Carbon cycling in wet soils
Research found that dynamic waterlogging enhances carbon dioxide emissions and depletes soil organic carbon. Microbes exhibit higher activity under fluctuating conditions, but not necessarily greater diversity.
Articles tagged with Soil Carbon
Research found that dynamic waterlogging enhances carbon dioxide emissions and depletes soil organic carbon. Microbes exhibit higher activity under fluctuating conditions, but not necessarily greater diversity.
A Colorado State University-led study found that afforestation may not be as effective at removing excess carbon dioxide from the atmosphere as previously thought. The research suggests that ratios of soil organic carbon underneath afforested areas vary greatly across different ecosystems and climates.
A University of Michigan study found that organic carbon in thawing permafrost soils can be converted to carbon dioxide by sunlight, known as photomineralization. This process could contribute an additional 14% of carbon dioxide into the atmosphere, increasing global warming by 0.3-0.4°C.
Research highlights the importance of soil biodiversity in achieving sustainability goals, including nutrient cycling, food production, and pollution remediation. Soil health is crucial for regulating climate and supporting human well-being, with traditional agricultural practices already leveraging its benefits.
New research reveals consistent patterns in permafrost soils across Alaska's North Slope, allowing scientists to predict how carbon and greenhouse gases are released. The findings will help improve climate models by providing direct permafrost soil information, filling a knowledge gap that has been around for 30 years.
Shinshu University researchers have developed a new method to capture carbon via root exudates in wild forests. The method, which is quick and gentle on fine-scale roots, detects and measures the organic compounds released from tree roots into the soil.
Researchers will gather new data on pyrogenic carbon and investigate its behavior in tropical savannahs, including the impact of soil depth and fire frequency. The study aims to update models and provide better forecasts of carbon cycle dynamics, informing land management and climate change policies.
A new study suggests that increased rainfall in tropical regions will enhance soil respiration and decrease soil carbon stocks, leading to further intensification of global warming. This process could release significant amounts of CO2 into the atmosphere, exacerbating climate change.
Soil microorganisms decompose organic nitrogen, releasing inorganic nitrogen for plant growth. The initial burst of microbial activity after CO2 flush is a key indicator of forthcoming soil nitrogen mineralization.
New research reveals that mature forests do not retain extra carbon absorbed from elevated CO2 levels, but instead release it back to the atmosphere. The study's findings have significant implications for climate models and future carbon sequestration strategies.
Research suggests mature forests cannot absorb additional carbon as atmospheric CO2 concentrations increase. Carbon is quickly cycled through the soil and returned to the atmosphere, with only half being stored by trees and half by fungi and bacteria.
Researchers have discovered that certain plant materials can help store more carbon in soils and reduce erosion. Using two-step experiments with biomass crops, they found that miscanthus and willow performed better than sorghum in storing long-term carbon, making sustainable farming on peatlands possible.
A study from the University of California, Davis found that whole orchard recycling can sequester 5 tons of carbon per hectare, increase water-use efficiency by 20 percent and boost crop yields by 19 percent. This practice also builds soil nutrients and water retention, mitigating climate change.
A new study reveals that soil has a significant role in mitigating climate change, with up to 25% of global potential for natural climate solutions. The research highlights the importance of agroforestry and improved agricultural practices in enhancing soil health and carbon sequestration.
Researchers found that cover crops can increase soil health in the Southern High Plains by retaining rainwater and reducing erosion. The study showed that biological activity improves soil structure and increases soil carbon storage, leading to reduced greenhouse gas emissions.
A study published in Science found that methane emissions from ancient carbon reservoirs are small and do not reach the atmosphere in large quantities. Researchers believe natural buffers such as ocean microbes and bacteria help prevent the release of methane.
The National Science Foundation has awarded $8 million in funding to seven research projects studying soil signals to advance sustainable agriculture, climate change and food production. Researchers will develop new methods to capture, communicate and analyze soil processes, including sensors and data tools.
A new study models the potential for growing major food crops in newly suitable regions due to climate change. The researchers found that Earth's agricultural landmass could increase by one-third, including vast new farming prospects in Canada and Russia's north.
Researchers have dated ancient Aboriginal rock art in the Kimberley region using wasp nests, confirming that Gwion style paintings are around 12,000 years old. The technique used involves analyzing the age of wasp nests under and over the paintings to establish a date range.
Researchers at McGill University have launched interactive story maps to highlight the importance of wetlands, which support a disproportionately high number of endangered species. Wetlands also naturally combat climate change by storing carbon dioxide underground.
New research reveals that adding carbon-rich organic matter to agricultural fields can cut plant-microbe links by up to 70%. This reduces the efficiency of nitrogen fixation, a symbiotic relationship between legume plants and rhizobial microorganisms.
Tiny meteorites found in ancient soils suggest carbon dioxide made up 25-50 percent of Earth's atmosphere 2.7 billion years ago, indicating a warm planet. Lower nitrogen levels resulting from lower pressure would allow for both high CO2 and cool conditions.
Researchers discovered that plants use flavonoids to communicate with microbes in the soil, but high levels of organic carbon in the soil can repress these signals. This allows plants to control whether they invest in expensive symbionts and avoid wasting photosynthate on unnecessary microbial help.
The decomposition of organic matter in permafrost soil during winter months can release substantial amounts of CO2 into the atmosphere, exceeding summer uptake. By 2100, this could increase by 41% if current greenhouse gas emissions continue.
Researchers found that tundra warming significantly increases VOC release from plants, shifting composition towards more reactive hydrocarbons. This change in VOCs could impact plant-animal interactions and ecosystem resilience.
The Everglades Agricultural Area is experiencing significant soil subsidence due to climate change, threatening the region's ecosystem and agricultural economy. Researchers recommend practices such as crop rotation with rice and adding plant material back into the soil to mitigate decomposition and increase soil carbon.
Researchers found that recycling nutrient-rich industrial waste products can enhance soil health while reducing carbon emissions and maintaining crop yields. The study used heat-inactivated spent microbial mass (SMB) as a fertilizer, which provided similar crop yields to conventional fertilizers but at greater rates.
Researchers at Colorado State University reveal that soil organic matter has two distinct components: particulate and mineral-associated organic matter, which differ in their origin, makeup, and persistence. Recognizing this diversity is essential for developing effective strategies to sequester carbon and promote soil health.
Researchers found that small forest remnants on farmland can store more carbon in the topsoil layer and host fewer ticks than larger forests. These tiny woodlands also provide benefits for roe deer populations and offer a lower risk of contracting tick-borne diseases.
Researchers found that converting degraded pasture to oil palm plantations reduces stored carbon loss associated with rainforest clearing, but can lead to initial soil organic carbon loss. However, the carbon is later redistributed within the soil, resulting in long-term recovery of topsoil organic carbon.
A group of scientists from the Science for Nature and People Partnership (SNAPP) urge policymakers to take action on soil carbon despite ongoing debates. They highlight the importance of rebuilding soil carbon for environmental and agricultural benefits, such as sustainable agriculture systems and water quality.
A new study reveals that human impacts have greatly reduced plant-fungus symbioses, which play a key role in sequestering carbon in soils. Restoring these ecosystems could help alleviate anthropogenic soil carbon losses and ameliorate increases in atmospheric greenhouse gases.
Karen Lloyd's research focuses on the effects of thawing permafrost on the environment, examining microbial processes that break down soil organic carbon and release greenhouse gases. By understanding these processes, future predictions can be made about the impact of microbial communities' activities on changes in released gases.
Researchers from RUDN University found that the rate of organic carbon accumulation in wild, cultivated, and abandoned soils depends mainly on soil type and composition. The study revealed that phaeozems release carbon easily, while chernozems contain more decomposition-resistant compounds.
A new study by Colorado State University researchers found that exposure to manure from cows administered antibiotics alters the soil microbiome and ecosystem functions, reduces soil carbon storage, and changes how plants allocate carbon below ground. The findings suggest that widespread use of antibiotics in livestock production has s...
Under climate warming up to 1.7 °C, sedge plants prioritize root growth over shoot growth due to nitrogen supply limitations; however, as warming intensifies, shoots become more prominent, indicating nitrogen supply now outpaces plant demand.
A Dartmouth-led study reveals that actively managed mixed wood forests in New Hampshire have significant carbon stores, both above and below ground. The research found that the forests' soil carbon is higher in subplots with more trees, especially fir and spruce species.
Australian marine ecosystems absorb and emit large amounts of greenhouse gases, including 20 million tonnes of CO2 annually. Human damage causes 3 million tonnes to be released back into the atmosphere, highlighting the importance of conservation and restoration.
A new study finds that warmer tropical soils release more car-bon, leading to a 9% increase in atmospheric CO2 by the century's end. The increased microbial activity and changes in soil microbes also promote a positive feedback loop, exacerbating global warming.
A new research study has revealed that humans lived in a low-carbon-dioxide atmosphere for 2.5 million years, with concentrations averaging 230 parts per million, until 1965. Today's levels are about 410 parts per million.
Researchers found increased rainfall reduces soil's water absorption rate, leading to more water in streams and lakes. Soil properties also affect carbon storage, potentially impacting climate models.
The Soviet Union's collapse led to a significant decrease in greenhouse gas emissions due to decreased meat consumption and abandonment of cultivated land. This resulted in a reduction of around 7.61 billion tons of carbon dioxide equivalent emissions from 1992 to 2001.
A recent study found that water availability in soil determines the direction of carbon-climate feedback, with land carbon uptake increasing below optimal moisture levels and decreasing above them. This discovery provides new insights into the complex relationships between climate change, ecosystem dynamics, and water availability.
A new study found that frequent and large wildfires are releasing stored carbon in boreal forests, transforming them into a source of carbon instead of a sink. This shift has significant implications for global climate change and greenhouse gas levels.
Research finds that older stands of trees protect legacy carbon from burning, while younger stands do not. This shift could change boreal forests from a carbon sink to a source, exacerbating climate change. The study's findings have global implications for future climate scenarios.
A new study reveals that phosphorus-deficient soils reduced projected carbon dioxide uptake by 50% in the Amazon compared to current estimates. The Amazon Basin plays a critical role in mitigating climate change, but outdated assumptions have been used in models, leading to inaccurate predictions.
Researchers found that adding compost and cover crops to organic-certified systems increased soil carbon content by 12.6% over a 19-year period, outperforming the international '4 per 1000' initiative. This approach stores more carbon than previously calculated, highlighting the importance of balancing diet for microorganisms in soils.
A recent study found that termite activity in wetlands improves soil structure and nutrient content. Termites help turn dead trees into valuable organic matter, increasing crucial soil carbon content.
The Stanford-led study, published in Nature Climate Change, explores the capacity of trees and plants to absorb carbon dioxide. The research suggests that trees will continue to sequester carbon dioxide at generous rates through at least the end of the century, with potential increases in plant biomass by 12% by the end of the century.
Researchers at Michigan State University discovered a new mechanism determining how carbon is stored in soils, which could improve climate resilience and reduce carbon footprints. Soils from ecosystems with higher plant diversity have more pores of the right size for stable carbon storage.
Researchers found drastic drops in organic material preserved in core samples from the Paleocene-Eocene Thermal Maximum event, suggesting soils emitted atmospheric carbon dioxide. The findings could mean global climate models overestimate terrestrial ecosystems' ability to mitigate future warming.
A new study found that microbial communities in Alaskan soil respond rapidly to warming, leading to increased methane and carbon dioxide production. Microbial species and genes involved in these processes became more abundant with warmer conditions.
Researchers found that deforested areas leach older, biodegradable organic carbon into rivers, which is consumed by microbes and released as CO2. This process could jeopardize local ecosystems and fuel the greenhouse effect.
Researchers tested different soils' responses to multiple biochar types but found no significant impact on plant growth. However, biochar did affect soil greenhouse gas emissions. The study's findings suggest that using biochar as an additive could prevent microbe-generated greenhouse gas emissions.
Researchers found that microaerobic Fe(II) oxidation coupled to carbon assimilation processes driven by microbes from paddy soil. The study identified the potential microaerophilic Fe(II)-oxidizing bacteria in paddy soil and confirmed their ability to couple iron cycling with carbon transformation.
Researchers used radiocarbon dating to track carbon release from thawing permafrost in Siberian-Arctic rivers. The study found that permafrost and peat carbon contributed significantly to dissolved organic carbon in the rivers, with seasonal differences suggesting gradual thaw of surface permafrost as the main source.
A new report highlights the urgent need for monitoring and modeling of Arctic permafrost due to rapid collapse, which can lead to catastrophic consequences such as subsidence, flooding, and landslides. The researchers estimate that this abrupt thaw could double the climate feedback associated with permafrost thawing.
Researchers successfully isolated a strain of methane-oxidizing soil bacteria that can grow in air and oxidize methane at atmospheric concentrations. The strain also exhibits metabolic flexibility, allowing it to metabolize multiple gases including CO2, N2, O2, CO, and H2.
A recent study published in Global Change Biology reveals that climate change primarily affects peatland CO2 gas exchange through changes in moisture conditions, rather than temperature. The research found that drying conditions led to increased photosynthesis and respiration, while warming had a minimal impact on CO2 exchange.
Coastal wetlands worldwide store more carbon than forests and can double their capacity when faced with rising seas. The study found that carbon concentrations in top soil layers increased by 2-4 times, while deeper layers saw a 5-9 times increase.