Articles tagged with Dissolved Organic Carbon
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Research reveals thousands of chemical compounds derived from coral reefs and seaweeds are available for microbial decomposition and utilization. Microbes can break down previously thought-to-be-harder-to-degrade chemicals, such as benzene rings and steroids.
Scientists are studying how microplastics affect microbial communities in ponds, with potential implications for carbon cycling and the global biosphere. Microbes have adapted to plastic surfaces, which could impact aquatic environments.
A recent study found that extreme climate events in fall 2022 pushed thousands of lakes in West Greenland across a tipping point, leading to changes in water quality, chemical properties, and biodiversity. The lakes, which previously provided drinking water and sequestered carbon, now emit more carbon dioxide.
Research in three Swedish fjords shows that organic carbon is effectively trapped, regardless of oxygen levels. The study highlights the importance of sediments in storing carbon, with up to 18 megatonnes buried annually, representing 11% of global ocean carbon capture.
A study published in Nature Geoscience elucidates the discrepancy between Martian and Earth-based organic matter. Researchers found that photodissociation of carbon dioxide in the atmosphere leads to organic matter with depleted carbon-13 content, pointing to an atmospheric process as the main source.
The study found that Ryugu and CIs share a common genetic heritage, but the asteroid's Cr isotopes exhibit anomalies that could be caused by water-driven processes. These anomalies are thought to have arisen from the physicochemical fractionation of presolar nanoparticles and secondary minerals.
New research from Bigelow Laboratory for Ocean Sciences reveals that coccolithophores can survive in low-light conditions by taking up dissolved organic forms of carbon. This finding challenges current understanding of the biological and alkalinity pumps driving carbon transport in the ocean.
A model predicting oxygen levels in freshwater streams, developed by WVU researcher Omar Abdul-Aziz, helps determine stream pollution and health. The tool allows citizen scientists to take action on stream pollution, with potential applications for implementing the Clean Water Act.
Research reveals hydrothermal vents as a previously undiscovered source of dissolved black carbon in the oceans, transporting it thousands of kilometers away. This discovery sheds light on the ocean's role as a carbon sink and provides insights into the formation of recalcitrant dissolved organic carbon.
New research reveals a relationship between virus concentration and organic carbon in wastewater treatment plant effluents. The study found that viruses can affect the concentration of organic carbon, leading to potential negative impacts on aquatic ecosystems nearby.
A new study reveals that plastic degradation releases organic compounds and CO2 into the water, causing a drop in pH levels. The study found that aged plastic contributes significantly more to ocean acidification than new plastic, with some types of plastic releasing up to 0.5 pH units.
Researchers at KAUST have developed a new type of carbon molecular sieve membrane that overcomes drawbacks of existing polymer membranes. The membrane, made from 6FDA-DMN, exhibits high rejection of small molecules and exceptional stability in various organic solvents.
Researchers in Acadia National Park found that regulations reducing atmospheric sulfur have led to a partial recovery of algae ecosystems, despite ongoing climate change impacts. Clear-water lakes like Jordan Pond are more sensitive to warming than brown-water lakes like Seal Cove Pond, leading to slower recovery rates.
A recent study used an eddy-resolving ocean model to analyze the seasonal changes in phytoplankton photosynthesis and storage of fixed carbon in the South China Sea. The research found that the biological carbon pump and microbial carbon pump play significant roles in sequestrating organic carbon.
Researchers at Bigelow Laboratory found that some coccolithophore species can use organic compounds as carbon sources, allowing them to thrive in dark conditions. This discovery has significant implications for understanding global ocean processes and the role of algae in the carbon cycle.
Scientists from Stellenbosch University found that phytoplankton are active during winter in the Southern Ocean, contradicting previous assumptions. This discovery improves predictive global climate models and sheds light on adaptation strategies of phytoplankton under adverse growth conditions.
The study tracks ocean microbes consuming different types of organic carbon produced by phytoplankton species, revealing predictable food source preferences. The findings have implications for understanding marine microbes and photosynthetic algae's impact on global carbon cycling.
A team of FSU researchers has found that newly uncovered Arctic landscapes are feeding lakes and streams with rich carbon sources, which is then degraded by intense sunlight. This discovery sheds light on the carbon cycle and its impact on climate change and the types of life these environments may support.
Researchers at the University of Delaware have discovered a direct link between ancient carbon, graphite particles from hydrothermal vents, and seafloor sediments. This finding sheds new light on the dynamics of the marine carbon cycle, revealing that organic carbon can be converted to graphite at vents.
A team of scientists has obtained direct images of dissolved organic carbon molecules from the ocean using atomic force microscopy. The visualization provides clues about their persistence in the marine environment and sheds light on the cycling of carbon in oceans, helping better understand the overall health of marine environments.
Researchers discovered that Arctic ponds can be hotspots for the degradation of dissolved organic carbon (DOC), releasing more carbon into the atmosphere. The study found that these ponds have distinct chemical compositions compared to rivers, and rapid permafrost thaw is adding carbon to them.
A University of Bristol team found that microbes on glacier surfaces produce significant amounts of bioreactive carbon, which is then released in streams and can stimulate other microbes in downstream ecosystems. The study suggests that active microbial processes during the melt season are crucial for this process.
Researchers at the University of Miami Rosenstiel School used data from international scientific cruises to map the distribution of dissolved organic carbon in the Atlantic Ocean. They found that one third of global ocean net production comes from this basin, with nutrient arrival predicting DOC production.
A Dartmouth-led study found that stream insects consumed by spiders transfer methylmercury to terrestrial predators, highlighting the importance of dissolved organic carbon in mediating mercury bioavailability. The research reveals a broader reach of mercury contamination than previously recognized.
Researchers have developed new tools to understand the complex relationships between ocean-borne compounds and microbes, revealing a vast network of molecular connections that store and transform atmospheric carbon in the world's oceans. The study focuses on dissolved organic matter, or DOM, as a central carbon reservoir.
Researchers found that dissolved organic carbon is efficiently removed from ocean water when heated to mimic hydrothermal vent conditions. This process converts the organic molecules into carbon dioxide, reducing oceanic carbon storage.
Researchers found that over half of the dissolved organic carbon in ancient yedoma permafrost decomposes within one week after thawing, producing significant amounts of carbon dioxide. This rapid decomposition is attributed to high concentrations of easily degradable organic acids, posing a critical threat to aquatic ecosystems.
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 Scripps Institution of Oceanography study finds that Alteromonas bacteria can consume as much dissolved organic carbon as diverse communities of organisms. This discovery sheds light on the complex mechanisms of ocean carbon cycling and highlights the importance of individual species in regulating atmospheric carbon dioxide.
A new study of Swedish lakes suggests that power station emissions may have played a smaller role in acidifying the lakes than previously assessed. Organic carbon from living organisms has been found to be a significant contributor to lake acidity, and pre-industrial levels were likely even higher.
A USGS study assessed the McKenzie River in Oregon, measuring optical properties to understand dissolved organic carbon and its impact on drinking water quality. The results indicated that sources of dissolved organic carbon originated upstream and were linked to human activity.
Research at Virginia Tech suggests that the oldest complex life forms fed by osmosis, absorbing nutrients through their outer membrane. The two groups of modular Ediacara organisms grew and constructed their bodies in different ways to maximize surface-area to volume ratios necessary for osmosis-based feeding.
A recent study reveals that dissolved organic carbon in Alaskan arctic rivers is remarkably labile during the spring flood period, challenging the prevailing paradigm. This finding suggests that riverine inputs of DOC may have a larger influence on coastal ocean biogeochemistry than previously realized.
Researchers studied the effects of the Mt. Pinatubo eruption on Earth's climate, finding that natural aerosols have a cooling effect and that coupled climate models should be tested for their response times. Additionally, scientists investigated the link between Antarctic and Indian Ocean temperatures, suggesting Subantarctic Mode Wate...
Mangroves are a significant source of dissolved organic carbon in the ocean, accounting for nearly triple the estimated amount previously thought to be released from smaller-scale estimates. The mangrove root system slows down the release of carbon-rich leaf litter into shallow sediment, where it is then leached into coastal waters.
Researchers studying Arctic rivers and ocean find most organic carbon is relatively young, but warming may release older, stored carbon into the atmosphere. This could lead to a positive feedback loop, enhancing greenhouse effects and accelerating global warming.