Climate change Is slowing Earth’s rotation

Climate change is subtly altering one of the most fundamental rhythms of our planet: the length of a day. New research from scientists at the University of Vienna and ETH Zurich shows that rising sea levels caused by melting ice sheets are slowing Earth’s rotation, causing days to grow slightly longer. Although the changes are extremely small—measured in milliseconds—the rate at which they are occurring is unprecedented in at least the past 3.6 million years.

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Phytoplankton blooms linked to ocean quakes

Deep beneath the ocean’s surface, the seafloor is a dynamic environment where tectonic plates grind, rocks fracture, and heat escapes from Earth’s interior. For many years, scientists assumed that these deep geological processes remained largely isolated from the sunlit surface waters where most marine life exists. However, new research suggests that this assumption is incomplete. Underwater earthquakes can trigger a chain of events that ultimately stimulates massive biological activity near the ocean surface, demonstrating how tightly connected Earth’s systems really are.

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New study challenges Pangea breakup theory

Around 200 million years ago during the Early Jurassic, the supercontinent Pangea began to fragment, dramatically reshaping Earth’s surface. As the landmass split apart, continents drifted away from one another and vast new oceans formed, gradually creating the global geography we recognize today. For decades, geoscientists believed that the Pangea breakup was primarily driven by a buildup of heat trapped beneath the enormous supercontinent. Because continents are thicker than oceanic crust, they were thought to act like insulating blankets, slowing the escape of heat from Earth’s interior and allowing temperatures in the underlying mantle to rise over tens of millions of years.

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Hidden geomagnetic reversals in Earth’s history

Earth’s magnetic field is dynamic and has repeatedly flipped polarity throughout geological history, events known as geomagnetic reversals. During these episodes, the planet’s magnetic north and south poles switch places, leaving behind magnetic signatures preserved in volcanic rocks, marine sediments, and oceanic crust. These records form the basis of the Geomagnetic Polarity Time Scale (GPTS), a critical tool used by geoscientists to date geological formations, reconstruct past plate movements, and understand changes in Earth’s interior. However, scientists have long suspected that the geological record is incomplete and that some geomagnetic reversals may remain undiscovered due to limitations in observational resolution.

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Tectonic origins of the Great Unconformity

In 1869, geologist John Wesley Powell made a startling discovery while exploring the Grand Canyon: a 520-million-year-old rock layer resting directly atop rocks 1.4 to 1.8 billion years old. Nearly a billion years of geological history appeared to be missing. This vast temporal gap, now known as the Great Unconformity, is not unique to the Grand Canyon. It appears on multiple continents, representing an extraordinary interruption in the rock record that spans anywhere from millions to over a billion years.

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The power of climate models explained

Weather forecasts and long-term climate projections may seem almost magical, but they rest on decades of scientific and computational advances. The Earth system is an intricate network of interacting components: oceans circulate heat across basins, forests exchange carbon with the atmosphere, storms redistribute moisture and energy, and human activities alter atmospheric composition. All of these processes are governed by fundamental physical laws, including conservation of mass, energy and momentum. Yet the system is also chaotic. Small disturbances can amplify over time, steering the planet toward very different outcomes — a phenomenon known as the butterfly effect.

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The growing gravity anomaly under Antarctica

Earth may appear nearly spherical, but its gravitational field tells a different story. Instead of a smooth shell, Earth’s gravity resembles a lumpy potato, shaped by uneven mass distribution deep inside the planet. One of the most striking features of this distorted field is the Antarctic Geoid Low—a broad depression beneath Antarctica where gravity is slightly weaker. New research shows this anomaly is not only ancient but continues to intensify, driven by slow, powerful movements within Earth’s mantle.

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AI vs physics in cloud feedback uncertainty

In 2008, atmospheric scientist Chris Bretherton flew through clouds above the Atacama Desert aboard an instrument-packed C-130 aircraft, gathering data on ice, water vapor, and air pressure. His goal was not sightseeing but confronting one of climate science’s hardest problems: understanding clouds. Nearly two decades later, as global temperatures have risen by about half a degree Celsius, clouds remain the single largest source of uncertainty in climate projections — a challenge often described as cloud feedback uncertainty.

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Life on Earth’s chemical goldilocks zone

A new study suggests that life on Earth may owe its existence to a remarkably precise set of chemical conditions during the planet’s formation — a narrow “sweet spot” that many rocky worlds may never achieve. Researchers found that Earth retained two elements essential for biology, phosphorus and nitrogen, because oxygen levels during its early core formation fell within an unusually tight range. Without that balance, a planet might appear habitable from a distance yet lack the chemical ingredients necessary to support living systems.

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Lunar settlement marks Musk’s strategic pivot

Elon Musk has signaled a major shift in space exploration priorities, placing plans for Mars on hold in favor of accelerating human habitation on the Moon. In a recent post on X, Musk said his company, SpaceX, is now focused on building a “self-growing city on the Moon,” arguing that this goal could be achieved in under a decade—far sooner than a comparable effort on Mars, which he estimates would take more than 20 years.

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