ICE AGE



How Global Warming May Cause the Next Ice Age...






While global warming is being officially ignored by the political arm of the Bush administration, and Al Gore's recent conference on the topic during one of the coldest days of recent years provided joke fodder for conservative talk show hosts, the citizens of Europe and the Pentagon are taking a new look at the greatest danger such climate change could produce for the northern hemisphere - a sudden shift into a new ice age. What they're finding is not at all comforting.
In quick summary, if enough cold, fresh water coming from the melting polar ice caps and the melting glaciers of Greenland flows into the northern Atlantic, it will shut down the Gulf Stream, which keeps Europe and northeastern North America warm. The worst-case scenario would be a full-blown return of the last ice age - in a period as short as 2 to 3 years from its onset - and the mid-case scenario would be a period like the "little ice age" of a few centuries ago that disrupted worldwide weather patterns leading to extremely harsh winters, droughts, worldwide desertification, crop failures, and wars around the world.
Here's how it works.
If you look at a globe, you'll see that the latitude of much of Europe and Scandinavia is the same as that of Alaska and permafrost-locked parts of northern Canada and central Siberia. Yet Europe has a climate more similar to that of the United States than northern Canada or Siberia. Why?
It turns out that our warmth is the result of ocean currents that bring warm surface water up from the equator into northern regions that would otherwise be so cold that even in summer they'd be covered with ice. The current of greatest concern is often referred to as "The Great Conveyor Belt," which includes what we call the Gulf Stream.
The Great Conveyor Belt, while shaped by the Coriolis effect of the Earth's rotation, is mostly driven by the greater force created by differences in water temperatures and salinity. The North Atlantic Ocean is saltier and colder than the Pacific, the result of it being so much smaller and locked into place by the Northern and Southern American Hemispheres on the west and Europe and Africa on the east.
As a result, the warm water of the Great Conveyor Belt evaporates out of the North Atlantic leaving behind saltier waters, and the cold continental winds off the northern parts of North America cool the waters. Salty, cool waters settle to the bottom of the sea, most at a point a few hundred kilometers south of the southern tip of Greenland, producing a whirlpool of falling water that's 5 to 10 miles across. While the whirlpool rarely breaks the surface, during certain times of year it does produce an indentation and current in the ocean that can tilt ships and be seen from space (and may be what we see on the maps of ancient mariners).
This falling column of cold, salt-laden water pours itself to the bottom of the Atlantic, where it forms an undersea river forty times larger than all the rivers on land combined, flowing south down to and around the southern tip of Africa, where it finally reaches the Pacific. Amazingly, the water is so deep and so dense (because of its cold and salinity) that it often doesn't surface in the Pacific for as much as a thousand years after it first sank in the North Atlantic off the coast of Greenland.
The out-flowing undersea river of cold, salty water makes the level of the Atlantic slightly lower than that of the Pacific, drawing in a strong surface current of warm, fresher water from the Pacific to replace the outflow of the undersea river. This warmer, fresher water slides up through the South Atlantic, loops around North America where it's known as the Gulf Stream, and ends up off the coast of Europe. By the time it arrives near Greenland, it's cooled off and evaporated enough water to become cold and salty and sink to the ocean floor, providing a continuous feed for that deep-sea river flowing to the Pacific.
These two flows - warm, fresher water in from the Pacific, which then grows salty and cools and sinks to form an exiting deep sea river - are known as the Great Conveyor Belt.
Amazingly, the Great Conveyor Belt is only thing between comfortable summers and a permanent ice age for Europe and the eastern coast of North America.
Much of this science was unknown as recently as twenty years ago. Then an international group of scientists went to Greenland and used newly developed drilling and sensing equipment to drill into some of the world's most ancient accessible glaciers. Their instruments were so sensitive that when they analyzed the ice core samples they brought up, they were able to look at individual years of snow. The results were shocking.
Prior to the last decades, it was thought that the periods between glaciations and warmer times in North America, Europe, and North Asia were gradual. We knew from the fossil record that the Great Ice Age period began a few million years ago, and during those years there were times where for hundreds or thousands of years North America, Europe, and Siberia were covered with thick sheets of ice year-round. In between these icy times, there were periods when the glaciers thawed, bare land was exposed, forests grew, and land animals (including early humans) moved into these northern regions.
Most scientists figured the transition time from icy to warm was gradual, lasting dozens to hundreds of years, and nobody was sure exactly what had caused it. (Variations in solar radiation were suspected, as were volcanic activity, along with early theories about the Great Conveyor Belt, which, until recently, was a poorly understood phenomenon.)
Looking at the ice cores, however, scientists were shocked to discover that the transitions from ice age-like weather to contemporary-type weather usually took only two or three years. Something was flipping the weather of the planet back and forth with a rapidity that was startling.
It turns out that the ice age versus temperate weather patterns weren't part of a smooth and linear process, like a dimmer slider for an overhead light bulb. They are part of a delicately balanced teeter-totter, which can exist in one state or the other, but transits through the middle stage almost overnight. They more resemble a light switch, which is off as you gradually and slowly lift it, until it hits a mid-point threshold or "breakover point" where suddenly the state is flipped from off to on and the light comes on.
It appears that small (less that .1 percent) variations in solar energy happen in roughly 1500-year cycles. This cycle, for example, is what brought us the "Little Ice Age" that started around the year 1400 and dramatically cooled North America and Europe (we're now in the warming phase, recovering from that). When the ice in the Arctic Ocean is frozen solid and locked up, and the glaciers on Greenland are relatively stable, this variation warms and cools the Earth in a very small way, but doesn't affect the operation of the Great Conveyor Belt that brings moderating warm water into the North Atlantic.
In millennia past, however, before the Arctic totally froze and locked up, and before some critical threshold amount of fresh water was locked up in the Greenland and other glaciers, these 1500-year variations in solar energy didn't just slightly warm up or cool down the weather for the landmasses bracketing the North Atlantic. They flipped on and off periods of total glaciation and periods of temperate weather.
And these changes came suddenly.
For early humans living in Europe 30,000 years ago - when the cave paintings in France were produced - the weather would be pretty much like it is today for well over a thousand years, giving people a chance to build culture to the point where they could produce art and reach across large territories.
And then a particularly hard winter would hit.
The spring would come late, and summer would never seem to really arrive, with the winter snows appearing as early as September. The next winter would be brutally cold, and the next spring didn't happen at all, with above-freezing temperatures only being reached for a few days during August and the snow never completely melting. After that, the summer never returned: for 1500 years the snow simply accumulated and accumulated, deeper and deeper, as the continent came to be covered with glaciers and humans either fled or died out. (Neanderthals, who dominated Europe until the end of these cycles, appear to have been better adapted to cold weather than Homo sapiens.)
What brought on this sudden "disappearance of summer" period was that the warm-water currents of the Great Conveyor Belt had shut down. Once the Gulf Stream was no longer flowing, it only took a year or three for the last of the residual heat held in the North Atlantic Ocean to dissipate into the air over Europe, and then there was no more warmth to moderate the northern latitudes. When the summer stopped in the north, the rains stopped around the equator: At the same time Europe was plunged into an Ice Age, the Middle East and Africa were ravaged by drought and wind-driven firestorms. .
If the Great Conveyor Belt, which includes the Gulf Stream, were to stop flowing today, the result would be sudden and dramatic. Winter would set in for the eastern half of North America and all of Europe and Siberia, and never go away. Within three years, those regions would become uninhabitable and nearly two billion humans would starve, freeze to death, or have to relocate. Civilization as we know it probably couldn't withstand the impact of such a crushing blow.
And, incredibly, the Great Conveyor Belt has hesitated a few times in the past decade. As William H. Calvin points out in one of the best books available on this topic ("A Brain For All Seasons: human evolution & abrupt climate change"): ".the abrupt cooling in the last warm period shows that a flip can occur in situations much like the present one. What could possibly halt the salt-conveyor belt that brings tropical heat so much farther north and limits the formation of ice sheets? Oceanographers are busy studying present-day failures of annual flushing, which give some perspective on the catastrophic failures of the past. "In the Labrador Sea, flushing failed during the 1970s, was strong again by 1990, and is now declining. In the Greenland Sea over the 1980s salt sinking declined by 80 percent. Obviously, local failures can occur without catastrophe - it's a question of how often and how widespread the failures are - but the present state of decline is not very reassuring."
Most scientists involved in research on this topic agree that the culprit is global warming, melting the icebergs on Greenland and the Arctic icepack and thus flushing cold, fresh water down into the Greenland Sea from the north. When a critical threshold is reached, the climate will suddenly switch to an ice age that could last minimally 700 or so years, and maximally over 100,000 years.
And when might that threshold be reached? Nobody knows - the action of the Great Conveyor Belt in defining ice ages was discovered only in the last decade. Preliminary computer models and scientists willing to speculate suggest the switch could flip as early as next year, or it may be generations from now. It may be wobbling right now, producing the extremes of weather we've seen in the past few years.
What's almost certain is that if nothing is done about global warming, it will happen sooner rather than later.



by Thom Hartmann



Increased Tropical Forest Growth Could Release Carbon from the Soil



A new study shows that as climate change enhances tree growth in tropical forests, the resulting increase in litterfall could stimulate soil micro-organisms leading to a release of stored soil carbon.



The research was led by scientists from the Centre for Ecology & Hydrology and the University of Cambridge, UK. The results are published online in the journal Nature Climate Change.



The researchers used results from a six-year experiment in a rainforest at the Smithsonian Tropical Research Institute in Panama, Central America, to study how increases in litterfall -- dead plant material such as leaves, bark and twigs which fall to the ground -- might affect carbon storage in the soil. Their results show that extra litterfall triggers an effect called 'priming' where fresh carbon from plant litter provides much-needed energy to micro-organisms, which then stimulates the decomposition of carbon stored in the soil.



Lead author Dr Emma Sayer from the UK's Centre for Ecology & Hydrology said, "Most estimates of the carbon sequestration capacity of tropical forests are based on measurements of tree growth. Our study demonstrates that interactions between plants and soil can have a massive impact on carbon cycling. Models of climate change must take these feedbacks into account to predict future atmospheric carbon dioxide levels."



The study concludes that a large proportion of the carbon sequestered by greater tree growth in tropical forests could be lost from the soil. The researchers estimate that a 30% increase in litterfall could release about 0.6 tonnes of carbon per hectare from lowland tropical forest soils each year. This amount of carbon is greater than estimates of the climate-induced increase in forest biomass carbon in Amazonia over recent decades. Given the vast land surface area covered by tropical forests and the large amount of carbon stored in the soil, this could affect the global carbon balance.



Tropical forests play an essential role in regulating the global carbon balance. Human activities have caused carbon dioxide levels to rise but it was thought that trees would respond to this by increasing their growth and taking up larger amounts of carbon. However, enhanced tree growth leads to more dead plant matter, especially leaf litter, returning to the forest floor and it is unclear what effect this has on the carbon cycle.



Dr Sayer added, "Soils are thought to be a long-term store for carbon but we have shown that these stores could be diminished if elevated carbon dioxide levels and nitrogen deposition boost plant growth."



Co-author Dr Edmund Tanner, from the University of Cambridge, said, "This priming effect essentially means that older, relatively stable soil carbon is being replaced by fresh carbon from dead plant matter, which is easily decomposed. We still don't know what consequences this will have for carbon cycling in the long term."


Read full story : http://www.sciencedaily.com/releases/2011/08/110814141445.htm

man-caused global warming a hoax






Plant scientist, I am concerned that Idaho and most states are planning to limit and reduce Carbon Dioxide (CO2) emissions. This is being done to supposedly reduce global warming. The states are adopting the 1997 Kyoto Climate Treaty which the U.S. Senate rejected 95-0 because it would destroy our economy while exempting developing nations like China which do not control pollution.

CO2 is not a pollutant and is not causing global warming. CO2 is necessary for life on the planet, as plants utilize CO2 to produce the oxygen we breathe and the food we eat! Global warming now and cooling of the 40’s to mid-seventies is caused by solar activity. We have an active sun now! The earth has been warming for 300 years with most of the increase prior to increased CO2 levels.

Also, 279 research project reports have shown that increasing CO2 increases crop production. Higher levels of CO2 is creating a lush environment for plants and animals and will improve the health (more oxygen), longevity and prosperity of all people.

Over 20,000 U.S. scientists have signed a petition opposing man-caused global warming and the benefits of increased CO2 levels, but the mass media totally ignore them. John Coleman, founder of The Weather Channel, stated that man-caused global warming is the biggest hoax ever perpetrated on mankind.

The biased United Nation’s panel and Al Gore are promoting a lie to scare us into a U.N. global government. The bottom line is that we need to produce more energy, not less. We have a 300 year U.S. supply of crude oil and unlimited nuclear power. There is no scientific reason to limit CO2 production because it is not causing global warming

Industrial pollution and global climate change




Ignorance is bliss, or so the saying goes; but what if that ignorance came with the price of destroying entire ecosystems? Although we've heard the phrase global warming in just about every news broadcast for the past decade, we still seem to be at a loss for what will happen if the delicate balance that gives us our temperate climates becomes off kilter.
A giant storm wouldn't form just out of the blue, flood part of the Earth, freeze a greater portion, sending lightning and wind storms that wipe out entire cities, and leave millions dead in just a matter of a few days like in the movie The Day After Tomorrow would it? We could survive another Ice Age that lasts hundreds, maybe even thousands of years with today's technology, couldn't we?
There is sufficient information to say that our planet is getting warmer. In the past 100 years, the Earth's temperature has risen around 1 Fahrenheit, which doesn't seem like much, but it truly has a larger impact than imagined. The Intergovernmental Panel on Climate Change is projecting a 3-10 rise in temperature by the year 2100. (National Geographic, 2008)
This temperature increase can dry up rivers and other water sources. In a severe drought condition, it is thought that an estimated 35% (around 1 million) of the Earth's species could disappear by the year 2050; some scientists say that that estimate is optimistic, at best. (Goodstein, February 2006) Glacier National Park in Montana has 27 glaciers; there were 150 in 1910. (National Geographic, 2008)
Science can only predict what is to come; however, the predictions scientists are forming come from the current trends they are observing. Most believe that global warming will lead to large-scale famine and drought. Rising temperatures will cause glaciers resting on top of mountains to melt completely. Many villages rely on the melting snow to fill their streams that water their crops and livestock. (Goodstein, February 2006)
Deserts will grow, destroying what was once farm land. A mini Ice Age could settle over Western Europe due to the shut-down of the conveyer belt that brings warm Caribbean waters north, giving places like Britain a milder climate. (National Geographic, 2008)
With glaciers melting not only from mountain tops, but also from the poles, ocean water levels will rise, changing the face of the Earth. Scientists are predicting a rise between 7 and 23 inches in sea level by the year 2100. A rise of just four inches would sink most of the South Seas islands and a large portion of South-East Asia. Around 100 million people live in these danger zones.
Florida and Louisiana are at risk of being flooded completely, destroying crops of fruits (such as oranges, strawberries, and melons) from Florida, and crops from Louisiana such as corn, cotton, and soy. Although neither Florida nor Louisiana are world producers, losing their contributions would still be felt, especially in the pocketbook.
Weather patterns will change and storms may become more severe. Hurricanes, tropical storms, droughts, heat-waves, and other natural disasters may become more intense and more frequent. Today's changing weather patterns supports this theory. Of the past twelve years, 11 of the hottest years have been recorded. (National Geographic, 2008)
Another dangerous possibility is looming: what happens if we can no longer control emissions finding their way into our atmosphere? It is called the Positive Feedback Effect, and it has the potential of making it impossible to control emissions, since we would be fighting Nature herself. Rising temperatures could release additional greenhouse gases into the atmosphere by freeing methane gas locked in permafrost and undersea deposits.
Carbon may also be released from sea ice with the melting of the glaciers. A rise in temperature will also cause an increase of water evaporation. Increased water evaporation will mean more cloud cover. More clouds floating about our atmosphere will act like a wool coat to our Earth, warming her more by not allowing heat to escape. (National Geographic, 2008)
Global Warming isn't going to just go away. This is a very real problem that humanity as a whole is facing. Even if we implemented clean air practices today, it would still take 'years' for these effects to show. Many greenhouse gases stay in our atmosphere years after they were released.
Technology isn't going to save us; our ability to adapt to a rapidly changing environment will be our saving grace. As a developed country (as well as the largest contributor to global warming), the United States should step up and take the lead in protecting our future. We need to educate the public about the repercussions of not acting upon this impending disaster. No, the world won't look like it did in the movie The Day After Tomorrow; however, I doubt we'll like the true results of global warming any more.
References:
Goodstein, E. (January 2006). Climate Change: What the World Needs Now IsPolitics. World Watch, 19(Issue 1), 25-27.
National Geographic News. Global Warming Fast Facts. Retrieved March 12, 2008, from
http://news.nationalgeographic.com/news/2004/12/1206 _041206_global_war
ming.html

Effects of Global Warming

The planet is warming, from North Pole to South Pole, and everywhere in between. Globally, the mercury is already up more than 1 degree Fahrenheit (0.8 degree Celsius), and even more in sensitive polar regions. And the effects of rising temperatures aren’t waiting for some far-flung future. They’re happening right now. Signs are appearing all over, and some of them are surprising. The heat is not only melting glaciers and sea ice, it’s also shifting precipitation patterns and setting animals on the move.

Some impacts from increasing temperatures are already happening.

•Ice is melting worldwide, especially at the Earth’s poles. This includes mountain glaciers, ice sheets covering West Antarctica and Greenland, and Arctic sea ice.
•Researcher Bill Fraser has tracked the decline of the Adélie penguins on Antarctica, where their numbers have fallen from 32,000 breeding pairs to 11,000 in 30 years.
•Sea level rise became faster over the last century.
•Some butterflies, foxes, and alpine plants have moved farther north or to higher, cooler areas.
•Precipitation (rain and snowfall) has increased across the globe, on average.
•Spruce bark beetles have boomed in Alaska thanks to 20 years of warm summers. The insects have chewed up 4 million acres of spruce trees.
.Other effects could happen later this century, if warming continues.

•Sea levels are expected to rise between 7 and 23 inches (18 and 59 centimeters) by the end of the century, and continued melting at the poles could add between 4 and 8 inches (10 to 20 centimeters).
•Hurricanes and other storms are likely to become stronger.
•Species that depend on one another may become out of sync. For example, plants could bloom earlier than their pollinating insects become active.
•Floods and droughts will become more common. Rainfall in Ethiopia, where droughts are already common, could decline by 10 percent over the next 50 years.
•Less fresh water will be available. If the Quelccaya ice cap in Peru continues to melt at its current rate, it will be gone by 2100, leaving thousands of people who rely on it for drinking water and electricity without a source of either.
•Some diseases will spread, such as malaria carried by mosquitoes.
•Ecosystems will change—some species will move farther north or become more successful; others won’t be able to move and could become extinct. Wildlife research scientist Martyn Obbard has found that since the mid-1980s, with less ice on which to live and fish for food, polar bears have gotten considerably skinnier. Polar bear biologist Ian Stirling has found a similar pattern in Hudson Bay. He fears that if sea ice disappears, the polar bears will as well.

Source :http://environment.nationalgeographic.com/environment/global-warming/gw-effects

US top court questions global warming lawsuit

(Reuters) - The Supreme Court on Tuesday questioned whether a global warming lawsuit against five big power companies can proceed, with several justices saying the U.S. Environmental Protection Agency, not federal judges, should deal with the issue.
The high court justices sounded a skeptical note during arguments when they asked whether complicated environmental issues, such as how much greenhouse gas pollution is allowable and how it should be curbed, should be left to federal judges.

The big environmental case stemmed from a 2004 lawsuit claiming that five coal-burning utilities have created a public nuisance by contributing to climate change. Its consequences, such as rising seas, reduced crop yields and destruction of some hardwood trees, would harm the states' citizens.

The lawsuit, now involving six states, seeks to have a federal judge in New York order the utilities to cut their carbon dioxide emissions.

Both liberal and conservative justices questioned whether the lawsuit can go forward.

Justice Ruth Bader Ginsburg, one of the court's liberals, took aim at the states' case, saying what they want is what the Environmental Protection Agency is trying to do with its proposed regulations of carbon emissions.

"How does a district judge decide what's reasonable and effective?" conservative Justice Samuel Alito asked rhetorically.

Another conservative, Chief Justice John Roberts, also asked whether a district court judge could conduct the cost-benefit analysis to determine what was reasonable to reduce global warming: "I think that's a pretty big burden to impose on a district court judge."

Liberal Justice Elena Kagan said the facts at issue in the lawsuit usually were determined by an agency such as the EPA, rather than the courts. "There is an administrative agency. There is a Clean Air Act," she said.


EPA'S ROLE

Lawyers for the power companies, including an Obama administration attorney representing the government-owned Tennessee Valley Authority, said the scope of the lawsuit was unprecedented in U.S. history, involving national and international issues outside the power of the courts.

"In the 222 years that the court has been sitting, there has never been a case with so many potential perpetrators and so many potential victims," said Neal Katyal, the administration's top courtroom lawyer.

The power companies -- American Electric Power Co Inc, Southern Co, Xcel Energy Inc and Cinergy Corp, which Duke Energy Corp acquired in 2006, along with TVA -- want the lawsuit dismissed.

The states -- California, Connecticut, Iowa, New York, Rhode Island and Vermont -- said their citizens have been harmed by global warming and urged the top court to allow their lawsuit to go forward.

It is the most sweeping climate change case to come before the high court since its landmark 2007 ruling that authorized the EPA to regulate greenhouse emissions if they endanger human health.

In their comments on Tuesday, the justices said Congress has given the federal environmental agency the authority to do just that.

But even though the EPA has found officially that greenhouse pollution poses a health hazard, it has not yet gone forward to impose regulations on emissions, and Republicans in Congress have sought to limit the agency's ability to do so.

Coal-fired power plants emit about twice as much carbon dioxide -- which warms the Earth by trapping solar heat in the atmosphere -- as natural gas-fired plants. Nuclear power plants emit virtually no greenhouse gases.

The five power utilities account for 10 percent of U.S. carbon dioxide emissions, said Barbara Underwood, who argued the case for the states.

A ruling is expected by the end of June.

(Editing by Bill Trott)

News Published by http://in.reuters.com on 20,april 2011

Life Sciences

A team of scientists has discovered that human-introduced, invasive species of plants can have positive ecological effects. Tomás Carlo, an assistant professor of biology at Penn State University, and Jason Gleditsch, a graduate student in the Department of Biology, have studied how invasive fruiting plants affect ecosystems and how those effects, contrary to prevailing ideas, sometimes can be beneficial to an ecological community. The team's research, which will be published in the journal Diversity and Distributions, is expected to affect the way environmental resource managers respond to ecosystem maintenance. "Among conservation biologists, ecologists, and managers, the default approach is to try to eliminate and root out non-native, invasive shrubs -- anything that seems to change an ecosystem," Carlo said. "The fundamental goal is to return a natural area to its original, pristine state, with the native species occupying the dominant position in the community. But the problem is that most native communities already have been changed beyond recognition by humans, and many native species are now rare." Carlo explained that his team wanted to test whether certain well-established, invasive fruiting species have negative or positive effects on bird and fruiting-plant communities. "We wondered: Are we sometimes doing more harm than good when we eradicate plants that, despite being introduced recently, have formed positive relationships with native animals?" To be considered invasive, a species of plant must have been introduced by humans, and it must be dominant numerically in the new environment. To test the impact of an invasive fruiting-plant species on native bird communities, Carlo and Gleditsch sectioned off an area of central Pennsylvania known as the Happy Valley region, where honeysuckle -- a non-native fruiting plant that is considered invasive -- grows in abundance. They then assessed the abundance of bird species and fruiting plants -- including honeysuckle -- within the area. After comparing their data with similar data from urban, agricultural, and forested areas, they determined that the abundance of honeysuckle predicted the numbers and diversity of birds within the region and even beyond the region. That is, the honeysuckle and bird communities had formed a relationship known as mutualism -- a term that describes how two or more species interact by benefiting mutually from each other's existence. "The abundance of fruit-eating birds in the Happy Valley region is linked to the abundance of honeysuckle," Carlo explained. "Honeysuckle comprises more than half of all the fruits available in the landscape, and it benefits birds by providing them with a source of food in the fall. Meanwhile, birds benefit honeysuckle by dispersing the plant's seeds across a wider geographical area, helping the species to occupy more and more territory in areas already affected by human activities." Carlo explained that returning this particular ecosystem to its honeysuckle-free state could harm many species of native birds that now seem to rely on honeysuckle as a major food source in the fall. The team also tested the honeysuckle's influence, not just on birds, but on other species of fruiting plants. First, they grew native fruiting plants known as American nightshades in pots in a greenhouse. When the fruits were ripe on each plant, they then placed them into both honeysuckle-dense areas and areas area without honeysuckle but dominated by other native and non-native fruiting species. "We chose the American nightshade because it is native and common in the Happy Valley region," Carlo said. "Also, it is easy to manipulate experimentally, and its fruits are eaten -- and thus dispersed -- by native birds." In the area in which honeysuckle grew in abundance, the rate of fruit-removal of Carlo's American nightshades was 30-percent higher than in the areas without honeysuckle. Carlo explained that in the honeysuckle-rich area, birds were present in abundance. These birds allowed the nightshades to receive more seed-dispersal services -- an ecological process known as facilitation. "The newly introduced plants piggybacked on the success of the honeysuckle, which is a common phenomenon because fruit-eating birds usually feed on a variety of fruit -- whatever happens to be available to them," Carlo explained. "The same birds that ate the honeysuckle also ate the American nightshade, dispersing the seeds of both plants. It's a win-win-win for all three: the birds, the honeysuckle, and the nightshades." Carlo also explained that in Pennsylvania there are now three to four times more fruit-eating birds such as robins and catbirds than there were just 30 years ago, especially in landscapes of high human presence. So scientists should conclude that, while some invasive, human-introduced plants are definitely problematic, others could serve to restore ecological balance by providing essential food resources to native migratory birds that populate areas affected by humans. "Invasive species could fill niches in degraded ecosystems and help restore native biodiversity in an inexpensive and self-organized way that requires little or no human intervention," Carlo said. In addition, Carlo explained, while eliminating an invasive species could result in harm to the newly formed balance of an ecosystem, large-scale attempts to remove species also could be a waste of time and tax dollars. He explained that when managers and agencies attempt to eradicate an invasive plant from a particular ecosystem, the species often ends up growing back anyway. "Nature is in a constant state of flux, always shifting and readjusting as new relationships form between species, and not all of these relationships are bad just because they are novel or created by humans," Carlo said. "We need to be more careful about shooting first and asking questions later -- assuming that introduced species are inherently harmful. We should be asking: Are we responding to real threats to nature or to our cultural perception and scientific bias?" Support for this research is provided by the Penn State Department of Biology and the Penn State Huck Institutes of the Life Sciences.- ready more at sciencedaily.com