Researchers have developed a new computer simulation to study carbon in deep Earth reservoirs, providing insights into the Earth's carbon cycle and climate change. The simulation reveals underestimated concentrations of bicarbonate ions under extreme pressure and temperature conditions.
Scientists found that periodic changes in Earth's orbit and volcanic activity controlled the global carbon cycle during ancient mass extinctions. The study suggests that solar system processes had a significant impact on climate and environmental change over 200 million years ago.
A study of carbon-isotope data from a Welsh mudstone core reveals anomalies consistent with orbital cycles of approximately 405,000 years. These findings indicate that the marine carbon cycle is particularly responsive to such astronomical signals.
A new study reveals that intensifying tropical land use is causing forests to contribute less to carbon dioxide uptake, affecting the global carbon cycle. Researchers used satellite data and dynamic vegetation models to estimate carbon dioxide absorption by different ecosystems worldwide.
Gelatinous zooplankton contributes significantly to marine carbon cycle, binding large amounts of carbon transported into deep ocean. This contribution is quantified for the first time globally using over 90,000 observations.
Scientists and innovators present the concept of the Circular Carbon Economy, a system where carbon emissions are reduced, reused, recycled, and removed. This approach is inspired by nature and aims to restore the balance of the carbon cycle.
A researcher is studying how carbon moves through landscapes and across land-water boundaries, exploring its impact on water quality and freshwater food webs. The goal is to understand the fate of terrestrial carbon and improve global carbon budgets.
International researchers have found that most of the black carbon transported to the Atlantic Ocean is 'young' and likely results from recent forest fires. The study, published in Nature Communications, used radiometric dating and molecular composition analysis to quantify and characterize the black carbon flowing in the Amazon River.
A study reveals a decline in forest carbon storage time, hindering forests' ability to absorb and re-emit carbon. Forests are crucial for regulating atmospheric carbon dioxide concentrations, and increased tree mortality is contributing to this decline.
Researchers at Max Planck Institute uncover forgotten metabolic pathway in ocean microorganisms, finding widespread distribution and ecological significance. The discovery provides valuable insights into the degradation of glycolic acid and its impact on global climate change.
A Yale University study reveals that the Cretaceous-Paleogene extinction event was triggered by a sharp drop in ocean acidity, leading to the demise of marine calcifiers and a 50% decline in species productivity. The research provides new insights into the recovery of marine life after the event.
UIC researchers have successfully developed a fully rechargeable prototype of a lithium-carbon dioxide battery, demonstrating its potential for advanced energy storage systems. The battery's efficiency and long-lasting cycle life are significantly improved due to the use of new materials and a hybrid electrolyte.
Research reveals that horizontal and vertical circulation of carbon-rich ocean water in the subpolar Southern Ocean work together to control carbon storage and release. The study found that large gyres, such as the Weddell Gyre, play a key role in transporting carbon-containing phytoplankton out of the region.
A new study published in Nature Climate Change offers a roadmap for detecting changes in the ocean due to climate change. The research found that sea temperature rise and ocean acidification have already emerged, while other impacts such as changes in ocean microbes will take several decades to a century to appear.
A world-leading team reveals ice sheets are no longer passive parts of the Earth's carbon cycle, but reactors that process rock and boost nutrient release. Ice sheets store vast amounts of organic carbon, fuel marine food webs, and influence global carbon sinks.
A University of Maryland Center for Environmental Science-led research cruise is exploring the marine carbon cycle in the deep Atlantic Ocean. Scientists are analyzing bacterial diversity and function to better understand how cyanobacteria contribute to the process.
Researchers at Toyohashi University of Technology have successfully fabricated a binder-less tin phosphide/carbon composite film electrode for lithium-ion batteries via aerosol deposition. The electrode exhibits improved charging and discharging cycling stabilities, enabling advanced Li-ion batteries with higher capacity.
A study found that pushing past a critical threshold in the carbon cycle can trigger extreme ocean acidification, potentially leading to mass extinctions. The research suggests that once this threshold is breached, the Earth's response becomes self-sustaining, amplifying the effects of initial triggers.
International study finds that as temperatures rise, trees grow faster but die younger, reducing the amount of carbon they store. This phenomenon has significant implications for global carbon cycle dynamics.
A new paper outlines critical mechanisms involved in the ocean carbon cycle, specifically the biological pump. Researchers found that particle injection pumps are a more efficient way of pulling carbon from the surface into the deep waters.
A new Yale study uncovers key relationship between storm events, ecology, and topography in moderating greenhouse gas release from rivers and streams. Concentrations of three greenhouse gases increase during rainstorms in wetland streams but decrease or remain constant in forested streams.
A new study reveals the microbial food web in Amazonian waters, consisting of 20% of the whole Amazon, produces 10 times more CO2 than the classical food chain by decomposing organic matter. This accounts for most of the carbon circulating in lakes, floodplains, and wetlands.
Scientists discovered over 1,000 buried wetland sites worldwide, revealing a record of wetland presence and peat burial. These findings suggest that peat burial can slow down the transfer of carbon from the atmosphere to land, potentially offsetting climate warming.
A new study reveals that peatlands have been a significant carbon sink over the past 130,000 years, storing carbon in their deposits and potentially slowing down climate change. The research, published in PNAS, fills a key knowledge gap about the global extent of peatlands and their role in the carbon cycle.
Researchers use X-ray nanotomography to study the 3D structure of coccolithophore calcite shells, revealing correlations between shell mass and organic template size. The findings provide new insights into the role of these tiny microorganisms in the global carbon cycle.
Recent studies found that dry inland waters play a significant role in the global carbon cycle, emitting around 0.2 gigatonnes of CO2 annually. Freshwaters also act as carbon sinks when water levels are high, but emit gases when they dry out. The team suggests reservoirs as potential targets for reducing CO2 emissions from inland waters.
A global collaboration of ecological researchers, including Kent State University's Dave Costello, has revealed new findings on the effect of climatic factors on river-based ecosystems. The study found that temperature and moisture influenced carbon-cycling rates of river ecosystems.
A new study reveals that animal movements can trigger direct or indirect feedback effects altering landscapes' capacity to absorb or release carbon. This integration of animal ecology and remote sensing can improve predictions and management of carbon cycling across ecosystems.
A new study found that mined lands undergo dramatic increases in chemical weathering rates, melting away bedrock up to 45 times faster than unmined areas. This process releases carbon dioxide into the atmosphere, offsetting 20-90% of the carbon absorbed by plants.
Daily fish migration fuels metabolism of single-celled heterotrophic prokaryotes, revealing a labile DOC source that supports microbial community growth. Higher microbial diversity found in mesopelagic zone than expected.
The study found that microbes mediate the microbial carbon pump (MCP), which takes up labile organic carbon and removes carbon dioxide from the atmosphere. The MCP's importance may increase under global warming due to changes in planktonic organisms favorable for MCP.
A new study by Florida State University researchers has found that tiny phaeodarian organisms in the ocean's twilight zone are consuming up to 20% of sinking, carbon-rich particles before they reach the deep ocean. This discovery suggests a significant impact on Earth's carbon cycle and challenges current climate dynamics.
A massive world-wide study of dry riverbeds has found they're contributing more carbon emissions than previously thought. The contribution of intermittent rivers and streams to the process of carbon cycling is largely ignored, but new data suggests this may be higher than initially estimated.
A team of researchers discovered that deep ocean aquifers can break down more refractory carbon than previously thought. Microbes in the aquifer consume carbon, changing the composition of the surrounding seawater. This finding has the potential to reshape our understanding of carbon cycling in the deep ocean.
Researchers discover a previously unknown connection between seafloor weathering and the slow carbon cycle. The study reveals that fluctuations in seafloor spreading rates drive changes in ocean crust capacity to store carbon dioxide.
Researchers have created detailed global maps of key plant traits that significantly impact carbon cycle calculations. The maps show substantial local diversity, contradicting previous simplistic models that assumed identical trait values across regions. This advancement will lead to more accurate modeling of carbon cycle feedbacks.
Researchers from Bigelow Laboratory discovered nitrite-oxidizing bacteria to be key players in the global carbon cycle, capturing more than 1.1 gigatons of CO2 annually. These large, relatively rare bacteria outperform archaea in carbon capture, highlighting a significant shift in our understanding of oceanic carbon cycling.
A recent analysis by Stanford University researchers found that places with high animal diversity correlate with areas that have the most carbon sequestered in soil. The team discovered that meal remnants from animals contribute to an increase in soil microbes, which convert organic material into stored carbon.
A study by MIT professor Daniel Rothman suggests that a sixth mass extinction may occur if the world's oceans hold enough carbon to destabilize the system. By 2100, human activities are estimated to add about 310 gigatons of carbon to the oceans, potentially tipping the planet into unknown territory.
Researchers observed atomic-level dissolution processes of calcite using high-speed FM-AFM, revealing an intermediate state called the transition region. The team proposes a new dissolution mechanism involving the formation of Ca(OH)2 monolayer and its effects on surface stability.
Researchers studied iron carbonate under extreme conditions to understand the deep Earth's carbon cycle and its role in global warming. They found unprecedented structural stability of a tetracarbonate phase at high pressures, suggesting self-oxidation-reduction reactions can preserve carbonates in the lower mantle.
The University of Oklahoma has secured an $161 million NASA contract for a groundbreaking Earth science mission. The Geostationary Carbon Cycle Observatory (GeoCarb) will monitor plant health and vegetation stress across the Americas, as well as probe carbon dioxide and methane exchange processes in the atmosphere.
Foraminifera, single-celled organisms that form the base of marine food webs, struggle to build their shells and make spines in high CO2 environments. This study suggests that stressed foraminifera could indicate a larger scale disruption of carbon cycling in the ocean.
Researchers have found that giant larvaceans, tiny plankton that live in the upper 400 meters of the ocean, filter carbon particles at higher rates than any other zooplankton. These structures sink to the sea floor, significantly contributing to moving organic materials into deeper water.
Researchers discovered that microbes in polar streams are producing organic material, potentially contributing to an underestimated 'dynamic local carbon cycle' as temperatures rise
A Florida State University researcher investigated how carbon moves from the ocean surface to greater depths and remains there for hundreds of years. The study found that certain areas of the sea, particularly fronts where temperature or salinity changes, act as giant conduits moving carbon to deeper depths.
Researchers use neutron diffraction to study high-pressure and high-temperature phases of solid carbon dioxide, shedding light on the Earth's carbon cycle and potential for carbon substitution with silicon dioxide. The study provides new insights into the behavior of carbon dioxide under extreme conditions.
A global study predicts that soils may release large quantities of carbon dioxide in response to warming, leading to even faster rates of warming globally. Soils in Arctic ecosystems are the most susceptible to releasing stored carbon when warmed.
The University of Oklahoma will monitor plant health and vegetation stress throughout the Americas using a commercial communications satellite. The mission aims to examine natural sources and processes that control carbon dioxide, carbon monoxide, and methane in the atmosphere.
Researchers simulate carbon dissolution in water-rich fluids at the Earth's upper mantle, revealing unexpected forms of carbon, and challenging previous geochemical models. The study suggests that water transports carbon mostly through highly active ions, not dissolved CO2 molecules.
The Colorado River delta's annual carbon cycle has changed dramatically due to poor water management, with fossil clam shells revealing vast amounts of carbon being added to the atmosphere. The reduced carbon emissions at the delta are vastly outweighed by the carbon emissions from transporting water to cities and farms.
Researchers estimate that seaweed globally sequesters 173 trillion grams of carbon per year, with 90% of this being due to transport into deep-sea sediments. This highlights the significance of seaweed as a major carbon sink, surpassing Amazonian forests.
Researchers at UTA examine global warming events during the Early Paleogene period, which occurred 66-45 million years ago. They aim to understand the effects of greenhouse gas emissions on life on Earth and provide analogs for current climate change.
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.
Two studies reveal how human-made forest changes affect the carbon cycle and air temperature. Replacing broadleaved forests with conifers increases evapotranspiration and albedo, contributing to warming. Forest clearing causes an increase in average and maximum surface temperatures, except at northern latitudes.
Researchers present a novel method to analyze apatite inclusions in magmatic zircon and titanite, allowing estimation of whole-rock Sr and SiO2 concentrations. This technique provides insight into petrogenesis and provenance, enabling better understanding of the continental crust's evolution.
Research suggests certain types of carbon-intensive algae are flourishing as carbon pumps, removing CO2 from the atmosphere. A shift in phytoplankton dominance occurred over the past millennium, with a more recent transition happening in less than 200 years.
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 in Alaska's Yukon Flats reveals massive carbon losses due to increasing fire frequency, challenging assumptions about recent fire activity. The study finds that the region has become a net exporter of carbon, posing a significant threat to the global carbon cycle and climate balance.
New research emphasizes the importance of preserving large fish populations to maintain carbon cycling in blue carbon ecosystems. The loss of top predators can have serious environmental consequences, including reduced carbon storage in coastal wetlands.