Washington Post: How fossilized marine diatoms ended up on top of a mountain range in Antarctica has long puzzled scientists. The fossils date from the Pliocene era, about 2 million to 5 million years ago. When the fossils were first discovered in 1984, two theories were proposed. The so-called dynamicists said that the melting of the East Antarctic Ice Sheet (EAIS) raised ocean levels and that isostatic uplift caused new landmasses to rise; the combination caused the diatoms to be transported from the seafloor to the mountaintops. The stabilists countered that the ice sheet did not change; instead, powerful winds blew the diatoms from the ocean into the mountains. According to a new study by Reed Scherer of Northern Illinois University and his colleagues, what actually happened was a combination of both: The EAIS did retreat, but not as far as previously thought, and winds carried the diatoms the rest of the way. Besides solving the diatom mystery, the study also points up the vulnerability of the EAIS to global warming and raises concerns as current atmospheric carbon levels approach those of the Pliocene.
The finding that the Saturnian moon may host layers of icy slush instead of a global ocean could change how planetary scientists think about other icy moons as well.
Modeling the shapes of tree branches, neurons, and blood vessels is a thorny problem, but researchers have just discovered that much of the math has already been done.
January 29, 2026 12:52 PM
Get PT in your inbox
PT The Week in Physics
A collection of PT's content from the previous week delivered every Monday.
One email per week
PT New Issue Alert
Be notified about the new issue with links to highlights and the full TOC.
One email per month
PT Webinars & White Papers
The latest webinars, white papers and other informational resources.