Microscopic grains of dust from a comet, found deep in ocean sediment, could point to a significant event from 12,800 years ago. This event, known as the Younger Dryas impact, is believed to have caused a sudden, 1,200-year cooling period, even as the Earth was warming. Some scientists are skeptical of this idea, arguing that without a large crater, it’s hard to believe such a world-altering explosion happened. Yet, new evidence suggests that the impact may not have left behind a crater but instead tiny traces in sediment.
A team led by geoscientist Christopher Moore at the University of South Carolina has unearthed compelling evidence from four sediment cores taken from Baffin Bay, near Greenland. These cores are like time capsules, revealing layers of sediment built up over thousands of years. Moore explained, “We chose these sites to avoid contamination from humans, and the sediment layers were relatively undisturbed.” This likely provides a clearer view of ancient events.
By using radiocarbon dating and a method called single-particle inductively coupled plasma time-of-flight mass spectrometry, the team looked for cometary materials. The results showed tiny metallic particles with characteristics that match comet dust, including low oxygen and high nickel content. Most of the microspherules are Earth material, but they do include signatures from an impact, likely from an airburst when the comet exploded in the atmosphere.
Moore stated that the sediment layers contain multiple indicators of an impact event: “We found twisted metallic dust and unique chemical signatures suggesting a comet or meteorite impact.” This supports earlier findings from various terrestrial sites worldwide, suggesting that the Younger Dryas impact was indeed a global event.
Research on this topic is increasingly gaining traction. Surveys indicate that around 40% of climate scientists find the Younger Dryas impact hypothesis plausible, showcasing a growing interest in the link between cosmic events and climate change. The research adds depth to our understanding of Earth’s past climate shifts, connecting cosmic activity with dramatic changes in Earth’s atmosphere.
The team’s work has been published in PLOS One, and they plan to explore ocean sediment from other locations to gather more evidence that could reshape our understanding of ancient climate events.
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