A new study suggests that the Earth’s tectonic activity may have begun as many as 4.4 billion years ago. The evidence stems from tiny minerals called zircons found in rocks of the Jack Hills region of Western Australia. Zircons, or zirconium silicate (ZrSiO₄), are amazing minerals because of the fact that they are very widespread, and can exist in igneous, sedimentary, or metamorphic rocks.

By analyzing tiny mineral inclusions found inside seven of the zircon crystals found in Western Australia ( seven out of 400 found) scientists were able to determine that there was tectonic activity in the earliest eon of our planet, the Hadean. These inclusions allowed the scientist to determine the temperature and pressures at which the zircons formed. Six of the seven bits of zircon contained inclusions composed of the mineral muscovite (KAl₂(AlSi₃O₁₀)(OH)₂). The Silicon to Aluminum ratio in these muscovite inclusions suggest that the rocks formed at depths of about 25 km beneath the Earth’s surface. Because of the amount of Titanium atoms present in the zircons, the scientists were able to determine that temperature of crystallization was between 665 and 745 degrees Celsius. The seventh inclusion consisted of a mineral known as hornblende ( (Ca,Na)_2-3(Mg,Fe,Al)₃Si₆(Si,Al)₂O₂₂(OH)₂) ). After analyzing the hornblende inclusions, (using methods similar to the above methods), scientists were able to confirm the determined results of the muscovite. However, because this discovery is based only on seven samples, there is some healthy criticism.

These temperatures and pressures indicate that the temperature flux during the zircon crystallization was approximately 75 mW/m². This flux is slightly higher than what is observed on Earth today. Because the Earth was so much hotter during its first six hundred million years, a higher paleo-flux is expected. However, the calculated flux was also determined to be about 1/5 lower than the expected flux of the hadean eon. It is because of this abnormally lower than average flux of the hadean eon zircons, that it was determined that the plate tectonics had to have begun so early in Earth’s history.

On Earth today, fluxes much lower than average occur above subduction zones, where one plate subducts beneath another. It is hypothesized that these zircons were formed as the descending plate subducted, bringing liquid water with it, where it cooled the surrounding mantle enough for the zircons, and the inclusion minerals, to crystallize out of solution. Zircon contains uranium isotopes, which allowed the year of this crystallization to be calculated using radiometric dating techniques.

This could be an important discovery because it will help us understand the evolution of terrestrial planets. Plate tectonics play a very important role in recycling the gasses which make up our atmosphere, and therefore directly affect the ability of a planet to sustain life. With the right atmospheres, Venus and Mars could have been within the habitable zone of our solar system, however neither planet is believed to have developed plate tectonics.

Besides providing clues to the development of plate tectonics, the zircons also contain oxygen isotopes that suggest that water was also present on the Earth some 4.4 billion years ago. These Western Australian zircons are the oldest minerals on Earth, and have provided us with great insight into the dawning hours of our planet.

Astronomers using two different telescopes and two different systems have started learning about microquasars. They’re learning new things that can then hopefully be applied to full size quasars as well.

A quasar is an extremely powerful, luminous and distant active galactic nucleus. While there was initially some controversy over the nature of these objects, there is now a scientific consensus that a quasar is a compact region surrounding the central supermassive black hole of a galaxy. Quasars show a very high redshift, meaning they are located a great distance from us. Quasars are active because the central black hole is accreting a lot of material. Near the black hole, intense magnetic fields in the disk accelerate material into tight jets that flow in opposite directions away from the hole.

Microquasars is a two-body system consisting of a stellar mass size black hole and a star, usually a red giant. The giant star is feeding material to the black hole. Which, needless to say creates some interesting dynamics. Astronomers have been looking at two systems, Swift1753.3-0127 and GX339-4, with the European Southern Observatory’s Very Large Telescope and NASA’s Rossi X-ray Timing Explorer to study microquasars. Microquasars are not only closer but change more rapidly, so a process that may take a normal quasar a year to undergo might only take a microquasar a few minutes.

Astronomers had thought that the visible light emission coming form microquasars was coming form far out in the accretion disk and thus did not give much information about the main actions going on. However, they were wrong. They now know that the optical and x-ray emission are intrinsically linked, probably by the same immense magnetic fields that hurl material into near light speed jets.

The data shows that light output typically drops just before x-ray output undergoes a large spike. The rapid variations in the x-ray and optical emission must have a common origin. The cool thing about discovering such patterns that stand out amidst chaotic fluctuations of light is that they give us a new handle on understanding the underlying physics. The best candidate is the strong magnetic fields as the dominant process behind it all.

So again what we once thought was wrong, we learned something new, but realize how much we don’t know yet. This data is a new clue about very mysterious and not yet understood systems. We still don’t know exactly what’s going on in these dynamic systems, but we have one more piece of the puzzle.

For the first time carbon dioxide has been found in the atmosphere of a planet outside of our own solar system. This is an important discovery because carbon dioxide is one the chemicals we would expect to find on a planet that harbors life, the other chemicals include: oxygen, water, and methane. Water vapor, along with carbon monoxide has previously been detected in the planet’s atmosphere.

Unfortunately, the discovery of carbon dioxide on this planet cannot be correlated to life. This Jupiter sized planet, which is located 63 light years from Earth, is known as HD 189733b. It has an orbital period of about 2.2 days and has a scorching surface temperature of about 1117 K. The close proximity of the planet to its host star may be responsible for the formation of carbon dioxide in the planet’s atmosphere. As the planet orbits, relatively close to its sun, it receives a high dosage of ultraviolet radiation. This radiation may have stripped apart other chemicals in the planet’s atmosphere while creating new chemicals, such as carbon dioxide.

The carbon dioxide was detected by analyzing the infrared spectrum of the planet. Because HD 189733b lies so close to its host star, the combined spectrum of the star/planet system had to first be analyzed and recorded. Scientists then waited for the planet to disappear behind its host star, so that the suns individual spectrum could be recorded. To obtain the planets individual spectrum, the spectrum of the star was subtracted from the star/planet system.

French astronomers discovered HD 189733b, in the constellation Vulpecula, on Oct. 5, 2005 by observing the transit of the planet across its host star. Since its discovery, the planet has reached a number of milestones. It was the first extrasolar planet to be mapped, it was the first found to contain water vapor and methane (which probably react in the high temperatures to form the carbon monoxide), and now it is the first exosolar planet known to contain carbon dioxide.

This discovery confirms our ability to detect the chemical compositions of planets outside of our solar system. If, and hopefully when, an Earth-like is discovered, analyzing the spectral signatures will be more difficult due to the small sizes of terrestrial planets. As we continue to develop our techniques by recording the spectral signatures of Jupiter-like planets, and super Earths, there should be little doubt that we will be ready to analyze the atmosphere of an Earth or Mars sized planet when the discovery occurs, bringing us one step closer to eventually detecting life on another planet.

Scientists believe they have found the answer to a mystery about a thought to be nearby galaxy. The funny thing is this answer was found by rather serendipitously after finding out our current estimates for the distance of the galaxy were wrong.

The galaxy named NGC 1569 was a bit of a mystery. It is an irregular shaped dwarf galaxy, which isn’t in itself strange, but the galaxy was going through a burst of star formation with no discernable reason. The galaxy was forming stars much faster than any other galaxies in its nearby region. Well then we realized that the problem with that statement was not NGC 1569 itself but the galaxies we thought were nearby it.

Scientists recently pointed the Hubble Space telescope at NGC 1569 to scan for red giant stars. The astronomers were hoping to get an estimate of the galaxies age by looking for red giants, as red giants can be used as reliable standard candles for measuring distance since they all burn at the same known brightness. However, the astronomers were only able to see the brightest red giants, even using Hubble, the stars were too dim to be resolved. This fact lead astronomers to question the previous estimate for how far away the galaxy actually is. And now after looking at the data astronomers have realized the galaxy is actually about one and a half times farther away than previously thought, making it about 11 million light years away.

The problem was before this the galaxy had only been studied with ground based telescopes, which have much less resolving power than space based telescopes, which can make estimates less accurate. With this new information the galaxy’s star formation makes more sense. This distance puts the galaxy in the middle of a cluster of ten other galaxies. The gravitational interaction of the galaxies tugging on each other would be enough to explain the high rate of star formation we see in this galaxy.

So using Hubble we have answered yet another question, good ol’Hubble. However, this instance makes one wonder how many other numbers that we have for things like distance or mass etc might be inaccurate after only being studied by ground-based telescopes. How many things should we go back over with space-based telescopes to make sure? And how many mysteries or unexplainable phenomena might be answered by simply rechecking our data??