Three Newly Discovered Species of Abyssinian Snail in the Pacific Ocean

Marine biologists have identified three new species of deep-sea catanus fish belonging to the Lipalidae family in the Eastern Abyssian area of the Pacific (depths of 3,268-4,119 m).



In situ images of Careproctus colliculi in Monterey Bay, California, USA. Image credit: mbari.

The family of these fish, known as Repalidae, thrives in temperate to cold waters across the ocean basin.

These species play a significant role in ecosystems ranging from the intertidal zones to the hadal trenches (over 6,000 m).

They are well adapted to various habitats, likely due to their rapid evolutionary rates.

In shallower waters, these fish utilize specialized ventral suction discs to cling to rocks, adopting a curled, snail-like posture which gives rise to their common English name.

“The family Ripalidae comprises 31 accepted genera and 450 recognized species, with 43 being described in the last decade,” stated Dr. Mackenzie Gellinger from the State University of New York.

“At the family level, these fish are distinguished by their skate-like body, ventral suction discs formed by modified pelvic fins in many genera, and their elongated body structure.”

“Given the ecological significance of this family, the rapid discovery of new snail fish, and the important efforts needed to revise catanus classification, studying snail taxonomy is essential for advancing our understanding of marine biodiversity.”

The three new species are the bumpy snail (Careproctus colliculi), the dark snail (Careproctus yanceyi), and the sophisticated snail (Paralyparis em).

Paralyparis em and Careproctus yanceyi were collected using a suction sampler from a depth of 4,100 m via the human occupied vehicle (HOV) Albin on the R/V Atlantis.

Careproctus colliculi was gathered by remotely operated vehicles (ROVs) Doc Ricketts on the R/V Western Flyer using a suction sampler from under 100 km off the coast of Monterey Bay, California.

To describe these new species, the authors utilized microscopy, micro-computed tomography (Micro-CT) scans, and meticulous measurements to gather specific data on size, shape, and various physical characteristics such as fin rays and vertebrae for each fish.

Careproctus colliculi is identified by its pink body, 22 cerebral rock rays, rounded head, eight caudal rays, large eyes, and well-formed wing-like structure that creates a large suction disc,” they explained.

Careproctus yanceyi features a medium-sized abdominal suction disc, a single nostril, and six branched rays, distinguishing it from other Eastern Pacific deep-sea snails, which have round heads and entirely black bodies with horizontal mouths.”

Paralyparis em is marked by its long, black, laterally compressed body, absence of a suction disc, sharply angled jaw, a single chest radial, anteriorly positioned anal fin, and five branched rays.”

Researchers also sequenced the DNA of the fish and compared it with other snail species to contextualize the new species within their evolutionary framework.

“Taxonomic methods are crucial for comprehending the organisms we share our planet with and for studying and safeguarding global biodiversity,” Dr. Gellinger asserted.

“The deep sea is home to an astonishing variety of creatures with remarkable adaptations.”

“These three catanus fish serve as a reminder of how much remains unknown about life, the thrill of curiosity, and the power of exploration on Earth.”

The research findings are detailed in a new paper published in the journal Ichthyology and Herpetology.

____

Mackenzie E. Gellinger et al. 2025. Description of three newly discovered Abyssal snails (Liparidae) from the Eastern Pacific Ocean. Ichthyology and Herpetology 113(3): 487-506; doi: 10.1643/i2024069

Source: www.sci.news

Ecosystem Unearthed 30,000 Feet Beneath the Pacific Ocean

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Researchers have identified flourishing ecosystems of clams, tubeworms, and other species more than 30,000 feet deep in the Pacific Ocean. According to findings published in the Nature Journal, these represent “the deepest and most extensive chemical synthesis-based communities recognized.”

Source: www.nbcnews.com

Private Space Flights Conclude with Pacific Splashdown for Astronauts from India, Poland, and Hungary

Cape Canaveral, Florida – a Private Space Flight from Poland and Hungary, featuring India’s first astronaut in over 40 years, concluded on Tuesday with a splashdown in the Pacific Ocean.

The SpaceX capsules detached from the International Space Station on Monday and parachuted into waters off Southern California less than 24 hours later.

Hungarian Tibor Kapu emerged from SpaceX capsules in Southern California on Tuesday.
SpaceX via AP

The four-member crew launched nearly three weeks ago on a mission arranged by Axiom Space from Houston.

Axiom’s Peggy Whitson, the most seasoned U.S. astronaut, served as commander. She was joined by Shuvansch Shukla from India, Slouz Uznansky Wysniewsky from Poland, and Tibor Kap from Hungary, with the countries collectively investing over $65 million in the mission.

SpaceX capsules carrying four astronauts parachute into the Pacific Ocean off Southern California on Tuesday.
SpaceX via AP

“Thank you for the wonderful ride and safe journey,” Whitson remarked post-splashdown. Her record now surpasses that of other American astronauts and women, encompassing a total of 695 days in space across five missions.

The visiting astronauts executed numerous experiments in orbit, celebrating their heritage. The last instance of India, Poland, and Hungary sending individuals into space was in collaboration with the Soviet Union during the late 1970s and 1980s. They waved and smiled as they exited the capsule one by one into the dim early morning.

Poland’s Slouz Uznanski Wysniewski made landfall in Southern California on Tuesday.
SpaceX via AP

This marked Axiom’s fourth mission for the orbital forward base since 2022 and is part of NASA’s ongoing efforts to expand access to space for more businesses and individuals. The company is among those developing their own space stations to succeed the current one. NASA plans to retire its space station by 2030 after over 30 years of service.

Source: www.nbcnews.com

Denisovan Expands its Territory to the Pacific Coast of Asia

For decades, fishermen sailing off the coast of Taiwan have occasionally discovered bones from other large mammals that lived tens of thousands of years ago, such as elephants, buffaloes, and other large mammals.

However, in 2010, Taiwanese paleontologists were presented with a particularly strange discovery. This fossil looks like half the jaw of a gorilla. Scientists have been baffled by it ever since.

The mystery of the underwater jaw has now been solved. Wednesday, the researchers team made an announcement that it was part of Denisovan, a member of the mystical human lineage associated with the Neanderthals. This finding greatly expands the range of well-identified denisovan fossils previously known from Siberia and Tibet.

“Indeed, Denisovan was east all the way to the coast,” says Frido Welker, a molecular anthropologist and author of the new study.

Chun-hsiang Chang, a paleontologist at the National Museum of Natural Sciences of Taiwan, first learned about the jaws from a private collector in 2010. After examining it, he quickly determined that it did not belong to a gorilla, as gorillas and other apes have U-shaped jaws. Instead, the fossil jaws were angled outward from the jaw, just like ours.

However, the jaws were missing the prominent jaws seen in modern-day humans. “At the time, I thought it looked human, but not like modern-day human,” Dr. Chang said. “I thought it was very important, so I pushed the private collector to lend it to my museum.”

Over the next five years, Dr. Chang studied the jaw anatomy, working with an international group of scientists. Its shape resembles the jaws of extinct relatives of humans known to have lived in Asia for over a million years. However, Penghu 1 also had distinctive features, including large teeth.

Determining the age of Penghu 1 was also a challenge, as they were not sure exactly where Dr. Chang discovered it on the seabed. He and his colleagues analyzed the chemistry of the jaw and discovered that it resembles that of fossils of hyena species that evolved in East Asia about 400,000 years ago.

At that time, Taiwan was separated from the mainland by water. However, 190,000 years ago, sea levels fell sufficiently to create a land bridge that lasted until 130,000 years ago. The ocean then rose again until 70,000 years ago. This pattern continued until 10,000 years ago when another land bridge formed. Dr. Chang and his colleagues believe that Penghu 1 lived in one of these periods when sea levels were lower.

One possibility was that Penghu 1 belonged to a mysterious group of humans called Denisovans. Researchers discovered Denisovan in 2010 while examining fossils from the Siberian Denisova Cave. The bones of teeth and fingers contain ancient DNA with unusual mutations, revealing previously unknown human strains.

Subsequent research shows that Denisovans, Neanderthals, and modern humans share common ancestors who lived in Africa about 600,000 years ago. The Neanderthal and Denisovan ancestors migrated from Africa, and then these two lineages split about 400,000 years ago, with the Neanderthals spreading to Europe in the west.

Denisovan’s spread was difficult to chart. For years, the only known Denisovan fossils have been teeth and bone fragments found in Denisova caves. However, a valuable clue comes from living humans. Many people in East Asia and the Pacific today have small amounts of Denisovan DNA, suggesting that Denisovans must have interbred with East Asian Homo sapiens before their extinction and lived far beyond Siberia.

Dr. Chang and his colleagues noticed that the teeth in the Penghu 1 jaw resemble the teeth found in the Denisova Cave. But those clues were not enough to link them. They attempted to search for DNA in their jaws but found nothing. This was not surprising given that the Penghu 1 fossils had been sitting on the seabed for thousands of years.

After Dr. Chan’s team revealed their analysis in 2015, Penghu 1 became an even more enigmatic, human-like fossil at the museum. “Our research was stagnant,” Dr. Chan said.

Over the next few years, Dr. Welker and other researchers pioneered ways to recover ancient proteins from fossils. They discovered that even if a fossil loses all its DNA, it could still retain protein fragments.

Using such methods, Dr. Welker studied the 160,000-year-old jaws found in a high-altitude cave in Tibet. In 2019, the team reported that Tibetan fossils contained fragments of ancient collagen and other proteins.

These proteins resemble modern human proteins but also exhibit differences indicating that the jaw belonged to a Denisovan.

With that discovery, Dr. Welker searched other Asian fossil scientific literature for jaws resembling the Tibetan jaws that could be tested for proteins.

“That’s when the lower jaw of Penghu came on my radar,” he said.

Both the Tibetan and Taiwanese jaws had very large teeth. Dr. Welker and his colleagues reached out to Dr. Chang. In 2023, Dr. Chang and his team flew to Copenhagen with their jaws. Analysis of the results revealed protein fragments that were only present in Denisovans.

“Since the first publication of Penghu’s lower jaw, many of us thought it might be Denisovan, mainly based on being in the right place at the right time,” said Bens Viola, a paleontologist at the University of Toronto, who was not involved in the study. “But of course, assumptions are assumptions, and we need actual data to validate them.”

Another clue came from fragments of enamel protein in the teeth. Modern humans carry enamel genes on the X chromosome, while men carry slightly different enamel genes on the Y chromosome. Denisovan was carrying the Y-chromosome version, indicating that it belonged to a male adult.

The two Denisovan jaw anatomy may turn out to be a hallmark of male Denisovan. Women’s Denisovan may have a thinner anatomy, but scientists will need more evidence to know for sure.

The discovery of other Denisovan fossils could expand the scope of humanity. In 2022, researchers found teeth from 160,000 years ago in a cave in Laos. They resemble the teeth of the jaw in Tibetan Denisovan. Anyone who lived there would have had to survive in the tropical forests far from Siberia.

However, Laos’ teeth do not contain DNA, and the protein fragments did not clarify the type of human it belonged to. However, the cave and its neighbors still retain many teeth that have not been fully analyzed. Other traces of Denisovan may not have been found in the museum yet.

But so far, evidence reveals that Denisovans were able to thrive for thousands of miles and in a variety of environments. Janet Kelso, a paleontologist at the Max Planck Institute for Evolutionary Anthropology, was impressed by the differences between the Penghu 1 protein and the protein found in Tibet. As Denisovans expanded throughout different environments, they adapted and became genetically distinct populations.

“There’s still a lot to learn about Denisovan,” she said.

Source: www.nytimes.com

Researchers find unusually high levels of cosmic formation beryllium in the Pacific Ocean

A team of scientists from Helmholtz Senturm Dresden Rossendorf, Tad Dresden Institute of Technology, and the Australian National University have discovered an “unexpected” accumulation of Beryllium-10 from the bottom of the central and North Pacific Oceans.

Col et al. Report on the discovery of anomalies in the beryllium-10 concentration profiles of several deep-sea ferromanganese crusts (stars) from the late Miocene central and North Pacific Oceans. The main bottom (blue line) and surface (red line) ocean currents of the thermal halin circulation are shown. Image credit: Koll et al., doi: 10.1038/s41467-024-55662-4.

Radionuclides are types of nuclei (isotopes) that decay into other elements over time.

They are used to date archaeological and geological samples, and radiocarbon dating is one of the best-known methods.

“The major ocean floors on Earth show one of the most pristine geological archives documenting environmental conditions and changes over millions of years, the ferromanganese crust,” Zentrum Dresden-Rossendorf and his colleagues.

“Dating these marine archives can be achieved through fossils through changes in biostratigraphy, isotope, or elemental composition. Alternatively, we can analyze the imprinted changes in the Earth's magnetic field due to magnetic stratigraphy. Masu.”

“Another commonly employed technique is dating space-forming nuclides,” they added.

“The radionuclide Beryllium-10 is continuously produced in the upper atmosphere, primarily through cosmic ray spallation for nitrogen and oxygen.”

“The residence time of Beryllium-10 in the atmosphere is about 1-2 years for it to adhere to the aerosol and precipitate.”

“In the ocean, atmospheric beryllium-10 mixes with the stable beryllium-9 of the lithosphere, which is transported to the ocean by river runoff and river dust, primarily after erosion of terrestrial minerals.”

Dr. Koll and co-authors have discovered long-term cosmicogenic beryllium-10 anomalies in central and North Pacific samples.

Such anomalies can be attributed to changes in ocean currents or astrophysical events that occurred during the late Miocene era around 10 million years ago.

The findings have the potential to serve as a global time marker for promising advances in dating geological archives over millions of years.

“For a period of millions of years, such space-forming time markers still do not exist,” Dr. Koll said.

“However, this beryllium abnormality can act as such a marker.”

result It will be displayed in the journal Natural Communication.

____

D. Koll et al. 2025. Cosmic genome 10It becomes abnormal in the late Miocene as an independent time marker for marine archives. Nut commune 16, 866; doi:10.1038/s41467-024-55662-4

Source: www.sci.news

Pacific Northwest prepares for severe weather from ‘bomb cyclone’ and atmospheric river

Thousands of homes lost power, as downed power lines and trees blocked highways in Washington state on Tuesday due to a powerful atmospheric river event, officials announced.

Forecasters stated that a storm could bring up to 15 inches of rain and heavy snowfall in the mountains. By 7 p.m. local time, about 100,000 homes and businesses in Washington and over 14,000 homes in Oregon were without power, as reported by news agencies on the Rack Website poweroutage.us.

The Bellevue, Washington, fire department warned, “Trees are falling across the city, hitting homes.” They advised residents to stay away from windows and not to go outside if possible. X was contacted on Tuesday around 8pm.

Weather forecasters warned of a whiteout snowstorm in the Cascade Range and possible 2 feet of snow in Mount Shasta, Northern California, along Interstate 5. High wind gusts of up to 90 mph were recorded on Mount Rainier and 52 mph in Seattle-Tacoma International Airport.

Known as bomb cyclones, these intense winds are caused by rapidly intensifying storm systems with decreasing atmospheric pressure. Scientists attribute this phenomenon to climate change generating more atmospheric rivers, which are significant contributors to precipitation on the West Coast.

An atmospheric river storm could bring significant rainfall over a three-day period in Northern California, with a flood watch issued in several areas. These storms help replenish water supplies after dry summers, but can also lead to severe flooding and damage.

Satellite images show a weather system moving towards the Pacific Northwest, prompting concerns of damaging winds, rain, and snow. Climate scientists are closely monitoring the storm and its potential impacts on various regions.

Satellite images show the weather system moving closer to the Pacific Northwest on Tuesday morning.
NOAA

As the storm progresses, residents in affected areas are advised to stay updated on weather alerts and follow safety guidelines to minimize risks and potential damage.

Source: www.nbcnews.com

Scientists uncover enigmatic subduction zone beneath Pacific Ocean

According to a team of geoscientists from the University of Maryland and the University of Maryland, between 250 million and 120 million years ago during the Mesozoic Era, the ancient ocean floor was formed by the East Pacific Rise, a plate boundary at the bottom of the southeastern Pacific Ocean. It is said to have sunk deep into the earth. University of Alberta.



A map of the East Pacific Ridge region where the ancient ocean floor was discovered. Image credit: Jingchuan Wang.

University of Maryland researcher Jingchuan Wang and his colleagues used innovative seismic imaging techniques to look deep into the Earth's mantle, the layer between the Earth's crust and core.

They discovered an unusually thick region in the mantle transition zone at depths of about 410 to 660 km below the Earth's surface.

This zone separates the upper and lower mantle and expands or contracts depending on temperature.

The newly discovered ocean floor may also explain the unusual structure of the Pacific Large Low Shear Velocity Province (LLSVP), a huge region in Earth's lower mantle. Because LLSVP appears to be divided by slabs.

“This thickened area is like a fossil fingerprint of an ancient ocean floor that sank into the Earth about 250 million years ago,” Wang said.

“This gives us a glimpse into Earth's past that we've never seen before.”

Subduction occurs when one tectonic plate slides beneath another and surface material is recycled into the Earth's mantle.

This process often leaves behind visible evidence of movement, such as volcanoes, earthquakes, and deep ocean trenches.

Geologists, on the other hand, typically study subduction by examining rock samples and sediments found at the Earth's surface.

By studying how seismic waves travel through the different layers of the Earth, researchers were able to create a detailed map of the structures hidden deep within the mantle.

“You can think of seismic imaging as similar to a CT scan. Essentially, it allows us to see a cross-section of the Earth's interior,” Dr. Wang said. .

“Typically, chunks of ocean material are completely consumed by the Earth, leaving no discernible traces on the surface.”

“But looking at ancient subducted slabs through this perspective has provided new insights into the relationship between the Earth's very deep structures and surface geology that were not previously clear.”

What the authors discovered surprised them. Matter was moving much more slowly through the Earth's interior than previously thought.

The unusual thickness of this region they found suggests the presence of cold material in this part of the mantle transition zone, where parts of the oceanic slab become stuck in the middle as they sink through the mantle. It suggests that there is.

“We found that material is sinking at about half the rate expected in this region. This may be due to the mantle transition zone acting like a barrier, slowing the movement of material through the Earth. “This suggests something,” Dr. Wang said.

“Our findings raise new questions about how the deep Earth influences what we see at the surface over vast distances and time scales.”

of result Published in a magazine scientific progress.

_____

Wang Jingchuan others. 2024. Intraoceanic subduction during the Mesozoic era formed the lower mantle beneath the East Pacific uplift. scientific progress 10(39);doi: 10.1126/sciadv.ado1219

Source: www.sci.news

Fires persist on the Pacific Crest Trail, leading to closures and evacuations

The Pacific Crest Trail (PCT) is facing increasing challenges due to wildfires and their aftermaths, making sections of the trail hazardous and leading to sudden road closures. Long-distance hikers are experiencing significant environmental transformations as wildfires ravage the area, while rural communities near the trail are stepping up to assist hikers during wildfire emergencies.

According to Riley, wildfires are becoming more frequent and unpredictable, affecting a larger number of trails, users, and communities. The PCT, which traverses diverse terrains like the Mojave Desert, Sierra Nevada Mountains, and Cascade Mountains, attracts thousands of long-distance hikers and hundreds of thousands of day hikers annually.

However, the combination of global warming-induced extreme temperatures and decades of aggressive fire suppression has led to intense wildfire seasons altering the landscape along the PCT. Climate change effects are noticeable along the trail, with local weather scientist John O’Brien remarking, “This is an extended tour of climate history.”

Trail crews on the Pacific Crest Trail pass through burned areas of the Eagle Creek Fire in the Columbia River Gorge near Portland, Oregon, in 2018.Jamie Hale/The Oregonian via The Associated Press

Apart from fire risks, climate change is intensifying water scarcity along the trail and affecting wildlife populations. Glacial retreat in higher elevations is exposing more slippery rock, while river levels are peaking earlier in the season, leading to hazardous crossings.

Hikers like Karen Altergott have faced extreme weather conditions, from heavy late-season snowfall to intense heat waves, prompting concerns about the impact on health. Altergott emphasized the need for preparedness and flexibility when dealing with changing trail conditions.

Karen Altergott.Courtesy of Karen Altergott

The PCT community is coming together to tackle these challenges, with the Pacific Crest Trail Association releasing a smartphone app to help hikers navigate wildfire closures. Local “trail angels” are also stepping up to provide aid, transport, and support to stranded hikers during emergencies.

Becky Wade and her partner Jeff McCabe.Courtesy of Becky Wade

Becky Wade and Jeff McCabe, who have experienced evacuations due to wildfires, exemplify the importance of community support. Their efforts in assisting hikers around fire-affected areas highlight the crucial role of local residents in ensuring hiker safety along the PCT.

Although wildfires and their aftermath present challenges, hikers like Will Geolis attest to the enduring value of the PCT experience. While adapting to changing trail conditions is necessary, the trail’s community and scenic beauty remain priceless.

Joris aptly sums up the essence of the PCT experience, emphasizing that it’s the people and the journey that truly matter, rather than completing a continuous hike along the trail.

Source: www.nbcnews.com

Scientists obtain sharper images of fault lines posing a threat to the Pacific Northwest

A silent colossus lurks off the Pacific coast, threatening hundreds of miles of coastline with tsunamis and devastating earthquakes.

For decades, scientists have been warning about the possibility of a major fault line breaking off from the Cascadia Subduction Zone, a megathrust fault that runs offshore along the coast from northern Vancouver Island to Cape Mendocino in California. The next time this fault, or parts of it, breaks, it could upend life in Oregon, Washington, and Northern California.

Of particular concern are signs of great earthquakes in the region’s geological history. Many researchers have been pursuing clues about the last “big quake,” a magnitude 8.7 earthquake that occurred in 1700. They have pieced together this history using centuries-old tsunami records, Native American oral histories, physical evidence of saltwater-flooded ghost forests, and limited maps of faults.

But no one had ever comprehensively mapped the fault structure until now. The study published Friday A paper published in the journal Science Advances describes the data collected during a 41-day research voyage, in which the ship dragged a mile-long cable along the fault, listening to the ocean floor and piecing together images.

The team completed a detailed map of the subduction zone, stretching more than 550 miles to the Oregon-California border.

Their work will give modelers a clearer picture of the impact of a megaquake in the region — a megaquake that occurs in a subduction zone, where one plate pushes under another — and give planners a more detailed, localized view of the risks to Pacific Northwest communities, which could help redefine earthquake-resistant building codes.

“It’s like wearing Coke-bottle glasses, and when you take them off, they give you the correct prescription,” said lead author Suzanne Calbott, a marine geophysicist and research professor at Columbia University’s Lamont-Doherty Earth Observatory. “Before, we only got very blurry, low-resolution images.”

Scientists have discovered that subduction zones are much more complex than previously thought. They are divided into four segments, and researchers believe each segment could rupture independently or simultaneously. Each segment has different rock types and different seismic properties, which means some segments may be more hazardous than others.

Earthquake and tsunami modelers are beginning to assess how the new data might affect earthquake scenarios in the Pacific Northwest.

Kelin Wang, a research scientist with the Geological Survey of Canada who was not involved in the study, said her team, which focuses on earthquake hazards and tsunami risk, is already using the data to make predictions.

“The accuracy and resolution is truly unprecedented, and this is an incredible dataset,” said Wang, who is also an adjunct professor at the University of Victoria in British Columbia. “This will allow us to better assess risk and inform building codes and zoning.”

Harold Tobin, co-author of the paper and director of the Pacific Northwest Seismic Network, said the data will help fine-tune predictions, but it won’t change the untenable reality of life in the Pacific Northwest.

“It could potentially produce earthquakes and tsunamis that are comparable in magnitude to the largest earthquakes and tsunamis the Earth has ever seen,” said Tobin, who is also a professor at the University of Washington. “It looks like Cascadia could produce an earthquake of magnitude 9 or a little less or a little more.”

A quake of that magnitude could cause shaking for about five minutes and generate a tsunami up to 80 feet high, damaging more than 500,000 buildings. According to emergency planning documents:.

Neither Oregon nor Washington are adequately prepared.


To map the subduction zone, researchers at sea used active seismic imaging, a technique that sends sound waves into the ocean floor and processes the returning echoes, a method often used in oil and gas exploration.

They towed more than nine miles of cables called streamers behind the ship and used 1,200 hydrophones to capture the returning sounds.

“This will give us an idea of ​​what the conditions are like underground,” Calbot said.

The research vessel Marcus Langes docked in Seattle after a 41-day survey along the Pacific coast that allowed researchers to map the Cascadia Subduction Zone.
Courtesy of Harold Tobin

Trained marine mammal spotters would alert the crew to any signs of whales or other animals. Sounds produced by this type of technology could be disruptive and potentially harmful to marine life.

Calbot said the new research makes it even clearer that the entire Cascadia Fault won’t rupture all at once.

“The next earthquake in Cascadia could rupture just one of these segments, or it could rupture the entire boundary,” Calbot said, adding that some individual segments are thought to have the potential to produce a quake of at least magnitude 8.


Over the past century, scientists have observed only five earthquakes of magnitude 9.0 or higher, all of which were the kind of giant quakes predicted in the Cascadia subduction zone.

Scientists have compiled the latest insights into the 1700 Cascadia earthquake, based on records of an unusual orphan tsunami that was not preceded by any shaking in Japan.

“It would take a magnitude 8.7 earthquake to send a tsunami all the way to Japan,” Tobin said.

Those in Japan who recorded the event had no idea that the earthquake occurred across the ocean in what is now the United States.

Right now, the Cascadia subduction zone is eerily quiet. At other subduction zones, Calbot says, scientists often observe small, frequent earthquakes that make it easier to map the region. But that’s not the case here.

Scientists have a few hypotheses as to why. Wang said the region could be getting quieter as stress builds on the fault, and that time may be approaching.

“The interval between big earthquakes in this subduction zone is about 500 years,” Wang said. “It’s hard to know exactly when it will happen, but it’s certainly quite late compared to other subduction zones.”

Source: www.nbcnews.com

Scientists uncover five previously unknown hydrothermal vents in the Pacific Ocean

Scientists on board the research vessel atlantis Five new deep-sea hydrothermal vents have been discovered on the ocean floor at a depth of 2,550 meters (1.6 miles). All exhaust fluids are hotter than 300 degrees Celsius (570 degrees Fahrenheit).



vehicle carried by humans alvin Arrived at the ocean floor. Image credits: J. McDermott, Lehigh University / T. Barreyre, CNRS / R. Parnell-Turner, Scripps Institution of Oceanography / D. Fornari, Woods Hole Oceanographic Institution / National Deep Diving Facility / Alvin Group.

Hydrothermal vents are rich in chemicals that provide energy for animal life, fueling rich and productive ecosystems.

The location of the new hydrothermal vent was discovered by a team of scientists during a research expedition funded by the National Science Foundation.

They are located on the East Pacific Ridge near 10 degrees north latitude and are part of the trans-Earth mid-ocean ridge volcanic mountains, where two tectonic plates are breaking apart at a rate of about 11 cm (4.3 inches) per year.

Expedition researchers used underwater robots to map the area at night guard.

rear guard Retrieved each morning, high-resolution maps from the vehicle’s sensors were used to plan the day’s dives by the manned vehicle. alvinThis gives scientists a first-hand look at the complex and ever-changing environments of places like the East Pacific Rise.

“High-resolution maps are guard There is a possibility that new hydrothermal areas will be discovered soon guard will be back on deck,” said Dr. Jill McDermott, a researcher at Lehigh University.

“This gives us great goals such as: alvin And the opportunity to make multiple discoveries in one dive.”

scientists infiltrate alvin He first discovered a hydrothermal vent in 1977 while exploring an oceanic ridge north of the Galapagos Islands.

The discovery has reshaped scientists’ understanding of the conditions that can support life on Earth and elsewhere in the solar system.

“Mid-ocean ridges account for more than 75% of all volcanic activity on Earth,” said CNRS researcher Dr. Thibault Valley.

“There are thousands of these deep-sea hot springs, which together extract 10 percent of the Earth’s total internal heat.”

“We want to better understand how hydrothermal vents release heat and chemicals as they flow beneath the ocean floor, impacting global oceans.”

“new guard “Using the map, we can see vital details of lava flows erupting in the deep ocean and target them for rock sample collection, just as geologists do on land.” said Dr. Daniel Fornari, a researcher at the institute.

“These new perspectives and analysis of rock samples will help us understand how fast the lava erupted, how far it traveled, and how deep-sea lava eruptions affect hydrothermal eruptions. I guess.”

“By working together these two state-of-the-art deep-sea submersibles, we will make surprising new discoveries about how the deep sea floor is constructed in some of the harshest environments on Earth. Yes, we can,” said Dr. Ross Parnell Turner., a researcher at Scripps Institution of Oceanography.

Source: www.sci.news

Discovery of four new species of deep-sea octopus in the Pacific Ocean

Marine biologist at Schmidt Ocean Institute R/V Falco Two expeditions in 2023 exploring seamounts off Costa Rica's Pacific coast discovered at least four new species of deep-sea octopus.



A newly hatched octopus swims away from its egg near a small rocky outcrop informally known as El Dorado Hill. Image credit: Schmidt Ocean Institute.

“The impact is that R/V Falco Research to understand Costa Rica's deep Pacific Ocean will continue into the future and hopefully generate awareness that will lead to policies that protect the country's deep sea,” said Dr. Jorge Cortés, a researcher at the University of Costa Rica.

“We hope this expedition will inspire new generations. Further international cooperation is needed to increase knowledge about our deep-sea heritage.”

During the first expedition in June 2023, Dr. Cortes and colleagues discovered two octopus farms associated with thermal springs.

Six months later, they returned to the nursery and confirmed that they appear to be active year-round.

They also observed several other new species of octopus away from the hot springs.

One of the new species belongs to the genus Octopus Muusocops The octopus is named after the small rocky outcrop, informally known as El Dorado Hills, where it was first discovered.

This is a different species, closely related to, but a different deep-sea octopus farm, found in California's Davidson Seamount in 2018.

Of the four new species in Costa Rica, only the dorado octopus was observed spawning in hot springs.

This discovery is Muusocops This genus evolved to raise its eggs in warm springs on the ocean floor.

“After hard work, our team has discovered a new hydrothermal spring off the coast of Costa Rica, which has become a nursery for deep-sea octopuses and a unique biodiversity site,” said Dr. Beth Orcutt, a researcher at the Bigelow Institute of Marine Science. We confirmed that this is the habitat.”

“It was less than 10 years ago that low-temperature hydrothermal eruptions were detected in ancient volcanoes located far from mid-ocean ridges.”

“These locations are very difficult to find because you can't detect any trace of it in the water column.”

Researchers also discovered a thriving deep-sea skating nursery on the top of another seamount in Costa Rican waters, which they named Skatepark.

They also discovered three hydrothermal springs within the region, located 10 to 30 nautical miles from each other.

These springs all differ from each other in the temperature and chemistry of their fluids, indicating that unique reaction processes drive their formation.

“The Schmidt Ocean Institute supports the global scientific community wherever it is located. Falcor ” said Dr. Jyothika Virmani, Executive Director. Schmidt Ocean Institute.

“Dr. Cortés and Dr. Orcutt have assembled a team that truly embodies international collaboration that empowers Costa Rica's domestic scientists and enriches local knowledge and understanding of the ocean.”

“We look forward to operating off the coasts of Peru and Chile in 2024 and welcoming scientists from South America.”

Source: www.sci.news

Should the Great Pacific Garbage Patch be a priority for plastic cleanup efforts?

Fish caught in discarded nets in the Great Pacific Garbage Patch

Ocean Voyages Institute/ZUMA Wire/Shutterstock

It was a bright sunny day in September 2023. Excitement filled the air and a rainbow appeared on the horizon as the team slowly pulled a giant net out of the glistening sea. ocean cleanup This project was trialling System 03 in the North Pacific. Basically she had two ships dragging a 2.2 kilometer long net designed to remove as much trash as possible. This time it was filmed for a promotional video, with one scoop weighing a record-breaking 18 tons.

Ocean Cleanup was founded in 2012 on the simple premise of trawling ocean plastic hotspots and mopping up floating debris. After years of testing and refining the technology, the organization says it is now ready to begin the planned cleanup of the Great Pacific Garbage Patch, a vast collection of plastic waste located between Hawaii and California. There is.

That sounds like a laudable goal. But in recent years, marine scientists have warned that efforts to mechanically remove plastic from the ocean are not only futile, but potentially harmful. It’s a waste, as we know that much of the ocean’s plastic waste is too small or out of reach to capture. And it’s probably harmful for two reasons. Firstly, new research shows that marine debris patches are home to all kinds of marine life, and secondly, cleanup efforts have removed such waste from its source. This is because efforts to stem the flow of the virus may be hindered.

So, given what we know…

Source: www.newscientist.com