Methane munchers in the deep sea rapidly respond to a seabed methane leak
Peer-Reviewed Publication
Updates every hour. Last Updated: 22-Oct-2026 18:16 ET (22-Oct-2026 22:16 GMT/UTC)
Human activity and climate change are estimated to increase the amount of seabed methane leakage. Much of the methane could be consumed by microbes, yet it is unclear how quickly such communities establish. Through six-year seabed monitoring, researchers found that an animal-microbe “biofilter” removing up to100% of the dissolved methane can develop in just 2–3 years, not the decades once thought. Fast-growing methane-oxidizing microbes feed burrowing animals, which churn the seafloor like tiny gardeners to help the microbes feast on the greenhouse gas. This discovery improves our understanding of seafloor methane removal capacity, which is critical to assess the effects of global warming and anthropogenic disturbance in the deep sea.
A new study led by the University of Plymouth has used more than six decades of data to show that plankton abundance is declining across vast swathes of the North East Atlantic – a region covering the Atlantic Ocean from Portugal to Norway, and the entirety of the North Sea.
Long-term conservation policies may help restore freshwater ecosystems and prevent extreme species loss, new research suggests.
A new study has uncovered a previously unknown antiviral defense mechanism in sea anemones, revealing that animals may have evolved more than one way to fight viral infections. Researchers discovered that a protein resembling a key component of the human immune system actually plays the opposite role, yet remains essential for effective antiviral protection. The findings challenge assumptions about the evolution of immunity and suggest that fundamentally different antiviral strategies have emerged across the animal kingdom.
The eastern tropical Pacific Ocean is known for its large low-oxygen zones that are increasing in size, putting marine life at risk. New research shows that 15 million years ago, the opposite was true. A Michigan State University study found that oxygen-deficient waters were distributed very differently during the mid-Miocene Epoch than they are today. The Pacific Ocean’s oxygen-deficient zones were much smaller, while the Atlantic’s were much larger. Scientists had never documented this reversal before. A computer model helped explain why. By recreating ancient ocean conditions, Associate Professor Dalton Hardisty’steam learned that a channel between North and South America allowed water to move freely between the Pacific and Atlantic oceans, reshaping ocean circulation and changing where low-oxygen waters formed.