Two odd balls

The marvelous line of discoveries made by the Kepler mission continued last week with the announcement (article) of two planets orbiting a hot B subdwarf — a star way past its prime. Both planetary candidates are smaller than the Earth and are on very short orbits which is already exciting on its own.

What makes them special, however, is their unusual history. The authors suggest that these are the remnants (cores) of larger planets that have been immersed inside the star as it expanded to become a Red Giant — the inevitable fate of our own planet. The two probably proceeded into spiraling ever deeper inside the envelope of the gigantic star, losing mass and possibly even driving the evolution of the host itself.

This discovery adds yet another example of the wide variety of environments extrasolar planets can be found in. More importantly, it show how…stubborn…and resourceful planets are in the game of survival. But of course, nothing less is to be expected of the carriers of this most fascinating and robust thing called life.

Pyruvate: a key molecule in metabolism

I was just reading about pyruvate to build my biochemistry literacy (the molecule is relevant to an NMR project I’m helping out on). Wikipedia describes pyruvate, which is the product of breaking down glucose, as a key intersection in several metabolic pathways, aerobic and anaerobic. Being at the heart of the chemistry of metabolism makes a molecule a candidate for being a very old player in biochemistry. Here’s how the Pyruvate article puts the molecule in the context of the origin of life:

Main article: iron-sulfur world theory

Current evolutionary theory on the origin of life posits that the first organisms were anaerobic because the atmosphere of prebiotic Earth was, in theory, almost barren of diatomic oxygen. As such, requisite biochemical materials must have preceded life. In vitro, iron sulfide at sufficient pressure and temperature catalyzes the formation of pyruvate. Thus, argues Günter Wächtershäuser, the mixing of iron-rich crust with hydrothermal vent fluid is suspected of providing the fertile basis for the formation of life.

Successful presence at the JHU Physics Fair

Our booth, which was in the main atrium of the Bloomberg Center for Physics and Astronomy on the Homewood campus, was home to a planet-detection simulator, ancient meteorites, and a model cell. We presented the science of astrobiology as “How to find a planet,” “How to build a planet,” and “How to build life.”

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