Microsoft’s carbon removal plans aren’t dead after all | TechCrunch
Microsoft is purchasing 650,000 metric tons of carbon removal credits from startup BioCirc, the company said today.
As carbon removal deals go, it’s not a big buy. But this one is notable because last month, two reports said the tech giant was pausing its carbon removal deals. BioCirc confirmed for TechCrunch that the purchase agreement was signed in May, weeks after Microsoft reportedly paused new deals.
For the carbon removal industry — and the startups that depend on it — there’s a big difference between a pause and a recalibration. Microsoft is reportedly responsible for more than 90% of the carbon removal credit market, meaning its purchasing decisions alone can determine whether young companies in the space survive.
Microsoft repeatedly denied that it had paused its carbon removal purchases. “Our carbon removal program has not ended,” Melanie Nakagawa, chief sustainability officer at Microsoft, told TechCrunch in a statement. “At times we may adjust the pace or volume of our carbon removal procurement as we continue to refine our approach toward sustainability goals.”
The new deal generates carbon removal credits from five BioCirc biogas projects. The biogas plants take biomass waste — frequently from agriculture — and use industrial bioreactors to turn it into methane and carbon dioxide. BioCirc captures the carbon dioxide and stores it in an underground reservoir offshore. The methane is then burned in a power plant.
Microsoft’s sustainability goals have been strained by the company’s push into AI. To power its data centers in Texas, Microsoft last month said it was working with Chevron and Engine No. 1 to build a natural gas power plant in the state that could eventually generate 5 gigawatts of electricity. Emissions from that project alone promise to dwarf the deal with BioCirc.
Internally, Microsoft employees have also been debating whether to abandon the company’s goal of matching zero emissions electricity with its energy use on an hourly basis. Today, the company matches on an annual basis. That approach gives the company more flexibility to, say, use more natural gas to power its data centers at night, but it also makes the company’s clean energy claims harder to verify.
If Microsoft continues to pursue fossil fuel power plants, it’ll need to ramp up its carbon removal purchases to meet its 2030 target of becoming a carbon negative company (one that removes more greenhouse gases from the atmosphere than it generates).
Last year, Microsoft signed several deals worth millions of tons of carbon removal credits. The program’s reported pause set off alarm bells throughout the carbon removal industry, which is still in its infancy.
The new deal suggests that Microsoft is, in fact, recalibrating its carbon removal program — not abandoning it. Whether that remains true as AI drives its energy consumption higher is something the industry will be watching.
Microsoft is purchasing 650,000 metric tons of carbon removal credits from startup BioCirc, the company said today.
As carbon removal deals go, it’s not a big buy. But this one is notable because last month, two reports said the tech giant was pausing its carbon removal deals. BioCirc confirmed for TechCrunch that the purchase agreement was signed in May, weeks after Microsoft reportedly paused new deals.
For the carbon removal industry — and the startups that depend on it — there’s a big difference between a pause and a recalibration. Microsoft is reportedly responsible for more than 90% of the carbon removal credit market, meaning its purchasing decisions alone can determine whether young companies in the space survive.
Microsoft repeatedly denied that it had paused its carbon removal purchases. “Our carbon removal program has not ended,” Melanie Nakagawa, chief sustainability officer at Microsoft, told TechCrunch in a statement. “At times we may adjust the pace or volume of our carbon removal procurement as we continue to refine our approach toward sustainability goals.”
The new deal generates carbon removal credits from five BioCirc biogas projects. The biogas plants take biomass waste — frequently from agriculture — and use industrial bioreactors to turn it into methane and carbon dioxide. BioCirc captures the carbon dioxide and stores it in an underground reservoir offshore. The methane is then burned in a power plant.
Microsoft’s sustainability goals have been strained by the company’s push into AI. To power its data centers in Texas, Microsoft last month said it was working with Chevron and Engine No. 1 to build a natural gas power plant in the state that could eventually generate 5 gigawatts of electricity. Emissions from that project alone promise to dwarf the deal with BioCirc.
Internally, Microsoft employees have also been debating whether to abandon the company’s goal of matching zero emissions electricity with its energy use on an hourly basis. Today, the company matches on an annual basis. That approach gives the company more flexibility to, say, use more natural gas to power its data centers at night, but it also makes the company’s clean energy claims harder to verify.
If Microsoft continues to pursue fossil fuel power plants, it’ll need to ramp up its carbon removal purchases to meet its 2030 target of becoming a carbon negative company (one that removes more greenhouse gases from the atmosphere than it generates).
Last year, Microsoft signed several deals worth millions of tons of carbon removal credits. The program’s reported pause set off alarm bells throughout the carbon removal industry, which is still in its infancy.
The new deal suggests that Microsoft is, in fact, recalibrating its carbon removal program — not abandoning it. Whether that remains true as AI drives its energy consumption higher is something the industry will be watching.
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#Microsofts #carbon #removal #plans #arent #dead #TechCrunchMicrosoft,biogas,Exclusive,carbon credits,carbon removal




![Scientists Found a Continent-Sized Geological Structure Hiding Beneath Antarctica
The East Antarctic Ice Sheet is almost unfathomably huge. Covering about 75% of the entire frigid continent (nearly everything on its side of the Transantarctic Mountains), the sheet covers about 3.9 million square miles (10.2 million square kilometers) and extends down 1.4 miles (2.2 km), on average, before coming into contact with Earth’s surface. At its deepest, the ice plunges down over 3 miles (4.9 km). For decades, scientists assumed that this literally continent-sized block of ice rested on an expansive and stable chunk of Earth’s crust known as a craton. A team of researchers has now complicated that picture—mapping a vast, interconnected geological structure that fans out from a troubling “tectonic deformation.” Beneath this ice sheet, thinner and more geologically recent slices of crusty lithosphere fan out into hidden valleys called “pull-apart basins.” These basins—30 elongated wedge-shaped valleys in total—constitute an entirely new, continental-scale geological region underneath Antarctica, in fact, one which the researchers have named the East Antarctic Fan-Shaped Basin Province (EAFBP). But it’s how they likely formed that has now caught researchers’ attention.
To put it bluntly, it turns out that about 90% of the planet’s fresh water ice may not be on solid ground. Geologist John Goodge called the team’s findings “provocative” in an independent commentary on the new study, published Thursday in the journal Nature Geoscience.
“East Antarctica is typically considered from seismic tomography and geodetics to be ancient and generally stable,” according to Goodge, who studies continental tectonics with the nonprofit Planetary Science Institute. “[But] something else is going on at depth.” Continental divides Goodge speculates that this seemingly “coherent pull-apart system,” as presented in the new study, might help explain a variety of mysterious heat and water flows beneath this ice sheet’s surface, like that enormous subglacial lake identified in 2016 or some of the hundreds more like it.
The study’s authors, led by geophysicist Egidio Armadillo at the University of Genoa in Italy, agreed: “Because these basins underlie about half of the East Antarctic Ice Sheet, they are likely to heavily influence both ice-flow and landscape evolution,” the researchers wrote in their study, also published Thursday in Nature Geoscience. Armadillo’s team, coordinating across Europe and the U.K., developed their new understanding of Antarctica’s hidden bedrock via an exhaustive set of sensory data. Gravitational and magnetic anomalies were mapped via low-altitude airborne surveys. Ground surface features were mapped with seismic tools, using sound waves that vibrate through the ice and ping back information about subglacial landscapes in 3D. The grey, magenta, and cyan lines represent the apparent new fault lines discovered. Credit: Nature Geoscience All of this data—the fruits of “multi-national efforts to image within and below the ice sheet,” as Goodge put it—had already revealed that regions of the continent were “undergoing more rapid movement and ice-mass loss than previously recognized.” Armadillo’s team merely helped to explain why.
The mechanism Armadillo and his colleagues proposed for the formation of these fan-shaped basins is called “distributed rotational extension.” It involves points called Euler poles around which tectonic plates pivot or rotate rather than smash into each other or pull apart. The result is a bit like decks of cards being spread out on a table, thinning out the stack of Earth’s crust as it moves. An icy situation Goodge took pains to spell out the basins’ implications for melting Antarctic ice due to climate change and the risk of rising global sea levels.
The mere existence of these basins, he wrote, “could introduce widespread, systemic instability to the East Antarctic Ice Sheet” via thinner layers of Earth’s crust and more heat flow from below. On top of that, a series of fault-line “troughs” documented between the basins appear “tailor-made to promote outward flow of ice streams from the interior” into the world’s oceans, he said. That said, the team’s findings are unlikely to end this debate. As Goodge noted, Antarctica is “the last continental frontier of scientific exploration.” It’s still a very mysterious place, one that’s challenging to study given its inhospitable temperatures and extreme geography. Its “cryptic subglacial geology” might stay that way for a while. #Scientists #ContinentSized #Geological #Structure #Hiding #Beneath #AntarcticaAntarctica,Geology,mapping,Plate tectonics Scientists Found a Continent-Sized Geological Structure Hiding Beneath Antarctica
The East Antarctic Ice Sheet is almost unfathomably huge. Covering about 75% of the entire frigid continent (nearly everything on its side of the Transantarctic Mountains), the sheet covers about 3.9 million square miles (10.2 million square kilometers) and extends down 1.4 miles (2.2 km), on average, before coming into contact with Earth’s surface. At its deepest, the ice plunges down over 3 miles (4.9 km). For decades, scientists assumed that this literally continent-sized block of ice rested on an expansive and stable chunk of Earth’s crust known as a craton. A team of researchers has now complicated that picture—mapping a vast, interconnected geological structure that fans out from a troubling “tectonic deformation.” Beneath this ice sheet, thinner and more geologically recent slices of crusty lithosphere fan out into hidden valleys called “pull-apart basins.” These basins—30 elongated wedge-shaped valleys in total—constitute an entirely new, continental-scale geological region underneath Antarctica, in fact, one which the researchers have named the East Antarctic Fan-Shaped Basin Province (EAFBP). But it’s how they likely formed that has now caught researchers’ attention.
To put it bluntly, it turns out that about 90% of the planet’s fresh water ice may not be on solid ground. Geologist John Goodge called the team’s findings “provocative” in an independent commentary on the new study, published Thursday in the journal Nature Geoscience.
“East Antarctica is typically considered from seismic tomography and geodetics to be ancient and generally stable,” according to Goodge, who studies continental tectonics with the nonprofit Planetary Science Institute. “[But] something else is going on at depth.” Continental divides Goodge speculates that this seemingly “coherent pull-apart system,” as presented in the new study, might help explain a variety of mysterious heat and water flows beneath this ice sheet’s surface, like that enormous subglacial lake identified in 2016 or some of the hundreds more like it.
The study’s authors, led by geophysicist Egidio Armadillo at the University of Genoa in Italy, agreed: “Because these basins underlie about half of the East Antarctic Ice Sheet, they are likely to heavily influence both ice-flow and landscape evolution,” the researchers wrote in their study, also published Thursday in Nature Geoscience. Armadillo’s team, coordinating across Europe and the U.K., developed their new understanding of Antarctica’s hidden bedrock via an exhaustive set of sensory data. Gravitational and magnetic anomalies were mapped via low-altitude airborne surveys. Ground surface features were mapped with seismic tools, using sound waves that vibrate through the ice and ping back information about subglacial landscapes in 3D. The grey, magenta, and cyan lines represent the apparent new fault lines discovered. Credit: Nature Geoscience All of this data—the fruits of “multi-national efforts to image within and below the ice sheet,” as Goodge put it—had already revealed that regions of the continent were “undergoing more rapid movement and ice-mass loss than previously recognized.” Armadillo’s team merely helped to explain why.
The mechanism Armadillo and his colleagues proposed for the formation of these fan-shaped basins is called “distributed rotational extension.” It involves points called Euler poles around which tectonic plates pivot or rotate rather than smash into each other or pull apart. The result is a bit like decks of cards being spread out on a table, thinning out the stack of Earth’s crust as it moves. An icy situation Goodge took pains to spell out the basins’ implications for melting Antarctic ice due to climate change and the risk of rising global sea levels.
The mere existence of these basins, he wrote, “could introduce widespread, systemic instability to the East Antarctic Ice Sheet” via thinner layers of Earth’s crust and more heat flow from below. On top of that, a series of fault-line “troughs” documented between the basins appear “tailor-made to promote outward flow of ice streams from the interior” into the world’s oceans, he said. That said, the team’s findings are unlikely to end this debate. As Goodge noted, Antarctica is “the last continental frontier of scientific exploration.” It’s still a very mysterious place, one that’s challenging to study given its inhospitable temperatures and extreme geography. Its “cryptic subglacial geology” might stay that way for a while. #Scientists #ContinentSized #Geological #Structure #Hiding #Beneath #AntarcticaAntarctica,Geology,mapping,Plate tectonics](https://gizmodo.com/app/uploads/2026/06/East-Antarctic-Fan-shaped-Basin-Province.jpeg)
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