What About August 21? A Limited-Time Eclipse OpportunityInquisitr: Space



Are you doing anything on August 21? If you’re not busy (or even if you are), you might consider the Great American Solar Eclipse. For many, this will be a once-in-a-lifetime chance to see a total solar eclipse. Think that’s not a big deal? Maybe you should read on.

Things To Consider About This Year’s Eclipse The last good time to view a total solar eclipse in the U.S. was almost 50 years ago. We did have one back on February 26, 1979. But, it could only be seen in a limited number of areas in the Northwest. This was because “the weather for the most part was bleak,” (via Astronomy) So, really the last good time was more like 1970.

The next good time to view a total solar eclipse in the U.S. won’t be in until April of 2024. Since none of us know what the future holds, next time might not be as convenient for you or your schedule.

Solar eclipses only happen at a New Moon. While solar eclipses happen at a New Moon, they don’t happen at every New Moon, and while solar eclipses always happen at a New Moon, lunar eclipses always happen at a Full Moon (but not every Full Moon).

Totality is totally “it.” If at all possible, you should definitely try to be in the “path of totality,” that path of the eclipse where there is 100 percent coverage. If not, you will really wonder what all the hoopla is about. To quote the words of Astronomy Magazine, “likening a partial eclipse to a total eclipse is like comparing almost dying to dying.” So, get into the path of totality, if you can.

The weather looks good for viewing. This time of year, the weather is good over large parts of the U.S. That means the chance that the weather will be good for eclipse viewing is high. And, since the viewing time for most will be less than two-and-a-half minutes, that is important.

Safety Is Key Since viewing a total solar eclipse might be a “bucket list” item for many people, paying attention to safety will be important. There will be lots of people trying to get a view. Here are some safety items to consider.

Consider getting to your viewing site early. With millions of people trying to find a good place to view the eclipse, things could get crowded and busy, especially right before viewing time. You can avoid the rush by having a plan for getting to your destination and getting there early.

If viewing the eclipse directly, consider wearing eclipse glasses. Good eclipse glasses can be obtained cheaply. Make the investment. Good eclipse glasses will block out the sun’s rays but allow you to see the special event clearly and in comfort.

If viewing the eclipse indirectly, construct or setup your pin-hole viewer at least an hour before the eclipse is scheduled to start. That way, if you have issues, you have time to fix them and not miss the event. Better yet, bring spare parts just to be sure.

Consider traveling away from the masses. A good plan for viewing might include getting away from the crowd. If possible, it might be a good idea to plan your viewing for out in the country. It may be easier to find open space.

August 21 will soon be upon us, and the path of totality may not be far from you. Consider a trip to see “the most spectacular sight in nature,” (via Great American Eclipse). The time and the weather may make this a great year for viewing. But, if you venture out, be safe. Make this August 21 a most positive experience that you can tell your friends and family about for years to come.


Effects of Global Warming

Global warming is expected to have far-reaching, long-lasting and, in many cases, devastating consequences for planet Earth.

Global warming, the gradual heating of Earth's surface, oceans and atmosphere, is caused by human activity, primarily the burning of fossil fuels that pump carbon dioxide (CO2), methane and other greenhouse gases into the atmosphere.

Despite political controversy about climate change, a major report released Sept. 27, 2013, by the Intergovernmental Panel on Climate Change (IPCC) stated that scientists are more certain than ever of the link between human activities and global warming. More than 197 international scientific organizations agree that global warming is real and has been caused by human action.

Already, global warming is having a measurable effect on the planet.

"We can observe this happening in real time in many places. Ice is melting in both polar ice caps and mountain glaciers. Lakes around the world, including Lake Superior, are warming rapidly — in some cases faster than the surrounding environment. Animals are changing migration patterns and plants are changing the dates of activity," such as trees budding their leaves earlier in the spring and dropping them later in the fall, Josef Werne, a professor of geology and environmental science at the University of Pittsburgh, told Live Science.

Here is an in-depth look at the changes wrought by global warming.

Increase in average temperatures and temperature extremes
One of the most immediate and obvious effects of global warming is the increase in temperatures around the world. The average global temperature has increased by about 1.4 degrees Fahrenheit (0.8 degrees Celsius) over the past 100 years, according to the National Oceanic and Atmospheric Administration (NOAA).

Since record keeping began in 1895, the hottest year on record worldwide was 2016, according to NOAA and NASA data. That year Earth's surface temperature was 1.78 degrees F (0.99 degrees C) warmer than the average across the entire 20th century. Before 2016, 2015 was the warmest year on record, globally. And before 2015? Yep, 2014. In fact, 16 of the 17 warmest years on record have happened since 2001, according to NASA.

For the contiguous United States and Alaska, 2016 was the second-warmest year on record and the 20th consecutive year that the annual average surface temperature exceeded the 122-year average since record keeping began, according to NOAA.

Extreme weather events
Extreme weather is another effect of global warming. While experiencing some of the hottest summers on record, much of the United States has also been experiencing colder-than-normal winters.

Changes in climate can cause the polar jet stream — the boundary between the cold North Pole air and the warm equatorial air — to migrate south, bringing with it cold, Arctic air. This is why some states can have a sudden cold snap or colder-than-normal winter, even during the long-term trend of global warming, Werne explained.

"Climate is, by definition, the long-term average of weather, over many years. One cold (or warm) year or season has little to do with overall climate. It is when those cold (or warm) years become more and more regular that we start to recognize it as a change in climate rather than simply an anomalous year of weather," he said.

Global warming may also lead to extreme weather other than cold or heat extremes. For example, hurricane formations will change. Though this is still a subject of active scientific research, current computer models of the atmosphere indicate that hurricanes are more likely to become less frequent on a global basis, though the hurricanes that do form may be more intense.

"And even if they become less frequent globally, hurricanes could still become more frequent in some particular areas," said atmospheric scientist Adam Sobel, author of "Storm Surge: Hurricane Sandy, Our Changing Climate, and Extreme Weather of the Past and Future" (HarperWave, 2014). "Additionally, scientists are confident that hurricanes will become more intense due to climate change." This is because hurricanes get their energy from the temperature difference between the warm tropical ocean and the cold upper atmosphere. Global warming increases that temperature difference.

"Since the most damage by far comes from the most intense hurricanes — such as typhoon Haiyan in the Philippines in 2013 — this means that hurricanes could become overall more destructive," said Sobel, a Columbia University professor in the departments of Earth and Environmental Sciences, and Applied Physics and Applied Mathematics. (Hurricanes are called typhoons in the western North Pacific, and they're called cyclones in the South Pacific and Indian oceans.)

Lightening is another weather feature that is being affected by global warming. According to a 2014 study, a 50 percent increase in the number of lightning strikes within the United States is expected by 2100 if global temperatures continue to rise. The researchers of the study found a 12 percent increase in lightning activity for every 1.8 degree F (1 degree C) of warming in the atmosphere.

NOAA established the U.S. Climate Extremes Index (CEI) in 1996 to track extreme weather events. The number of extreme weather events that are among the most unusual in the historical record, according to the CEI, has been rising over the last four decades.

Scientists project that extreme weather events, such as heat waves, droughts, blizzards and rainstorms will continue to occur more often and with greater intensity due to global warming, according to Climate Central. Climate models forecast that global warming will cause climate patterns worldwide to experience significant changes. These changes will likely include major shifts in wind patterns, annual precipitation and seasonal temperatures variations.

In addition, because high levels of greenhouse gases are likely to remain in the atmosphere for many years, these changes are expected to last for several decades or longer, according to the U.S. Environmental Protection Agency (EPA). In the northeastern United States, for example, climate change is likely to bring increased annual rainfall, while in the Pacific Northwest, summer rainfall is expected to decrease, the EPA said.

Ice melt
One of the primary manifestations of climate change so far is melt. North America, Europe and Asia have all seen a trend toward less snow cover between 1960 and 2015, according to 2016 research published in the journal Current Climate Change Reports. According to the National Snow and Ice Data Center, there is now 10 percent less permafrost, or permanently frozen ground, in the Northern Hemisphere than there was in the early 1900s. The thawing of permafrost can cause landslides and other sudden land collapses. It can also release long-buried microbes, as in a 2016 case when a cache of buried reindeer carcasses thawed and caused an outbreak of anthrax.

One of the most dramatic effects of global warming is the reduction in Arctic sea ice. Sea ice hit record-low extents in both the fall and winter of 2015 and 2016, meaning that at the time when the ice is supposed to be at its peak, it was lagging. The melt means there is less thick sea ice that persists for multiple years. That means less heat is reflected back into the atmosphere by the shiny surface of the ice and more is absorbed by the comparatively darker ocean, creating a feedback loop that causes even more melt, according to NASA's Operation IceBridge.

Glacial retreat, too, is an obvious effect of global warming. Only 25 glaciers bigger than 25 acres are now found in Montana's Glacier National Park, where about 150 glaciers were once found, according to the U.S. Geological Survey. A similar trend is seen in glacial areas worldwide. According to a 2016 study in the journal Nature Geoscience, there is a 99 percent likelihood that this rapid retreat is due to human-caused climate change. Some glaciers retreated up to 15 times as much as they would have without global warming, those researchers found.

Sea levels and ocean acidification
In general, as ice melts, sea levels rise. In 2014, the World Meteorological Organization reported that sea-level rise accelerated 0.12 inches (3 millimeters) per year on average worldwide. This is around double the average annual rise of 0.07 in. (1.6 mm) in the 20th century.

Melting polar ice in the Arctic and Antarctic regions, coupled with melting ice sheets and glaciers across Greenland, North America, South America, Europe and Asia, are expected to raise sea levels significantly. And humans are mostly to blame: In the IPCC report released on Sept. 27, 2013, climate scientists said they are at least 95 percent certain that humans are to blame for warming oceans, rapidly melting ice and rising sea levels, changes that have been observed since the 1950s.

Global sea levels have risen about 8 inches since 1870, according to the EPA, and the rate of increase is expected to accelerate in the coming years. If current trends continue, many coastal areas, where roughly half of the Earth's human population lives, will be inundated.

Researchers project that by 2100, average sea levels will be 2.3 feet (.7 meters) higher in New York City, 2.9 feet (0.88 m) higher at Hampton Roads, Virginia, and 3.5 feet (1.06 m) higher at Galveston, Texas, the EPA reports. According to an IPCC report, if greenhouse gas emissions remain unchecked, global sea levels could rise by as much as 3 feet (0.9 meters) by 2100. That estimate is an increase from the estimated 0.9 to 2.7 feet (0.3 to 0.8 meters) that was predicted in the 2007 IPCC report for future sea-level rise.

Sea level isn't the only thing changing for the oceans due to global warming. As levels of CO2 increase, the oceans absorb some of that gas, which increases the acidity of seawater. Werne explains it this way: "When you dissolved CO2 in water, you get carbonic acid. This is the same exact thing that happens in cans of soda. When you pop the top on a can of Dr Pepper, the pH is 2 — quite acidic."

Since the Industrial Revolution began in the early 1700s, the acidity of the oceans has increased about 25 percent, according to the EPA. "This is a problem in the oceans, in large part, because many marine organisms make shells out of calcium carbonate (think corals, oysters), and their shells dissolve in acid solution," said Werne.  "So as we add more and more CO2 to the ocean, it gets more and more acidic, dissolving more and more shells of sea creatures. It goes without saying that this is not good for their health."

If current ocean acidification trends continue, coral reefs are expected to become increasingly rare in areas where they are now common, including most U.S. waters, the EPA reports. In 2016 and 2017, portions of the Great Barrier Reef in Australia were hit with bleaching, a phenomenon in which coral eject their symbiotic algae. Bleaching is a sign of stress from too-warm waters, unbalanced pH or pollution; coral can recover from bleaching, but back-to-back episodes make recovery less likely.

Plants and animals
The effects of global warming on the Earth's ecosystems are expected to be profound and widespread. Many species of plants and animals are already moving their range northward or to higher altitudes as a result of warming temperatures, according to a report from the National Academy of Sciences.

"They are not just moving north, they are moving from the equator toward the poles. They are quite simply following the range of comfortable temperatures, which is migrating to the poles as the global average temperature warms," Werne said. Ultimately, he said, this becomes a problem when the rate of climate change velocity (how fast a region changes put into a spatial term) is faster than the rate that many organisms can migrate. Because of this, many animals may not be able to compete in the new climate regime and may go extinct.

Additionally, migratory birds and insects are now arriving in their summer feeding and nesting grounds several days or weeks earlier than they did in the 20th century, according to the EPA.

Warmer temperatures will also expand the range of many disease-causing pathogens that were once confined to tropical and subtropical areas, killing off plant and animal species that formerly were protected from disease.

These and other effects of global warming, if left unchecked, will likely contribute to the disappearance of up to one-half of Earth's plants and one-third of animals from their current range by 2080, according to a 2013 report in the journal Nature Climate Change.

Social effects
As dramatic as the effects of climate change are expected to be on the natural world, the projected changes to human society may be even more devastating.

Agricultural systems will likely be dealt a crippling blow. Though growing seasons in some areas will expand, the combined impacts of drought, severe weather, lack of accumulated snowmelt, greater number and diversity of pests, lower groundwater tables and a loss of arable land could cause severe crop failures and livestock shortages worldwide.

North Carolina State University also notes that carbon dioxide is affecting plant growth. Though CO2 can increase the growth of plants, the plants may become less nutritious.

This loss of food security may, in turn, create havoc in international food markets and could spark famines, food riots, political instability and civil unrest worldwide, according to a number of analyses from sources as diverse as the U.S Department of Defense, the Center for American Progress and the Woodrow Wilson International Center for Scholars.

In addition to less nutritious food, the effect of global warming on human health is also expected to be serious. The American Medical Association has reported an increase in mosquito-borne diseases like malaria and dengue fever, as well as a rise in cases of chronic conditions like asthma, most likely as a direct result of global warming. The 2016 outbreak of Zika virus, a mosquito-borne illness, highlighted the dangers of climate change. The disease causes devastating birth defects in fetuses when pregnant women are infected, and climate change could make higher-latitude areas habitable for the mosquitos that spread the disease, experts said. Longer, hotter summers could also lead to the spread of tick-borne illnesses.
Largest ever dinosaur may have been as long as 7 elephants
 


Fossilised bones from six dinosaurs may have belonged to the biggest animal ever to have walked the Earth.

The fossils, which include vertebrae and rib bones, are from six young adult dinosaurs, and were all found in the same Patagonian quarry in Argentina. The species, named Patagotitan mayorum, is thought to have weighed around 62 tonnes and measured more than 35 metres from nose to tail.

If you’re struggling to picture that, it’s about seven elephants, or more than two buses, or half the width of a football pitch, or somewhere between a standard swimming pool and an Olympic pool. That’s longer than Brachiosaurus was, and blue whales are today – both these species reach a maximum of about 30 metres.

Patagotitan lived 100 million years ago, during the Cretaceous period, and was a sauropod – a huge plant-eater with a long tail and neck, that stood on four legs.

The species has competition for the crown of largest ever land animal. A similar dinosaur called Argentinosaurus has been calculated to have weighed more than 80 tonnes, but Jose Carballido, from the Museo Paleontologico Egido Feruglio, Argentina, says vertebrae fossils suggest this species was in fact 10 per cent smaller than Patagotitan.

New Map Of The Universe Probes The Enduring Mystery Of Dark Matter

One of science’s most enduring mysteries was the subject of a new map of the Universe that was released earlier this week.

The product of over five years of intense study by The Dark Energy Survey (DES), the map is the most accurate yet of the substance. In order to produce the map, researchers collected light from 26 million galaxies and studied how the light from them has changed over the course of the preceding seven billion years. Observing the shapes of these galaxies enabled them to map patterns of dark matter, making it possible to compile a map showing its distribution across the known galaxy.

Mapping the entire Universe is no mean feat, necessitating a tremendous amount of manpower and a good deal of innovation. Four hundred scientists from seven countries were involved in the project, collaborating to build a 570-megapixel camera for use at the four-meter Victor M. Blanco telescope at the Cerro Tololo Inter-American Observatory in Chile.

Most of the Universe is Dark
According to the data collected, dark matter accounts for 26 percent of the Universe’s contents, with dark energy providing 70 percent and ordinary matter making up the remaining four percent. This is in line with findings conducted to this point, and it reinforces the ΛCDM (Lambda cold dark matter) model, also known as the “standard” model, of cosmology that gained wide acceptance within the scientific community in the mid-1990s.

Chair of the DES Advisory Board Professor Ofer Lahav of University College London (UCL) is optimistic that the data collected and the findings made as a result of this project will lead to significant leaps in achieving a more complete theory of physics.
Dark matter is long assumed.little understood
Though postulated as far back as 1884 by Lord Kelvin (for whom the kelvin temperature scale is named), dark matter remained an elusive subject for study until the 1930’s. Continued studies by Vera Rubin and Kent Ford in the 1960’s and 1970’s led to conclusions that most galaxies likely contained around six times more dark mass as they do visible mass.

Radio telescope observations in the 1980’s lent further credence to the idea, with studies of the phenomena undertaken using gravitational lensing, velocity dispersion, and the cosmic microwave background.

आप स्टूडेंट हैं तो ये चार मोबाइल ऐप्स आपके लिए हैं बेहद काम के...

अगर आप स्टूडेंट हैं तो ये चार मोबाइल ऐप्स आपके लिए हैं बेहद काम के...


आज के दौर में मोबाइल न केबल एक सेफ्टी के लिहाज से जरुरी हो गया है बल्कि दिनों दिन यह हमारे दैनिक जीवन को सुलभ बनाने में भी बहुत योगदान दे रहा है
अगर आप स्टूडेंट हैं तो ये चार मोबाइल ऐप्स आपके लिए हैं बेहद काम के...
स्टूडेंटस के मोबाइल में जरूरी हैं ये चार ऐप्स- प्रतीकात्मक फोटो
नई दिल्ली: आज के दौर में मोबाइल न केवल एक सेफ्टी के लिहाज से जरुरी हो गया है बल्कि दिनों दिन यह हमारे दैनिक जीवन को सुलभ बनाने में भी बहुत योगदान दे रहा है. रात को सोने से पहले तक, सुबह जागने के बाद मोबाइल ही एक ऐसी चीज है जो एक तरह से हर समय हमारे पास रहती है. ऐसे में मोबाइल जगत के ऐप्स हम सभी के जीवन में हमारी जरुरतों के हिसाब से बहुत सहायक होते जा रहे हैं. इसी कड़ी में आज हम आपको बताएंगे मोबाइल से जुडे ऐसे ऐप्स जो स्टूडेंटस के लिए हैं काम के :

पीडीएफ कन्वर्टर (Pdf converter) : इससे आप किसी भी फाइल को pdf में  कनवर्ट कर सकते हैं इससे ऐप के द्वारा आप इमेजिस, क्लिप वोर्ड, फाइल्स मैसेजिस, मेल और यहां तक कि आपके फोन में मौजूद कॉन्टेक्ट्स को भी आप pdf में कनवर्ट कर सकते हैं. सबसे पहले अपने फोन के गूगल ड्राइव को ओपन कर के टाइप करें pdf converter. इसके बाद आप वहां दिये गये Appsbuyout के Pdf converter app को डाउनलोड करें. डाउनलोड हो जाने के बाद ऐप को ओपन करें. अब आपके सामने एक विंडो खुलेगी,  अब आपको जिस फाइल को pdf में कन्वर्ट करना है उसके आयकन को सिलेक्ट करें,  इसके बाद फाइल सिलेक्ट करें जिसे आपको कंवर्ट करना है, अपनी सुविधा के लिए फाइल का नाम दें और  OK क्लिक करते ही आपकी फाइल pdf में कन्वर्ट हो जाएगी.

कैम स्कैनर (Cam Scanner) : इस ऐप के जरिये आप किसी भी डाक्युमेंट की फोटो को मार्केट में होने बाली स्कैन कॉपी की तरह ही कुछ सेकंड्स में अपने मोबाइल की मदद से स्कैन कर सकते हैं. INTSIG Information Co. Ltd द्वारा तैयार इस ऐप को एक बार डाउनलोड करने के बाद आपको अपनी फोन गैलरी से किसी भी डाक्युमेंट की इमेज सिलेक्ट करनी है या आप ऐप  में मौजूद कैमरा को यूज कर किसी डाक्युमेंट की फोटो क्लिक भी कर सकते हैं. ये ऐप फोटो को कुछ ही सेकंड में स्कैन की हुई इमेज की तरह बना देता है. इसमें फोटो को अच्छा दिखाने के लिए आप वहां मौजूद फिल्टरों का इस्तेमाल कर सकते हैं. अपनी सुविधा के हिसाब से फोटो के साइज को क्रॉप और रोटेट भी कर सकते हैं. ऐप की मदद से आप अपनी स्केन की हुई फोटो पर अपना वॉटरमार्क भी दे सकते हैं. जिस तस्वीर को आप कन्वर्ट कर रहे हैं, यह उसे शेयर भी कर सकता है. ऐसा करते समय आपके पास दो ऑप्शन आएंगे- एक तो कि फाइल को jpeg में भेजें और दूसरा pdf में भेजें. अपनी जरुरत के मुताबिक जो मर्जी फॉर्मेट सिलेक्ट कर लें.

स्पीच नोट्स (Speech Notes) : इस ऐप के द्वारा स्टूडेंट्स अपने टीचर के या किसी जरूरी लेक्चर को टेक्स्ट मे बदल सकते हैं. आपको बस ऐप डाउनलोड करने के बाद ऐप में मौजूद माइक आयकन को टच करना है और आप रिकॉर्डिंग शुरू कर सकते हैं. रिकॉर्डिग शुरू होते ही आपका ये ऐप वॉयस को टेक्स्ट में बदल देगा. यही नहीं आप टेक्स्ट को एडिट भी कर सकते हैं और नोट्स को सेव कर आप इसे शेयर भी कर सकते हैं.

फोटो मैथ (Photo Math) : इस ऐप से आप गणित की किसी भी इक्युऐशन को बहुत आसानी से सुलझा सकते हैं. आपको बस ऐप की मदद से इक्युऐशन को स्कैन करना है. देखते ही देखते ही देखते आपकी इक्युऐशन का उत्तर आपकी फोन की स्क्रीन पर होग. वहां मौजूद steps के ऑप्शन पर क्लिक कर आप स्टैप-बाई-स्टैप सॉल्यूशन को भी देख सकते हैं. साथ ही अपने दोस्त को सॉल्यूशन शेयर भी कर सकते हैं.


हमने आपको काम के ऐप्स के बारे में बता दिया है. अब यह आपके ऊपर है कि इनमें से किसका उपयोग आप करना चाहेंगे. वैसे आप चाहें तो गूगल प्ले स्टोर से अपनी जरूरतानुसार अन्य ऐप भी चुन सकते हैं.

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Tarak Mehta
जन्मदिन विशेष: मधुबाला से शादी करने के लिए किशोर दा बन गए थे मुसलमान... जानिए ऐसी ही 10 दिलचस्प बातें
मशहूर कॉमेडी शो ‘तारक मेहता’ में नजर आने वाली एक्ट्रेस दयाबेन (दिशा वकानी) जल्द ही मां बनने वाली हैं. जी हां, एक्ट्रेस अपने पहले बच्चे को जन्म देने वाली हैं. कुछ दिनों पहले ऐसी भी खबर थी कि मेकर्स उन्हें रिप्लेस करने वाले हैं.

अपने दमदार एक्टिंग से शो में जान भर देने वाली एक्ट्रेस जल्द ही मैटरनिटी लीव लेने वाली हैं. लेकिन अब शो के प्रोड्यूसर इन सभी खबरों को गलत बताते हुए कहा कि हम ज्यादा से ज्यादा एपिसोड की शूटिंग कर रहे हैं.

खबरों की मानें तो क्लोजअप शॉट्स के लिए दिशा के घर में शूटिंग भी हो सकती है. ताकि उन्हें सेट पर आने की परेशानी ना हो.

बता दें कि ‘सब’ पर प्रसारित होने वाला शो ‘तारक मेहता का उल्टा चश्मा’ काफी पॉपुलर है. लोग इसके कंटेंट को काफी पसंद करते हैं.

DNA Data storage for the next frontier


How DNA Became The Next Frontier Of Data Storage
International Business Times: Technology


Humanity is producing data at an unimaginable rate, to the point that storage technologies can’t keep up. Every five years, the amount of data we’re producing increases 10-fold, including photos and videos. Not all of it needs to be stored, but manufacturers of data storage aren’t making hard drives and flash chips fast enough to hold what we do want to keep. Since we’re not going to stop taking pictures and recording movies, we need to develop new ways to save them.

Over millennia, nature has evolved an incredible information storage medium – DNA. It evolved to store genetic information, blueprints for building proteins, but DNA can be used for many more purposes than just that. DNA is also much denser than modern storage media: The data on hundreds of thousands of DVDs could fit inside a matchbox-size package of DNA. DNA is also much more durable – lasting thousands of years – than today’s hard drives, which may last years or decades. And while hard drive formats and connection standards become obsolete, DNA never will, at least so long as there’s life.

The idea of storing digital data in DNA is several decades old, but recent work from Harvard and the European Bioinformatics Institute showed that progress in modern DNA manipulation methods could make it both possible and practical today. Many research groups, including at the ETH Zurich, the University of Illinois at Urbana-Champaign and Columbia University are working on this problem. Our own group at the University of Washington and Microsoft holds the world record for the amount of data successfully stored in and retrieved from DNA – 200 megabytes.

Preparing bits to become atoms Traditional media like hard drives, thumb drives or DVDs store digital data by changing either the magnetic, electrical or optical properties of a material to store 0s and 1s.

To store data in DNA, the concept is the same, but the process is different. DNA molecules are long sequences of smaller molecules, called nucleotides – adenine, cytosine, thymine and guanine, usually designated as A, C, T and G. Rather than creating sequences of 0s and 1s, as in electronic media, DNA storage uses sequences of the nucleotides.

There are several ways to do this, but the general idea is to assign digital data patterns to DNA nucleotides. For instance, 00 could be equivalent to A, 01 to C, 10 to T and 11 to G. To store a picture, for example, we start with its encoding as a digital file, like a JPEG. That file is, in essence, a long string of 0s and 1s. Let’s say the first eight bits of the file are 01111000; we break them into pairs – 01 11 10 00 – which correspond to C-G-T-A. That’s the order in which we join the nucleotides to form a DNA strand.

Digital computer files can be quite large – even terabytes in size for large databases. But individual DNA strands have to be much shorter – holding only about 20 bytes each. That’s because the longer a DNA strand is, the harder it is to build chemically.

So we need to break the data into smaller chunks, and add to each an indicator of where in the sequence it falls. When it’s time to read the DNA-stored information, that indicator will ensure all the chunks of data stay in their proper order.

Now we have a plan for how to store the data. Next we have to actually do it.

Storing the data After determining what order the letters should go in, the DNA sequences are manufactured letter by letter with chemical reactions. These reactions are driven by equipment that takes in bottles of A’s, C’s, G’s and T’s and mixes them in a liquid solution with other chemicals to control the reactions that specify the order of the physical DNA strands.

This process brings us another benefit of DNA storage: backup copies. Rather than making one strand at a time, the chemical reactions make many identical strands at once, before going on to make many copies of the next strand in the series.

Once the DNA strands are created, we need to protect them against damage from humidity and light. So we dry them out and put them in a container that keeps them cold and blocks water and light.

But stored data are useful only if we can retrieve them later.

Reading the data back To read the data back out of storage, we use a sequencing machine exactly like those used for analysis of genomic DNA in cells. This identifies the molecules, generating a letter sequence per molecule, which we then decode into a binary sequence of 0s and 1s in order. This process can destroy the DNA as it is read – but that’s where those backup copies come into play: There are many copies of each sequence.

And if the backup copies get depleted, it is easy to make duplicate copies to refill the storage – just as nature copies DNA all the time.

At the moment, most DNA retrieval systems require reading all of the information stored in a particular container, even if we want only a small amount of it. This is like reading an entire hard drive’s worth of information just to find one email message. We have developed techniques – based on well-studied biochemistry methods – that let us identify and read only the specific pieces of information a user needs to retrieve from DNA storage.

Remaining challenges At present, DNA storage is experimental. Before it becomes commonplace, it needs to be completely automated, and the processes of both building DNA and reading it must be improved. They are both prone to error and relatively slow. For example, today’s DNA synthesis lets us write a few hundred bytes per second; a modern hard drive can write hundreds of millions of bytes per second. An average iPhone photo would take several hours to store in DNA, though it takes less than a second to save on the phone or transfer to a computer.

These are significant challenges, but we are optimistic because all the relevant technologies are improving rapidly. Further, DNA data storage doesn’t need the perfect accuracy that biology requires, so researchers are likely to find even cheaper and faster ways to store information in nature’s oldest data storage system.

Luis Ceze, Associate Professor of Computer Science and Engineering, University of Washington and Karin Strauss, Researcher in Computer Architecture, Microsoft Research; Affiliate Associate Professor of Computer Science and Engineering, University of Washington

This article was originally published on The Conversation.

The (first) flower on earth

This is what the first flower on Earth might have looked like
New Scientists

Three was the magic number for the very first flowering plant. The largest study into their early evolution has concluded that its flowers probably had petal-like tepals and pollen-bearing stamens arranged in layered whorls of three. It bore similarities with magnolias, buttercups and laurels – but was unlike any living flower.

The origin of flowering plants and their rapid conquest of the world’s habitats has been a puzzle for nearly a century and a half. In 1879, Charles Darwin described it as an “abominable mystery” that flowers had evolved so late in the history of life yet were still able to take over from the more ancient seed-bearing pines and cycads.

Today, flowering plants account for nine out of every 10 plants – meaning they far outnumber the once-dominant seed plants like conifers that emerged between 350 and 310 million years ago.

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Studying their evolutionary roots is tricky, though: the delicacy of flowers means they rarely become fossilised. The oldest so far discovered is the 130- million-year-old aquatic plant Montsechia vidalii unearthed in Spain in 2015. However it is thought that flowering plants first appeared much earlier than this, sometime between 250 and 140 million years ago.

Picking flower traits
To unravel what the very first flower was like, a 36-strong team led by Hervé Sauquet of the University of Paris-South, France, spent six years analysing the anatomical evidence of nearly every type of flowering plant to identify their most ancestral traits.

They calibrated their results with dates derived from molecular analyses and constructed evolutionary trees that modelled the earliest stages in flower evolution.

“We looked at the big bang of flowering plant evolution when they first evolved,” says Sauquet.

They discovered that the first flower probably had 11 or more tepals and stamens, generally grouped in threes and carried both male and female reproductive structures. It was arranged in a unique way unlike any living flower. It’s unclear how large the first flower was, but it may have been just 1 centimetre or less in diameter.

One surprise is how many petal-like tepals the first flower had compared with most living flowers. Reducing their number allowed later flowers to develop a dazzling array of specialised shapes and sizes and consequently diversify along with their animal pollinators into the enormous range of ecosystems  they occupy today. There are some 300,000 living flowering plants.

The findings mean that the living flowers identified as being most ancient, such as Amborella from New Caledonia, and water lilies, are actually quite evolved compared with their ancient ancestors.

Journal reference: Nature Communications

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