Hidden chunk of Earth's crust that seeded birth of 'Scandinavia' discovered through ancient river crystals
Finland's river crystals hold clues about the formation of 'Scandinavia's' oldest bedrock 3.75 billion years ago.
Get the world’s most fascinating discoveries delivered straight to your inbox.
You are now subscribed
Your newsletter sign-up was successful
Want to add more newsletters?
Delivered Daily
Daily Newsletter
Sign up for the latest discoveries, groundbreaking research and fascinating breakthroughs that impact you and the wider world direct to your inbox.
Once a week
Life's Little Mysteries
Feed your curiosity with an exclusive mystery every week, solved with science and delivered direct to your inbox before it's seen anywhere else.
Once a week
How It Works
Sign up to our free science & technology newsletter for your weekly fix of fascinating articles, quick quizzes, amazing images, and more
Delivered daily
Space.com Newsletter
Breaking space news, the latest updates on rocket launches, skywatching events and more!
Once a month
Watch This Space
Sign up to our monthly entertainment newsletter to keep up with all our coverage of the latest sci-fi and space movies, tv shows, games and books.
Once a week
Night Sky This Week
Discover this week's must-see night sky events, moon phases, and stunning astrophotos. Sign up for our skywatching newsletter and explore the universe with us!
Join the club
Get full access to premium articles, exclusive features and a growing list of member rewards.
By studying river crystals in Finland, researchers have identified traces of a hidden chunk of Earth's crust from the heart of an ancient continent, a new study has found.
The crystals, from the mineral zircon, formed deep within the crust and provide clues as to how some of Europe's oldest bedrock formed 3.75 billion years ago.
To make the discovery, the team studied three geochemistry tracers — uranium–lead, Lutetium–hafnium and Oxygen — to date the crystals and match their signatures to other ancient crust. The analysis revealed that part of the crust is about 250 million years older than scientists previously thought, and that it likely originated in Greenland, according to a University of Copenhagen statement released March 21.
The study sheds light on the formation and growth of Archean cratons, the oldest parts of the continental crust that formed during the Precambrian's Archean era (4 billion to 2.5 billion years ago), when life first arose.
"Understanding how continents formed helps us understand why ours is the only planet in the solar system with life on it," lead author Andreas Petersson, a geochemist at the University of Copenhagen, said in the statement. "Because without fixed continents and water in between them, we wouldn't be here. Indeed, continents influence both ocean currents and climate, which are crucial for life on Earth."
The researchers presented their findings in a study published Dec. 28, 2023, in the journal Geology.
Related: Greenland is losing so much ice, it's getting taller
Get the world’s most fascinating discoveries delivered straight to your inbox.
Previous research uncovered evidence for early Archean crust in the Pudasjärvi and Suomujärvi regions of Finland, according to the study. The team got the zircon crystals from river sands in these regions and discovered that the crystals had a similar isotope record to rocks in West Greenland's North Atlantic craton, suggesting that part of Finland's crust formed in Greenland.
"The zircon crystals we found in river sand and rocks from Finland have signatures that point towards them being much older than anything ever found in Scandinavia, while matching the age of Greenlandic rock samples," Petersson said. "At the same time, the results of three independent isotope analyses confirm that Scandinavia's bedrock was most likely linked to Greenland."
All of these countries sit above a section of crust called the Fennoscandian Shield or Baltic Shield. The researchers now think this crust broke away from Greenland and moved around for hundreds of millions of years, before taking root where Finland is today. It then accumulated new geological material and grew to become Scandinavia, according to the statement. (Here, the research team uses the term "Scandinavia" to represent the Fennoscandian geological region, which includes Finland.)
Back when this split happened, Earth may have been completely covered in water. "Earth was probably a watery planet, like in the movie 'Waterworld,' but without any oxygen in the atmosphere and without emergent crust," Tod Waight, a geologist at the University of Copenhagen, said in the statement. "But, because that's so far back in time, we can't be really be sure about what it actually looked like."
Discovering a "seed" from an ancient continent that grew into what we see today may help us understand how other landmasses on Earth formed. "Our study provides us with another important clue in the mystery of how continents formed and spread across Earth — especially in the case of the Fennoscandian Shield," Waight said. "But there is still plenty that we don't know. In Australia, South Africa and India, for example, similar seeds have been found, but we're unsure of whether they all come from the same 'birthplace,' or whether they originated independently of one another in several places on Earth."

Patrick Pester is the trending news writer at Live Science. His work has appeared on other science websites, such as BBC Science Focus and Scientific American. Patrick retrained as a journalist after spending his early career working in zoos and wildlife conservation. He was awarded the Master's Excellence Scholarship to study at Cardiff University where he completed a master's degree in international journalism. He also has a second master's degree in biodiversity, evolution and conservation in action from Middlesex University London. When he isn't writing news, Patrick investigates the sale of human remains.
