for understanding atmospheric oxygenation and global climate oscillations.
The team of researchers analyzed a global database of the chemistry of tiny zircon grains commonly found in the Earth’s continental rock record. The research team includes other scientists from Michigan Technological University and ETH Zurich in Switzerland.
The study was featured on the cover of the February issue of GSA Today by the Geological Society of America, which highlights timely, innovative articles that appeal to a broad geoscience audience.
“Oceans cover 70% of Earth’s surface, setting it apart from the other terrestrial planets in the solar system,” said Paulsen, the lead author on the paper. “Geologists have long recognized that there have been profound changes in ocean chemistry over time.”
Yet there are significant questions about the drivers for changes in ocean chemistry in Earth’s past, especially associated with the ancient rock record leading up to the Cambrian explosion of life approximately 540 million years ago.
“Continents tend to be worn down by weathering and rivers tend to transport this sediment to the oceans leaving scattered puzzle pieces for geologists to fit together,” said Deering, a coauthor on the paper. “There is increasing evidence that important pieces of the puzzle are found in the ancient beach and river sediments produced through continental weathering and erosion.”
The researchers’ findings, based on an analysis of an exceptionally large zircon data set from sandstones recovered from Earth’s major continental landmasses, may signify key links in the evolution of the Earth’s rock cycle and its oceans.
“Our results suggest that two major increases in continental input from rivers draining the continents were related to the break-up and dispersal of continents, which caused increased weathering and erosion of a higher proportion of radiogenic rocks and high-elevation continental crust,” Paulsen said.
“Both episodes are curiously associated with snowball Earth glaciations and associated steps in oxygenation of the atmosphere-ocean system. Geologists have long recognized that oceans are required to make continents. It would appear based on our analyses that the continents, in turn, shape the Earth’s oceans, atmosphere and climate.”
Materials provided by University of Wisconsin Oshkosh. Original written by Natalie Johnson. Note: Content may be edited for style and length.