Articles tagged with Organic Carbon
A recent study published in Science Advances has analyzed the nanostructure of chicken eggshells to better understand their role in embryo development. The findings suggest that specific characteristics of the eggshell could be genetically selected to produce healthier, more robust eggs.
Researchers estimate that 67% of organic carbon within bedrock is released during erosion, with certain microbe populations using the carbon for nourishment. The findings suggest that this process could negate geological carbon dioxide consumption and impact Earth's climate.
Researchers studying the Black Sea's oxygen-deprived waters found that chemical and biological processes similar to those in the deep ocean occur. This provides new insights into the ocean's role as a storage reservoir for carbon, helping to dampen the effects of human-driven climate change.
Researchers at Hokkaido University have synthesized an organic compound with a record-long C-C bond of 1.806 angstroms, surpassing previously reported world records. The novel polycyclic hydrocarbon named 10c is stable and exhibits unique properties due to its extended C-C bond length.
Researchers found that thawing permafrost is increasing the concentration of organic matter in Arctic and subarctic ponds. This leads to oxygen depletion and cooler water at the bottom of the ponds, impacting microbial activity and greenhouse gas production.
A study by RUDN University scientists suggests that urbanization can increase soil organic carbon stocks, particularly on less fertile soils. This process could help mitigate the impacts of climate change.
A new estimation approach for total organic carbon (TOC) content is validated using well data from the Goldwyer Formation. The method provides reliable TOC estimates for wells inside and outside the Barbwire Terrace, as well as global lacustrine shale. This improves assessments of shale play prospects and potential hydrocarbon resource.
A 94-million-year-old climate change event showed severe oxygen depletion in ancient oceans, with a similar rate of decline observed in contemporary oceans. Researchers used Thallium isotope analysis to examine organic-rich sediment and found evidence of rapid oxygen loss before a major climate event.
Researchers at Osaka University have developed a new method for building complex organic molecules by selectively transforming strong carbon-fluorine bonds. This breakthrough enhances the control over chemical reactions, enabling more synthetic freedom for constructing intricate carbon structures.
Researchers at Tohoku University have created a new synthesis route for alternative catalysts of noble metals, overcoming stability issues with organic-based and carbonaceous materials. This breakthrough could lead to more efficient and cost-effective eco-friendly technologies, including fuel cell vehicles and CO2 reduction.
A global data set reveals that volcanic arcs mobilize carbon from crustal carbonate platforms, particularly in Italy and Indonesia. This finding requires a downward revision of past organic carbon burial estimates.
Researchers at the University of Warwick discovered that phototrophic and heterotrophic bacteria collaborate to cycle nutrients, feeding the ecosystem. This interaction is crucial for maintaining a balanced nutrient level, supporting half of the planet's primary production and oxygen supply.
Researchers introduce a new bottom-up approach to pattern emissive polymers, enabling efficient creation of multi-colored OLED arrays. The method uses designer iridium photocatalysts and could potentially enable high-throughput manufacturing of OLEDs using various technologies.
Researchers found that man-made dam reservoirs trap nearly one-fifth of the organic carbon moving from land to ocean via rivers. This lack of representation in climate models highlights the need for better understanding of reservoir impacts on the Earth's climate.
Scientists from the University of Exeter found that a 183 million-year-old oceanic oxygen depletion event ended after one million years due to increased atmospheric oxygen and rising fire activity. This study highlights the critical need to limit carbon emissions to prevent future anoxic events in the modern ocean.
A Rice University study found that fossilized organic carbon could have been deeply buried in the mantle starting around 2.4 billion years ago, during a critical period known as the great oxidation event. The researchers discovered that the chemical composition of subducting crustal rock plays a crucial role in determining whether carb...
A study by Colorado State University researchers found that an extreme flooding event in 2013 eroded over 500,000 cubic meters of sediment, equivalent to 115 years of weathering products. The flood also discharged large amounts of organic carbon and wood into reservoirs, affecting water storage capacity.
New research finds that warming soil layers can increase CO2 release by 34-37% due to deeper storage of carbon. This suggests a significant source of uncertainty in climate projections and highlights the need for better understanding of soil's role in climate change.
Scientists have detected aliphatic organic compounds on Ceres, suggesting that they formed on the asteroid itself. The findings indicate that the extreme heat from an impact would have destroyed these types of compounds, ruling out external delivery.
A Spanish-Italian team has discovered that carbonaceous chondrites can synthesise complex organic compounds in the presence of water and formamide. This suggests that these meteorites played a vital role in the origins of life in the universe.
A new study found that melting permafrost during a past warming spike led to the massive release of stored carbon into the atmosphere, with severe deepening of the active layer and enhanced microbial respiration. The research provides crucial insights into how permafrost will respond to future climate change.
Researchers developed a synthetic pathway to convert carbon dioxide into organic compounds more quickly than plants. This breakthrough has potential applications in enhancing plant photosynthesis and creating new carbon-based feed for cattle or chemical products.
Scientists at NREL made a groundbreaking discovery that Clostridium thermocellum can take up and utilize both CO2 and cellulose, counter-intuitive in heterotrophic microbes. This pathway enables the bacterium to use both CO2 and organic carbons during growth.
Researchers at UTA have demonstrated that polyaniline, an organic semiconductor polymer, can convert carbon dioxide into alcohol fuels without a co-catalyst. This breakthrough could lead to cheaper and more energy-effective solar fuel cells.
The article discusses a scientific plan developed by UCSB researchers to quantify present conditions in the ocean's carbon cycle and predict its future states. The plan, known as EXPORTS, combines modeling, satellite data, and field sampling to understand how carbon is processed by the world's oceans.
Scientists have discovered a major metabolic pathway in cyanobacteria that can efficiently convert carbon dioxide into organic compounds. The pathway, led by NREL scientists, has the potential to produce chemicals and biofuels from CO2 or plant biomass, reducing reliance on natural gas.
Researchers have developed a new class of materials for organic electronics, featuring polymeric carbon nitrides with high charge mobility and long lifetimes. These materials show promise for building durable and efficient components for organic electronics applications.
A new study finds that Alaskan permafrost soil is biodegradable, releasing its stored carbon directly back into the atmosphere as CO2. The process occurs rapidly, with almost half of the carbon being consumed by microbes within 200 hours.
Research reveals that hydrothermal vent systems convert long-lived organic carbon into more readily available forms, balancing the continuous supply from surface oceans. This mechanism addresses the long-standing question of why deep ocean dissolved organic carbon (DOC) levels remain constant.
A new study by researchers from Umea University found that historical land use has a significant impact on carbon cycling in northern lakes. The study analyzed lake-sediment records and found that organic carbon concentrations varied depending on natural dynamics and human impacts over thousands of years.
Researchers estimate that fjords bury about 18 million tonnes of organic carbon annually, equivalent to 11% of global marine carbon burial. Fjords are 'hotspots' for carbon burial due to their deep and stable environments.
Researchers at Woods Hole Oceanographic Institution discovered that stressed and dying phytoplankton release chemicals that stimulate marine bacteria to quickly convert organic carbon back into CO2. This process reduces the amount of sinking detritus, releasing more CO2 into the shallow ocean and atmosphere.
Researchers estimate that 50% more organic carbon will be exported in glacier outflow over the next 35 years, equivalent to half of the Mississippi River's annual organic carbon influx. This increase has major implications for high-latitude marine ecosystems, particularly those surrounding ice sheets.
A 12-year University of Illinois study shows that cover crops increase soil organic carbon stock without improving crop yields. The practice is found to sequester the most soil organic carbon in no-till systems with hairy vetch and cereal rye cover crops.
A Johns Hopkins University-led team has discovered a rich variety of organic carbon species in deep fluids, suggesting they could spark the formation of diamonds and potentially become food for microbial life. These findings, published in Nature Geoscience, provide new insights into the Earth's mantle and its role in the origin of life.
Phytoplankton, tiny photosynthetic organisms, play a crucial role in regulating the Earth's carbon content. A new study reveals that viruses can rapidly wipe out blooms, fixing large amounts of organic carbon in the process.
Scientists at the University of Miami re-evaluate the global carbon cycle by analyzing marine sediment cores, suggesting that post-depositional changes can mimic ancient trends. This new perspective highlights the importance of understanding geological context in interpreting carbon isotope records.
A team of researchers from Arizona State University has discovered a common mineral that can catalyze the breaking and making of carbon-hydrogen bonds in hydrothermal environments. This finding has significant implications for the Earth's deep carbon cycle, astrobiology, and Green Chemistry.
A team of researchers found that some studies have shown no-till systems without cover crops may not increase soil organic carbon stocks as claimed. The review suggests that different definitions and methods can lead to conflicting findings, and the accuracy of determining soil organic carbon sequestration depends on the method used.
A novel mechanistic model assesses the global ocean carbon export by incorporating the lifecycle of phytoplankton and zooplankton into a food-web-based approach. The researchers found that oceans are a central component in the global carbon cycle, with a mean global carbon export flux of 6 petagrams per year.
A study published in Nature Communications reveals that mesopelagic fish have a stock estimated at 10,000 million tons, surpassing previous estimates of 1,000 million tons. This discovery has significant implications for the understanding of carbon fluxes in the ocean and the operation of ocean deserts.
Researchers have found that funeral pyres in South Asia emit significant amounts of sunlight-absorbing organic carbon aerosols, known as brown carbon. This finding highlights the importance of quantifying and characterizing regional combustion activities to enhance climate models.
Recent studies examine sea-level change offshore New Jersey, the geological processes of the Sierra Nevada mountain range, and post-subduction magmatism in northern California. These articles provide new insights into the geological history of these regions and their ongoing tectonic activity.
Elevated carbon dioxide levels boost growth of tiny plankton, consuming nutrients that larger species rely on. This shift may weaken ocean's ability to absorb CO2 and support cloud formation.
Researchers at Swiss Federal Laboratories for Materials Science and Technology (EMPA) have developed non-toxic flame retardants, replacing conventional halogenated chemicals. The new compounds, derived from organic phosphorus, have been shown to be effective without harming the manufacturing process or environment.
Experiments show high sinking speed for dead gelatinous plankton species, contributing to the biological pump. Fast sinking provides high-quality food resources for benthic organisms and releases CO2 that can be stored without direct contact with the atmosphere.
A new protocol has been developed to measure soil organic carbon sequestration more accurately. The protocol considers the impact of tillage practices on soil organic carbon storage and loss over time.
Researchers have identified a new class of Martian meteorite that likely originated from the Mars' crust, containing an order of magnitude more water than any other Martian meteorite. The unique meteorite, dubbed Northwest Africa (NWA) 7034, has similarities to but is distinct from other Martian meteorites known as SNC.
Researchers have discovered that Alpine glaciers contain diverse biogeochemical complexes of dissolved organic matter, which is surprisingly bioavailable. This finding highlights the importance of glaciers as 'freezers' that preserve organic matter for microbial heterotrophs.
Underground organisms like arbuscular mycorrhizal fungi play a dual role in soil carbon sequestration, both storing and releasing carbon as atmospheric carbon levels rise. The study challenges assumptions about their protective effects on organic carbon.
Fungi found in plants stimulate decomposition rates of organic materials when exposed to higher carbon dioxide levels, limiting soil's ability to store extra carbon. This can lead to higher greenhouse gas emissions and reduced capacity to mitigate climate change.
A new study finds that microorganisms may convert old organic matter to methane under oxygen-deprived conditions in sedimentary basins beneath the Antarctic Ice Sheet. This could lead to significant methane release if the ice sheet shrinks, exacerbating global climate change.
A new study suggests that beneath Antarctica's ice sheet lies a massive potential methane reservoir, with estimates suggesting up to 400 billion tonnes of carbon. Microorganisms in sub-ice environments have been found to metabolize organic carbon into methane gas, which could be released during future ice-sheet collapse.
A new study by Carnegie's Andrew Steele provides strong evidence that Martian organic carbon originates from the planet itself, not Earth or other meteorites. The findings reveal insights into Mars' volcanic history and suggest the presence of organic chemistry throughout its history.
A team of scientists developed a new method to calculate the pace of life in deep sediments, using amino acid signatures to determine microorganism activity. They found that metabolism occurs at a much slower rate in the deep seabed compared to other ecosystems.
A team of researchers has developed a new method to calculate the activity level of microorganisms in the deepest layers of the seabed. The study reveals that these slow-growing bacteria play a crucial role in the global storage of organic carbon, affecting the oxygen content of the atmosphere.
Researchers from the University of Manchester have discovered that commercially available graphite crystals contain micron-sized clusters of predominantly iron, which explain their weak signs of magnetism. This finding could be a breakthrough for utilising graphite as a bio-compatible magnet for medicine and biology.
Researchers developed a practical and general method to synthesize organoboron compounds for Suzuki reactions, improving yields and reducing waste. The new approach enables the creation of diverse organic molecules, including novel drugs and materials.
Researchers found that fully photosynthetic orchids associate with specific fungal clades, not shared with other sympatric orchids, and depend on their symbionts for nutrition. The study used stable isotope analysis to assess how much of the organic carbon and nitrogen in orchid tissue was acquired from their fungal partners.
A new study reveals that jellyfish blooms drastically alter marine food webs by shunting food energy toward bacteria. This shift can lead to a detour of energy away from higher trophic levels and towards bacteria, altering the microbial community composition.