Can we tap the ocean’s power to capture carbon?
Reports and Proceedings
Updates every hour. Last Updated: 3-Dec-2025 16:11 ET (3-Dec-2025 21:11 GMT/UTC)
The oceans have to play a role in helping humanity remove carbon dioxide from the atmosphere to curb dangerous climate warming. But are we ready to scale up the technologies that will do the job?
Seawalls and other unyielding structures meant to keep rising waters at bay and to protect against storm surges can cause other significant harm to the coast, often by disrupting natural processes and accelerating erosion. The gap between protection and preservation might be bridged with a softer, nature-inspired solution, according to an international research team.
Just a few million years after the end-Permian mass extinction event (EPME), aquatic reptiles and other vertebrates had recovered to form thriving and diverse oceanic ecosystems, according to a study of an Early Triassic-age fossil site in the Arctic. The findings challenge previous assumptions of a slow and gradual establishment of mid-Triassic marine communities and suggest that vertebrate evolution paralleled the rapid resurgence of invertebrate life in the Early Triassic. The EPME, which occurred roughly 251.9 million years ago (Ma), wiped out upwards of 90% of all marine species on Earth. It has long been thought that recovery of ocean ecosystems following this event was slow, taking over eight million years. However, recent evidence indicates that, for some communities, such as invertebrates and bony fish, populations rebounded much more quickly than previously believed. The establishment and diversification of marine tetrapod communities – which first emerged in post-EPME oceans – is far less understood and is still considered to have been a long, gradual process with staged ecological complexification.
Here, Aubrey Roberts and colleagues describe new findings from the Grippia Bonebed (GBB), a mid-Early Triassic (~249 Ma) fossil site on the Arctic island of Spitsbergen in Svalbard, Norway. According to Roberts et al., the GBB fossil assemblage is notably rich, containing tens of thousands of fossils from an array of oceanic vertebrate species, and represents the earliest known marine tetrapod community from a stratigraphically constrained deposit. Using large-scale taxonomic comparisons and diversity analyses of the GBB fauna, the authors identified a highly diverse and complex marine community, composed of aquatic reptiles and amphibians, including apex-predator ichthyosaurs, smaller ichthyopterygians, durophagous ichthyosauriforms, semi-aquatic archosauromorphs, euryhaline temnospondyls, as well as a variety of fish species, all occupying multiple trophic levels. The findings suggest that many marine tetrapod lineages had already diversified and adapted to oceanic life soon after – or even before – the EPME.
More than 30,000 teeth, bones and other fossils from a 249 million-year-old community of extinct marine reptiles, amphibians, bony fish and sharks have been discovered on the remote Arctic island of Spitsbergen. These record the earliest radiation of land-living animals into oceanic ecosystems following cataclysmic extinction and extreme global warming at the dawn of the Age of Dinosaurs.
Fish species living in the deep sea feature a surprisingly large range of body shapes that evolved in different ways and at different rates depending on where the fishes live in the ocean, new research shows.