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Kamis, 12 Juli 2007

MOUNT EVEREST


Mount Everest is so famous for being so high that you've probably heard of it before. It has been known the world over since the early 1950s when Sir Edmund Hillary and Tenzig Norgay first climbed to its awesome summit. Hillary surveyed Everest at the time and determined that it was 29,000 ft/8840m high - a figure amazingly close to the current reading of 29,035 ft/8850m, which was confirmed using radar and global positioning satellite (GPS) technology.
Using state-of-the-art technology Professor Brad Washburn of the Boston Museum of Science, the world's foremost mountain cartographer, and his team have calculated that earth's highest elevation is actually 7 feet higher than the previous record. That makes the official height 29,035 ft/8850m. Thanks to some engineering whizzes at the Massachusetts Institute of Technology who developed really light, high-tech gear, the work of Washburn was made easier because he was able to hand carry a radar device to the top of Everest where it could be positioned to measure the actual height of the mountain - underneath all that snow. GPS technology was also deployed near the summit, which uses satellite signal relays to take readings from the top of Everest. After months of crunching numbers Washburn's team arrived at the new, official world-record elevation.
They've also determined that the Himalayan Mountains are still growing higher, at a rate of about 2.4 in/6.1cm per year. That's twice as fast as previously thought. A growth rate of 2.4 in/6.1cm per year doesn't sound like very much. If you think about it, that means in the last 26,000 years the Himalayans have risen almost a mile into the upper reaches of the earth's atmosphere!
When Hillary and Norgay climbed to the top of Everest they wore oxygen tanks. Because Everest is so high it juts into the upper reaches of the earth's atmosphere, where there are much lower concentrations of oxygen than at sea level. What that means to folks trekking up the side of Everest is that their bodies get less oxygen from each breath they breathe while climbing. But their brains and muscles require the same amount of oxygen to perform as they would at sea level. That makes it especially tough to climb Everest.
Try to imagine what it feels like to climb up a mountain with very little oxygen in your body - you get dizzy, your nose, fingers and feet get numb and tingly, your heart thunders in your chest trying furiously to keep up with the muscles' demand for oxygen. You feel sleepy, confused, downright stupid as your brain struggles to function on limited oxygen. Every step you take is extremely slow and plodding, requiring every ounce of will you have. Hillary and Norgay had extra oxygen to help them make the trip, but there have been a few people who have made the trip since who did it without the aid of oxygen - taking one step about every five minutes! About 4,000 climbers have attempted the summit of Everest, but only 660 have made it. One-hundred forty-two people have died trying.

Highest MountainsMount Everest is just one of over 30 peaks in the Himalayas that are over 24,000 ft/7315m high. Himalaya is a Sanskrit word meaning, "abode of snow", which is so true. The snowfields which dominate many of the peaks in the Himalayas are permanent. Yes, they never melt (not even in the summer). That means there are glaciers in the Himalayas - lots of them. Mount Everest is permanently covered in a layer of ice, topped with snow. The "top" of the mountain at which the elevation was measured can vary as much as twenty feet or more, depending on how much snow has fallen on its peak. Scientists believe that the actual tip of the rock lies tens of feet below the ice and snow on its summit. There are current plans to use ground penetrating radar to get a reading of the actual height of the mountain beneath all that snow. Although the Himalayan Range is only 1,550 miles/2480km long, the average height of all the major peaks in the Himalayas easily makes it the highest mountain range on land.

The Birth of a Mountain

Mountains aren't just big piles of dirt, they're made of solid rock. Believe it or not, the rocks that make up the Himalayan mountains used to be an ancient sea floor. Over millions of years, rivers washed rocks and soil from existing mountains on the Indian subcontinent and nearby Asia into a shallow sea where the sediment was deposited on the floor. Layer upon layer of sediment built up over millions of years until the pressure and weight of the overlying sediment caused the stuff way down deep to turn into rock. Then about 40 million years ago, in a process called "uplifting", the sea floor began to be forced upward forming mountains.

Plate Tectonics in Action
What caused the sea floor to be pushed up toward the sky was the result of the action of plate tectonics. The theory of plate tectonics was developed about thirty years ago by scientists who discovered that the earth's crust is made up of many "plates" which are constantly moving around. They are still moving around, even today, but the speeds at which they move are REALLY SLOW. In human terms the movement can't even be seen, but it can be felt occasionally when we have earthquakes. Earthquakes happen when plate margins (edges) move past, or bump into each other. In the case of the Himalayan mountains, the continent of India is part of a plate that "crashed" into southwest Asia, but it didn't stop when it hit. It continued to push northward, crushing and rumpling the earth's crust, resulting in the mountains we see today. If you go back to the map of the Himalayas, you can see that the mountains look kind of like a rumpled blanket. India is still pushing northward today, raising the Himalayas even higher!

news source of http://www.extremescience.com/

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Amphipods from the Challenger Deep


A series of hadal surveys using the ROV "Kaiko" was conducted by Japan Marine Science and Technology Center (JAMSTEC) to clarify distributional chartacteristics of megabenthos at the Challenger Deep (approx. 10,900m deep) located southwestern edge of the Mariana Trench.
During the survey, over 130 specimens of amphipods, Hirondellea gigas, were collected by baited traps. The total length of the largest specimen was over 45mm. It was first collected in the Kurile-Kamchatka Trench in a plankton tow deeper than 6,000m and then in the Philippine Trench and the Mariana Trench between depths of 7,350m and 10,590m.
This is the deepest record to capture the amphipod which is known as endemic scavenger in some trenches. JAMSTEC has a plan to collect amphipods from the Japan Trench and other trenches, and to study phylogenic relationships applying molecular biological techniques.


news source of www.mext.go.jp
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CHALLENGER DEEP


Challenger Deep got its name from the British survey ship Challenger II, which pinpointed the deep water off the Marianas Islands in 1951. Then in 1960, the US Navy sent the Trieste (a submersible - a mini-submarine designed to go really deep) down into the depths of the Marianas trench to see just how far they would go (read the original press release). They touched bottom at 35,838 ft/10,923m. That means, while they were parked on the bottom in the bathyscaphe, there were almost seven miles/11km of water over their heads! If you cut Mount Everest off at sea level and put it on the ocean bottom in the Challenger Deep, there would still be over a mile of water over the top of it!
Hydrostatic Pressure When you get into the ocean (or any body of water) and you start diving down from the surface, the deeper you dive the more water is over the top of you. The more gallons of water you put between you and the surface of the ocean, the greater the pressure is on your body because of the weight of the water over the top of you. This pressure is called hydrostatic pressure.
You can really get a sense of hydrostatic pressure when you go into a swimming pool and dive all the way to the bottom of the deep end. You'll feel the hydrostatic pressure against your ear drums, like they're being squeezed or pushed in. Well, you can imagine how incredible the pressure must be in the Challenger Deep with almost seven miles of water overhead - it's 16,000 pounds per square inch!
The Trieste in 1960. Plate Tectonics and the Subduction Zone
So how come the Challenger Deep is so deep? Well, the earth's crust isn't one solid piece of rock, it's really pretty thin, like the shell of an egg is compared to the size of the egg. In fact, it's made up of huge plates of thin crust that "float" on the molten rock of the earth's mantle. While floating around on the mantle the edges of these plates slide past each other, bump into each other, and sometimes even crash. The oceanic crust is much heavier than the continental crust so when the plates crash into each other, the oceanic plate plunges downward toward the molten mantle, while the lighter, continental plate rides up over the top. The forces driving the two plates together are really intense so the underlying oceanic plate (the subducted plate) creates a trench where it drags the edge of the continental crust down as it descends underneath (check out the picture at left).
This is what's happening on the bottom of the Pacific Ocean off the Marianas islands. The really deep part of the ocean is in the bottom of the trench created by the subducting ocean crust.
So, How Do They Know?
In 1984 the Japanese sent a highly specialized survey vessel out to the Marianas Trench and collected some data using a piece of equipment called a narrow, multi-beam echo sounder.
What an echo sounder does is send high frequency sound waves (outside the range of human hearing) through the water down to the ocean bottom. Sound waves will travel through water, even faster than they travel through the air, and bounce off solid objects, such as the ocean bottom. The echo sounder measures precisely how long it takes for the sound waves to be returned to the surface and determines the depth based on the rate of return. These soundings are plotted on a graph by a computer to make an "echo map" of the ocean bottom.

The deepest measurement of the Challenger Deep currently available was taken by the Japanese and was found to be 35,838 feet.

news source of www.extremescience.com
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ANTARCTICA Land of Extremes

You want to talk about world records, Antarctica is the land of extremes. It is the coldest, windiest, and highest continent anywhere on earth. With an average elevation about 7,544ft/2,300 meters above sea level it is the highest continent. Even though it is covered in ice it receives some of the least amount of rainfall, getting just slightly more rainfall than the Sahara Desert, making it the largest desert on earth. Most people have the misconception that a desert is a hot, dry, sandy, lifeless place, but the true definition of a desert is any geographical location that receives very, very little rainfall. Even though there's ice on the ground in Antarctica, that ice has been there for a very long time. Antarctica is the only continent that has never had an indigenous population of humans because it has always been such an extreme environment. Just the boat ride getting to the continent is over the most treacherous seas anywhere in the world. The inaccessibility of the place and the lack of reliable food and means for constructing shelter has kept humans away for thousands of years. But the new technologies developed over the last 200 years made it possible for people to reach these icy shores to explore and study the Antarctic for the first time in human history. Since there are no people who claim Antarctica as their homeland, exploration of the continent has been shared by all nations of the world. Scientists from all over the world - Russia, Japan, the United States, United Kingdom, Australia, New Zealand, South America, and many others - come to this place in an internationally cooperative agreement to study the truly unique qualities of Antarctica. Many scientific stations have been constructed on Antarctica to provide shelter and supplies for scientists doing field work there. Meet a scientist who's been to Antarctica - even went diving under the ice! Some scientists actually live on Antarctica for part of the year to conduct their research. Very few scientists stay there more than six months at a time. The sun rises and sets only once a year at the South Pole, which means there are six months of daylight, followed by six months of darkness. During the winter when there is no sun, the Antarctic becomes an even more hostile place to be - colder than cold, BONE-CHILLING cold, and no daylight. Can you imagine living in darkness 24 hours a day? That would almost be like living out in space! Hey.....
The World's Biggest Laboratory
At first, the scientific value of studying the Antarctic was just for the sake of understanding this strange place. Recently, scientists have theorized that the conditions in the Antarctic are similar to those on Mars. Because of the similarities exploration of the Antarctic has taken on a new meaning for the search for signs of life in the most extreme environments. Antarctica is not only fascinating itself, but serves as an excellent laboratory for studying the effects of space travel, developing new technologies for exploring other planets and finding extraterrestrial (yeah, alien) life.
Many, many fascinating things have been discovered in the Antarctic that have challenged some of our most basic ideas about what life on earth means. Some really cool factoids:
Deepest Earth Depression: The lowest point on earth is located in the basin of the Bentley Subglacial Trench. At -2,555 meters (8,325 feet) below sea level it is the world's lowest elevation not under seawater. It is not accessible because it is buried under the thickest ice yet discovered.
90% of the ice on earth is located in Antarctica. There is so much ice there you could carve up a block of ice the size of the Great Giza pyramid for every human being on the planet! 98% of Antarctica is covered in ice.
Marine Life: Some species of fish that live in the waters around Antarctica are specially adapted to life in near-freezing waters. Most living creatures on this planet have hemoglobin in their blood, which gives it that red color we all know so well. These particular species of fish, however, have extremely low levels of hemoglobin in their blood. So low that their blood isn't even red! They also have natural antifreeze in their bodies to protect them from freezing to death. (Even if you're a fish and the water in all the cells of your body freezes and turns to ice crystals, you die. 'Nuff said). If you were to catch one of these fish and cut it open the blood, gills and all the organs would be WHITE.
Weather: Yes, the Antarctic has the coldest temperatures on the earth, but that shouldn't surprise you. (Coldest reported temperature ever was -89.4°C/-129°F.) What most people don't know is that the South Pole has the clearest, calmest weather anywhere on earth. Most of the wickedly high winds that everyone associates with the cold and the ice of the Antarctic are around the edges of the continent at the shores. These winds are so fast and so fierce they are world-famous and they have a special name, too - katabatic winds - and they can blow with hurricane force up to 304kmh/190 mph!
Believe it or not with all the ice in the Antarctic, there is very little actual snowfall or precipitation. It does snow on the ice during the austral winter, but measured on an annual basis the Antarctic is as dry as the Sahara Desert.
Antarctic Ice - The Ultimate Cool
Many scientists study Antarctic ice because it is more than just ice. It has accumulated over time, layer upon layer, building up over the millennia to create a type of sedimentary rock. Yes, rock. Ice crystals can be considered a type of mineral, and glacial ice is composed of crystals of the "mineral" water. Just like sedimentary rock is created over time by the repeated layering of particles of clay or sand, glacial ice builds up over millions of years by the build up of snow that never melts.
Scientists drill down deep into the ice with a drill that works kind of like a cookie cutter, only it cuts out some really deep cookies of ice. These core samples contain many layers of ice that represent what the earth's atmosphere was like at the time each layer of ice was formed. By studying the layers of ice in the core samples scientists can learn about how the earth's atmosphere has changed over geologic time.
In the winter time the ocean around Antarctica freezes for thousands of miles in all directions. This vast expanse of ice surrounding the already immense Antarctic ice sheet covers over eleven million square kilometers. The annual freezing of the ocean around Antarctica generates deep ocean currents worldwide. Differences in ocean temperature are what cause weather all over the globe. Some scientists fear that if the global climate gets too warm or too cold it could affect the formation of Antarctic ice, changing the climate as we know it all over the world.


news source of www.extremescience.com
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The Amazon - Home of Extremes


The Amazon River is not only the greatest in the world, it is home to many other "Extremes" of the natural world. Have you ever seen a catfish? They're usually found in warm, slow moving waters of lakes and streams, and some people keep them as pets in aquariums. Catfish are pretty creepy looking fish with big flat heads and "whiskers" on either side of their heads (hence the name, catfish). Most catfish that we're familiar with here in the U.S. are anywhere from eight inches long to about five feet, weighing in at up to 60 pounds. But the catfish that live in the world's greatest river have all the room in the world to grow as big as nature will allow - they have been captured weighing over 200 pounds! One of the largest freshwater fish in the world is found living in the waters of the Amazon River. Arapaima, also known locally as Pirarucu, Arapaima gigas are the largest, exclusively fresh water fish in the world. They have been found to reach a length of 15 ft/4m and can weigh up to 440lbs/200kg. And yes, for you smartypants out there, sturgeon are even larger than this, but they are not exclusively freshwater fish. Sturgeon spend most of their lives at sea, or in brackish water, and only swim into freshwater rivers to spawn. (Read about the biggest freshwater fish in the world.)
(Buy this Photographic Print at AllPosters.com) The Amazon is also home to some other extreme creatures, featured here in "Extreme Science"; the Anaconda (biggest snake), and Piranha (most ferocious). Check it out!


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How Great is the Amazon River?


The Amazon is the greatest river in the world by so many measures; the volume of water it carries to the sea (approximately 20% of all the freshwater discharge into the oceans), the area of land that drains into it, and its length and width. It is one of the longest rivers in the world and, depending upon who you talk to, is anywhere between 6,259km/3,903mi and 6,712km/4,195mi long.
For the last century the length of the Amazon and the Nile Rivers have been in a tight battle for title of world's longest river. The exact length of the two rivers varies over time and reputable sources disagree as to their actual length. The Nile River in Africa is reported to be anywhere from at 5,499km/3,437mi to 6,690km/4,180mi long. But there is no question as to which of the two great rivers carries the greater volume of water - the Amazon River.

At its widest point the Amazon River can be 11km/6.8 mi wide during the dry season. The area covered by the Amazon River and its tributaries more than triples over the course of a year. In an average dry season 110,000 square km of land are water-covered, while in the wet season the flooded area of the Amazon Basin rises to 350,000 square km. When the flood plains and the Amazon River Basin flood during the rainy season the Amazon River can be up to 40km/24.8 mi wide. Where the Amazon opens at its estuary the river is over 325km/202 mi wide!
Because the Amazon drains the entire Northern half of the South American continent (approx. 40% landmass), including all the torrential tropical rains that deluge the rainforests, it carries an enormous amount of water. The mouth of the Amazon River, where it meets the sea, is so wide and deep that ocean-going ships have navigated its waters and traveled as far inland as two-thirds the way up the entire length of the river.

Amazon River Facts
So, how did the Amazon get to be so big? The first reason has to do with its location - right at the equator. Around the "belt line" of the earth lies a warm, tropical zone where over 400 in/1016cm of rain fall every year. That averages out to more than an inch (3cm) of rain, everyday! A lot of water falls onto the land surrounding the river, what is called the "Amazon River drainage basin". A good way to understand what a drainage basin is to think of the whole northern half of the continent of South America as a shallow dish, or saucer. Whenever rain falls and lands anywhere in the river basin it all runs into the lowest place in the pan, which happens to be the Amazon River. The sheer volume of rain in the Amazon jungle, as well as the slope of the surrounding land, combine to create the enormous river known as the Amazon.


news source of www.extremescience.com
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Krakatoa Volcano: The Son Also Rises


As Americans watch the volcanic activity of Mount St. Helens with awe and unease, on the other side of the world, in Indonesia, tourists flock to the site of one of the most spectacular volcanic explosions ever recorded.
Krakatoa, west of Java, erupted with such fury in 1883 that it reportedly was heard as far away as Bangkok and Australia. It blew the island of Rakata to pieces and killed more than 30,000 people. Some scientists say it was the biggest bang in recorded history.
Anak Krakatau (the "son of Krakatoa") emerged from almost the same spot and is growing every day. At roughly 1,300 feet high, it's a popular tourist destination. Many wonder whether -- or when -- it too might erupt. NPR's Michael Sullivan reports.



news source of www.npr.org

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Dodo


Dodo
The Dodo (Raphus cucullatus) was a flightless bird that lived on the islands of Mauritius. Related to pigeons and doves, it stood about a metre tall (three feet), lived on fruit and nested on the ground.
The dodo has been extinct since the mid-to-late 17th century. It is commonly used as the archetype of an extinct species because its extinction occurred during recorded human history, and was directly attributable to human activity. The phrase "as dead as a dodo" means undoubtedly and unquestionably dead.

Etymology
The etymology of the word dodo is not clear. It may be related to dodaars ("plump-arse"), the Dutch name of the Little Grebe. The connection may have been made because of similar feathers of the hind end or because both animals were ungainly. However, the Dutch are also known to have called the Mauritius bird the walghvogel ("loathsome bird" or "nauseating fowl") in reference to its taste. This last name was used for the first time in the journal of vice-admiral Wybrand van Warwijck who visited and named the island Mauritius in 1598. Dodo or Dodaerse is recorded in captain Willem van West-Zanen's journal four years later, but it is unclear whether he was the first one to use this name, because before the Dutch, the Portuguese had already visited the island in 1507, but did not settle permanently.
According to Encarta Dictionary and Chambers Dictionary of Etymology, "dodo" comes from Portuguese doudo (currently doido) meaning "fool" or "crazy". However, the present Portuguese name for the bird, dodô, is of English origin. The Portuguese word doudo or doido may itself be a loanword from Old English (cf. English "dolt").
Yet another possibility is that dodo was an onomatopoeic approximation of the bird's own call, a two-note pigeony sound like 'doo-doo'.

Biology
Systematics and evolution
The dodo is a close relative of modern pigeons and doves. mtDNA cytochrome b and 12S rRNA sequences analysis suggests that the dodo's ancestors diverged from those of its closest known relative, the Rodrigues Solitaire (which is also extinct), around the Paleogene-Neogene boundary. As the Mascarenes are of volcanic origin and less than 10 million years old, both birds' ancestors remained most likely capable of flight for considerable time after their lineages' separation. The same study has been interpreted[6] to show that the Southeast Asian Nicobar Pigeon is the closest living relative of the dodo and the Reunion Solitaire.
However, the proposed phylogeny is rather questionable as regards the relationships of other taxa and must therefore be considered hypothetical pending further research; considering biogeographical data, it is very likely to be erroneous. All that can be presently said with any certainty is that the ancestors of the didine birds were pigeons from Southeast Asia or the Wallacea, which agrees with the origin of most of the Mascarenes' birds. Whether the dodo and Rodrigues Solitaire were actually closest to the Nicobar Pigeon among the living birds, or whether they are closer to other groups of the same radiation such as Ducula, Treron or Goura pigeons is not clear at the moment.
For a long time, the dodo and the Rodrigues Solitaire (collectively termed "didines") were placed in a family of their own, the Raphidae. This was because their relationships to other groups of birds (such as rails) had yet to be resolved. As of recently, it appears more warranted to include the didines as a subfamily Raphinae in the Columbidae.
The supposed "White Dodo" is now thought to be based on misinterpreted reports of the Réunion Sacred Ibis and paintings of apparently albinistic dodos; a higher frequency of albinos is known to occur occasionally in island species (see also Lord Howe Swamphen).

Morphology and flightlessness
In October 2005, part of the Mare aux Songes, the most important site of dodo remains, was excavated by an international team of researchers. Many remains were found, including bones from birds of various stages of maturity, and several bones obviously belonging to the skeleton of one individual bird and preserved in natural position. These findings were made public in December 2005 in the Naturalis in Leiden. Before this, few associated dodo specimens were known, most of the material consisting of isolated and scattered bones. Dublin's Natural History Museum and the Oxford University Museum of Natural History, among others, have a specimen assembled from these disassociated remains. A Dodo egg is on display at the East London museum in South Africa. Until recently, the most intact remains, currently on display at the Oxford University Museum of Natural History, were one individual's partly skeletal foot and head which contain the only known soft tissue remains of the species.
In June 2007, adventurers exploring a cave in the Indian Ocean discovered the most complete and well-preserved dodo skeleton ever
The remains of the last known stuffed dodo had been kept in Oxford's Ashmolean Museum, but in the mid-18th century, the specimen - save the pieces remaining now - had entirely decayed and was ordered to be discarded by the museum's curator or director in or around 1755. According to the current curator, Malgosia Nowak-Kemp, the commonly-cited story that the remains were merely damaged - implying that more material could or should have been salvaged, and/or that the present remains were serendipitiously saved against the curator's orders - is an urban legend arising from a mistranslation of the Latin museum records.[citation needed] Nevertheless, from artists' renditions we know that the Dodo had greyish plumage, a 23-centimetre (9-inch) bill with a hooked point, very small wings, stout yellow legs, and a tuft of curly feathers high on its rear end. Dodos were very large birds, weighing about 23 kg (50 pounds). The sternum was insufficient to support flight; these ground-bound birds evolved to take advantage of an island ecosystem with no predators.
The traditional image of the dodo is of a fat, clumsy bird, but this view has been challenged in recent times. The general opinion of scientists today is that the old drawings showed overfed captive specimens. As Mauritius has marked dry and wet seasons, the dodo probably fattened itself on ripe fruits at the end of the wet season to live through the dry season where food was scarce; contemporary reports speak of the birds' "greedy" appetite. Thus, in captivity, with food readily available, the birds would become overfed very easily.

Diet
The tambalacoque, also known as the "dodo tree", was hypothesized by Stanley Temple to have been eaten from by Dodos, and only by passing through the digestive tract of the dodo could the seeds germinate; he claimed that the tambalacocque was now nearly extinct due to the dodo's disappearance. He force-fed seventeen tambalacoque fruits to wild turkeys and three germinated. Temple did not try to germinate any seeds from control fruits not fed to turkeys so the effect of feeding fruits to turkeys was unclear. Temple also overlooked reports on tambalacoque seed germination by A. W. Hill in 1941 and H. C. King in 1946, who found the seeds germinated, albeit rarely, without abrading.

Extinction
As with many animals evolving in isolation from significant predators, the dodo was entirely fearless of people, and this, in combination with its flightlessness, made it easy prey. But journals are full of reports regarding the bad taste and tough meat of the dodo, while other local species such as the Red Rail were praised for their taste. It is commonly believed that the Malay sailors held the bird in high regard and killed them only to make head dressings used in religious ceremonies. However, when humans first arrived on Mauritius, they also brought with them other animals that had not existed on the island before, including dogs, pigs, cats, rats, and Crab-eating Macaques, which plundered the dodo nests, while humans destroyed the forests where the birds made their homes; currently, the impact these animals — especially the pigs and macaques — had on the dodo population is considered to have been more severe than that of hunting. The 2005 expedition's finds are apparently of animals killed by a flash flood; such mass mortalities would have further jeopardized an already extinction-prone species.
Although there are scattered reports of mass killings of dodos for provisioning of ships, archaeological investigations have hitherto found scant evidence of human predation on these birds. Some bones of at least two dodos were found in caves at Baie du Cap which were used as shelters by fugitive slaves and convicts in the 17th century, but due to their isolation in high, broken terrain were not easily accessible to dodos naturally. By 1755, Cossigny reports that the number of refugees and settlers which cut down the inland forest was so high that the well-flighted Mauritius Blue Pigeon was rapidly declining all over the island.[citation needed]
There is some controversy surrounding the extinction date of the dodo. Roberts & Solow state that "the extinction of the Dodo is commonly dated to the last confirmed sighting in 1662, reported by shipwrecked mariner Volkert Evertsz" (Evertszoon), but many other sources suggest the more conjectural date 1681. Roberts & Solow point out that because the sighting prior to 1662 was in 1638, the dodo was likely already very rare by the 1660s, and that thus a disputed report from 1674 cannot be dismissed off-hand. Statistical analysis of the hunting records of Issac Johannes Lamotius, carried out by Julian Hume and coworkers,[citation needed] give a new estimated extinction date of 1693, with a 95% confidence interval of 1688 to 1715. Considering more circumstantial evidence such as travellers' reports and the lack of good reports after 1689, it is likely that the dodo became extinct before 1700; thus, the last Dodo died barely more than a century after the species' discovery in 1581.Few took particular notice of the extinct bird. By the early 19th century it seemed altogether too strange a creature, and was believed by many to be a myth. With the discovery of the first batch of dodo bones in the Mare aux Songes and the reports written about them by George Clarke, government schoolmaster at Mahébourg, from 1865 on,[22] interest in the bird was rekindled. In the same year in which Clarke started to publish his reports, the newly-vindicated bird was featured as a character in Lewis Carroll's Alice's Adventures in Wonderland. With the popularity of the book, the dodo became a well-known and easily recognizable icon of extinction.

news source of www.wikipedia.org
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