Science Daily

At current emission rates, we re just over three years away from blowing through the remaining carbon budget to limit warming to 1.5 C. This new international study paints a stark picture: the pace of climate change is accelerating, seas are rising faster than ever, and the Earth is absorbing more heat with devastating consequences from hotter oceans to intensified weather extremes.

South Australia’s tiny pygmy bluetongue skink is baking in a warming, drying homeland, so Flinders University scientists have tried a bold fix—move it. Three separate populations were shifted from the parched north to cooler, greener sites farther south. At first the lizards reacted differently—nervous northerners diving for cover, laid-back southerners basking in damp burrows—but after two years most are settling in, suggesting they can ultimately thrive.

Over 300 million years ago, Earth experienced powerful bursts of carbon dioxide from natural sources—like massive volcanic eruptions—that triggered dramatic drops in ocean oxygen levels. These ancient "carbon burps" led to dangerous periods of ocean anoxia, which stalled marine biodiversity and potentially reshaped entire ecosystems. In a groundbreaking study, scientists combined high-tech climate models with deep-ocean sediment analysis to pinpoint five such events. The alarming part? Today's human-driven CO₂ emissions are skyrocketing at speeds hundreds of times faster than those ancient upheavals—raising urgent questions about how modern oceans, particularly coastal zones rich in marine life, might react.

Ancient coral fossils from the remote Seychelles islands have unveiled a dramatic warning for our future—sea levels can rise in sudden, sharp bursts even when global temperatures stay steady.

A century-old mystery of a stubborn cold patch in the North Atlantic is finally being unraveled. A new study links this anomaly to a long-term weakening of the Atlantic Meridional Overturning Circulation (AMOC) a massive ocean current system that regulates climate across the Northern Hemisphere. Using over 100 years of temperature and salinity data, researchers showed that only models with a weakening AMOC could recreate the observed changes. The implications are vast, influencing everything from European weather to marine ecosystems, and casting doubt on many recent climate models that underestimated this oceanic shift.

Arctic peatlands are expanding with rising temperatures, storing more carbon at least for now. But future warming could reverse this benefit, releasing massive emissions.

During Earth's ancient Snowball periods, when the entire planet was wrapped in ice, life may have endured in tiny meltwater ponds on the surface of equatorial glaciers. MIT researchers discovered that these watery refuges could have supported complex eukaryotic life, serving as sanctuaries for survival amid extreme conditions. Their investigation into Antarctic melt ponds revealed not only evidence of eukaryotes but a striking diversity shaped by factors like salinity. These findings reshape our understanding of how life weathered one of the harshest climate events in Earth s history and ultimately set the stage for the evolution of complex life forms.

A breakthrough study has uncovered that the Southern Ocean's power to pull carbon dioxide from the atmosphere fluctuates dramatically depending on winter sea ice. When sea ice lingers longer into winter, the ocean absorbs up to 20% more CO2, thanks to a protective effect that blocks turbulent winds from stirring up deeper, carbon-loaded waters. This subtle seasonal shield plays a vital role in buffering our planet against climate change. But here s the twist: winter data from the Southern Ocean is notoriously scarce due to its brutal conditions, meaning we might be missing a key piece of Earth s climate puzzle.

What if all life on Earth followed a surprisingly simple pattern? New research shows that in every region, species tend to cluster in small hotspots and then gradually thin out. This universal rule applies across drastically different organisms and habitats from trees to dragonflies, oceans to forests. Scientists now believe environmental filtering shapes this global distribution, providing new tools to predict how life responds to climate change and biodiversity threats.

For millions of years, large herbivores like mastodons and giant deer shaped the Earth's ecosystems, which astonishingly stayed stable despite extinctions and upheavals. A new study reveals that only twice in 60 million years did environmental shifts dramatically reorganize these systems once with a continental land bridge, and again with climate-driven habitat change. Yet the ecosystems adapted, with new species taking on old roles. Now, a third, human-driven tipping point threatens that ancient resilience.

Frogs, salamanders, and other amphibians are not just battling habitat loss and pollution they're now also contending with increasingly brutal heat waves and droughts. A sweeping 40-year study shows a direct link between the rise in extreme weather events and the growing number of species landing on the endangered list. Europe, the Amazon, and Madagascar have become danger zones, with amphibians unable to adapt quickly enough. But there s hope scientists are calling for focused conservation efforts like habitat restoration and micro-refuges to help these vulnerable creatures survive.

A new study details processes that keep pollutants aloft despite a drop in emissions.

Collapse of the West Antarctic Ice Sheet could be triggered with very little ocean warming above present-day, leading to a devastating four meters of global sea level rise to play out over hundreds of years according to a new study. However, the authors emphasize that immediate actions to reduce emissions could still avoid a catastrophic outcome.

New research adds to our understanding of how rapidly rising sea levels due to climate change foreshadow the end of the Great Barrier Reef as we know it. The findings suggest the reef can withstand rising sea levels in isolation but is vulnerable to associated environmental stressors arising from global climate change.

Global warming is continuously advancing. How quickly this will happen can now be predicted more accurately than ever before, thanks to a method developed by climate researchers. Anthropogenic global warming is set to exceed 1.5 degrees Celsius by 2028 and hence improved quantification of the Paris goals is proposed.

While scientists have long studied currents of large eddies, the smaller ones -- called submesoscale eddies -- are notoriously difficult to detect. These currents, which range from several kilometers to 100 kilometers wide, have been the 'missing pieces' of the ocean's puzzle -- until now. Using data from the new Surface Water and Ocean Topography (SWOT) satellite, scientists finally got a clear view of these hard-to-see currents, and they are a lot stronger than anyone thought.

The fossils of ancient salamander-like creatures in Scotland are among the most well-preserved examples of early stem tetrapods -- some of the first animals to make the transition from water to land. Thanks to new research, scientists believe that these creatures are 14 million years older than previously thought. The new age -- dating back to 346 million years ago -- adds to the significance of the find because it places the specimens in a mysterious hole in the fossil record called Romer's Gap.

A new study finds that if global warming exceeds the Paris Climate Agreement targets, the non-polar glacier mass will diminish significantly. However, if warming is limited to 1.5 degrees Celsius, at least 54 per cent could be preserved -- more than twice as much ice as in a 2.7 C scenario.

Anthropologists have examined the societal consequences of global glacier loss.

Forest-based agroforestry can restore forests, promote livelihoods, and combat climate change, but emerging agroforestry initiatives focusing only on tree planting is leading to missed opportunities to support beneficial outcomes of forest management, scientists found.