A study of the Lancang River basin found that silicate weathering rates decrease with increasing erosion, while carbonate and sulfide oxidation rates increase. The study suggests that lithology, suspended sediment weathering, and groundwater input control chemical weathering and its carbon effect in large river basins.
Scientists propose a colossal cliff across ancient North America may have exposed Grand Canyon's oldest rocks nearly a billion years before it was carved by the Colorado River. The study suggests the 'great escarpment' of steep rocky cliffs formed when the supercontinent Rodinia broke apart 800 million years ago.
Researchers analysed stone blocks and bricks from the Dutch East India Company's ship Batavia, revealing the materials came from at least two different quarry areas in what is now Germany. The study used advanced geochemical techniques to trace the origin of the cargo, uncovering hidden details about global trade routes.
A research team found that enhanced silicate weathering contributed to CO2 drawdown and the onset of the Late Paleozoic Ice Age, reducing atmospheric CO2 levels by approximately 800 ppm. This process also boosted marine nutrient supply and productivity, leading to the observed shifts in carbon isotopes.
Researchers found a surprising correlation between West Antarctic Ice Sheet retreat and marine algae growth over the past 500,000 years. The study suggests that global warming may lead to reduced CO2 uptake if the ice sheet continues to shrink.
Researchers find ocean sediment supply crucial for salt marshes to keep pace with rising seas. Southern New England marshes are showing signs of stress due to declining coastal sediment supply.
A new study found that land and ocean weathering processes are linked, influencing the amount of carbon stored or released into the atmosphere. The research proposes a continuum approach to studying weathering reactions on both land and in the ocean.
A new Stanford study suggests that unvegetated meandering rivers can leave sedimentary deposits similar to those of braided rivers, rewriting the story of plants and rivers' relationship with Earth. This finding has implications for understanding Earth's ancient and future climate, including carbon storage in floodplains.
An international team of earth scientists proposes a new framework to understand the factors influencing CO2 removal, revealing their complex interactions and potential for enhanced weathering techniques. This integrated approach aims to enhance natural carbon storage, helping achieve Paris Agreement targets.
Researchers at Göttingen University developed a method to reconstruct the early Earth's atmosphere using fossilized micrometeorites. The study found that intact micrometeorites can preserve reliable traces of oxygen isotopes over millions of years.
A large region of unusually hot rock deep beneath the Appalachian Mountains in the United States could be linked to Greenland and North America splitting apart 80 million years ago. The 'mantle wave' theory suggests that hot, dense rock slowly peels away from the base of tectonic plates after continents break apart.
A new study revisits forecasts made in 2002 about the world's rocky shorelines, finding some threats have materialized while others have not. The researchers highlight the importance of addressing issues like ocean acidification and plastic pollution to protect coastlines.
Researchers have found extensive, previously unmapped flat surfaces beneath a 3,500 km stretch of the East Antarctic coastline, which were formed by large rivers after East Antarctica and Australia broke apart. These surfaces may currently be regulating the rate of ice loss from the East Antarctic Ice Sheet.
Stanford researchers have developed a practical and low-cost method to remove atmospheric carbon dioxide from the air using common minerals. The new process, known as enhanced weathering, uses heat to transform silicates into materials that capture and store CO2, offering a potentially scalable solution to mitigate global warming.
A research team from the University of Göttingen investigated the influence of the Zagros Mountains on Earth's surface bending. They found that the Neotethys oceanic plate is breaking off horizontally, creating a depression in the region.
A new Stanford review of hundreds of studies found little to no sediment dating back to the 34 million-year-old Eocene-Oligocene climate transition, contradicting conventional models. The researchers attribute this globally extensive gap in the geologic record to vigorous ocean bottom currents triggered by major climate shifts.
Researchers found that rising temperatures accelerate weathering of rocks in the Canadian Arctic, leading to increased CO2 release and a positive feedback loop. This process could contribute significantly to climate change, with predicted emissions doubling by 2100 under moderate emission scenarios.
A study reveals a global unconformity, or gap in the rock record, around the edges of every continent at the time of the greenhouse-to-icehouse climatic transition. The finding challenges traditional ideas about sediment movement and accumulation in deep oceans.
A new study suggests that using special fertilizers and crushed basalt rocks can reduce agricultural nitrous oxide emissions without harming the ozone layer. The research found a 25% reduction in N2O emissions, aligning with efforts to reach net-zero emissions while supporting increased food production.
A new study finds that mountains can switch from being a sink of carbon dioxide to a source as their erosion rate increases. The optimal erosion rate for maximizing carbon dioxide removal through mineral weathering is approximately 0.1 millimeter per year.
Research reveals that low-relief mountain ranges with moderate erosion rates have the highest CO2 capture through silicate weathering. In contrast, high-eroded regions release more CO2 due to faster carbonate and sulfide weathering. These findings suggest a complex relationship between erosion rates and the carbon cycle.
Researchers found that historically low volcanic carbon dioxide emissions, combined with weathering of a large pile of volcanic rocks in Canada, led to the prolonged Sturtian glaciation. The team used plate tectonic modeling and computer simulations to investigate the cause and duration of this ice age.
A clay mineral called smectite, formed through plate tectonics, efficiently traps organic carbon and could help buffer global warming. Smectite's accordion-textured folds effectively trap dead organisms, preventing them from being consumed by microbes.
Researchers use rhenium as a proxy for carbon to quantify the rate of fossil carbon dioxide release into the atmosphere. The study found that high rates of carbon breakdown persist from mountaintop to floodplain, offering valuable insights into the planet's history and response to climate challenges.
A new study led by University of Maryland Professor Sujay Kaushal reveals that human activities are making the planet's air, soil, and freshwater increasingly salty. This acceleration of the natural salt cycle poses an 'existential threat' to ecosystems and human health if current trends continue.
Researchers at UC Davis and Cornell University found that crushed rock can store carbon dioxide in soils for short time scales, equivalent to taking 350,000 cars off the road every year. The study tested this technology in a dry climate and showed promising results, suggesting a new way to verify carbon removal via enhanced weathering.
A new study by the University of Oxford found that ancient carbon in rocks can release significant amounts of CO2 into the atmosphere, rivaling volcanic emissions. This discovery challenges current understanding of the natural carbon cycle and has important implications for climate change modeling.
Researchers discovered that blending crushed rock with arable soil could help reduce global temperatures. The process, known as enhanced chemical weathering, works by releasing calcium and magnesium from rocks, which bind atmospheric carbon dioxide and prevent its release back into the atmosphere.
A new study quantifies the climate benefits of enhanced weathering, applying ground-up silicate rock to Midwestern farm fields to capture significant amounts of carbon dioxide. The method reduced net carbon loss to the atmosphere by 42% in maize plots and more than doubled carbon storage in miscanthus plots.
A new study suggests that applying crushed volcanic rocks to agricultural fields can draw down 217 gigatons of carbon dioxide, meeting the lower end of the IPCC's 2100 target. The method, called enhanced rock weathering, is more efficient in hot and wet tropical regions and works well in warmer temperatures.
Scientists at the UK Centre for Ecology & Hydrology are trialling crushed rock dust to remove large amounts of carbon dioxide from the atmosphere. The Enhanced Rock Weathering project has the potential to boost crop yield while reducing greenhouse gas emissions.
Research finds that flash droughts are becoming more frequent due to human-caused climate change, posing a major challenge for climate adaptation. The transition to flash droughts is predicted to accelerate in a warmer future, with irreversible impacts on ecosystems.
A model shows enhanced rock weathering will only leak minimal carbon if its products are stored in the ocean. The technique may help constrain global warming below 1.5ºC or 2ºC by century's end.
Researchers found that Greenlandic glacial rock flour can capture large amounts of CO2 through enhanced weathering, improving crop yields by up to 24% in Danish fields. The fine powder also acts as a natural fertilizer, providing a wider array of nutrients than commercial organic fertilizers.
A research team uncovered a specific kill mechanism responsible for several biotic disruptions during the late Devonian Period. The discovery linked sea level changes, climate fluctuations, and ocean chemistry to mass extinctions, with implications for today's oceans affected by global warming.
A new study led by Penn State scientists sheds light on the temperature sensitivity of silicate rock weathering, a process that helps control Earth's climate. The research combines laboratory measurements and soil analysis to create a global estimate for how weathering responds to temperature changes.
A new method reveals that small vascular plants, not trees, played a greater role in reducing atmospheric CO2 levels. The study suggests that weathering, a process that involves the breakdown of minerals, is a more effective way to remove CO2 from the atmosphere.
Scientists have confirmed the existence of a 'stabilizing feedback' mechanism that regulates Earth's temperature over hundreds of thousands of years. Silicate weathering is believed to be the likely cause, drawing carbon dioxide out of the atmosphere and into ocean sediments.
Researchers found that the return of radiolarians, a tiny marine organism, helped restore habitable conditions after the massive extinction event. The study suggests that every microorganism plays a vital role in regulating biogeochemical cycles and conservation of the planet.
Researchers at TU Wien found that silicate nanoparticles can strengthen porous rock by forming colloidal crystals, which create new connections between mineral surfaces. The size of the particles is crucial for optimal strength gain, with smaller particles creating more binding sites.
Friedhelm von Blanckenburg's project DEVENDRA explores the weathering of basalt and carbonate rocks, measuring their transformation into soil and subsequent erosion. The goal is to establish a novel method for calibrating the laws governing weathering and CO2 drawdown.
Researchers at UBC Okanagan have adapted a plastination technique to strengthen bamboo and reduce its degradation rate, making it more environmentally friendly. The innovation has the potential to significantly reduce non-degradable waste in industries such as construction and packaging.
Researchers detected 43 trillion miniature plastic particles in Switzerland every year, with estimates suggesting up to 3,000 tonnes of nanoplastics covering the country annually. The study reveals that nanoplastics originate primarily from urban areas and global emissions, posing potential health risks when inhaled.
A recent study analyzing air bubbles preserved in Antarctic ice for up to 1.5 million years suggests that glacial erosion is likely responsible for the decline of atmospheric oxygen levels over the past 800,000 years.
Research finds climate stabilized due to increased rock weathering and erosion, which converts CO2 into insoluble carbonate; this process took 20,000-50,000 years. Lithium isotope analysis supports theory, showing increased weathering and erosion during Paleocene-Eocene Thermal Maximum.
A new study reveals that Earth's natural habitats can remove significant amounts of carbon dioxide due to previously undiscovered rock nitrogen weathering reactions. Preserving these ecosystems is vital to conserve the planet's carbon sink service and combat climate change.
Researchers found that lake breach floods played a crucial role in shaping the Martian surface, creating river valleys with nearly a quarter of the Red Planet's total volume. The study's findings suggest that these floods had a lasting impact on the surrounding landscape, influencing the formation of other nearby river valleys.
Researchers from the University of Hong Kong propose that sedimentary rocks measured by Curiosity rover represent sand and silt deposited by air-fall and reworked by wind. The discovery suggests a reducing atmosphere on ancient Mars with conditions similar to those found in modern-day deserts.
Researchers explore the potential of using finely ground rock to remove CO2 from the atmosphere, finding substantial CO2 removal rates of up to 2.5 gigaton per year. Basalt powder is found to have high weatherability and can enhance soil fertility, leading to increased ecosystem carbon storage.
A team at the Natural History Museum is testing spectral instruments for the ExoMars rover to identify meteorites on Mars. The rover's success rate is significantly higher than dedicated meteorite hunts on Earth, with one meteorite found per kilometre travelled.
The study estimates global plastic emissions range from 9 to 23 million metric tons per year, with similar amounts emitted onto land yearly. Remote environments are particularly under threat as plastic debris cannot be removed by cleanups, leading to unpredictable effects on ecosystems.
Researchers studied sediment scour and bedrock erosion in waterfall plunge pools, finding mass balance controls on these processes. Climate change was also explored during the end-Permian extinction, with a focus on the impact of chemical weathering and land surface temperature.
A new study found that rock weathering and water storage follow similar patterns across hill slopes, improving wildfire and landslide risk predictions. The findings also suggest that computer models can use this scaling trend to model weathering in undulating terrain.
A study in Taiwan found that mountain growth influences the greenhouse effect, with high erosion rates releasing more CO2 than sequestering it. Low erosion rates, on the other hand, lead to greater CO2 sequestration due to weathering processes that bind carbon dioxide.
Researchers reconstructed chemical weathering history in the western Himalaya using sediment records since 17 million years ago. In California, a study analyzed late Pleistocene rock uplift and faulting rates along the boundary between the southern Coast Ranges and western Transverse Ranges.
A new study published in Frontiers in Marine Science demonstrates that oil in the ocean can undergo photooxidation, a process that breaks down crude oil into persistent compounds. This process occurs within hours to days and reduces the effectiveness of chemical dispersants used to clean up spills.
Researchers found that weathering rates and atmospheric composition are crucial for a planet's habitability. Geochemistry plays a key role in determining the balance between radiation and liquid water, with extreme temperatures potentially altering this balance.
A recent study led by University of Arkansas geologist Jill A. Marshall found that cold temperatures during North America's last ice age shaped landscapes well beyond the reach of glaciers, affecting areas from Oregon to Georgia and as far south as Texas and Arkansas. The research suggests past cold climates have had a significant impa...
Researchers have identified evidence of tropical cyclone impacts on Earth's surface, while new modeling reveals the optimal structural context for giant porphyry copper deposits. The study utilizes apatite fission-track thermochronology to constrain the episodic cooling and exhumation history of the Catskill Mountains in New York State.
A study by the University of Wyoming reveals that climate and erosion rates significantly impact the relative importance of physical and chemical weathering in rock breakdown. Anisovolumetric weathering, a previously underrecognized process, is now recognized as a common occurrence, influenced by environmental conditions.