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Tuesday, September 30, 2008

New Facility Uses Algae to Turn Coal Pollution Into Fuel

NASA Mars Lander Sees Falling Snow, Soil Data Suggest Liquid Past

Martian sunrise This sequence of nine images taken by NASA's Phoenix Mars Lander shows the sun rising on the morning of the lander's 101st Martian day after landing. Image credit: NASA/JPL-Caltech/University of Arizona/Texas A&M University

PASADENA, Calif. -- NASA's Phoenix Mars Lander has detected snow falling from Martian clouds. Spacecraft soil experiments also have provided evidence of past interaction between minerals and liquid water, processes that occur on Earth.

A laser instrument designed to gather knowledge of how the atmosphere and surface interact on Mars has detected snow from clouds about 4 kilometers (2.5 miles) above the spacecraft's landing site. Data show the snow vaporizing before reaching the ground.

"Nothing like this view has ever been seen on Mars," said Jim Whiteway, of York University, Toronto, lead scientist for the Canadian-supplied Meteorological Station on Phoenix. "We'll be looking for signs that the snow may even reach the ground."

Phoenix experiments also yielded clues pointing to calcium carbonate, the main composition of chalk, and particles that could be clay. Most carbonates and clays on Earth form only in the presence of liquid water.

"We are still collecting data and have lots of analysis ahead, but we are making good progress on the big questions we set out for ourselves," said Phoenix Principal Investigator Peter Smith of the University of Arizona, Tucson.

Since landing on May 25, Phoenix already has confirmed that a hard subsurface layer at its far-northern site contains water-ice. Determining whether that ice ever thaws would help answer whether the environment there has been favorable for life, a key aim of the mission.

The evidence for calcium carbonate in soil samples from trenches dug by the Phoenix robotic arm comes from two laboratory instruments called the Thermal and Evolved Gas Analyzer, or TEGA, and the wet chemistry laboratory of the Microscopy, Electrochemistry and Conductivity Analyzer, or MECA.

"We have found carbonate," said William Boynton of the University of Arizona, lead scientist for the TEGA. "This points toward episodes of interaction with water in the past."

The TEGA evidence for calcium carbonate came from a high-temperature release of carbon dioxide from soil samples. The temperature of the release matches a temperature known to decompose calcium carbonate and release carbon dioxide gas, which was identified by the instrument's mass spectrometer.

The MECA evidence came from a buffering effect characteristic of calcium carbonate assessed in wet chemistry analysis of the soil. The measured concentration of calcium was exactly what would be expected for a solution buffered by calcium carbonate.

Both TEGA, and the microscopy part of MECA, have turned up hints of a clay-like substance. "We are seeing smooth-surfaced, platy particles with the atomic-force microscope, not inconsistent with the appearance of clay particles," said Michael Hecht, MECA lead scientist at NASA's Jet Propulsion Laboratory in Pasadena, Calif.

The Phoenix mission, originally planned for three months on Mars, now is in its fifth month. However, it faces a decline in solar energy that is expected to curtail and then end the lander's activities before the end of the year. Before power ceases, the Phoenix team will attempt to activate a microphone on the lander to possibly capture sounds on Mars.

"For nearly three months after landing, the sun never went below the horizon at our landing site," said Barry Goldstein, JPL Phoenix project manager. "Now it is gone for more than four hours each night, and the output from our solar panels is dropping each week. Before the end of October, there won't be enough energy to keep using the robotic arm."

The Phoenix mission is led by Smith at the University of Arizona. Project management is the responsibility of JPL with development partnership by Lockheed Martin in Denver. International contributions come from the Canadian Space Agency; the University of Neuchatel, Switzerland; the universities of Copenhagen and Aarhus, Denmark; Max Planck Institute, Germany; and the Finnish Meteorological Institute.

More information about Phoenix is at http://www.nasa.gov/phoenix .
Media contacts: Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webster@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

Sara Hammond 520-626-1974
University of Arizona, Tucson
shammond@lpl.arizona.edu

Original here

Ancient yeast reborn in modern beer

Eric Bland
Discovery News
beer closeup

The beer has been made using a yeast that has a unique metabolism (Source: iStockphoto)

A tiny colony of yeast trapped inside a Lebanese weevil covered in ancient Burmese amber for up to 45 million years, has been brought back to life in barrels of beer.

Emeritus Professor Raul Cano of the California Polytechnic State University, originally extracted the yeast a decade ago, along with more than 2000 different kinds of microscopic creatures.

Today, Cano uses the reactivated yeast to brew barrels of pale ale and German wheat beer.

"You can always buy brewing yeast, and your product will be based on the brewmaster's recipes," says Cano. "Our yeast has a double angle: We have yeast no one else has and our own beer recipes."

The beer received good reviews at the Russian River Beer Festival and from other reviewers. The Oakland Tribune beer critic, William Brand, said the beer has "a weird spiciness at the finish," and The Washington Post said the beer was "smooth and spicy."

Part of that taste comes from the yeast's unique metabolism. "The ancient yeast is restricted to a narrow band of carbohydrates, unlike more modern yeasts, which can consume just about any kind of sugar," says Cano.

Eventually the yeast will likely evolve the ability to eat other sugars, which could change the taste of the beer. Cano plans to keep a batch of the original yeast to keep the beer true to form.

If this has a ring of deja vu, it could be because Cano's amber-drilling technique is the same one popularised in the movie Jurassic Park, where scientists extracted ancient dinosaur DNA from the bellies of blood-sucking insects trapped in fossilised tree sap.

Cano's original goal was to find ancient microscopic creatures that might have some kind of medical value, particularly pharmaceutical drugs.

Going to sleep

While that particular avenue of research didn't yield significant results, the larger question of how microscopic creatures survived for millions of years could help scientists understand certain diseases, says Professor Charles Greenblatt, a scientist at Hebrew University in Jerusalem who studies ancient bacteria.

"We've got cases of guys who contracted [tuberculosis] during World War II and lived with it for 60, 70 years," says Greenblatt. "Then suddenly they get another disease, the TB wakes up from its dormancy and kills them."

Inducing dormancy could be a new way to fight disease and infection, says Greenblatt.

Instead of outright killing infectious creatures, doctors could instead put them to sleep. The infection would still be present in the patient's body, but it wouldn't hurt the patient.

Neither Cano nor Greenblatt can say what the upper limit for hibernating yeast or bacteria is - it could be hundreds of million years.

But while other scientists work on that, Cano plans to spend his time tossing back a few cold ones, and hoping others will too.

"We think that people will drink one beer out of curiosity," says Cano. "But if the beer doesn't taste good, no one will drink a second."

Original here