Environment-Clean-Generations

Environment-Clean-Generations
THE DEFINITIVE BLOG FOR EVERYTHING YOU NEED TO KNOW ABOUT THE ENVIRONMENT YOU LIVE IN, WITH REFERENCE TO LIFE, EARTH AND COSMIC SPACE SCIENCES, PRESENTED BY ENVIRONMENTAL ENGINEER DORU INDREI, ENVIRONMENTAL QUALITY AND ENERGY SPACIALIST
"Life is not about what we know, but what we don't know, craving the unthinkable makes it so amazing, that is worth dying for." Doru Indrei
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Showing posts with label Seriously. Show all posts
Showing posts with label Seriously. Show all posts

Why Do Leaves Change Color? No, Seriously!



The secrets of why the leaves of trees change yellow or red in the autumn are slowly being revealed. Those eye-seducing hues, it appears, are a lot more than pretty. They're the result of trees doing their utmost to survive. They're the shades of evolutionary success. 

Let's start with the green leaf: We all learned in school that it's the result of the most abundant pigment in the leaf being the green chlorophyll. When the cool air and shorter days of autumn arrive, leaves change to red or yellow not because the leaves are dying, but because of a series of clever processes underway.



Not so surprisingly, yellow leaves undergo one sort of color changing process and red leaves another. As the chlorophyll is being turned off, most leaves turn yellow, which is just a color that's already in the leaves but is usually flooded by green the rest of the growing season. 


But over the last decade or so, researchers have discovered something very different goes on in red leaves. As their chlorophyll drops, they would also turn yellow if not for the sudden rapid production of a brand new red pigment call anthocyanin, which was not previously present in the leaves.

This surprising revelation has led to a surge of interest by scientists who are trying to explain why a leaf with only a week or so to live would bother producing an entirely new pigment.


One theory for explaining red leaves is that they are the result of 35 million years of trees battling insects looking for places to get a last meal and lay their eggs in the fall. Red leaves are harder for insects like aphids to see, for instance, so they tend to go for the yellow leaves.

Some evidence for this theory can be found in the differences of fall colors between North America and Europe. There are few native European trees that turn red in fall, but they are mostly yellow. In North America, however, there are ample red-turning trees, as well as yellow. 

The reason for this may be that in North America, as well as in East Asia, North-South running mountain ranges allowed forests to shift their ranges North and South with climate changes, carrying their insects -- and their long-standing battles -- along the way.

In Europe, however, the major mountain ranges run east-west. So as climate warms or cools, trees have nowhere to go and simply die out -- along with the insects that live off of them. So in Europe, the insect-tree battles have a much shorter history, and so less time to evolve strategies like anthocyanins to fend them off. 
This theory was put forward by Simcha Lev-Yadun of the Department of Science Education- Biology at the University of Haifa-Oranim and Jarmo Holopainen of the University of Kuopio in Finland, and published in the journal New Phytologist.


Another theory suggests that the variation of red anthocyanin in leaves of trees that live in the same area might have more to do with the richness or poverty of the soil in which a tree grows and so it reflects the lengths trees must go to hang onto the nutrients they have invested in their leaves.

In a preliminary study by a student in Charlotte, N.C., it was found that fall leaf colors and the soils under sweet gum and red maple trees show a significant nutrient difference that matches autumn tree color patterns. The richer lowland soils corresponded to more yellow leaves and poorer highland soils correlated to redder leaves.



"It's very clear that there's a correlation," said plant physiologist Bill Hoch of Montana State University in Bozeman. What's more, it matches what he has discovered about the function of that stunning red anthocyanin.

Experiments make a pretty strong case for anthocyanin serving as a protective pigment that helps trees in nutrient-poor or stressed places to maximize the nutrients they can draw from the leaves before they are dropped to the ground, Hoch told Discovery News in an October 2007 article.

"They pull as many of the nutrients back into the plants as possible," said Hoch.


The red pigment protects any remaining green, food-making chloroplasts in the leaves from damage. This is especially valuable for trees in nutrient-poor soils or stressful situations because this "photo-protection" allows the leaves to keep making sugars in their leaves longer.

This, in turn, is vital for pulling nutrients out of the leaves because the only way the nutrients can be extracted from leaf to trunk is by hitching a ride on the trunk-bound sugars.


The bottom line, Hoch explained, is that the longer photosynthesis can continue on an autumnal, coloring leaf, the more nutrients can be drawn out of it for re-use in the spring. So where every drop of nutrient counts the most -- like perhaps on some nutrient-poor hillsides of North Carolina -- red is the color of autumn.


by "environment clean generations"

Why The Sky Is Blue? No, Seriously



The answer is a little more complicated than you may think. It may have a lot to do with rocks, phosphorous and ancient algae, according to a new study.

For the first two billion years of Earth's history or so, the sky was probably orange. We're not sure whether that's really true -- no one's been able to hop in a time machine and go back and check -- but based on what we know about the chemistry of that time period, there's a good chance the atmosphere's primary component was methane (CH4), which would've cast a strange pall over our young planet.

These days, the atmosphere is mostly nitrogen and oxygen. Sunlight is made up of all the colors of the rainbow (as well as many wavelengths we can't see); as it jostles through air molecules, blue light is most efficiently reflected, so our eyes end up experiencing a beautiful azure shade.
How did it change from orange to blue? About 2.5 billion years ago, the newest fad in organisms was photosynthesis -- the ability to to turn sunlight, carbon dioxide (CO2) and water into sugar. Armed with the latest evolutionary accoutrement, ancient algae had it made -- an everlasting food source and all the world's oceans to expand into. 

Only one problem. Algae need more than sugar for a balanced diet; they need nutrients like phosphorous, too. Dominic Papineau of the Carnegie Institution for Science thinks they got it in a burst of erosion from 2.5 to 2 billion years ago, a period of time when Earth's atmosphere got its first big injection of oxygen.

The way Papineau sees it, the "Great Oxidation Event" lines up nicely with a rise in continental rifting and widespread glacial deposits. So it's possible that enhanced tectonic activity and a change in climate eroded large amounts of phosphorous-rich rocks, which washed into the ocean over a period of several hundred million years.

With plenty of phosphorous to munch, algae were off to the races, churning out oxygen that flooded the atmosphere, Papineau reasons in this press release. It's not unlike humans' prodigious use of fertilizers today, which can cause large algal blooms in rivers, lakes and even the Gulf of Mexico:

"Today, this is happening very fast and is caused by us," he says, "and the glut of organic matter actually consumes oxygen. But during the Proterozoic this occurred over timescales of hundreds of millions of years and progressively led to an oxygenated atmosphere."
The first episode only got us about 10 percent of the way toward present-day oxygen levels, though. It wasn't until about a billion years ago that the atmosphere got another hit of O2, bringing us to the air we breathe today. This period, from 1 billion to 540 million years ago, is known as the "Cambrian explosion" after the riot of diverse life found in the fossil record. 

In some ways, it's one of the most important moments in the history of life on Earth. Organisms went on a rampage of evolutionary innovation, giving rise to complex life forms the likes of which the planet had never seen before, and Papineau thinks phosphorous was behind it:
"This increased oxygen no doubt had major consequences for the evolution of complex life. It can be expected that modern changes will also strongly perturb evolution," (Papineau) adds. "However, new lineages of complex life-forms take millions to tens of millions of years to adapt. In the meantime, we may be facing significant extinctions from the quick changes we are causing."

by "environment clean generations"

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