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Plastic bag bans seem to work, at least when it comes to shoreline pollution

Plastic bag bans seem to work, at least when it comes to shoreline pollution

Researchers find that nationwide policies to ban plastic bags may be paying off, with fewer showing up during coastal cleanups.
Ever since their invention in 1959, plastic bags have become synonymous with shopping. For many people, it's difficult to imagine a quick grocery run without the crinkle of a plastic bag, and even harder to believe that using an alternative could make a meaningful difference in reducing plastic pollution — but a new national study suggests that, in many places, it already has.
A 2021 global survey found that plastic bags accounted for 14% of 12 million marine litter items gathered during beach cleanups — making them by far the most common type of trash in the study. They're lightweight, rarely recycled, and easily caught and transported by winds, making them especially likely to end up in waterways, where they can persist for decades. This combination of durability and disposability has made plastic bags one of the most stubborn contributors to environmental pollution, particularly along coastlines.
However, a growing body of evidence suggests that instituting regulations on plastic bag usage — where California has long been a national leader — has had a real effect on how often such waste shows up on and near beaches.
In a study published Thursday in Science, researchers Anna Papp of Columbia University and Kimberly Oremus of the University of Delaware found that local and state plastic bag policies enacted from 2016 to 2023, including bans and fees, reduced by as much as 47% the share of waste consisting of plastic bags that is collected during shoreline cleanups. (California's state-wide rules requiring a $0.10 charge of reusable bags was passed in 2014, and went into effect two years later — though industry watchers largely say while the law was well-intended, its implementation has been ineffective.)
The findings offer clear evidence that legislation can be used to curb plastic pollution — a growing concern as global waste generation is projected to more than triple by the end of the century . As of 2025, more than 100 countries have enacted national or local regulations on plastic bags, and 175 nations are negotiating what could become the world's first legally binding United Nations treaty to end plastics pollution, so such data may prove essential in determining what environmental policy strategies actually work.
In the study, researchers analyzed information from more than 45,000 beach cleanups conducted between January 2016 and December 2023 that is in a database maintained by the Ocean Conservancy, an environmental advocacy nonprofit. The researchers then cross-referenced the data with 182 local bag policies enacted over the same time period in ZIP Codes that had shoreline cleanups, and then applied a series of statistical methods to isolate the effects of these policies.
They found that plastic-bag litter dropped significantly in areas with bag laws, even as the national share of plastic bags found during cleanups increased to 6.7% in 2023 from 4.5% in 2016. No similar decline was observed for other types of plastic litter, including plastic straws, bottles, caps and containers, suggesting that the effects were specific to the target policies and not coincidental due to general trends in plastic usages.
Perhaps even more striking, the study found evidence suggesting that the structure of a given bag policy — whether it imposes a full ban, partial ban or a fee — played a crucial role in how much plastic waste it actually reduced.
Full bans prohibit all single-use plastic bags at checkout, while partial bans primarily target thin, single-use plastic bags, often allowing for thicker plastic bags to remain in circulation as so-called reusables. Fees, meanwhile, charge customers a small amount for each bag they take at checkout.
Although the study found that there were relative decreases in plastic litter as a result of both bans and fees, the magnitude of the decrease was larger for fee-based policies compared with full bans and especially partial bans, which were least effective. This suggests that how a policy is designed may matter as much as whether it exists at all — a key insight for lawmakers hoping to craft effective environmental legislation.
California's history of efforts to curb plastic waste serve as a prime example of this finding. With the passing of Senate Bill 270 in 2014, which barred the use of single-use plastic shopping bags in many retail settings, California became the first U.S. state to enact a plastic bag ban. Although this ban initially reduced plastic bag litter, it only prohibited the use of bags thinner than 2.25 millimeters, permitting grocery stores and large retailers to charge for thicker plastic bags and ultimately leading to an unexpected jump in plastic bag waste. This is reflected by California's 2021 Disposal Facility-Based Waste Characterization study , overseen by CalRecycle, which reported that plastic bag waste rose to 231,072 tons in 2021 from 157,385 tons in 2014 — a nearly 47% increase.
'It was a nasty loophole,' said Meredith McCarthy, the senior director of community outreach and partnerships at Heal the Bay, a Santa Monica-based nonprofit that organizes coastal cleanups and advocates for plastic reduction policies. 'I think a lot of people were thinking: 'Wait, we banned it? And now we use more? How is that possible?''
Even so, McCarthy, who's spent 20 years monitoring trends in plastic pollution on Los Angeles beaches, said that even this imperfect policy has helped implement a noticeable change. 'It's almost rare now to find a plastic bag,' McCarthy said.
The study also found evidence that plastic bag laws may reduce harm to marine life: in areas with bag policies, there was a 30% to 37% reduction in entangled animals relative to areas without such laws. Although the researchers caution that these findings are imprecise, in part because of the fact that we don't fully understand how wildlife interacts with plastic bags compared with other shoreline litter, the results do point to a potential environmental benefit of regulating single-use plastics.
In September, Gov. Gavin Newsom signed Senate Bill 1053 , banning all single-use plastic bags statewide. In theory, starting Jan. 1, 2026, such bags will disappear entirely from checkout lines altogether — meaning customers in California will need to use a reusable bag, pay for a paper bag, or hand carry their purchase.
California's new ban won't solve the plastic problem overnight, but this research shows that the right kind of policy — one with stricter laws and fewer loopholes — can make a measurable difference. Want proof? Just head to your nearest beach.

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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

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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

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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

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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.'

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