The Grand Canyon is one of the sites that preserves the Great Unconformity. Image: Saad Chaudhry on Unsplash
ABSTRACT breaks down mind-bending scientific research, future tech, new discoveries, and major breakthroughs.
For over a century, scientists have debated the cause of this immense geological blackout, which erased a huge chunk of the Neoproterozoic era. Two main explanations have emerged, which are not mutually exclusive: One suggests that tectonic activity associated with the assembly and breakup of the supercontinent Rodinia created the Unconformity, while another points to erosion from widespread glaciation during our planet’s “Snowball Earth” phase some 700 million years ago. Now, a team led by Kalin McDannell, a postdoctoral researcher in earth sciences at Dartmouth College, has presented new evidence that glaciers were the main force that carved out this mysterious gap in time. The researchers discovered a strong “cooling signal” at four very different geological locations across North America, suggesting that continental-scale glaciation may be “the only foreseeable process that can account for both the formation and preservation of the Great Unconformity,” according to a study published Tuesday in The Proceedings of the National Academy of Sciences. “Something really unique was going on in terms of global geodynamics and surface processes that allowed the Great Unconformity to both form and then be preserved,” said McDannell in a joint call with C. Brenhin Keller, assistant professor of earth sciences at Dartmouth and a co-author of the study. “That’s my perspective on why this has captured people's imaginations.”
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Researchers used thermochronometric data from four North American locations to determine the cause of the Great Unconformity. Figure by Kalin McDannell.
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