Wednesday, March 20, 2024

4394 - FIRE - under the ocean?

 

-    4394  -  FIRE   -  under the ocean? -  A sleeping subduction zone could awaken and form a new 'Ring of Fire' that swallows the Atlantic Ocean.   This slumbering subduction zone below the Gibraltar Strait is active and could break into the Atlantic Ocean in 20 million years' time, giving birth to an Atlantic "Ring of Fire."

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--------------------------  4394 -      FIRE   -  under the ocean?

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-    This subduction zone is creeping westward and could one day "invade" the Atlantic Ocean, causing the ocean to slowly close up.   The subduction zone, also known as the “Gibraltar arc” or trench, currently sits in a narrow ocean corridor between Portugal and Morocco.

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-    Its westward migration began around 30 million years ago, when a subduction zone formed along the northern coast of what is now the Mediterranean Sea, but it has stalled in the last        5 million years, prompting some scientists to question whether the Gibraltar arc is still active today.

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-   It appears that the arc is merely in a period of quiet.  This lull will likely last for another 20 million years, after which the Gibraltar arc could resume its advance and break into the Atlantic in a process known as "subduction invasion."

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-   The Atlantic Ocean hosts two subduction zones that researchers know of,  the “Lesser Antilles” subduction zone in the Caribbean and the “Scotia arc”, near Antarctica.   These subduction zones invaded the Atlantic several million years ago.   We are approaching the tipping point.

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-    Modeling of this kind requires advanced tools and computers that weren't available even a few years ago.  We can now simulate the formation of the Gibraltar arc with great detail and also how it may evolve in the deep future.

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-    If the Gibraltar arc invades the Atlantic Ocean, it could contribute to forming an Atlantic subduction system analogous to a chain of subduction zones that circles the Pacific Ocean, called the “Ring of Fire”. A similar chain forming in the Atlantic would lead to oceanic crust being recycled into the mantle via subduction on both sides of the Atlantic, gradually swallowing and closing up this ocean.

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-    The Gibraltar arc's grinding advance over the last 5 million years could explain the relative lack of seismicity and volcanism in the region. The subduction zone's tectonic silence is a direct result of its extended period of stalled movement.

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-    If the movement along the subduction interface were small, the accumulation of the seismic strain would be slow and may take hundreds of years to accumulate.  This agrees with the long recurrence period estimated for big earthquakes in the region.

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-   Although many smaller earthquakes have been recorded since, the last major earthquake to rock the region was the “1755 Great Lisbon Earthquake”, which reached an estimated 8.5 to 9.0 on the moment magnitude scale.

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-    What are the deepest spots in Earth's oceans?  Could there be a volcano down there?

What types of sea creatures live at these depths?   There are deep realms on our planet that seem almost extraterrestrial. Translucent fish flit back and forth while strange, flower-like crinoids sway in the water. But of all the submarine canyons and trenches out there, what are the deepest, darkest spots in each of the world's five oceans?

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-   The deepest place in the Pacific Ocean (and on Earth) is the Mariana Trench. The trench's deepest point is the Challenger Deep near the U.S. territory of Guam.  This is a plunge that's almost 36,000 feet below the water's surface.

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-    The deepest region in the Atlantic Ocean is the Milwaukee Deep in the 27,585-foot-deep axis of the Puerto Rico Trench. Coming in at 23,917 feet deep is a nameless region at the bottom of the Indian Ocean.

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-     The Southern Ocean (also known as the Antarctic Ocean) goes all the way down to 24,229 feet in the South Sandwich Trench, and the Arctic Ocean goes down to 16,000 feet deep at Molloy Deep in the Fram Strait.

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-    Such areas are far from the reach of the sun and may appear to be nothing but gaping mouths of impenetrable darkness. But what do scientists know about these final frontiers?  Why are there so many giants in the deep sea?

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-   The Mariana Trench is a 1,580-mile-long oceanic abyss where several of the planet's deepest points can be found.   Only 27 people have ever been to the Challenger Deep, the Mariana Trench's deepest point: The first to go there were explorer Jacques Piccard and Navy Lt. Don Walsh, who ventured there in 1960.

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-   Mackenzie Gerringer went on an expedition in 2014 to the 34,448-foot-deep Sirena Deep (one of the other deepest parts of the trench) with colleagues from the University of Hawaii at Mānoa.    There's no sunlight.  Temperatures are cold, typically about 1-2°C [33.8 to 35.6 degrees Fahrenheit]. Pressures are high, up to 15,000 pounds per square inch at the ocean's greatest depths. 

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-   Despite the extreme conditions, life exists in the deepest parts of our planet's seas.   The types of creatures that thrive at extreme depths tend to be similar, even though different species might be unique to different regions.  Certain creatures appear at specific depths.  The bottom of a species' depth range is controlled by adaptations to pressure, and the top of its range may be controlled by predation or competition.

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-    During Gerringer's expedition they discovered a new species of Mariana snailfish. The newfound critter was a hadal snailfish, named for the hadal zone, the part of the ocean that is between about 19,700 feet and 36,000 feet deep and only occurs in marine trenches.

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-   Critters like this are specially adapted to survive in the deep extreme pressures that push against the body and impair enzymes and proteins. Mariana snailfish and other hadal species are equipped to handle this with enzymes that operate more effectively under extremely high pressure. They also produce a molecule known as TMAO (trimethylamine N-oxide) to keep the pressure from messing with the proteins in their bodies.

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-   In the Mariana Trench,16,000 feet  down, cusk eels and rattail fish swam among decapod shrimp. As probe cameras dove deeper, these species gave way to snailfish and giant amphipods, and deeper still, different species of mostly smaller amphipods and shrimp appeared. The deepest at which any fish were seen was 26,250 feet.

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-     Off the coast of Puerto Rico and south of the tip of Florida, the Puerto Rico Trench is evidence of an ancient subduction event.  Most of these hadal habitats are trenches that form via subduction, where one tectonic plate slides under another, creating a deep valley.

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-    Shifting tectonic plates also explain the presence of a group of volcanic islands scattered nearby, as subduction is the same kind of tectonic activity that can cause magma to rise up from beneath Earth's crust.

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-    Those are not the only volcanoes around this trench. Deep underwater, a volcano that erupted in mud was found close to the 26,000-foot-depth mark.   Areas around this trench are prone to earthquakes and tsunamis because of subduction. There is even a fault in the Puerto Rico Trench that looks eerily like a submerged version of the San Andreas Fault.

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-   The deepest part of the trench is the Milwaukee Deep, which explorer Victor Vescovo dived to in a crewed submersible in 2018 (Vescovo had previously gone down to the Mariana Trench and was the first person to ever dive to the Challenger Deep twice).

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-    The deepest parts of the Indian Ocean's Java Trench and the Antarctic Ocean's South Sandwich Trench were both determined by the Five Deeps Expedition (FDE) in 2021.  These unnamed regions had been mostly unexplored.   The South Sandwich Trench, the only hadal zone on Earth that experiences sub-zero temperatures, had not been explored at all before this mission.

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-    The expedition's researchers explored the hidden depths of the ocean by sending down remotely operated vehicles (ROVs). The team used a Deep Submergence Vehicle (DSV) and three additional landers, robots carrying multiple instruments, such as sensors, that fall to the bottom and probe the seafloor.

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-    In the Java Trench, cameras on the FDE landers observed hadal snailfish, sea cucumbers and weird-looking lifeforms, such as a sea squirt that floated in the dark waters like a ghostly balloon.  Topical Studies in Oceanography highlighted the fauna in the South Sandwich Trench. In these freezing waters, researchers found snailfish amphipods, brittle stars, sea cucumbers, sponges and crinoids.

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-    Going from the Antarctic to the Arctic Ocean, the Five Deeps Expedition next investigated the “Molloy Deep” in the Fram Strait, between the east of Greenland and the Svalbard islands off the northern coast of Norway. No other mission had ever seen the bottom of the Molloy Deebefore.

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-    In the Fram Strait, fluctuations in levels of fresh and salt water impact populations of phytoplankton and other microbes. Climate change has impacted the Arctic Ocean the most out of any of the world's five oceans, and the thickness of sea ice has been steadily decreasing since 1990.

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-    Few creatures live in the Molloy Deep. It is essentially an enormous crater, and organic matter gathers and falls down the sides, but there are not many creatures that inhabit this barren region, scientists at the Maier-Kaiser Lab (which is part of the Woods Hole Oceanographic Institution in Massachusetts) found when they searched it for larvae. The only animal that has been caught on camera there is a type of deep-sea sea cucumber known as a sea pig.

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-    The deep sea is closely connected to the surface oceans.  Human activities such as plastic pollution and climate change are already influencing deep-sea habitats and it's important that we understand, appreciate, and protect these ecosystems.

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March 18, 2023                 FIRE   -  under the ocean?                        4394

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--------------------- ---  Wednesday, March 20, 2024  ---------------------------------

 

 

 

 

 

           

 

 

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