Latest news with #Zanclean
Yahoo
29-04-2025
- Science
- Yahoo
How the biggest flood in the history of the Earth created the Mediterranean
Six million years ago, the Mediterranean Sea wasn't nearly as picturesque as it is today. It was barely even a sea; tectonic activity had raised a mountain range in the Strait of Gibraltar, cutting off the Mediterranean from the Atlantic. Without a constant inflow of water the sea evaporated under the baking sun, and all that remained were a few scattered, briny lakes surrounded by mile after mile of salt and gypsum. Today, scientists call this the Messinian Salinity Crisis: in the dying days of the Miocene epoch, most of the Mediterranean died. But if, on a certain day about 5.3 million years ago, you happened to go for a stroll along that mountain range, you might have discovered something odd: a trickle of water, making its way down one of the mountains from the Atlantic ocean beyond it. The mountains had been slowly sinking until their summits were level with the ocean's surface; one day, the mountains sank just enough for some of the water to spill over their edges. Once they did, the water carved an unstoppable path downhill. The trickle turned into a stream, which widened into a river, and soon the ocean was pouring into the desiccated Mediterranean basin with the force of a thousand Amazon Rivers, suddenly ending the 600,000-year-long dry spell. The water moved so quickly — 32 meters per second, or about 72 miles per hour, by the time it hit the coast of modern-day Sicily — that it dragged the air behind it, creating tropical storm-force winds as it moved. If you managed to somehow see through all the muddy sediment stirred up by the flood waters, you might have found a few surprised fish in the depths, stunned or struck dead outright by the force of the rapids that carried them in from the Atlantic. As the water refilled the Mediterranean, it ushered in a new geological era: the Zanclean. 'I don't think any human has ever seen anything like this,' says Aaron Micallef, a National Geographic Explorer and marine geoscientist at the Monterey Bay Aquarium Research Institute who studies this event, called the Zanclean megaflood. Micallef and his colleagues have spent years putting together the puzzle pieces of what the flood looked like, and this story is largely built on their research, which melds geologic evidence with computer modeling. While evidence for the flood is still accumulating, this is the scientist's best picture yet of what's likely the largest flood in the history of the Earth. Micallef and his colleagues found that the Mediterranean, which had been obliterated once when the sea dried up, was transformed completely again by the megaflood. The fossil record is difficult to read in much detail, but scientists think that before the sea dried up it was filled with all kinds of creatures, from ancient sharks and pinnipeds to fish and a rainbow of coral. Only eighty-six of the 780 or so species from the sea that existed before the salinity crisis have survived into the modern-day Mediterranean, and the fact that they lived through the flood is a minor miracle. Those creatures, a collection of mollusks, plankton, and one standout sea slug, most likely survived by finding refuge in the few patches of water that remained after the sea dried up. (Rome is teeming with mysterious crypts filled with popes—and secrets) As the water poured in, the western Mediterranean began refilling at a tremendous rate; Micallef estimates the water flowed at a rate of somewhere between 68 and 100 million cubic meters per second, filling the sea by as much as ten meters, or nearly 33 feet, each day. The weight of the rising waters pressed down on the Earth's crust, making it slide across the molten mantle underneath. This, says Daniel Garcia-Castellanos, a Geophysicist at CSIC Barcelona and a pioneer on research into the Zanclean megaflood, would have triggered earthquakes that rippled through the region. For the goat-antelope creature Myotragus, which had walked across the dry sea to make its home on modern-day Mallorca and Menorca, the earthquakes, water, and wind combined must have sounded like the roar of a monstrous predator — surely, this was the end of the world as they knew it. Eventually, the rising waters streamed over the lip of Sicily, and as the current moved east it ate away at the land, leaving behind hundreds of long ridges as if a giant hand had clawed through the dirt. A little bit further east, the water hit another wall that we now call the Malta Escarpment. This barrier divided the Mediterranean into west and east, turning the western mediterranean into a giant bowl: for the water to make its way east, it first had to fill the western half of the sea. Once the western half of the sea filled up enough for the water to make its way over the top of the wall, it tipped over into the east and down a cliff about 1.5 kilometers deep, creating the largest waterfall in the history of our planet; imagine the Niagara Falls, but 30 times taller. The crash of the water triggered more earthquakes, and the flood dumped mounds of sediment at the bottom of the sea as it rushed into the east. As the water rose in the east to meet the waters of the western Mediterranean, the earth stopped shaking. The wind died down. The water started clearing as it settled, sediment falling to the sea floor. Somewhere between two and sixteen years after the first waters broke through the Strait of Gibraltar — not even the blink of an eye in geological time — the Mediterranean leveled off with the Atlantic. From the surface, all signs of upheaval disappeared. The Atlantic flowed lazily into the newly reformed Mediterranean, which was now free of walls or waterfalls. This sea, with its comparatively mild waters, looked much as it would millions of years later, when ancient Greece and Rome established themselves on its edges, When the Greek poet Homer wrote of the sea monsters Scylla and Charybdis living off the coast of Sicily, he had no way of knowing that Charybdis, who often takes the form of a whirlpool pulling unfortunate sailors to their death in the depths, had already been upstaged by the sea's own history. It would take surprisingly long for any new sea creatures, monstrous or otherwise, to make a home in the Mediterranean. 'In geological terms, we should have been seeing marine fauna immediately, but that's not what is happening,' Konstantina Agiadi, a geologist at the University of Vienna who co-authored a paper on the impact of the salinity crisis and flood on marine biodiversity. The water in the immediate aftermath of the flooding would have made a poor home, devoid of nutrients and far too salty for most creatures to live in; the ones that existed in the sea before the flood struggled by for a few millennia before the water became hospitable enough for any potential newcomers, and even today the Mediterranean is considerably saltier than the Atlantic. 'It took a lot of time for the situation to settle enough for organisms that were coming from the Atlantic to actually establish healthy populations and grow,' Agiadi the sea is a biodiversity hotspot, filled with all varieties of sea creatures. (How archaeologists found one of the oldest cities on Earth) Even though the flood happened millions of years ago, Micallef says, it holds important clues about the future of our planet. Climate change is making flooding from melting glaciers more common, and understanding the dynamics of the Zanclean megaflood — even though it was much larger than anything we have seen from glaciers so far — can help us model what future flooding will look like, mapping both the flow of water and its effect on the landscape around it. And, says Agiadi, there's another important lesson too: The world transformed when the Messinian Salinity Crisis and Zanclean megaflood happened, and there was no going back. The creatures that live in the Mediterranean now, wonderful as they may be, are nothing like what lived there before it dried up. That's true of climate change too. 'The flood is kind of like a natural experiment,' Agiadi says. 'The Mediterranean, after the flooding, eventually became a marine basin that is a biodiversity hotspot today. But it never became, even after millions of years, what it was before. So it's kind of a natural test of if we can fix things. If you try to bring back a species without fixing the underlying problems, it will never be okay. But it might be something different.' The nonprofit National Geographic Society, committed to illuminating and protecting the wonder of our world, funded Explorer Aaron Micallef's work. Learn more about the Society's support of Explorers.
National Geographic
28-04-2025
- Science
- National Geographic
How the biggest flood in the history of the Earth created the Mediterranean
The mediterranean was once a dried-up expanse of salt and gypsum. Then the floodwaters came rushing in. Photograph by NASA/Six million years ago, the Mediterranean Sea wasn't nearly as picturesque as it is today. It was barely even a sea; tectonic activity had raised a mountain range in the Strait of Gibraltar, cutting off the Mediterranean from the Atlantic. Without a constant inflow of water the sea evaporated under the baking sun, and all that remained were a few scattered, briny lakes surrounded by mile after mile of salt and gypsum. Today, scientists call this the Messinian Salinity Crisis: in the dying days of the Miocene epoch, most of the Mediterranean died. But if, on a certain day about 5.3 million years ago, you happened to go for a stroll along that mountain range, you might have discovered something odd: a trickle of water, making its way down one of the mountains from the Atlantic ocean beyond it. The mountains had been slowly sinking until their summits were level with the ocean's surface; one day, the mountains sank just enough for some of the water to spill over their edges. Once they did, the water carved an unstoppable path downhill. The trickle turned into a stream, which widened into a river, and soon the ocean was pouring into the desiccated Mediterranean basin with the force of a thousand Amazon Rivers, suddenly ending the 600,000-year-long dry spell. The water moved so quickly — 32 meters per second, or about 72 miles per hour, by the time it hit the coast of modern-day Sicily — that it dragged the air behind it, creating tropical storm-force winds as it moved. If you managed to somehow see through all the muddy sediment stirred up by the flood waters, you might have found a few surprised fish in the depths, stunned or struck dead outright by the force of the rapids that carried them in from the Atlantic. As the water refilled the Mediterranean, it ushered in a new geological era: the Zanclean . 'I don't think any human has ever seen anything like this,' says Aaron Micallef, a National Geographic Explorer and marine geoscientist at the Monterey Bay Aquarium Research Institute who studies this event, called the Zanclean megaflood. Micallef and his colleagues have spent years putting together the puzzle pieces of what the flood looked like, and this story is largely built on their research, which melds geologic evidence with computer modeling . While evidence for the flood is still accumulating, this is the scientist's best picture yet of what's likely the largest flood in the history of the Earth. A 3D rendering depicts how the Zanclean flood may have progressed. InTheBox/Daniel García-Castellanos How the modern Mediterranean was formed Micallef and his colleagues found that the Mediterranean, which had been obliterated once when the sea dried up, was transformed completely again by the megaflood. Get a bonus issue with all magazines EXPLORE SUBSCRIPTION OPTIONS The fossil record is difficult to read in much detail, but scientists think that before the sea dried up it was filled with all kinds of creatures, from ancient sharks and pinnipeds to fish and a rainbow of coral. Only eighty-six of the 780 or so species from the sea that existed before the salinity crisis have survived into the modern-day Mediterranean, and the fact that they lived through the flood is a minor miracle. Those creatures, a collection of mollusks, plankton, and one standout sea slug, most likely survived by finding refuge in the few patches of water that remained after the sea dried up. (Rome is teeming with mysterious crypts filled with popes—and secrets) As the water poured in, the western Mediterranean began refilling at a tremendous rate; Micallef estimates the water flowed at a rate of somewhere between 68 and 100 million cubic meters per second, filling the sea by as much as ten meters, or nearly 33 feet, each day. The weight of the rising waters pressed down on the Earth's crust, making it slide across the molten mantle underneath. This, says Daniel Garcia-Castellanos , a Geophysicist at CSIC Barcelona and a pioneer on research into the Zanclean megaflood, would have triggered earthquakes that rippled through the region. For the goat-antelope creature Myotragus, which had walked across the dry sea to make its home on modern-day Mallorca and Menorca, the earthquakes, water, and wind combined must have sounded like the roar of a monstrous predator — surely, this was the end of the world as they knew it. This video animates the evolution, and end, of the Messinian salinity crisis. University of Malta/Aaron Micallef, D. Garcia-Castellanos, and A. Camerlenghi. Eventually, the rising waters streamed over the lip of Sicily, and as the current moved east it ate away at the land, leaving behind hundreds of long ridges as if a giant hand had clawed through the dirt. A little bit further east, the water hit another wall that we now call the Malta Escarpment. This barrier divided the Mediterranean into west and east, turning the western mediterranean into a giant bowl: for the water to make its way east, it first had to fill the western half of the sea. Once the western half of the sea filled up enough for the water to make its way over the top of the wall, it tipped over into the east and down a cliff about 1.5 kilometers deep, creating the largest waterfall in the history of our planet; imagine the Niagara Falls, but 30 times taller. The crash of the water triggered more earthquakes, and the flood dumped mounds of sediment at the bottom of the sea as it rushed into the east. As the water rose in the east to meet the waters of the western Mediterranean, the earth stopped shaking. The wind died down. The water started clearing as it settled, sediment falling to the sea floor. Somewhere between two and sixteen years after the first waters broke through the Strait of Gibraltar — not even the blink of an eye in geological time — the Mediterranean leveled off with the Atlantic. Life returned… eventually From the surface, all signs of upheaval disappeared. The Atlantic flowed lazily into the newly reformed Mediterranean, which was now free of walls or waterfalls. This sea, with its comparatively mild waters, looked much as it would millions of years later, when ancient Greece and Rome established themselves on its edges, When the Greek poet Homer wrote of the sea monsters Scylla and Charybdis living off the coast of Sicily, he had no way of knowing that Charybdis, who often takes the form of a whirlpool pulling unfortunate sailors to their death in the depths, had already been upstaged by the sea's own history. It would take surprisingly long for any new sea creatures, monstrous or otherwise, to make a home in the Mediterranean. 'In geological terms, we should have been seeing marine fauna immediately, but that's not what is happening,' Konstantina Agiadi , a geologist at the University of Vienna who co-authored a paper on the impact of the salinity crisis and flood on marine biodiversity. The water in the immediate aftermath of the flooding would have made a poor home, devoid of nutrients and far too salty for most creatures to live in; the ones that existed in the sea before the flood struggled by for a few millennia before the water became hospitable enough for any potential newcomers, and even today the Mediterranean is considerably saltier than the Atlantic. 'It took a lot of time for the situation to settle enough for organisms that were coming from the Atlantic to actually establish healthy populations and grow,' Agiadi the sea is a biodiversity hotspot, filled with all varieties of sea creatures. (How archaeologists found one of the oldest cities on Earth) Even though the flood happened millions of years ago, Micallef says, it holds important clues about the future of our planet. Climate change is making flooding from melting glaciers more common, and understanding the dynamics of the Zanclean megaflood — even though it was much larger than anything we have seen from glaciers so far — can help us model what future flooding will look like, mapping both the flow of water and its effect on the landscape around it. And, says Agiadi, there's another important lesson too: The world transformed when the Messinian Salinity Crisis and Zanclean megaflood happened, and there was no going back. The creatures that live in the Mediterranean now, wonderful as they may be, are nothing like what lived there before it dried up. That's true of climate change too. 'The flood is kind of like a natural experiment,' Agiadi says. 'The Mediterranean, after the flooding, eventually became a marine basin that is a biodiversity hotspot today. But it never became, even after millions of years, what it was before. So it's kind of a natural test of if we can fix things. If you try to bring back a species without fixing the underlying problems, it will never be okay. But it might be something different.' The nonprofit National Geographic Society, committed to illuminating and protecting the wonder of our world, funded Explorer Aaron Micallef's work. Learn more about the Society's support of Explorers.
The Independent
14-04-2025
- Science
- The Independent
What we know about the cataclysmic ‘megaflood' considered the largest in Earth's history
A little over 5 million years ago, water from the Atlantic Ocean found a way through the present-day Strait of Gibraltar. According to this theory, oceanic water rushed faster than a speeding car down a kilometre-high slope towards the empty Mediterranean Sea, excavating a skyscraper-deep trough on its way. The Med was, at the time, a largely dry and salty basin, but so much water poured in that it filled up in just a couple of years – maybe even just a few months. At its peak, the flood discharged about 1,000 times the water of the modern-day Amazon river. At least, that's the thesis one of us put forward in a 2009 study of an underwater canyon excavated along the Strait of Gibraltar, which he presumed to have been carved out by this massive flood. If correct, (and some scientists do dispute the theory), the so-called Zanclean megaflood would be the largest single flood recorded on Earth. But extraordinary claims like this require extraordinarily solid evidence. Our latest research investigates sedimentary rock from the Zanclean era that seems to record how the water surged through a gap between modern-day Sicily and mainland Africa to refill the eastern half of the Mediterranean. How scientists tracked down the megaflood Our finding is the latest twist in a story that began in the late 19th century. That's when geologists studying salt-rich rock outcrops around the Mediterranean became increasingly aware that something unusual had happened between roughly 5 and 6 million years ago, well before the glaciations of recent ice ages: the sea had dried up. They named that age 'Messinian' and the drying up eventually became known as the Messinian salinity crisis. In the 1970s, scientists for the first time drilled deep below the Mediterranean into sedimentary rocks from the Messinian age. They made three surprising discoveries. First, they found a massive layer of salt – kilometres thick – below much of the seafloor. This confirmed that a vast environmental change had happened about 6 million years ago, just when tectonic plates shifted and the sea became largely isolated from the Atlantic Ocean. Second, right above this salt layer, they found sediment with fossils from shallow, low-salt lakes. This suggested that the Mediterranean Sea dropped to more than a kilometre below today's level, and as most of the water evaporated, salt was left behind. A series of lakes would have remained in the lowest parts of the basin, refreshed and kept relatively salt-free by streams. This interpretation was also supported by seismic surveys of the seabed which revealed rivers once cut through a dry landscape. And third, the rocky layers above the salt abruptly shifted back to more typical deep sea sediment. (We now know that less than 11% of Mediterranean marine species survived the crisis, showing just how big and lasting the impact was on life in the sea). The term Zanclean Flood was coined in the 1970s to refer to the end of the crisis, without scientists really knowing what it consisted of or the timescale taken to refill the dry Mediterranean basin. The next breakthrough came in 2009, when geophysical data for the planned Africa-Europe tunnel through Gibraltar suggested that a huge underwater trench between the Atlantic Ocean and the Mediterranean Sea must have been created by a sudden and cataclysmic flood. Our latest research backs up this hypothesis. As part of a team led by Maltese seabed scientist Aaron Micallef, we explored the region where the flood water filling the western basin of the Mediterranean should have run into a ridge of higher land connecting modern-day Africa and Italy, known as the Sicily Sill. Was there any evidence, we wondered, of a second megaflood as the eastern Mediterranean filled up? Giovanni Barreca, one of our co-authors on the recent paper, grew up in southern Sicily. He long ago realised that the low hills near the coast are an extension of the Sicily Sill over which the megaflood must have progressed from west to east. The area, he thought, might contain clues. Our team visited this part of Sicily and noticed that the hills were indeed unusual. Their aligned and streamlined shapes separated by deeply eroded depressions are very similar to streamlined hills in Washington state in the US. Those Washington hills were carved out by a megaflood at the end of the last Ice Age when the vast Lake Missoula dammed up behind a glacier and emptied catastrophically. If those hills and depressions in Sicily were also shaped by a huge flood, then rock debris eroded from the base of the depressions should be found dumped on top of the hills, more than 5 million years later. Sure enough, we did find jumbled and contorted rock debris up to boulder size along the crest of the hills. They were the same types of rock found within the depressions as well as further inland. To double check our work, we developed a computer simulation (or 'model') of how flood waters might have crossed one part of the Sicily Sill. It showed that the flood flow would indeed mimic the direction of the streamlined hills. In fact, the model showed that the hills would have been carved out by water 40 metres or more deep, travelling at 115 kilometres per hour (71mph). In the one area we modelled, 13 million cubic metres of water per second would have flooded into the eastern Mediterranean basin (for reference: the Amazon today is about 200,000 cubic metres per second). Remarkably, this is still only a fraction of the water that first flowed through Gibraltar and then into the eastern Mediterranean basin near Sicily. Daniel García-Castellanos is an Earth scientist at Instituto de Geociencias de Barcelona (Geo3Bcn – CSIC).
The Independent
13-04-2025
- Science
- The Independent
The latest twist in the story of the megaflood that refilled the Mediterranean
A little over 5 million years ago, water from the Atlantic Ocean found a way through the present-day Strait of Gibraltar. According to this theory, oceanic water rushed faster than a speeding car down a kilometre-high slope towards the empty Mediterranean Sea, excavating a skyscraper-deep trough on its way. The Med was, at the time, a largely dry and salty basin, but so much water poured in that it filled up in just a couple of years – maybe even just a few months. At its peak, the flood discharged about 1,000 times the water of the modern-day Amazon river. At least, that's the thesis one of us put forward in a 2009 study of an underwater canyon excavated along the Strait of Gibraltar, which he presumed to have been carved out by this massive flood. If correct, (and some scientists do dispute the theory), the so-called Zanclean megaflood would be the largest single flood recorded on Earth. But extraordinary claims like this require extraordinarily solid evidence. Our latest research investigates sedimentary rock from the Zanclean era that seems to record how the water surged through a gap between modern-day Sicily and mainland Africa to refill the eastern half of the Mediterranean. How scientists tracked down the megaflood Our finding is the latest twist in a story that began in the late 19th century. That's when geologists studying salt-rich rock outcrops around the Mediterranean became increasingly aware that something unusual had happened between roughly 5 and 6 million years ago, well before the glaciations of recent ice ages: the sea had dried up. They named that age 'Messinian' and the drying up eventually became known as the Messinian salinity crisis. In the 1970s, scientists for the first time drilled deep below the Mediterranean into sedimentary rocks from the Messinian age. They made three surprising discoveries. First, they found a massive layer of salt – kilometres thick – below much of the seafloor. This confirmed that a vast environmental change had happened about 6 million years ago, just when tectonic plates shifted and the sea became largely isolated from the Atlantic Ocean. Second, right above this salt layer, they found sediment with fossils from shallow, low-salt lakes. This suggested that the Mediterranean Sea dropped to more than a kilometre below today's level, and as most of the water evaporated, salt was left behind. A series of lakes would have remained in the lowest parts of the basin, refreshed and kept relatively salt-free by streams. This interpretation was also supported by seismic surveys of the seabed which revealed rivers once cut through a dry landscape. And third, the rocky layers above the salt abruptly shifted back to more typical deep sea sediment. (We now know that less than 11% of Mediterranean marine species survived the crisis, showing just how big and lasting the impact was on life in the sea). The term Zanclean Flood was coined in the 1970s to refer to the end of the crisis, without scientists really knowing what it consisted of or the timescale taken to refill the dry Mediterranean basin. The next breakthrough came in 2009, when geophysical data for the planned Africa-Europe tunnel through Gibraltar suggested that a huge underwater trench between the Atlantic Ocean and the Mediterranean Sea must have been created by a sudden and cataclysmic flood. Our latest research backs up this hypothesis. As part of a team led by Maltese seabed scientist Aaron Micallef, we explored the region where the flood water filling the western basin of the Mediterranean should have run into a ridge of higher land connecting modern-day Africa and Italy, known as the Sicily Sill. Was there any evidence, we wondered, of a second megaflood as the eastern Mediterranean filled up? Giovanni Barreca, one of our co-authors on the recent paper, grew up in southern Sicily. He long ago realised that the low hills near the coast are an extension of the Sicily Sill over which the megaflood must have progressed from west to east. The area, he thought, might contain clues. Our team visited this part of Sicily and noticed that the hills were indeed unusual. Their aligned and streamlined shapes separated by deeply eroded depressions are very similar to streamlined hills in Washington state in the US. Those Washington hills were carved out by a megaflood at the end of the last Ice Age when the vast Lake Missoula dammed up behind a glacier and emptied catastrophically. If those hills and depressions in Sicily were also shaped by a huge flood, then rock debris eroded from the base of the depressions should be found dumped on top of the hills, more than 5 million years later. Sure enough, we did find jumbled and contorted rock debris up to boulder size along the crest of the hills. They were the same types of rock found within the depressions as well as further inland. To double check our work, we developed a computer simulation (or 'model') of how flood waters might have crossed one part of the Sicily Sill. It showed that the flood flow would indeed mimic the direction of the streamlined hills. In fact, the model showed that the hills would have been carved out by water 40 metres or more deep, travelling at 115 kilometres per hour (71mph). In the one area we modelled, 13 million cubic metres of water per second would have flooded into the eastern Mediterranean basin (for reference: the Amazon today is about 200,000 cubic metres per second). Remarkably, this is still only a fraction of the water that first flowed through Gibraltar and then into the eastern Mediterranean basin near Sicily. Daniel García-Castellanos is an Earth scientist at Instituto de Geociencias de Barcelona (Geo3Bcn – CSIC).
Yahoo
27-01-2025
- Science
- Yahoo
Scientists Found Evidence of a Megaflood that Shaped Earth's Geologic History
"Hearst Magazines and Yahoo may earn commission or revenue on some items through these links." For 600,000 years during the tail end of the Miocene epoch, the Mediterranean was a dried-up salt plain cut off from the Atlantic Ocean. Around 5.3 million years ago, the eastern and western Mediterranean basins were suddenly refilled during an event known as the Zanclean megaflood. Now, a new study finds evidence of this flood in ridges along the Sicily Sill and in channels that likely formed from this sudden and powerful deluge. Ages, epochs, periods, and even eras are often defined by some sort of geologic trauma. The Chicxulub asteroid, for example, pushed the Earth into the Cenozoic Era, and 65 million years later, experts are pondering if we've entered a new geologic age induced by modern humans (and their predilection for greenhouse gasses). In many ways, Earth's story for the past 550 million years has largely been a cyclical tale of trauma and recovery—one that consistently yields to new forms of life. However, one particular geologic event in that half-a-billion-year-long epic still has scientists scratching their heads. Around 6 million years ago, between the Miocene and Pliocene epochs—or more specifically, the Messinian and Zanclean ages—the Mediterranean Sea was cut off from the Atlantic Ocean and formed a vast, desiccated salt plain between the European and African continents. Until, that is, this roughly 600,000-year-long period known as the Messinian Salinity Crisis suddenly came to an end. At first, scientists believed that the water's return to the Mediterranean took roughly 10,000 years. But the discovery of erosion channels stretching from the Gulf of Cadiz to the Alboran Sea in 2009 challenged this idea, suggesting instead that a powerful megaflood may have refilled the Mediterranean Basin in as little as two to 16 years. That likely means this flooding event—now known as the Zanclean megaflood—featured discharge rates of roughly 68 to 100 Sverdrups (one Sverdrup equals one million cubic meters per second). New research by an international team of scientists has uncovered more evidence of this incredible event, and also developed a computer model showing exactly how this geologic deluge unfolded. The results of the study were published in the journal Communications Earth & Environment. 'The Zanclean megaflood was an awe-inspiring natural phenomenon, with discharge rates and flow velocities dwarfing any other known floods in Earth's history,' Aaron Micallef, lead author of the study from the Monterey Bay Aquarium Research Institute, said in a press statement. 'Our research provides the most compelling evidence yet of this extraordinary event […]. These findings not only shed light on a critical moment in Earth's geological history but also demonstrate the persistence of landforms over five million years.' Researchers spotted this new evidence along 300 asymmetric ridges in the Sicily Sill, which was once a landbridge that separated the eastern and western Mediterranean basins. In finding that the tops of these ridges contained rocky material eroded from the ridge flanks, the scientists realized that this rock must've been deposited quickly and with a stunning amount of force. The researchers also note that this particular rock layer lies directly on the boundary where the Messinian transitions into the Zanclean, which is around the time of this landscape-altering megaflood. 'The morphology of these ridges is compatible with erosion by large-scale, turbulent water flow with a predominantly north easterly direction,' Paul Carling, a co-author of the study from the University of Southampton, said in a press statement. The authors also found evidence of w-shaped flood channels using seismic data and developed computer models to simulate how the flood waters would've refilled the Mediterranean Basin. This model shows that flooding could have reached speeds of 72 miles per hour, carving deep channels as observed in the seismic data. The geologic story of Earth may be somewhat cyclical, but that doesn't mean it can't be exciting. You Might Also Like The Do's and Don'ts of Using Painter's Tape The Best Portable BBQ Grills for Cooking Anywhere Can a Smart Watch Prolong Your Life?
