Latest news with #StacFada
Yahoo
07-05-2025
- Science
- Yahoo
UK's Geological Past Shaken by Billion-Year-Old Meteorite Find
In a recent groundbreaking discovery, scientists have identified evidence of a meteorite impact in north-west Scotland that dates back 1 billion years. The space rock is considered the oldest known meteorite strike in the United Kingdom and one of the oldest recorded on Earth. These new findings have prompted many researchers to revise parts of the geological history of the British Isles. The evidence was uncovered by geologists studying rocks from the Stac Fada Member of the Stoer Group, located in the remote parts of the Highlands. Evidence was found by studying rocks in the Highlands (Tony Prave) These rocks were long suspected to be linked to an ancient impact, but until now, solid confirmation had been missing. Unmistakable signs of a catastrophic impact Professor Kirkland, the lead author from Curtin's Frontier Institute for Geoscience Solutions within the School of Earth and Planetary Sciences, said 'When a meteorite hits, it partially resets the atomic clocks inside the zircon crystals and these 'broken timepieces' are often unable to be dated but we developed a model to reconstruct when the disturbance occurred, confirming the impact at 990 million years ago.' Professor Chris Kirkland dated the impact to 990 million years ago (Curtin University) Before the discovery, it was previously believed that the impact occurred 1.2 billion years ago. ADVERTISEMENT Advertisement But the new research used tiny zircon crystals as geological time capsules to get a better understanding of when the impact occurred, which they have now placed at 990 million years ago. Scotland's geological timeline revised The impact crater itself has not yet been found, however, many scientists believe it may lie under the Minch, the strait that separates mainland Scotland from the Outer Hebrides. Estimates suggest the crater could be between 15 and 20 kilometres in diameter. Given the age of the rocks and the tectonic changes that have occurred since the impact, locating the original site might prove to be challenging. ADVERTISEMENT Advertisement Despite the missing crater, the fallout from the strike was preserved in the Stac Fada deposits. Dr Kirkland stated 'While the impact crater itself has yet to be found, this study has collected further clues that could finally reveal its location. "Understanding when meteorite impacts occurred helps us explore their potential influence on Earth's environment and the expansion of life beyond the oceans,' he went on to say. 'The revised dating suggests these life forms in Scotland appeared at a similar time to a meteorite impact. "This raises fascinating questions about whether large impacts may have influenced environmental conditions in ways that affected early ecosystems." ADVERTISEMENT Advertisement The 1 billion-year-old meteorite strike significantly predates the more famous Chicxulub impact that killed the dinosaurs, which itself was around 600 million years ago. While not as globally catastrophic, the Scottish event is significant in helping scientists understand how Earth evolved in its early years, making it a vital piece of research to help us fully understand our planet's history.
Yahoo
29-04-2025
- Science
- Yahoo
1 billion years ago, a meteorite struck Scotland and influenced life on Earth
We've discovered that a meteorite struck northwest Scotland 1 billion years ago, 200 million years later than previously thought. Our results are published today in the journal Geology. This impact now aligns with some of Earth's earliest known, land based, non-marine microbial fossils, and offers new insights into how meteorite strikes may have shaped our planet's environment and life. The Torridonian rocks of northwest Scotland are treasured by geologists as some of the finest archives of the ancient lakes and river systems that existed a billion years ago. Those water bodies were home to microbial ecosystems consisting of eukaryotes. Eukaryotes are single-celled organisms with complex internal structures that are the ancestors of all plants and animals. But the Torridonian environments and their associated microbial communities were dramatically disrupted when a meteor slammed into the planet. The record of this event is preserved in a geological unit known as the Stac Fada Member. It is comprised of unusual layers of rock fragments broken and melted by the impact. Also, crucially, there are shock-altered minerals that closely resemble those found in famous impact sites such as Chicxulub (Mexico) and Sudbury (Canada). In the case of the Stac Fada, these minerals were engulfed in high-energy, ground-hugging flows of smashed rock triggered by the impact that spread across the ancient landscape. What is exciting about our new date for the Stac Fada impact is that it now overlaps in age with microfossils preserved elsewhere in the Torridonian rocks. This raises some interesting questions. For example, how did the meteorite strike influence the environmental conditions those early non-marine microbial ecosystems relied on? Determining when a meteorite struck is no easy task. We can use minerals to constrain the age, but they have to be the right kind. In this case it means something that wasn't overly altered by the intense heat, pressure and fluids generated by the impact, yet robust enough to survive the ravages of deep geological time. Suitable minerals are extremely rare, but we found a few in the Stac Fada rocks. One was reidite, a mineral that only forms under extreme pressure. The other was granular zircon, a uranium-bearing mineral formed by immense impact temperatures. These minerals are, in effect, tiny stopwatches whose clocks start 'ticking' at the time they form. Although these clocks are often damaged during the impact and the ensuing pulse of heat, we used mathematical modelling to determine the most probable time of impact. Together, these techniques consistently pointed to an event 1 billion years old, not 1.2 billion years old as previously suggested. Given such vast spans of time, a 20% change in age might not seem dramatic. However, the new age shows the timing of the impact coincides with early non-marine eukaryotic fossils. It also lines up with a major mountain-building event. This means the Torridonian lifeforms had to cope with significant, environment-altering phenomena. The origin of life is a deeply complex process that likely began with a series of pre-biotic chemical reactions. While much remains unknown, it is intriguing that two ancient meteorite impacts, the 3.5-billion-year-old North Pole impact in Western Australia and now the 1-billion-year-old Stac Fada deposit in northwest Scotland, occur close in time to major milestones in the fossil record. The North Pole impact occurs in a sequence of rocks containing stromatolites, some of the oldest-known fossils considered to be indicative of microbial life. All life requires energy. The earliest forms of life are thought to be associated with volcanic hydrothermal springs. Impacts offer a plausible alternative. The immediate aftermath of a meteorite strike is extreme and hostile, and would ruin your day. But the long-term effects could support key biological processes. Meteorite strikes fracture rocks, generate long-lived hydrothermal systems and form crater lakes that enable the concentration of important ingredients for life, such as clays, organic molecules and phosphorus. The latter is a key element for all forms of life. In Scotland, the Stac Fada impact lies within an ancient river and lake environment that housed microbial ecosystems colonising the land. What makes the Stac Fada impact deposits fascinating is that, unlike most other impacts on Earth, they preserve the environments in which those pioneering organisms lived immediately prior to the impact. Further, the impact deposits were subsequently buried as non-marine microbial habitats became reestablished. So, the Stac Fada rocks provide an opportunity to see how microbial life recovered from impact. Extraterrestrial visitors in the form of meteorite collisions may not just have scarred Earth's surface, but shaped its future, turning catastrophic events into natural crater-cradles of life. This article is republished from The Conversation. It was written by: Chris Kirkland, Curtin University; Timmons Erickson, Curtin University, and Tony Prave, University of St Andrews Read more: Echidna ancestors lived watery lifestyles like platypuses 100 million years ago – new study Here's how to make your backyard safer and cooler next summer Granular systems, such as sandpiles or rockslides, are all around you − new research will help scientists describe how they work The authors do not work for, consult, own shares in or receive funding from any company or organisation that would benefit from this article, and have disclosed no relevant affiliations beyond their academic appointment.
