Distinguished University Professor and Geology Department Chair Roberta Rudnickis trying to crack a mystery that lies far beneath the ground we walk on. Rudnick studies the evolution of the Earth’s continental crust. “Interestingly, none of the other planets in our solar system have continents,” she points out. “Understanding continent formation can broaden our knowledge about many processes on Earth, including our own species’ evolution.”
Geologists agree that the continental crust formed when magma melted in the Earth’s mantle, erupting to the surface. “The perplexing thing is that the continental crust is comprised of rocks that could not have come directly from the Earth’s mantle,” says Rudnick, “so other processes must have been involved.” The crust has an andesitic bulk composition, while geologists would expect it to have a basaltic composition, like the Earth’s oceanic crust and terrestrial areas on Mars and Venus. This “Crust Composition Conundrum” puzzles Rudnick, and she has traveled the globe for answers.
Her research currently takes her to Eastern China, where she looks for clues in rock samples brought to the surface through volcanic eruptions—what Rudnick calls a poor man’s drill hole. “We would love to drill down and collect samples, but it’s hugely expensive, and is not feasible past 12 kilometers,” says Rudnick, who explains that the base of the crust is 40 kilometers deep and the underlying lithosphere is 150 kilometers below the Earth’s surface.
Back in the campus geochemical laboratories, her research team has analyzed the samples extensively, finding evidence to explain the conundrum. One theory, called “recycling of the lower crust,” posits that millions of years ago the crust was basaltic, but that over time the denser minerals, containing iron and magnesium, accumulated in the lower crust and eventually sank into the mantle. Her lab also unearthed evidence that chemical weathering has changed the crust composition over the ages by removing soluble elements, such as magnesium.
Rudnick, an elected member of the National Academy of Sciences, is also reassessing the continental crust composition to derive a better estimate of its radioactive elements. In the past year, she and her collaborators have traveled to Central China, South Africa, Namibia, Canada, as well as Idaho and Wyoming, to collect samples from glacial tillites—rock material deposited during ice ages throughout history. The information could help uncover further mysteries of continent evolution, including how weathering of continents responded to the rise of atmospheric oxygen some 2.4 billion years ago.
Writer: Beth Panitz