The discovery of hundreds of colossal sand formations beneath the North Sea has left scientists stunned. Using advanced 3D seismic imaging and data from numerous wells, researchers from The University of Manchester have uncovered vast mounds of sand that appear to defy fundamental geological principles.

These massive formations, dubbed “sinkites,” are estimated to be several kilometers wide and seem to have sunk downward, displacing older, lighter materials beneath them. This phenomenon is known as stratigraphic inversion, where younger rocks typically rest on top of older ones. However, the sinkites have reversed this order on an unprecedented scale.

The researchers believe that these structures formed millions of years ago during periods of earthquakes or sudden shifts in underground pressure, which may have caused the sand to liquefy and sink through natural fractures in the seabed. This process displaced the underlying ooze rafts – composed largely of microscopic marine fossils – sending them floating upwards, creating lighter features known as “floatites.”

The implications of this discovery are far-reaching, particularly for carbon storage. Understanding how fluids and sediments move around in the Earth’s crust can significantly change how we assess underground reservoirs, sealing, and fluid migration. This knowledge could help predict where oil and gas might be trapped and ensure safe storage of carbon dioxide.

Professor Mads Huuse from The University of Manchester, lead author of the study, emphasized that this discovery reveals a geological process previously unseen on such a scale. “We’ve found structures where dense sand has sunk into lighter sediments, effectively flipping the conventional layers we’d expect to see and creating huge mounds beneath the sea.”

As researchers continue to document other examples of this phenomenon and assess its impact on our understanding of subsurface reservoirs and sealing intervals, time will tell just how widely applicable the model is. The study has been published in the journal Communications Earth & Environment.

The discovery of 332 colossal submarine canyons beneath Antarctica’s ice has shed new light on the mysteries of our planet’s ocean floors. A recent article published in Marine Geology has brought together the most detailed catalogue to date of Antarctic submarine canyons, identifying a total of 332 canyon networks that reach depths of over 4,000 meters. This find is five times as many canyons as previous studies had identified.

The catalogue was produced by researchers David Amblàs and Riccardo Arosio from the University of Barcelona and University College Cork respectively. Their study shows that Antarctic submarine canyons may have a more significant impact than previously thought on ocean circulation, ice-shelf thinning, and global climate change, especially in vulnerable areas such as the Amundsen Sea and parts of East Antarctica.

Submarine canyons are valleys carved into the seafloor that play a decisive role in ocean dynamics. They transport sediments and nutrients from the coast to deeper areas, connect shallow and deep waters, and create habitats rich in biodiversity. Despite their ecological, oceanographic, and geological value, submarine canyons remain underexplored, especially in polar regions.

The Antarctic canyons resemble those in other parts of the world but tend to be larger and deeper due to the prolonged action of polar ice and immense volumes of sediment transported by glaciers to the continental shelf. The steep slopes of the submarine terrain combined with the abundance of glacial sediments amplifies the effects of turbidity currents, which carry suspended sediments downslope at high speed, eroding the valleys they flow through.

The new study uses Version 2 of the International Bathymetric Chart of the Southern Ocean (IBCSO v2), the most complete and detailed map of the seafloor in this region. It describes 15 morphometric parameters that reveal striking differences between canyons in East and West Antarctica.

Some of the submarine canyons analyzed reach depths of over 4,000 meters, with the most spectacular being in East Antarctica. These canyons are characterized by complex, branching canyon systems that often begin with multiple canyon heads near the edge of the continental shelf and converge into a single main channel that descends into the deep ocean.

In contrast, West Antarctic canyons are shorter and steeper, with V-shaped cross sections. This morphological difference supports the idea that the East Antarctica Ice Sheet originated earlier and has experienced a more prolonged development.

The study also highlights the importance of submarine canyons in facilitating water exchange between the deep ocean and the continental shelf. They allow cold, dense water formed near ice shelves to flow into the deep ocean and form Antarctic Bottom Water, which plays a fundamental role in ocean circulation and global climate.

Additionally, these canyons channel warmer waters such as Circumpolar Deep Water from the open sea toward the coastline. This process drives the basal melting and thinning of floating ice shelves, which are critical for maintaining the stability of Antarctica’s interior glaciers.

The study emphasizes that current ocean circulation models do not accurately reproduce the physical processes that occur at local scales between water masses and complex topographies like canyons. These processes include current channeling, vertical mixing, and deep-water ventilation, which are essential for the formation and transformation of cold, dense water masses like Antarctic Bottom Water.

The researchers conclude that further gathering of high-resolution bathymetric data in unmapped areas, observational data both in situ and via remote sensors, and improvement of climate models will be necessary to better represent these processes and increase the reliability of projections on climate change impacts.

The world’s oceans have reached unprecedented levels of heat, according to a recent study. The research reveals that the 2023 global marine heatwaves (MHWs) were more intense, prolonged, and widespread than ever recorded before. This phenomenon poses significant threats to marine life and has severe economic implications for industries like fisheries and aquaculture.

Marine heatwaves are episodes of abnormally warm ocean temperatures that can last for months. They often result in mass coral bleaching events and the death of countless marine species. Climate change is driving an alarming increase in these events, making it essential to understand their causes and consequences.

The 2023 MHWs affected regions across the globe, including the North Atlantic, Tropical Pacific, South Pacific, and North Pacific. However, researchers have struggled to pinpoint the exact drivers behind these events. To shed more light on this issue, scientists analyzed satellite data and ocean reanalysis information from various sources, including the ECCO2 project.

The results showed that the 2023 MHWs set new records for intensity, duration, and geographic extent. They lasted four times longer than the historical average and covered an astonishing 96% of the world’s oceans. The most significant warming occurred in the North Atlantic, Tropical Eastern Pacific, North Pacific, and Southwest Pacific regions.

Researchers discovered that increased solar radiation due to reduced cloud cover, weakened winds, and ocean current anomalies contributed to the formation and persistence of these events. These findings suggest a fundamental shift in ocean-atmosphere dynamics, which may be an early warning sign of an approaching climate tipping point.

The consequences of this tipping point could be catastrophic for marine ecosystems, global economies, and human societies as a whole. It is crucial that policymakers and researchers work together to address the root causes of these heatwaves and develop strategies to mitigate their impact.