Researchers from the University of Sydney and Université Grenoble Alpes have found that the Earth system flips between two distinct modes that determine the pace of climate recovery from carbon shocks. They combined plate-tectonic reconstructions, global surface processes and climate simulations, with ecological modelling to reconstruct shallow-water carbonate production back to the Triassic Period. 

A new FAU survey finds that 36% of Floridians have moved or are considering moving due to hazards such as hurricanes, flooding and extreme heat. Nearly a quarter of North Floridians say weather hazards have influenced their past moves and about 20% of respondents in the rest of the Peninsula south say they are considering a move at least in part due to weather hazards. More than 60% are concerned about stronger storms and flooding, and nearly half are concerned about homeowner’s insurance costs.

A new study published in Scientific Reports reports the discovery of a remarkably extensive hydrothermal vent field on the shelf of Milos Island, Greece. The vents were identified during the METEOR expedition M192, where the research team used a combination of different methods, including underwater technologies such as an autonomous and a remotely operated vehicles, to survey the seafloor. These approaches revealed previously undocumented venting between 100 and 230 meters depth. This makes Milos home to one of the largest known shallow-to-intermediate hydrothermal systems in the Mediterranean and substantially expands current knowledge of vent distribution in the region.

Slow earthquakes have been discovered to exhibit anomalously slow, long-lasting, and small slips, adjacent to regular earthquakes where we sometimes feel catastrophic vibration. However, no one knows the reason why they show such strange characteristics. In a study published in a scientific journal Nature Communications, researchers at The University of Osaka succeeded in experimentally reproducing the multiple features of slow earthquakes in the lab and suggested the grain-scale origin of them based on their direct observations.