Has the tomb of Vlad III the Impaler, the historical Dracula, been found in the center of Naples in Italy? Not really.
Experts and bloggers are now debunking the claim that circulated late last week, saying it’s not rooted in real history but rather resembles a Da Vinci Code conspiracy novel.
According to a report in the Italian daily Il Mattino, the remains of the 15th century Romanian prince upon which Bram Stoker's gothic novel "Dracula" is based, lie in a cloister in the Santa Maria La Nova church in Naples.
The report cited historian Raffaele Glinni, his brother Giandomenico, a researcher at the University of Tallin in Estonia, and Nicola Barbatelli, director of Italy’s Museum of Ancient Populations as the team behind the discovery.
Following a tip from a student Erika Stella, who was researching the cloister of Santa Maria Nova in Naples for her doctorate, Glinni and colleagues investigated a marble tomb covered in what they believe are clear symbols pointing to Dracula: a dragon and two opposing sphinxes.
"The dragon means Dracula and the two opposing sphinxes represent the city of Thebes which the Egyptians called Tepes. In these symbols, the very name of count Dracula Tepes is written," Raffaello Glinni told Il Mattino.
Glinni and colleagues, who have already filed an official request to open the tomb, believe Vlad III, the Prince of Wallachia, didn’t die in a battle sometime between October 31 and December 31, 1476, as it was previously assumed, but was imprisoned by the Turks.
According to the researchers, his daughter Maria Balsa, who was brought to the Neapolitan court at the age of seven and later married to Count Giacomo Alfonso Ferrillo, paid the ransom. Vlad eventually died in Naples and was buried in the church of Santa Maria Nova in the grave of the Ferrillo family.
As intriguing as it might sound, the story appears to have many holes.
"The article doesn’t say how credible these researchers are. A simple Google search would have been enough. In 2009 they claimed to have discovered a Leonardo da Vinci self portrait," art historian Tomaso Montanari wrote in the daily Il Fatto Quotidiano.
Raffaele Glinni, a lawyer and self declared historian, appears with his brother in the website "Mysterious Lucania" which reveals his somewhat mixed area of research.
"Knights Templar? Check. Freemasonry? Check. Da Vinci? You bet. Gibberings about non-specific magical vortices? Not looking too good," The BS Historian wrote.
The blogger noted that basic errors emerge in Glinni quotes: "Vlad was not a 'Count' like his fictional namesake, he was a voivode (prince)." Glinni should have known that.
Moreover, while the dragon was indeed the main element in the badge of the Order of the Dragon to which Vlad III's father belonged, none of the Order dragon depictions resemble that on the Italian bas-relief.
As for the sphinxes, the "Thebes/Tepes connection seems to be entirely spurious," the BS Historian said.
"Thebes itself is a Greek placename, Tepes a Turkish word for Impaler. Where's the connection?" the blogger asked.
It is unlikely the Tepes nickname was used in Vlad’s lifetime since it was considered an insult.
Indeed Vlad, born sometime between 1428 and 1431, probably in Sighişaora, Transylvania, gained the infamous nickname from his cruel method of execution. During the fight against Mehmed II of the Ottoman Empire in 1462, he impaled some 20,000 people outside the city of Targoviste. The sight was so shocking that the Ottomans retreated to Constantinople.
As for Vlad's secret daughter, a historical figure named Maria Balsa does exist, but there is no account which links her to Vlad, whose recorded offspring are only sons.
Most historians believe that Dracula was killed on a road between Bucharest and Giurgiu, Romania, during a fight to reconquer Wallachia from its Turkish ruler Basarab Laiota.
Laiota beheaded Vlad and sent the head as a trophy to Constantinople.
"The body was buried without special ornaments or a more distinguished tombstone, in the nearest church built by or connected to his name," medieval historian Constantin Rezachevici, chief researcher with the Nicolae Iorga Institute of History of the Romanian Academy, wrote in a paper presented at a symposium on Vlad the Impaler in Romania in 2001.
According to Rezachevici, one such building in the area was the monastery of Comana. Built by Vlad III himself, it was demolished about one century after his death.
As for the carved dragon on the alleged Dracula tomb in Naples, historical records associate it to the coat of arms of Matteo Ferrillo, Maria Balsa's father-in-law.
"There you have it. The tomb is that of a known Italian noble, with recognized arms," Jason Colavito writes in his blog. He found in Arthur Charles Fox-Davies’s Art of Heraldry (1904) the exact description of Ferrillo's arms.
"Just to put a nail in the coffin, so to speak, on the same page Fox-Davies gives two more examples of Italian nobles who also had nearly identical dragon's head arms on their tombs," Colavito writes.
Read more at Discovery News
Jun 17, 2014
Remains of Ancient Egyptian Epidemic Uncovered
Archaeologists have uncovered the remains of an epidemic in Egypt so terrible that one ancient writer believed the world was coming to an end.
Working at the Funerary Complex of Harwa and Akhimenru in the west bank of the ancient city of Thebes (modern-day Luxor) in Egypt, the team of the Italian Archaeological Mission to Luxor (MAIL) found bodies covered with a thick layer of lime (historically used as a disinfectant). The researchers also found three kilns where the lime was produced, as well as a giant bonfire containing human remains, where many of the plague victims were incinerated.
Pottery remains found in the kilns allowed researchers to date the grisly operation to the third century A.D., a time when a series of epidemics now dubbed the "Plague of Cyprian" ravaged the Roman Empire, which included Egypt. Saint Cyprian was a bishop of Carthage (a city in Tunisia) who described the plague as signaling the end of the world.
Occurring between roughly A.D. 250-271, the plague "according to some sources killed more than 5,000 people a day in Rome alone," wrote Francesco Tiradritti, director of the MAIL, in the latest issue of Egyptian Archaeology, a magazine published by the Egypt Exploration Society.
Tiradritti's team uncovered the remains of this body-disposal operation between 1997 and 2012. The monument his team is excavating was originally built in the seventh century B.C. for a grand steward named Harwa. After Harwa's death, the Egyptians continuously used the monument for burial (Akhimenru was a successor who built his own tomb there). However, after its use for body disposal during the plague, the monument was abandoned and never used again.
The use of the complex "for the disposal of infected corpses gave the monument a lasting bad reputation and doomed it to centuries of oblivion until tomb robbers entered the complex in the early 19th century," Tiradritti writes.
Cyprian left a gut-wrenching record of what the victims suffered before they died. "The bowels, relaxed into a constant flux, discharge the bodily strength a fire originated in the marrow ferments into wounds of the fauces (an area of the mouth)," he wrote in Latin in a work called "De mortalitate." The "intestines are shaken with a continual vomiting, the eyes are on fire with the injected blood," he wrote, adding that "in some cases the feet or some parts of the limbs are taken off by the contagion of diseased putrefaction …"
Cyprian believed that the world was coming to an end.
"The kingdom of God, beloved brethren, is beginning to be at hand; the reward of life, and the rejoicing of eternal salvation, and the perpetual gladness and possession lately lost of paradise, are now coming, with the passing away of the world …" (translation by Philip Schaff, from the book "Ante-Nicene Fathers", volume 5, 1885).
While the world, of course, did not end, the plague weakened the Roman Empire. "It killed two Emperors, Hostilian in A.D. 251 and Claudius II Gothicus in A.D. 270," wrote Tiradritti. It is "a generally held opinion that the 'Plague of Cyprian' seriously weakened the Roman Empire, hastening its fall."
The newly unearthed remains at Luxor underscore the plague's potency. Tiradritti'steam found no evidence that the victims received any sort of religious rites during their incineration. "We found evidence of corpses either burned or buried inside the lime," he told Live Science in an interview. "They had to dispose of them without losing any time."
The plague may have been some form of smallpox or measles, accordingto modern day scientists. While the discovery of human remains associated with the plague will give anthropologists new material to study, Tiradritti cautions they will not be able to extract DNA from the bodies.
While stories about researchers extracting DNA from mummies (such as Tutankhamun) have made headlines in recent years, Tiradritti told Live Science he doesn't believe the results from such ancient specimens. "In a climate like Egypt, the DNA is completely destroyed," he said. DNA breaks down over time, and permafrost (something not found in Egypt) is the best place to find ancient DNA samples, Tiradritti said.
Read more at Discovery News
Working at the Funerary Complex of Harwa and Akhimenru in the west bank of the ancient city of Thebes (modern-day Luxor) in Egypt, the team of the Italian Archaeological Mission to Luxor (MAIL) found bodies covered with a thick layer of lime (historically used as a disinfectant). The researchers also found three kilns where the lime was produced, as well as a giant bonfire containing human remains, where many of the plague victims were incinerated.
Pottery remains found in the kilns allowed researchers to date the grisly operation to the third century A.D., a time when a series of epidemics now dubbed the "Plague of Cyprian" ravaged the Roman Empire, which included Egypt. Saint Cyprian was a bishop of Carthage (a city in Tunisia) who described the plague as signaling the end of the world.
Occurring between roughly A.D. 250-271, the plague "according to some sources killed more than 5,000 people a day in Rome alone," wrote Francesco Tiradritti, director of the MAIL, in the latest issue of Egyptian Archaeology, a magazine published by the Egypt Exploration Society.
Tiradritti's team uncovered the remains of this body-disposal operation between 1997 and 2012. The monument his team is excavating was originally built in the seventh century B.C. for a grand steward named Harwa. After Harwa's death, the Egyptians continuously used the monument for burial (Akhimenru was a successor who built his own tomb there). However, after its use for body disposal during the plague, the monument was abandoned and never used again.
The use of the complex "for the disposal of infected corpses gave the monument a lasting bad reputation and doomed it to centuries of oblivion until tomb robbers entered the complex in the early 19th century," Tiradritti writes.
Cyprian left a gut-wrenching record of what the victims suffered before they died. "The bowels, relaxed into a constant flux, discharge the bodily strength a fire originated in the marrow ferments into wounds of the fauces (an area of the mouth)," he wrote in Latin in a work called "De mortalitate." The "intestines are shaken with a continual vomiting, the eyes are on fire with the injected blood," he wrote, adding that "in some cases the feet or some parts of the limbs are taken off by the contagion of diseased putrefaction …"
Cyprian believed that the world was coming to an end.
"The kingdom of God, beloved brethren, is beginning to be at hand; the reward of life, and the rejoicing of eternal salvation, and the perpetual gladness and possession lately lost of paradise, are now coming, with the passing away of the world …" (translation by Philip Schaff, from the book "Ante-Nicene Fathers", volume 5, 1885).
While the world, of course, did not end, the plague weakened the Roman Empire. "It killed two Emperors, Hostilian in A.D. 251 and Claudius II Gothicus in A.D. 270," wrote Tiradritti. It is "a generally held opinion that the 'Plague of Cyprian' seriously weakened the Roman Empire, hastening its fall."
The newly unearthed remains at Luxor underscore the plague's potency. Tiradritti'steam found no evidence that the victims received any sort of religious rites during their incineration. "We found evidence of corpses either burned or buried inside the lime," he told Live Science in an interview. "They had to dispose of them without losing any time."
The plague may have been some form of smallpox or measles, accordingto modern day scientists. While the discovery of human remains associated with the plague will give anthropologists new material to study, Tiradritti cautions they will not be able to extract DNA from the bodies.
While stories about researchers extracting DNA from mummies (such as Tutankhamun) have made headlines in recent years, Tiradritti told Live Science he doesn't believe the results from such ancient specimens. "In a climate like Egypt, the DNA is completely destroyed," he said. DNA breaks down over time, and permafrost (something not found in Egypt) is the best place to find ancient DNA samples, Tiradritti said.
Read more at Discovery News
Earth's Most Abundant, But Hidden Mineral Revealed
Earth's most abundant mineral lies deep in the planet's interior, sealed off from human eyes. Now, scientists for the first time have gotten a glimpse of the material in nature, enclosed inside a 4.5-billion-year-old meteorite. The result: They have characterized and named the elusive mineral.
The new official name, bridgmanite, was approved for the mineral formerly known by its chemical components and crystal structure — silicate-perovskite.
The magnesium-silicate mineral was named after Percy Bridgman, a 1946 Nobel Prize-winning physicist, according to the American Geophysical Union blog.
"It is a very exciting discovery," Chi Ma of Caltech and Oliver Tschauner, of the University of Nevada, Las Vegas, told Live Science in an email.
"We finally tracked down natural silicate-perovskite (now bridgmanite) in a meteorite after a five-year investigation, and got to name the most abundant mineral on Earth. How cool is that?"
The mineral likely resides beneath Earth's surface in an area called the lower mantle, between the transition zone in the mantle and the core-mantle boundary, or between the depths of416 and 1,802 miles (670 and 2,900 kilometers), scientists said.
Scientists have been searching for the mineral for a long time, because in order to identify a mineral one must know its chemical composition and crystal structure, Ma said.
Researchers found the bridgmanite in a meteorite that had fallen to Earth near the Tenham station in western Queensland, Australia, in 1879.
The meteorite, Ma said, is highly shocked, meaning it endured high temperatures and pressures as it slammed into other rocks in space. Those impacts can create shock veins of minerals within the meteorites.
"Scientists have identified high-pressure minerals in its shock-melt veins since 1960s. Now we have identified bridgmanite," Tschauner said, referring to the Tenham meteorite.
The meteorite is considered a chondrite, the most common type of meteorite found on Earth; scientists think these meteorites are remnants shed from the original building blocks of planets.
Most meteors (which are called meteorites once they strike Earth) are fragments of asteroids, while others are the cosmic dust discarded by comets. Rarely, meteorites represent impact debris from the moon and from Mars.
Read more at Discovery News
The new official name, bridgmanite, was approved for the mineral formerly known by its chemical components and crystal structure — silicate-perovskite.
The magnesium-silicate mineral was named after Percy Bridgman, a 1946 Nobel Prize-winning physicist, according to the American Geophysical Union blog.
"It is a very exciting discovery," Chi Ma of Caltech and Oliver Tschauner, of the University of Nevada, Las Vegas, told Live Science in an email.
"We finally tracked down natural silicate-perovskite (now bridgmanite) in a meteorite after a five-year investigation, and got to name the most abundant mineral on Earth. How cool is that?"
The mineral likely resides beneath Earth's surface in an area called the lower mantle, between the transition zone in the mantle and the core-mantle boundary, or between the depths of416 and 1,802 miles (670 and 2,900 kilometers), scientists said.
Scientists have been searching for the mineral for a long time, because in order to identify a mineral one must know its chemical composition and crystal structure, Ma said.
Researchers found the bridgmanite in a meteorite that had fallen to Earth near the Tenham station in western Queensland, Australia, in 1879.
The meteorite, Ma said, is highly shocked, meaning it endured high temperatures and pressures as it slammed into other rocks in space. Those impacts can create shock veins of minerals within the meteorites.
"Scientists have identified high-pressure minerals in its shock-melt veins since 1960s. Now we have identified bridgmanite," Tschauner said, referring to the Tenham meteorite.
The meteorite is considered a chondrite, the most common type of meteorite found on Earth; scientists think these meteorites are remnants shed from the original building blocks of planets.
Most meteors (which are called meteorites once they strike Earth) are fragments of asteroids, while others are the cosmic dust discarded by comets. Rarely, meteorites represent impact debris from the moon and from Mars.
Read more at Discovery News
Moon Bumps: Earth's Gravity Creates Lunar Bulges
Earth's gravitational pull is so powerful that it creates a small bulge on the surface of the moon. For the first time, scientists have observed this bump from orbit, using NASA satellites.
The gravitational tug-of-war between Earth and the moon is enough to stretch both celestial bodies, so they each end up having a slight oval shape, with the tapered ends facing each other.
On Earth, this gravitational tension shows up in the form of tides. The moon's pull has a strong effect on Earth's oceans because water has so much freedom of movement.
The corresponding distorting effect on the moon, called the lunar body tide, is more difficult to see, because the moon is solid except for a molten core. But Earth's pull raises a small bulge about 20 inches (50 centimeters) from the surface on the near side of the moon and a matching bulge on the far side.
"The deformation of the moon due to Earth's pull is very challenging to measure, but learning more about it gives us clues about the interior of the moon," Erwan Mazarico, a scientist who works at NASA’s Goddard Space Flight Center, said in a statement.
The same side of the moon always faces Earth, but the bulge does move around a few inches over time, wobbling and following Earth's pull like a magnet, as the moon shifts slightly during its orbit.
Scientists observed the lunar body tide using NASA's Lunar Reconnaissance Orbiter satellite, which is mapping the height of features on the moon's surface, and NASA's Gravity Recovery and Interior Laboratory satellite, which is mapping the moon's gravitational field. The satellites measured the height of 350,000 locations spread across areas of the moon closest to Earth and areas of the moon on the opposite side from Earth. The satellites passed over each location several times, so scientists could compare the height of each spot from one satellite pass to the next. By identifying which spots changed height, the researchers could track the lunar tide.
Read more at Discovery News
The gravitational tug-of-war between Earth and the moon is enough to stretch both celestial bodies, so they each end up having a slight oval shape, with the tapered ends facing each other.
On Earth, this gravitational tension shows up in the form of tides. The moon's pull has a strong effect on Earth's oceans because water has so much freedom of movement.
The corresponding distorting effect on the moon, called the lunar body tide, is more difficult to see, because the moon is solid except for a molten core. But Earth's pull raises a small bulge about 20 inches (50 centimeters) from the surface on the near side of the moon and a matching bulge on the far side.
"The deformation of the moon due to Earth's pull is very challenging to measure, but learning more about it gives us clues about the interior of the moon," Erwan Mazarico, a scientist who works at NASA’s Goddard Space Flight Center, said in a statement.
The same side of the moon always faces Earth, but the bulge does move around a few inches over time, wobbling and following Earth's pull like a magnet, as the moon shifts slightly during its orbit.
Scientists observed the lunar body tide using NASA's Lunar Reconnaissance Orbiter satellite, which is mapping the height of features on the moon's surface, and NASA's Gravity Recovery and Interior Laboratory satellite, which is mapping the moon's gravitational field. The satellites measured the height of 350,000 locations spread across areas of the moon closest to Earth and areas of the moon on the opposite side from Earth. The satellites passed over each location several times, so scientists could compare the height of each spot from one satellite pass to the next. By identifying which spots changed height, the researchers could track the lunar tide.
Read more at Discovery News
Jun 16, 2014
Bachelor Party Finds Massive Mastodon Skull
Some guys have trouble remembering just what happened during their bachelor party, but a group of men on a recent stag send-off in New Mexico aren’t likely to forget their celebration very soon — since they stumbled upon a perfectly preserved three-million-year-old mastodon skull.
The party was on a hike in Elephant Butte Lake State Park near Albuquerque when they saw a bone jutting one to two inches from the sand, according to a recent report in the Telegraph. They started digging and uncovered the enormous skull. Their first thought was it could be the remains of a woolly mammoth so they snapped photos and sent them to the New Mexico Museum of Natural History and Science.
Scientists there made the identification — it wasn’t a woolly mammoth, but, in fact, a much more exciting find. The skull belonged to a stegomastodon -- a prehistoric ancestor of the woolly mammoth — as well as today’s elephants. The massive animal stood about 9 feet tall, weighed six tons and walked the Earth during the Ice Age, according to Gary Morgan, a paleontologist at the museum who analyzed the fossil. He estimates the animal was about 50 years old when it died on a sandbar of the ancient Rio Grande River.
The family of mastodons migrated to North America around 15 million years ago and died out around 10,000 years ago.
“This is far and away the best one we’ve ever found,” said Morgan about the bachelor party’s discovery.
Scientists, following up on the party’s tip, went to the site and sealed the skull, which weighed more than 1,000 pounds, in a cast. It was transported to the museum, where it will eventually will be placed on display.
Read more at Discovery News
The party was on a hike in Elephant Butte Lake State Park near Albuquerque when they saw a bone jutting one to two inches from the sand, according to a recent report in the Telegraph. They started digging and uncovered the enormous skull. Their first thought was it could be the remains of a woolly mammoth so they snapped photos and sent them to the New Mexico Museum of Natural History and Science.
Scientists there made the identification — it wasn’t a woolly mammoth, but, in fact, a much more exciting find. The skull belonged to a stegomastodon -- a prehistoric ancestor of the woolly mammoth — as well as today’s elephants. The massive animal stood about 9 feet tall, weighed six tons and walked the Earth during the Ice Age, according to Gary Morgan, a paleontologist at the museum who analyzed the fossil. He estimates the animal was about 50 years old when it died on a sandbar of the ancient Rio Grande River.
The family of mastodons migrated to North America around 15 million years ago and died out around 10,000 years ago.
“This is far and away the best one we’ve ever found,” said Morgan about the bachelor party’s discovery.
Scientists, following up on the party’s tip, went to the site and sealed the skull, which weighed more than 1,000 pounds, in a cast. It was transported to the museum, where it will eventually will be placed on display.
Read more at Discovery News
Million-Year-Old Fossils Show Hippos Going for a Swim
More than a million years ago, hippopotamuses paddled across a shallow pool in the region that's now northern Kenya, occasionally scraping their feet on the sandy bottom. Today, researchers have evidence of the hippos' fleeting swim in the form of fossilized footprints.
The newly identified prints represent the first known tracks of ancient mammals taking a dip, joining previously discovered trace fossils left behind by swimming dinosaurs, turtles and crocodiles, the researchers said.
The hippo foot impressions were found in Kenya's Koobi Fora region, which is part of the Lake Turkana Basin, considered the cradle of human evolution because the area contains some of the oldest fossils from hominins — a group that comprises multiple species that came after Homo, the human lineage, split from chimpanzees. In fact, early humans may have witnessed the aquatic adventures of these ancient hippos; hominin footprints were discovered on the same geologic surface a mere 230 feet (70 meters) from the hippo tracks.
'Bottom walkers'
Recent excavations in Koobi Fora revealed dozens of large animal tracks, dating back to 1.4 million years ago, but a majority of the prints appear to have been left by a four-toed animal "bottom walking" in a shallow water body, study leader Matthew Bennett, of the United Kingdom's Bournemouth University, and his colleagues said.
Because of the size and shape of the prints, the team thinks the tracks could belong to adults and juveniles of the species Hippopotamus gorgops, which went extinct during the Ice Age, and perhaps the pygmy hippo species Hippopotamus aethiopicus.
At the time, the Lake Turkana area was much more fertile than it is today. The semi-arid environment had lots of shallow pools and channels, all feeding into larger lakes, and it supported a striking diversity of plants and animals, Bennett said.
The hippo prints appear to have been pressed into fine sands and silts deposited on the floor of a shallow body of water, before being buried by a layer of coarser sand, likely during a small flood, Bennett explained in an email to Live Science.
Today's gliding hippos
To look for a modern comparison to these extinct animals, the researchers observed the swimming styles of two female common Nile hippopotamuses (Hippopotamus amphibius) through a glass tank at the Adventure Aquarium in Philadelphia.
Underwater, the Nile hippos would glide with their limbs folded beneath their bodies. They would occasionally scratch the bottom of the tank with one leg, dragging only their digits across the ground. Sometimes, the hippos would thrust upward, toward the water surface, using both of their hind legs. These movements were reflected in the shape of the ancient tracks, the researchers said.
Read more at Discovery News
The newly identified prints represent the first known tracks of ancient mammals taking a dip, joining previously discovered trace fossils left behind by swimming dinosaurs, turtles and crocodiles, the researchers said.
The hippo foot impressions were found in Kenya's Koobi Fora region, which is part of the Lake Turkana Basin, considered the cradle of human evolution because the area contains some of the oldest fossils from hominins — a group that comprises multiple species that came after Homo, the human lineage, split from chimpanzees. In fact, early humans may have witnessed the aquatic adventures of these ancient hippos; hominin footprints were discovered on the same geologic surface a mere 230 feet (70 meters) from the hippo tracks.
'Bottom walkers'
Recent excavations in Koobi Fora revealed dozens of large animal tracks, dating back to 1.4 million years ago, but a majority of the prints appear to have been left by a four-toed animal "bottom walking" in a shallow water body, study leader Matthew Bennett, of the United Kingdom's Bournemouth University, and his colleagues said.
Because of the size and shape of the prints, the team thinks the tracks could belong to adults and juveniles of the species Hippopotamus gorgops, which went extinct during the Ice Age, and perhaps the pygmy hippo species Hippopotamus aethiopicus.
At the time, the Lake Turkana area was much more fertile than it is today. The semi-arid environment had lots of shallow pools and channels, all feeding into larger lakes, and it supported a striking diversity of plants and animals, Bennett said.
The hippo prints appear to have been pressed into fine sands and silts deposited on the floor of a shallow body of water, before being buried by a layer of coarser sand, likely during a small flood, Bennett explained in an email to Live Science.
Today's gliding hippos
To look for a modern comparison to these extinct animals, the researchers observed the swimming styles of two female common Nile hippopotamuses (Hippopotamus amphibius) through a glass tank at the Adventure Aquarium in Philadelphia.
Underwater, the Nile hippos would glide with their limbs folded beneath their bodies. They would occasionally scratch the bottom of the tank with one leg, dragging only their digits across the ground. Sometimes, the hippos would thrust upward, toward the water surface, using both of their hind legs. These movements were reflected in the shape of the ancient tracks, the researchers said.
Read more at Discovery News
Human Ancestors Got Herpes from Chimps
A herpes virus that infects humans originated in chimpanzees before it jumped into early human ancestors, according to a new study.
Researchers found that herpes simplex virus 1 (HSV-1) infected hominids before their evolutionary split from chimpanzees 6 million years ago, whereas herpes simplex 2 (HSV-2) was transferred from ancient chimpanzees to human ancestors such as Homo erectus about 1.6 million years ago, long before the rise of early modern humans about 200,000 years ago.
"Before we were human, there was still cross-species transmission into our evolutionary lineage," study author Joel O. Wertheim, assistant research scientist at the University of California, San Diego AntiViral Research Center, told Live Science.
About two-thirds of the human population is infected with at least one kind of herpes simplex virus, according to the researchers. HSV-1 commonly manifests itself as cold sores on the mouth or lips, whereas HSV-2 can cause blisters on the genitals.
Humans are also the only primate species that can be infected by more than one herpes simplex virus, the researchers said.
In the study, the researchers compared human herpes viruses with those of other primates. They used advanced models of molecular evolution to estimate when and how exactly the viruses had diverged from each other, and how they were introduced into humans.
According to a previous hypothesis, HSV-1 was thought to have been introduced to humans "potentially from another ape species, like orangutans," Wertheim said. And the split between HSV-2 and its chimpanzee counterpart was thought to have coincided with the split between humans and chimpanzees.
In contrast, the new study suggests that HSV-2 is the result of cross-species transmission to humans from ancestors of modern chimpanzees, and that HSV-1 is the result of a split between the human and chimpanzee viruses, he said.
Now, humans and chimpanzees have their own version of the HSV-1 virus, he said.
The results may help scientists better understand the mechanism of species-to-species transmission, which still happens, the study authors said. For instance, people today often get infected with a macaque simplex virus, which can result in severe illness, the researchers wrote in the study. But human-to-human transmission of this virus is extremely rare, they wrote.
"Understanding how and when we acquired viruses that currently infect us can give us perspective on future, potential cross-species transmission events that would lead to the introduction of new human viruses," Wertheim said.
Read more at Discovery News
Researchers found that herpes simplex virus 1 (HSV-1) infected hominids before their evolutionary split from chimpanzees 6 million years ago, whereas herpes simplex 2 (HSV-2) was transferred from ancient chimpanzees to human ancestors such as Homo erectus about 1.6 million years ago, long before the rise of early modern humans about 200,000 years ago.
"Before we were human, there was still cross-species transmission into our evolutionary lineage," study author Joel O. Wertheim, assistant research scientist at the University of California, San Diego AntiViral Research Center, told Live Science.
About two-thirds of the human population is infected with at least one kind of herpes simplex virus, according to the researchers. HSV-1 commonly manifests itself as cold sores on the mouth or lips, whereas HSV-2 can cause blisters on the genitals.
Humans are also the only primate species that can be infected by more than one herpes simplex virus, the researchers said.
In the study, the researchers compared human herpes viruses with those of other primates. They used advanced models of molecular evolution to estimate when and how exactly the viruses had diverged from each other, and how they were introduced into humans.
According to a previous hypothesis, HSV-1 was thought to have been introduced to humans "potentially from another ape species, like orangutans," Wertheim said. And the split between HSV-2 and its chimpanzee counterpart was thought to have coincided with the split between humans and chimpanzees.
In contrast, the new study suggests that HSV-2 is the result of cross-species transmission to humans from ancestors of modern chimpanzees, and that HSV-1 is the result of a split between the human and chimpanzee viruses, he said.
Now, humans and chimpanzees have their own version of the HSV-1 virus, he said.
The results may help scientists better understand the mechanism of species-to-species transmission, which still happens, the study authors said. For instance, people today often get infected with a macaque simplex virus, which can result in severe illness, the researchers wrote in the study. But human-to-human transmission of this virus is extremely rare, they wrote.
"Understanding how and when we acquired viruses that currently infect us can give us perspective on future, potential cross-species transmission events that would lead to the introduction of new human viruses," Wertheim said.
Read more at Discovery News
Maria Mystery: Why Moon's Far Side Has No 'Face'
Heat radiating from the young Earth could help solve the more than 50-year-old mystery of why the far side of the moon, which faces away from Earth, lacks the dark, vast expanses of volcanic rock that define the face of the Man in the Moon as seen from Earth, researchers say.
The Man in the Moon was born when cosmic impacts struck the near side of the moon, the side that faces Earth. These collisions punched holes in the moon's crust, which later filled with vast lakes of lava that formed the dark areas known as maria or "seas."
In 1959, when the Soviet spacecraft Luna 3 transmitted the first images of the "dark" or far side of the moon, the side facing away from Earth, scientists immediately noticed fewer maria there. This mystery — why no Man in the Moon exists on the moon's far side — is called the Lunar Farside Highlands Problem.
"I remember the first time I saw a globe of the moon as a boy, being struck by how different the far side looks," study co-author Jason Wright, an astronomer at Pennsylvania State University, said in a statement. "It was all mountains and craters. Where were the maria?"
Now scientists may have solved the 55-year-old mystery; heat from the young Earth as the newborn moon was cooling caused the difference. The researchers came up with the solution during their work on exoplanets, which are worlds outside the solar system.
"There are many exoplanets that are really close to their host stars,"lead study author Arpita Roy, also of Penn State, told Space.com. "That really affects the geology of those planets."
Similarly, the moon and Earth are generally thought to have orbited very close together after they formed. The leading idea explaining the moon's formation suggests that it arose shortly after the nascent Earth collided with a Mars-size planet about 4.5 billion years ago, with the resulting debris coalescing into the moon. Scientists say the newborn moon and Earth were 10 to 20 times closer to each other than they are now.
"The moon and Earth loomed large in each other's skies when they formed, " Roy said in a statement.
Since the moon was so close to Earth, the mutual pull of gravity was strong. The gravitational tidal forces the moon and Earth exerted on each other braked their rotations, resulting in the moon always showing the same face to Earth, a situation known as tidal lock.
The moon and Earth were very hot shortly after the giant impact that formed the moon. The moon, being much smaller than Earth, cooled more quickly. Since the moon and Earth were tidally locked early on, the still-hot Earth — more than 4,530 degrees Fahrenheit (2,500 degrees Celsius) — would have cooked the near side of the moon, keeping it molten. On the other hand, the far side of the moon would have cooled, albeit slowly.
The difference in temperature between the moon's halves influenced the formation of its crust. The lunar crust possesses high concentrations of aluminum and calcium, elements that are very hard to vaporize.
"When rock vapor starts to cool, the very first elements that snow out are aluminum and calcium," study co-author Steinn Sigurdsson of Penn State said in a statement.
Aluminum and calcium would have more easily condensed in the atmosphere on the colder far side of the moon. Eventually, these elements combined with silicates in the mantle of the moon to form minerals known as plagioclase feldspars, making the crust of the far side about twice as thick as that of the near side.
"Earthshine, the heat of Earth soon after the giant impact, was a really important factor shaping the moon," Roy said.
Read more at Discovery News
The Man in the Moon was born when cosmic impacts struck the near side of the moon, the side that faces Earth. These collisions punched holes in the moon's crust, which later filled with vast lakes of lava that formed the dark areas known as maria or "seas."
In 1959, when the Soviet spacecraft Luna 3 transmitted the first images of the "dark" or far side of the moon, the side facing away from Earth, scientists immediately noticed fewer maria there. This mystery — why no Man in the Moon exists on the moon's far side — is called the Lunar Farside Highlands Problem.
"I remember the first time I saw a globe of the moon as a boy, being struck by how different the far side looks," study co-author Jason Wright, an astronomer at Pennsylvania State University, said in a statement. "It was all mountains and craters. Where were the maria?"
Now scientists may have solved the 55-year-old mystery; heat from the young Earth as the newborn moon was cooling caused the difference. The researchers came up with the solution during their work on exoplanets, which are worlds outside the solar system.
"There are many exoplanets that are really close to their host stars,"lead study author Arpita Roy, also of Penn State, told Space.com. "That really affects the geology of those planets."
Similarly, the moon and Earth are generally thought to have orbited very close together after they formed. The leading idea explaining the moon's formation suggests that it arose shortly after the nascent Earth collided with a Mars-size planet about 4.5 billion years ago, with the resulting debris coalescing into the moon. Scientists say the newborn moon and Earth were 10 to 20 times closer to each other than they are now.
"The moon and Earth loomed large in each other's skies when they formed, " Roy said in a statement.
Since the moon was so close to Earth, the mutual pull of gravity was strong. The gravitational tidal forces the moon and Earth exerted on each other braked their rotations, resulting in the moon always showing the same face to Earth, a situation known as tidal lock.
The moon and Earth were very hot shortly after the giant impact that formed the moon. The moon, being much smaller than Earth, cooled more quickly. Since the moon and Earth were tidally locked early on, the still-hot Earth — more than 4,530 degrees Fahrenheit (2,500 degrees Celsius) — would have cooked the near side of the moon, keeping it molten. On the other hand, the far side of the moon would have cooled, albeit slowly.
The difference in temperature between the moon's halves influenced the formation of its crust. The lunar crust possesses high concentrations of aluminum and calcium, elements that are very hard to vaporize.
"When rock vapor starts to cool, the very first elements that snow out are aluminum and calcium," study co-author Steinn Sigurdsson of Penn State said in a statement.
Aluminum and calcium would have more easily condensed in the atmosphere on the colder far side of the moon. Eventually, these elements combined with silicates in the mantle of the moon to form minerals known as plagioclase feldspars, making the crust of the far side about twice as thick as that of the near side.
"Earthshine, the heat of Earth soon after the giant impact, was a really important factor shaping the moon," Roy said.
Read more at Discovery News
Jun 15, 2014
Arctic warming linked to fewer European and US cold weather extremes, new study shows
Climate change is unlikely to lead to more days of extreme cold, similar to those that gripped the USA in a deep freeze last winter, new research has shown.
The Arctic amplification phenomenon refers to the faster rate of warming in the Arctic compared to places further south. It is this phenomenon that has been linked to a spike in the number of severe cold spells experienced in recent years over Europe and North America.
However, new research by University of Exeter expert Dr James Screen has shown that Arctic amplification has actually reduced the risk of cold extremes across large swathes of the Northern Hemisphere.
The intriguing new study, published in the scientific journal Nature Climate Change, questions growing fears that parts of Europe and North America will experience a greater number, or more severe, extreme cold days over the course of the next century.
Dr Screen, a Mathematics Research Fellow at the University of Exeter, said: "Autumn and winter days are becoming warmer on average, and less variable from day-to-day. Both factors reduce the chance of extremely cold days."
The idea that there was a link between Arctic amplification and extreme weather conditions became prevalent during the severe winter weather that plagued large areas of the United States in January 2014, leading to major transport disruption, power cuts and crop damage.
In his study, Dr Screen examined detailed climate records to show that autumn and winter temperature variability has significantly decreased over the mid-to-high latitude Northern Hemisphere in recent decades.
He found that this has occurred mainly because northerly winds and associated cold days are warming more rapidly than southerly winds and warm days.
Dr Screen said: "Cold days tend to occur when the wind is blowing from the north, bringing Arctic air south into the mid-latitudes. Because the Arctic air is warming so rapidly these cold days are now less cold than they were in the past."
Read more at Science Daily
The Arctic amplification phenomenon refers to the faster rate of warming in the Arctic compared to places further south. It is this phenomenon that has been linked to a spike in the number of severe cold spells experienced in recent years over Europe and North America.
However, new research by University of Exeter expert Dr James Screen has shown that Arctic amplification has actually reduced the risk of cold extremes across large swathes of the Northern Hemisphere.
The intriguing new study, published in the scientific journal Nature Climate Change, questions growing fears that parts of Europe and North America will experience a greater number, or more severe, extreme cold days over the course of the next century.
Dr Screen, a Mathematics Research Fellow at the University of Exeter, said: "Autumn and winter days are becoming warmer on average, and less variable from day-to-day. Both factors reduce the chance of extremely cold days."
The idea that there was a link between Arctic amplification and extreme weather conditions became prevalent during the severe winter weather that plagued large areas of the United States in January 2014, leading to major transport disruption, power cuts and crop damage.
In his study, Dr Screen examined detailed climate records to show that autumn and winter temperature variability has significantly decreased over the mid-to-high latitude Northern Hemisphere in recent decades.
He found that this has occurred mainly because northerly winds and associated cold days are warming more rapidly than southerly winds and warm days.
Dr Screen said: "Cold days tend to occur when the wind is blowing from the north, bringing Arctic air south into the mid-latitudes. Because the Arctic air is warming so rapidly these cold days are now less cold than they were in the past."
Read more at Science Daily
Plate tectonics: Studies show movements of continents speeding up after slow 'middle age'
Two studies show that the movement rate of plates carrying Earth's crust may not be constant over time. This could provide a new explanation for the patterns observed in the speed of evolution and has implications for the interpretation of climate models. The work is presented today at Goldschmidt 2014, the premier geochemistry conference taking place in Sacramento, California, USA.
Earth's continental crust can be thought of as an archive of Earth's history, containing information on rock formation, the atmosphere and the fossil record. However, it is not clear when and how regularly crust formed since the beginning of Earth history, 4.5 billion years ago.
Researchers led by Professor Peter Cawood, from the University of St. Andrews, UK, examined several measures of continental movement and geologic processes from a number of previous studies. They found that, from 1.7 to 0.75 billion years ago (termed Earth's middle age), Earth appears to have been very stable in terms of its environment, with little in the way of crust building activity, no major fluctuations in atmospheric composition and few major developments seen in the fossil record. This contrasts markedly with the time periods either side of this, which contained major ice ages and changes in oxygen levels. Earth's middle age also coincides with the formation of a supercontinent called Rodinia, which appears to have been stable throughout this time.
Professor Cawood suggests this stability may have been due to the gradual cooling of Earth's crust over time. "Before 1.7 billion years ago, the Earth's crust would have been substantially hotter, meaning that continental plate movement may have been governed by different rules to those that operate today," said Professor Cawood. "0.75 billion years ago, the crust reached a point where it had cooled sufficiently to allow modern day plate tectonics to start working, in particular allowing subduction zones to form (where one plate of the crust moves under another). This increase in activity could have kick-started a myriad of changes including the break-up of Rodinia and changes to levels of key elements in the atmosphere and seas, which in turn may have induced evolutionary changes in the life forms present."
This view is backed up by work from Professor Kent Condie from New Mexico Tech, USA, which suggests the movement rate of Earth's crust is not constant but may be speeding up over time. Professor Condie examined how supercontinents assemble and break up. "Our results challenge the view that the rate of plate movement is stable over time," said Professor Condie. "The interpretation of data from many other disciplines such as stable isotope geochemistry, palaeontology and paleoclimatology in part rely on the assumption that the movement rate of the Earth's crust is constant."
Read more at Science Daily
Earth's continental crust can be thought of as an archive of Earth's history, containing information on rock formation, the atmosphere and the fossil record. However, it is not clear when and how regularly crust formed since the beginning of Earth history, 4.5 billion years ago.
Researchers led by Professor Peter Cawood, from the University of St. Andrews, UK, examined several measures of continental movement and geologic processes from a number of previous studies. They found that, from 1.7 to 0.75 billion years ago (termed Earth's middle age), Earth appears to have been very stable in terms of its environment, with little in the way of crust building activity, no major fluctuations in atmospheric composition and few major developments seen in the fossil record. This contrasts markedly with the time periods either side of this, which contained major ice ages and changes in oxygen levels. Earth's middle age also coincides with the formation of a supercontinent called Rodinia, which appears to have been stable throughout this time.
Professor Cawood suggests this stability may have been due to the gradual cooling of Earth's crust over time. "Before 1.7 billion years ago, the Earth's crust would have been substantially hotter, meaning that continental plate movement may have been governed by different rules to those that operate today," said Professor Cawood. "0.75 billion years ago, the crust reached a point where it had cooled sufficiently to allow modern day plate tectonics to start working, in particular allowing subduction zones to form (where one plate of the crust moves under another). This increase in activity could have kick-started a myriad of changes including the break-up of Rodinia and changes to levels of key elements in the atmosphere and seas, which in turn may have induced evolutionary changes in the life forms present."
This view is backed up by work from Professor Kent Condie from New Mexico Tech, USA, which suggests the movement rate of Earth's crust is not constant but may be speeding up over time. Professor Condie examined how supercontinents assemble and break up. "Our results challenge the view that the rate of plate movement is stable over time," said Professor Condie. "The interpretation of data from many other disciplines such as stable isotope geochemistry, palaeontology and paleoclimatology in part rely on the assumption that the movement rate of the Earth's crust is constant."
Read more at Science Daily
Subscribe to:
Posts (Atom)










