Scientists disagree on what the find means for a controversial comet-impact hypothesis
Natural History Museum of Denmark, Cryospheric Sciences Lab/NASA Goddard Space Flight Center
They hadn’t set out to find a crater. But in 2015, glaciologists studying ice-penetrating radar images of Greenland’s ice sheet, part of an annual survey by NASA’s Operation IceBridge mission, noticed an oddly rounded shape right at the northern edge of Hiawatha Glacier. If the 31-kilometer-wide depression is confirmed to be the remnant of a meteorite impact — and the team has produced a wealth of evidence suggesting that it is (SN: 12/8/18, p. 6) — the discovery is exciting in and of itself. It’s rare to find a new crater, let alone one on land that has retained its perfect bowl shape.
“This is just a straight-up exciting discovery that starts with this wonderful element of serendipity,” says team member Joseph MacGregor, a glaciologist with Operation IceBridge.
Proponents of the Younger Dryas impact hypothesis say that the remnants of a comet exploded in Earth’s atmosphere and that the airbursts sparked wildfires across North America. Soot and other particles from the fires blocked out the sun, causing the cold snap, which has been blamed for everything from the extinction of the mammoths to the disappearance of a group of people known as the Clovis.
Most scientists reject that an impact was responsible, refuting the idea that there were vast wildfires at the time or that the Clovis people even disappeared. Another big objection: the lack of a smoking gun, a crater dating to the onset of the Younger Dryas.
The “mammoth in the room,” therefore, is whether the Greenland crater might be that smoking gun. But a large, recent impact would be extremely unlikely, given the rarity of such impacts on Earth, particularly on land, says planetary scientist Clark Chapman of the Southwest Research Institute in Boulder, Colo., who was not involved with the discovery.
Indeed, one sticking point is that there are no direct dates for the newly discovered crater, because it is still buried beneath all that ice. The radar data offer only tantalizing clues to the age, suggesting that the crater is between 2.6 million and 11,700 years old.
That’s a huge time range, but the proponents of the hypothesis are convinced that this crater is what they’ve been waiting for. “I think it’s transformational in terms of convincing a lot of skeptics,” says James Kennett, a geologist at the University of California, Santa Barbara.
BIG HIT If an iron-rich asteroid hit Earth in the distant past, it may help explain a cold snap known as the Younger Dryas.
There’s another big sticking point when it comes to linking this crater to the impact hypothesis: Instead of a fragment of a comet, the discoverers think the Hiawatha impactor was an iron meteorite. That determination is based on measurements of platinum and other elements in glacial outwash, sediments carried by meltwater from beneath the ice. An iron meteorite impact would probably not produce the kinds of explosive airbursts that could ignite continent-scale wildfires, says Michail Petaev, a geochemist at Harvard University.
Petaev and colleagues previously found a hint that an iron meteorite might have smacked into Greenland about 13,000 years ago. In 2013, his group examined Greenland ice cores and found a strange platinum anomaly dating to right before the Younger Dryas. The ratio of platinum to iridium measured in the ice cores points to an iron meteorite, the team reported.
Despite the platinum data, the impact hypothesis proponents hold firmly to the idea that the Hiawatha impactor was a comet. Because little is known about comet compositions, Kennett says, a comet might well have been the source for the platinum found in the glacial outwash and the ice cores. But Petaev maintains that the observed platinum ratios just wouldn’t occur in a comet, which is made of the primitive stuff of the universe. Instead, he says, those ratios require the cycles of melting and recrystallizing that form iron meteorites, the ancient cores of asteroids or planets.
Instead, the crater’s discoverers are planning to collect more sediments from the glacial outwash, and perhaps even drill directly into the crater to retrieve sediment cores that can be dated. And there may be other craters lurking beneath Greenland’s ice, or even Antarctica’s — perhaps more easily identifiable once you know what to look for, says MacGregor.
Asked whether the team has actually identified any other round shapes of interest, he pauses. Then MacGregor says, cryptically, “stay tuned.”
K.H. Kjær et al. A large impact crater beneath Hiawatha Glacier in northwest Greenland. Science Advances. Published online November 14, 2018. doi: 10.1126/sciadv.aar8173.
M.I. Petaev et al. Large Pt anomaly in the Greenland ice core points to a cataclysm at the onset of Younger Dryas. Proceedings of the National Academy of Sciences. Vol. 110, August 6, 2013, p. 12917. doi: 10.1073/pnas.1303924110.
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