Articles tagged with Ocean Chemistry
A study published in Nature Communications reveals that ancient ocean chemistry created a self-sustaining cycle that kept oxygen levels high after they first rose. This cycle, fueled by phosphorus recycling, allowed for biological productivity and maintained oxygen in the atmosphere.
Chemical signatures in Ediacaran fossils indicate a long-standing symbiotic relationship between early animals and microbes, dating back to 635 million years ago. This ancient chemosymbiosis allowed early animals to survive and spread throughout the ocean, setting the stage for the evolution of complex life forms.
Dr. Michael Twardowski, Ph.D., an internationally recognized expert in optical oceanography, has been named Edwin A. Link Ocean Technology and Defense Endowed Professor at FAU Harbor Branch. He will focus on developing innovative ocean-sensing technologies for marine science and national defense.
A new mesocosm experiment on Gran Canaria is testing whether concrete rubble can increase ocean alkalinity, mimicking natural rock weathering to absorb CO2 from the atmosphere. The study aims to standardize measurement methods for Ocean Alkalinity Enhancement (OAE) and assess its ecological acceptability.
New measurements show that human-induced carbon dioxide emissions have penetrated deep into the North Atlantic, altering the ocean's isotopic signature. The Suess effect is detectable in nearly all North Atlantic water masses, with strongest signals in young, subsurface waters.
Researchers found that fluctuations in seawater chemistry followed the rhythm of ice ages, driven by Icelandic ice sheet dynamics. Volcanic material from Iceland released neodymium with distinct radiogenic signatures, influencing ocean circulation and geochemical cycles.
High-resolution sediment samples off the coast of Brazil show that the Atlantic Meridional Overturning Circulation was more dynamic than previously thought during the Heinrich Event. The circulation was strengthened in two periods, impacting tropical precipitation patterns and carbon storage in the ocean.
Researchers investigated adding iron to the ocean to boost CO2 removal, finding varying effects on marine ecosystems. The Southern Ocean offers a favorable balance of climate impact and ecological consequences, while other regions face more severe consequences.
Scientists used chemical clues in microscopic fossils to find evidence that ocean acidification caused one of the largest extinction events in planktic foraminifera history. The study suggests that volcanic eruptions and rising CO2 levels led to a decrease in shell-building ability, ultimately contributing to the extinction.
Researchers have discovered that microorganisms actively contribute to mineral formation on the ocean floor, using compounds such as sulfate and sulfur to promote pyrite formation. The study reveals a complex interplay between biological and geological processes at the ocean floor.
Researchers find that methane oxidation in African and European rivers is insufficient to offset the expected rise in methane emissions due to global warming and nitrate pollution. The natural filter, more active in African rivers, remains diminished by human perturbations and invasive species.
A recent study reveals that over 90% of the Mar Menor's key nutrients degrading the ecosystem come from recirculated underground flows, not traditional sources like streams or groundwater. This discovery highlights a previously overlooked pathway of contamination and its impact on eutrophication episodes.
A new study has analyzed over 2100 samples to build a genetic dataset containing more than 500 million unique genes, revealing the immense potential of deep-sea biodiversity for developing new technologies. The research found that despite vast genetic diversity, deep-sea organisms rely on stable, core designs to survive extreme conditi...
Researchers found that phytoplankton in the eastern equatorial Pacific were fertilized by iron from the seafloor during ice-age transitions. This suggests a possible feedback loop connecting sea level, seafloor volcanism, and ocean biology, with potential implications for climate change.
A team of 14 West African Master's students, accompanied by experienced scientists, will conduct research at depths of up to 4,900 meters on the POLARSTERN research vessel. The 'Floating University' program aims to document long-term changes in the ocean and investigate marine biodiversity.
A new chemical model developed by researchers at GEOMAR accurately predicts iron chemistry in the South Pacific Ocean, taking into account diverse organic matter properties. The findings improve understanding of the marine iron cycle and its implications for climate change.
A new study finds that water masses from the Southern Hemisphere have been a major contributor to the Indonesian Throughflow for over 800,000 years. The researchers measured nitrogen isotopes in sediment cores and found a remarkable long-term stability of the nitrogen cycle along the equatorial Pacific.
A new study provides a solutions-focused pathway to implementing the High Seas Treaty, highlighting the need for enhanced data resources and sharing. The researchers identify major scientific and technical developments that can help address challenges in biodiversity monitoring and connectivity between areas.
Researchers investigated the Mississippi River's hydrological trends, ocean carbon storage, and gender dynamics in flood mortality. A study found that precipitation increases, but soil moisture decreases, while high-resolution models reveal stronger Southern Ocean carbon absorption. Additionally, data showed men are overrepresented in ...
Researchers at the University of Gothenburg measured carbon dioxide and oxygen levels in 23 mangrove areas, revealing global patterns in environmental stress. The study found that extreme conditions, including low oxygen and high carbon dioxide levels, are becoming more frequent and severe, posing a threat to sensitive fish species.
A new study reveals that deep-sea microbes like Nitrosopumilus maritimus can adapt to warmer, nutrient-poor waters, maintaining their role in nitrogen cycling and primary production. This finding suggests that these microbes may play an important role in reshaping ocean-nutrient distribution in a changing climate.
A new study finds hitchhiking bacteria dissolve essential ballast in ubiquitous
A Rutgers researcher finds bacteria accelerate calcium carbonate dissolution in shallow seas, potentially slowing carbon sequestration and influencing climate change. The discovery sheds light on the ocean's biological carbon pump and its future implications.
Researchers found that certain salinity patterns can fuel El Niño development, increasing its intensity by 20%. This process makes extreme El Niño events more likely and causes catastrophic flooding and severe droughts. The study identified global patterns in salinity preceding major El Niño events over the past 65 years.
An international team has successfully documented and sampled freshened water within a zone nearly 200 metres thick beneath the ocean floor. This discovery sheds light on offshore freshened groundwater systems and their relevance to coastal communities relying on groundwater for freshwater supply.
Researchers used clumped-isotope palaeothermometry to reconstruct large temperature fluctuations at depths of up to 4,000 meters in the Southern Ocean. These fluctuations occurred simultaneously with changes in oxygen isotopes and Earth's orbital eccentricity, suggesting a climatic forcing.
A new study has found that the ocean's ability to absorb CO2 is stronger than previously assumed, with air bubbles playing a key role in this process. The research suggests that the ocean absorbed around 0.3-0.4 petagrams more carbon per year, about 15% more than previous estimates.
A new study found that deep underwater earthquakes can spur massive phytoplankton blooms at the ocean surface. Phytoplankton are microscopic, plant-like organisms that float in upper ocean layers and serve as the foundation of the oceanic food chain.
A team of scientists, led by UC Santa Barbara's David Siegel, embarked on a research expedition to the North Atlantic to study the ocean's carbon cycle. They found that tiny organic particles, known as marine snow, transport carbon from the surface to depths, and this process is critical for understanding Earth's climate.
Scientists at the University of East Anglia used an autonomous underwater vehicle to survey beneath the Dotson Ice Shelf, finding that the shape of the seabed is more important than current speed in influencing warm water circulation. This leads to melting at the underside of the ice shelf, contributing to sea level rise.
Marine Animal Forests are complex habitats that provide essential ecological services, including biodiversity hotspots, nursery areas, and carbon cycling. Scientists urge immediate action to protect these ecosystems from destructive fishing practices, pollution, and climate change.
Researchers from UCSB have challenged the prevailing view of how carbon is fixed in the ocean's sunless depths. They found that microbes beyond autotrophic archaea and heterotrophs could be responsible for fixing carbon dioxide, providing a new understanding of deep-ocean food web dynamics.
Researchers found three major vent areas aligned with active fault zones, controlled by the island's tectonic fabric. The discovery establishes Milos as a natural laboratory for studying hydrothermal activity, volcanism, and tectonics.
A new study published in Nature Geoscience shows the key role of Antarctic Bottom Water in the transition from the last Ice Age. The expansion of AABW played a central role in releasing carbon dioxide into the atmosphere, which helped reduce atmospheric CO2 concentrations.
Sixty-million-year-old rock samples have revealed how massive amounts of carbon dioxide are stored in piles of lava rubble on the seafloor. This discovery sheds light on the importance of breccia, a geological sponge for carbon in the long-term carbon cycle.
A new paper outlines a global coalition dedicated to conserving microbial biodiversity, which accounts for 99% of life on Earth. The Microbial Conservation Specialist Group will develop Red List-compatible metrics, pilot restoration projects, and promote public awareness to ensure microbes are recognized as essential to planetary health.
A new study reveals that ocean acidification is accelerating at a rate outpacing atmospheric CO2 levels, with the Northeastern Pacific Ocean experiencing rapid acidification. The research analyzed coral skeletons from the past century, showing that CO2 has been accumulating in North American waters faster than in the atmosphere.
A study published in Nature Climate Change found that mesoscale horizontal stirring intensifies considerably in the Arctic and Southern Oceans, driven by stronger ocean flow and turbulence resulting from sea ice loss. This intensification could alter heat and nutrient transport, impacting marine ecosystems.
A new study reveals that 16% of the Arctic Ocean's dissolved organic carbon comes from land, primarily from thawing permafrost and coastal erosion. This finding has significant implications for understanding how terrestrial organic matter affects Arctic marine ecosystems and the ocean's ability to store CO2.
Researchers discovered that tiny diatom skeletons transform into clay minerals in just 40 days, rapidly shaping ocean chemistry. This process, known as reverse weathering, influences carbon dioxide levels, nutrient recycling, and marine ecosystems.
Researchers analyzed sediment cores from three sites in the Arctic, finding that year-round ice coverage corresponded with less cosmic dust. This study suggests that tracking cosmic dust can help predict changes to sea ice coverage and understand warming trends.
Researchers track benthic nutrient fluxes using a new device called CAROSEL, which measures nitrogen released from sediments in real-time. The findings reveal daily rhythms in oxygen fluxes and highlight the importance of understanding sediment-water interactions in managing aquatic ecosystems.
Research reveals that microorganisms in ocean hypoxic zones convert nitrate into nitrous oxide to generate energy, producing this climate-damaging gas. The study's findings suggest that organic material in these zones increases the oxygen tolerance of bacteria, allowing for more regions of nitrous oxide production.
Climate models oversimplify the role of calcifying plankton in capturing and cycling carbon, potentially underestimating the ocean's capacity to respond to climate change. Ignoring these organisms' diversity risks oversimplifying how the ocean responds to climate stressors.
Researchers found that hydrothermal systems release iron that can be transported far beyond vent sites through environmental parameters and plume chemistry. This process has significant consequences for ocean productivity and the global carbon cycle.
Researchers at University of Hawaiʻi at Mānoa identified Caulobacter inopinatus, a previously unknown species found in seawater collected near Oʻahu's south shore. The discovery highlights the connection between land and sea ecosystems through microbial exchanges.
Scientists have found new complex organic molecules spewing from Saturn's moon Enceladus, confirming that complex chemical reactions are taking place within its underground ocean. The discovery strengthens the case for a dedicated European Space Agency (ESA) mission to orbit and land on Enceladus.
Dr. Tanja Stratmann's project investigates how deep-sea sponges have processed nitrogen since ancient times, influencing their ecosystems and shaping past environmental conditions. The study uses incubation chambers and fossilized sponges to determine the role of sponges in past ocean environments.
The 2026 Ocean Sciences Meeting will be held in Glasgow, Scotland from February 22-27, 2025. The event will bring together 6,000 scientists, students, and educators to discuss breaking research on the ocean sciences and critical issues affecting a sustainable future for our oceans.
A recent study published in Nature Communications has made a groundbreaking discovery about the contribution of phytoplankton to the global carbon cycle. Phytoplankton can directly pump stubborn carbon into the ocean, where it may persist for centuries, contradicting decades of conventional scientific wisdom.
A new study reveals that North Pacific waters are acidifying more rapidly below the surface than previously thought. Researchers analyzed a 35-year record of ocean carbon measurements and found increases in carbon from natural decomposition, with accelerated acidification associated with fresher and colder waters.
A new deep-sea hydrothermal system was discovered in the Western Pacific, producing massive hydrogen emissions. The Kunlun system is notable for its exceptionally high hydrogen flux and unique geological setting.
A new study reveals that a decline in ocean oxygen levels is disrupting mesopelagic fish populations and ecosystems. The findings suggest that these events could destabilize ecological balances, impair the ocean's role in carbon cycling, and threaten marine biodiversity and food security.
Scientists reconstructed ocean pH levels 201 million years ago and found a massive drop in acidity, leading to mass extinction. The research links this event to volcanic activity and a significant increase in atmospheric CO2.
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 will study how ocean currents and nutrients from land influence the health and productivity of MCEs, which support diverse marine life and important fisheries. The project aims to fill critical knowledge gaps and provide science-based solutions for environmental protection and sustainable growth in the gulf region.
University of Leicester researchers analyzed coral cores to spot the start of industrial deforestation in Malaysian rainforest and its impact on coastal ecosystems. The study found that sediment concentrations remained low before 1950, but increased after, indicating enhanced soil erosion due to deforestation.
A groundbreaking study reveals that small zooplankton like copepods and krill enhance carbon sequestration through seasonal migrations. These tiny creatures store around 65 million tonnes of carbon annually in the deep ocean.
A USC-developed shipboard system using limestone and seawater can remove up to half of carbon dioxide emitted from shipping vessels, cutting maritime CO2 emissions by 50%. The process mimics a natural chemical reaction in the ocean, where CO2 is absorbed into water pumped onboard and then neutralized through a bed of limestone.
A study by University of California, Riverside researchers finds that the Atlantic Meridional Overturning Circulation's slowdown is responsible for the persistent cold water anomaly south of Greenland. This weakening circulation leads to cooler surface waters and fresher salinity, impacting weather patterns across Europe.