logo
Human-caused emissions have delayed Earth's next ice age, study says. But by how long?

Human-caused emissions have delayed Earth's next ice age, study says. But by how long?

Yahoo02-03-2025

A new study suggests that Earth's next ice age should begin within the next 11,000 years - except our impact on the planet may delay it, potentially by thousands of years.
Scientists have long known that shifts in Earth's orbit influence transitions between ice ages and warmer interglacial periods. But until now, they could not pinpoint which orbital factors affected the timing of these glacial cycles the most.
A research team led by the University of Cardiff tracked Earth's natural climate cycles over the past million years and compared this data to variations in the tilt, wobble and shape of the planet's orbit around the Sun.
Published in the academic journal Science, their study offers clear insights into how these factors influence glacial cycles - as well as how human-driven greenhouse gas emissions may have disrupted them.
'The pattern we found is so reproducible that we were able to make an accurate prediction of when each interglacial period of the past million years or so would occur and how long each would last,' lead author Stephen Barker, a professor at the University of Cardiff explained to AFP.
Over the past million years, Earth has alternated between ice ages and warm periods. The last ice age, or glacial period, ended about 11,700 years ago. That transition ushered in the Holocene, an era of relative climate stability which enabled human civilisations to flourish.
Since the 1970s, scientists have tried to identify the start of our next glacial period, but determining an accurate time frame has proven to be difficult.
Related
Melting polar ice may be slowing Earth's spin and messing with how we measure time
'Unprecedented': CO2 in the atmosphere is rising 10 times faster than at any point over 50,000 years
While researchers have previously tried to link orbital changes to specific periods, such as the beginning of an ice age, Barker's team took a broader view. They analysed how temperatures rose and fell over time rather than exploring the onset of ice age transitions.
They discovered that every ice age over the past 900,000 years has occurred at a precise interaction between the tilt, wobble and shape of Earth's orbit.
'[This] confirms the natural climate change cycles we observe on Earth over tens of thousands of years are largely predictable and not random or chaotic,' said study co-author Lorraine Lisiecki, a professor at the University of California, Santa Barbara.
Without human interference, Earth's next glaciation would 'occur within the next 11,000 years, and it would end in 66,000 years' time,' according to Barker. But with carbon dioxide levels now at their highest in at least 800,000 years, that timeline has shifted dramatically.
The findings highlight the immense and long-lasting influence of human activity on the planet. While climate change is often measured in decades, this research underscores consequences that will play out over geological time scales.
Barker warned against interpreting the delay of an ice age as a positive outcome. While an ice age would bring challenging conditions for human civilisation, today's unchecked emissions are already causing devastating consequences, including rising sea levels, extreme weather and biodiversity loss.
Related
The Arctic tundra has transformed from carbon sink to carbon source, report finds
Black snow, emissions and bird flu: How Antarctic cruises hurt more than they help
With human activity now overriding the rhythms that have guided Earth's climate for millennia, the research team plans to explore how continued fossil fuel use will further reshape the planet's natural climate cycles. The study suggests it could be significant.
If carbon emissions continue at their current rate, Antarctica could be ice-free in 8,000 years, leading to a global sea-level rise of around 70 metres, they claim.
'Instead of there being glaciers, you'll be underwater,' Barker cautioned.

Orange background

Try Our AI Features

Explore what Daily8 AI can do for you:

Comments

No comments yet...

Related Articles

Woo! Science: The Worcester area holds clues to the Earth's distant past
Woo! Science: The Worcester area holds clues to the Earth's distant past

Yahoo

time7 hours ago

  • Yahoo

Woo! Science: The Worcester area holds clues to the Earth's distant past

Woo! Science is a column of science news and newsmakers in Worcester and the region. Got a science news idea? Email Margaret Smith at msmith@ So, dig. Literally. Maybe. As we go about our day, on the streets and roads of Worcester, all around us, the hills, the rivers, the valleys and even the earth under the pavement has a story to tell us. But exploration means taking good care, and respecting the land. Rocks, minerals, fossils and findings that took over a billion years to make can be completely messed up in a few minutes by humans running out the cosmic clock. As it happens, Worcester sits neatly in a veritable treasure of time, as far west as New York state, as far north as Maine, and dipping into the lower New England states. Marty Christiansen, collections management specialist at the EcoTarium science and nature museum, said, "Most of the stone under Worcester was born in the Mesoproterozoic Era." Eras are a way scientists classify significant time periods, The Mesoproterozoic Era, part of the Precambrian period, takes us back to a time of some of the earliest known, surviving geologic records. We're talking some 4.6 billion years ago, with the Mesoproterozoic Era going back to about 1.2 billion years. So, the time when Earth was starting to become the lovable planet that we call home. In these parts, Christiansen said, "We don't have many good fossils here, but it is some of the oldest surviving stone on the planet." Christiansen said, "The geology underneath Worcester was shaped by the continent collision that formed the Appalachian Mountain range. It's also a place of former mines for graphite, lead, coal and garnet, known in popular culture as a birthstone for January, and originating in silicate materials with colors ranging from orange to purple, and even colorless forms. And you can find delightful stones, minerals and other amazing things, some very particular to their own region. "In western Massachusetts, obviously, quartz, lots and lots of quartz around here," said Sara Furbush, president of the Worcester Mineral Club. The club hosts expeditions to look for geological wonders in the area, but also to cultivate interest in mineralogy, geology, paleontology, gemology, lapidary, jewelry making, and more. As for Worcester, Furbush said, "There are 31 minerals you can find in the Worcester area." Respect to that. Your basic rock comprises one or more minerals, while minerals are basically the building blocks of rocks, with an orderly internal structure and characteristic chemical composition, crystal form, such as quartz, feldspar, mica, amphibole, olivine, and calcite. Rocks are classified in three categories, and there are examples of all three throughout the region: igneous rocks, or rocks formed by volcanic activity, such as granite, pumice, and pegmatite, which Furbush said has been found throughout New England, with large crystals within; sedimentary rocks, which can even contain matter from dead plants, animal skeletons, along with sand and dirt, such as shale, and coal, literally a fossil fuel; metamorphic rocks, which start out as one type of rock, and changed through pressure and heat within the Earth, such as slate. One helpful tool for learning is a database created by the Virginia-based Hudson Institute of Mineralology. "You can basically look in any locality, or any town, and it will tell you minerals that have been found in the area," Furbush said. "In Worcester, there has been coal, graphite, silver. Now, whether you are going to find them nowadays or not is a different story." Calcite, fluorite, graphite, garnet and other minerals have turned up in the area, Furbush said. And then there is a rock crystal with a unique look, and story. Chiastolite bears a brown marking resembling a cross. It has been found in Lancaster's George Hill area, as well as in Sterling, Clinton and Boylston. They can appear as little bumps among boulders and rocks. But when a rock or mineral has a compelling look, it can draw many seekers on a quest. "We really know of one place, and that place is getting over dug-out, and overmined," said Furbush. So, how to strike a balance? Furbush said responsible rock and mineral clubs have guidelines and rules, among them: "Don't take everything, but take enough, as you may never return to this location," Furbush said. "You want to leave stuff for other people to find. If you dig holes, you fill it back in."Furbush said, "It's very 'take care of the land,' and whatnot. But people who don't know these things, they go, and it's creating chaos. Boulders that have been smashed to smithereens." As a cautionary tale, Furbush cited the example of the New England Forestry Foundation's Hartnett Manhan Memorial Forest in Easthampton, a town in Western Massachusetts. "It's public land. A river ran through it, and it was great, a great place to bring kids on a hot day." Nearby is the site of a former button factory, and buttons would turn up in the water. "You could find buttons. You could find really cool specimens. But people have been going there, and just destroying the place. There were holes dug everywhere. Trees were knocked down, cut down. The river beds were pushed back. And it got so bad that they closed it, and now it's gone for everyone." Christiansen evoked the traditional Girl Scout principle: "Leave only footprints. Do not disturb the area. Not to disturb the natural position of rocks, but instead, appreciate them without disturbing the area." What's special about the region's character is well worth protecting. "In a lot of New England, the glaciers scraped and passed over. A lot of our lakes were glacially formed." Along the way, glaciers not only carved the character of much of landscape; they picked up and dropped off gifts of the Earth's harvest that would delight humans eons later. Furbush said favorite finds include rodanite, a bright pink rock found in western Massachusetts. "And then you go up to Keene, New Hampshire, and you can find beautiful tourmalines ... go over to Rhode Island, and you are finding amethyst ... so, a very unique area." Christiansen said the area is also home to "glacial erratics," that is, objects and materials that started someplace else, but which were carried great distances by glaciers that had run over the tops of mountains. These include some boulders. "You get a lot of the big ones, that were dropped off with the glacier melt," said Christiansen. Places such as Purgatory Chasm and Millstone Hill, in Worcester's Green Hill Park, bear witness to the work of the glaciers. This article originally appeared on Telegram & Gazette: Woo! Science: In Worcester area, you're never too old to 'rock'

NASA's Mars rover proves these peculiar ridges have secrets to tell
NASA's Mars rover proves these peculiar ridges have secrets to tell

Yahoo

time12 hours ago

  • Yahoo

NASA's Mars rover proves these peculiar ridges have secrets to tell

NASA's Curiosity rover has started drilling into a bizarre landscape on Mars that could upend assumptions about when the Red Planet truly dried out. After a long drive, the Mini Cooper-sized robot reached a so-called boxwork region, where a gridlike pattern of ridges splays over six to 12 miles. For years, orbiters had observed this area from space but never up close. Scientists had hypothesized before the rover arrived that the peculiar ridges formed with the last trickles of water in the region before it dried out for good. But mineral veins discovered in the boxwork suggest groundwater stuck around longer than anyone expected. The bedrock between the ridges contains tiny white veins of calcium sulfate, a salty mineral left behind as groundwater seeps into rock cracks. Deposits of the material were plentiful in lower rock layers from an earlier Martian period. But no one thought they'd appear in the layer Curiosity is exploring now, which formed much later. "That's really surprising," said Curiosity's deputy project scientist, Abigail Fraeman, in a statement. "These calcium sulfate veins used to be everywhere, but they more or less disappeared as we climbed higher up Mount Sharp. The team is excited to figure out why they've returned now." SEE ALSO: Rubin Observatory's first images flaunt millions of galaxies. Take a look. Ancient Mars used to be wetter — flush with rivers, lakes, and maybe even oceans — but over billions of years, it turned into a dusty, cold desert. What's unclear is when that shift happened and how long conditions suitable for life might have lingered. Curiosity's new findings complicate what scientists thought they knew about the timeline. The rover has spent more than a decade in Gale Crater climbing Mount Sharp, reading the rock layers like pages in a planetary chronicle. The layer it's on now is chock-full of magnesium sulfates, salty minerals that typically form as water evaporates. That fits the narrative researchers had expected: This was supposed to be a chapter when Mars was well on its way to arid. That's why a new sample Curiosity drilled this month, dubbed Altadena, could be enlightening. As the rover analyzes the boxwork's composition, scientists may gain a better understanding of how it formed, what minerals are present, and whether any clues about ancient single-celled microorganisms might be hidden there. The rover will drill more ridges in the coming months to compare them and evaluate how groundwater may have changed over time. Bedrock between the boxwork ridges contains tiny white veins of calcium sulfate. Credit: NASA / JPL-Caltech / MSSS The mission's next targets lie farther into the boxwork region, where the patterns grow larger and more distinct. Curiosity will keep looking for organic molecules and other potential evidence of a habitable environment in Mars' ancient past. The rover team has begun nicknaming features after places near Bolivia's Salar de Uyuni, one of the driest, saltiest places on Earth. It's reminiscent of the Martian landscape Curiosity is sightseeing today. "Early Earth microbes could have survived in a similar environment," said Kirsten Siebach, a rover scientist based in Houston, in an earlier statement. "That makes this an exciting place to explore."

Obscure rock formation in Canada may contain the world's oldest minerals
Obscure rock formation in Canada may contain the world's oldest minerals

Yahoo

timea day ago

  • Yahoo

Obscure rock formation in Canada may contain the world's oldest minerals

When you buy through links on our articles, Future and its syndication partners may earn a commission. An obscure rock formation on the eastern shore of Canada's Hudson Bay may contain the oldest known rocks on Earth, a new study claims. The analysis dated the site's streaky gray rocks, part of an outcrop called the Nuvvuagittuq Greenstone Belt, to 4.16 billion years ago — meaning they're remnants from our 4.57 billion-year-old planet's earliest crust. The dating, performed by two methods that used the decay of radioactive isotopes (versions of elements) to measure the age of ancient magma trapped inside the rocks, significantly bolsters a controversial past study by the same scientists. If their findings, published June 26 in the journal Science, stand up, they could offer a unique window into our planet's ancient history and the geochemical stage where life emerged. "The volcanic rocks have to be at least 4.16 billion years old or older; I would argue that the best age for them is 4.3 billion years old," study co-author Jonathan O'Neil, a professor of environmental science at the University of Ottawa, told Live Science. "No known rocks are older." Earth began as a ball of red-hot lava. It slowly cooled over its first 600 million years, known as the Hadean eon, when pockets of solid rock started to form. This was a tumultuous time for our young planet, which was repeatedly pummeled by asteroids and even sustained a cataclysmic blow from the protoplanet Theia, which tore off a chunk of Earth to form our moon. Related: Did plate tectonics give rise to life? Groundbreaking new research could crack Earth's deepest mystery Then, as early as 3.8 billion years ago, Earth's surface splintered into tectonic plates, which dived beneath each other to be recycled into Earth's interior or to build up vast mountain ranges or trenches. This subduction means that many of the rocks on our planet's surface have long been chemically altered by intense heat and pressure. Yet some regions are far enough from tectonic plate boundaries to contain rocks that have remained unchanged for billions of years. One of these is in northeastern Canada, and its most ancient part is the Nuvvuagittuq Greenstone Belt (NGB). Scientists agree that this outcrop is at least 3.8 billion years old. Then, in 2008, O'Neil and his colleagues published a study suggesting that the NGB was 4.3 billion years old — which would mean it contained the oldest rocks in the world. But other geologists objected, suggesting there were flaws in the researchers' methods. Old rocks are typically dated using a mineral called zircon, which is chemically stable over billions of years. The volcanic rocks in the NGB, however, don't contain zircon, which forced the scientists to measure the rocks' age by the decay of the element samarium into neodymium. Yet trouble lurked within this new method. Samarium can decay into neodymium through two pathways (samarium-146 into neodymium-142, or samarium-147 into neodymium-143), creating two isotopic clocks with different decay speeds. The first decay path leads to a half-life — the period of time required for half the original element to remain — of about 96 million years, while the second pathway has a half-life spanning trillions of years. This means that the two decay pathways produced wildly different estimates for the ages of the rocks. This is because with the longer-lived clock ticking to the present day, it is especially susceptible to tectonic events muddling its isotopes part way through the decay process. "Any 'cooking' of the rocks or metamorphism after 4 billion years ago won't really affect that short-lived clock but can reset the long-lived clock and cause the age difference between these two systems," O'Neil said. RELATED STORIES —Hidden 36 million-year-long cycles may fuel biodiversity on Earth, ancient rocks reveal —Zealandia, Earth's hidden continent, was torn from supercontinent Gondwana in flood of fire 100 million years ago —Is Africa splitting in two? To sidestep this issue, the team went back to the formations to search for sections where magma from Earth's mantle, or middle layer, intruded into the planet's primordial crust. Because these intrusions had to be younger than the rock they seeped into, they could be used as a minimum age. The new analysis revealed that within these sections of the NGB, both samarium to neodymium decays offered the same age: 4.16 billion years. If further research does confirm that the rocks are as old as O'Neil's team believes, they could offer vital insight into how life emerged on our planet and potentially beyond it. "Some rocks from the Nuvvuagittuq Greenstone Belt were formed by precipitation from seawater, and these can help understand the composition of our first oceans, their temperature, perhaps the atmosphere and also could host the oldest traces of life on Earth," O'Neil said. "Understanding the environment where life could have started on our planet also helps in our quest to find traces of life elsewhere, such as Mars.'

DOWNLOAD THE APP

Get Started Now: Download the App

Ready to dive into a world of global content with local flavor? Download Daily8 app today from your preferred app store and start exploring.
app-storeplay-store