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The following post was posted to sci.astro. It's a long post the basic argument of which is that a recently discovered microbe may provide a biological explanation for the Viking life experiment results.
Of the three Viking life experiments, no biological explanation had been offered for one of them the Gas Exchange Experiment. The results of this experiment showed oxygen to be evolved in the dark. For Earth microbes, oxygen had been known to be produced as a product of photosynthesis which requires light. However, the recently discovered microbes do have just this capability to evolve oxygen in the dark. I also suggest the experiments in the Atacama that sought to replicate the Labeled Release experiment results without biology may also have been detecting this species of microbe. Bob Clark From: "Robert Clark" <rgregoryclark> Newsgroups: sci.astro,alt.sci.planetary,sci.chem,sci.physics,s ci.bio.misc Subject: Possibilities for life on Mars - a surprising new microbe. Date: Sat, 22 Jan 2005 01:25:58 -0800 The famous Viking life experiments provided perplexing results in regard to life on Mars. They gave "positive" indications but they were different from the ones expected for Earth life. Because a separate experiment designed to detect organic molecules called the gas chromatograph-mass spectrometer (GCMS) was unable to detect any organics, the accepted conclusion in regard to the life experiments was that it was exotic chemistry not biology that caused the unusual reactions. However, the Principal Investigator for one of the experiments Dr. Gil Levin still believes his experiment called the Labeled Release Experiment did in fact detect life on Mars [1],[2],[3]. There have been several attempts to explain the biology experiment results by chemistry alone, usually by invoking oxidants: see the Science article [4] and the references contained therein (also see Levin's response following it). All such explanations have difficulties explaining all three experiments. Levin believes biology is at least as simple an explanation as the various combinations of oxidants required to explain all three experiments. The three biology experiments were the Labeled Release Experiment, the Pyrolytic Release Experiment, and the Gas Exchange Experiment. The NASA report [5] available online has a summary of these experiments. The book "The Search for Life on Mars" [6] provides a detailed review of the life experiments and the opinions of the scientists involved in the Viking mission. Levin believes his experimental results do mimic results he's seen with Earth life at low numbers of microbes (other scientists dispute this.) The Pyrolitic Release positive indications could also be explained by low numbers of microbes, on the order of a few thousand per gram. Note that normal Earth soils typically contain billions of microbes per gram. However, in regards to a life explanation the Gas Exchange Experiment offers a puzzle. It detects life by evolution of oxygen and carbon dioxide. Both of these were observed but again in small amounts. However, what is really curious about the GEx is that the oxygen evolution occurred in the dark. There were no known examples of microbes that evolved oxygen in the dark. The usual way microbes evolve oxygen is through photosynthesis which of course requires light. However, recently there has been discovered a microbe with just this capability to evolve oxygen in the dark [7],[8],[9],[10]: Presto! Bacteria Turn Toxic Wastes into Salt Component and Oxygen. "A research team has discovered a variety of bacteria that can break down certain toxic wastes into a component of ordinary table salt and other harmless chemicals. As an added bonus, the microbes can be made to produce oxygen as a by-product of the breakdown process, meaning this may be a new source of that essential, life-giving, breathable gas." ... "If these bacteria exist all over the place and they naturally break down toxic wastes such as perchlorate, why then is perchlorate pollution a problem anywhere? Well, in some cases, the microbes are breaking down these toxic wastes without any help from us. But the reason it's not happening at a faster pace all over is that the right carbon sources are often lacking, Achenbach and Coates explain. Carbon sources are like food for the bacteria. By adding acetate or other cheap carbon sources to soil or water targeted for cleanup, the researchers were able to kick the bacteria's natural toxic waste degrading abilities into high gear."[7] Newly Discovered Bacteria Can Generate Oxygen. "A diverse group of bugs, they all share a trait unique in the microbial world: Given the right kind of 'food,' they will crank out oxygen. "An organism that in the absence of air can produce oxygen got us to thinking about possible applications - - and there are many,' said microbial physiologist John D. Coates, who heads one of two SIUC research teams studying the bacteria. "Among others, they could supply air tanks for deep-sea diving or long-distance space travel, and because oxygen inhibits the growth of the agent that causes gas gangrene, they could be used to develop the first-ever field treatment for deep-wound injuries' - - all possibilities for which Coates has applied for patents."[8] BENZENE BUSTERS. "The newly discovered microbes, bacteria known as Dechloromonas strain RCB and Dechloromonas strain JJ, degrade benzene to carbon dioxide anaerobically—that is, without oxygen. (Most bacteria are aerobic, needing oxygen to live.) ... "When contamination occurs, such as an oil spill or chemical tank leak, aerobic bacteria start breaking down the pollutants—but they often get stopped in their tracks because they use up all the available oxygen. Coates’s lab previously had isolated several Dechloromonas species capable of breaking down chlorite (another pollutant) and giving off oxygen, a rare feat for microbes. That oxygen production can fuel aerobic bacteria to continue their cleanup work."[9] BREATH OF LIFE. Fated to Exhale "Despite their diversity, these organisms share the same highly specialized metabolism. They take in chlorate for respiration and use certain forms of organic carbon as food. They convert the chlorate to chlorite, another toxic compound, which they then break apart into oxygen and chloride. They use the oxygen molecules to help process the carbon, and they dump the chloride, a benign waste product. In essence, says Coates, the bacteria "breathe in chlorate and breathe out chloride.' "Chlorate-using bacteria are now being used to treat chlorate-contaminated wastes, such as rocket fuel wastes and wastes from pulp and paper mills. But the patent applications Coates has filed rest on another unusual characteristic of these microbes.' "About three years ago, researchers in the Netherlands working with the first known chlorate-using species discovered something interesting. If they withheld carbon and chlorate, but supplied chlorite, the bacteria still would break down the chlorite. But, since the bacteria had no carbon to process, they gave off both oxygen and chloride as byproducts." ... "In lab experiments at SIUC, it took less than 10 seconds for a population of chlorate-using bacteria to produce oxygen from chlorite."[10] This last fact about these new microbes is also relevant to the Viking experiments because part of the reason for doubting the biological origin of the positive life results was that the gases were evolved so quickly that they were thought to be the result of chemistry. A recent experiment on Earth may provide a means of testing the likelihood of these microbes for providing a match for the Viking life results [11]. The experiment attempted to replicate the Labeled Release experiment results using samples from the Atacama desert in Chile. The experimenters took samples from different parts of the desert with varying moisture contents. They found they were able to get a response from the experiment both in the (relatively) wetter areas as well in the driest areas. In the wetter areas they were able to find detectable microbes from DNA tests. However, in the driest areas they were not able to find detectable microbes even though the Labeled Release analogue gave a positive response. They concluded that the LRx positive response could not be due to life in these driest areas. However, curiosly they were able to detect organics in these samples using a device analogous to the Viking GCMS, though at levels below that which the Viking GCMS could have detected them. As with Mars, the scientists concluded oxidants must be the origin of the positive responses. However, they were not able to identify this chemical oxidant. This is curious. The oxidants proposed for Mars were all pretty simple inorganic compounds. That it couldn't be identified suggests a more complex compound, which may in fact be organic. But this would be in conflict with the *interpretation* of no organics on Mars. The other possibility that yet remains is that it could be microbes that caused these responses in the Atacama samples - perhaps the newly discovered oxygen-evolving microbes. One factor that suggests it could be is because of a curious fact in the geochemistry of Atacama: it is one of the only, if not the only, places known to have large natural deposits of perchlorate. Scientists Coates and Achenbach found the oxygen-evolving microbes to be ubiquitous wherever they looked, including the extremely dry desert of Antarctica [12],[13]. Since the microbes feed on perchlorates and Atacama has large deposits of perchlorate, they are very likely to be found there as well. Note though that the Labeled Release experiment detects evolved carbon dioxide, not oxygen. However, interestingly some strains of the microbe can convert benzene to carbon dioxide [9],[13] and benzene was indeed found in the samples from the driest areas of Atacama. But the Atacama experimenters did not find DNA in their samples from the driest areas. However, they used the method of PCR to detect DNA. This requires the use of a primer to generate recognizable DNA. If you use the wrong primer you won't generate detectable DNA [14]: Genetic Regulation of Perchlorate Reduction. "In order to track (per)chlorate-reducing bacteria in the environment, we have designed primer sets specific to the most predominant groups of perchlorate reducers in the environment. However, due to the extreme phylogenetic diversity of perchlorate-reducing bacteria, 16S ribosomal RNA primer sets can only be designed to detect a few specific genera of (per)chlorate-reducing bacteria in the environment (e.g. Dechloromonas and Dechlorosoma). A more inclusive approach for the detection of bacteria capable of (per)chlorate reduction is to develop a metabolic gene probe. We were recently the first to sequence and genetically characterize a novel gene involved in (per)chlorate reduction, the gene for chlorite dismutase."[14] Coates and Achenbach have developed a genetic probe for the presence of their oxygen-evolving bacteria [15],[16]. I recommend using these tests to determine if the microbe is present in the Atacama samples. Another method that might determine if the Atacama results were due to biology is an idea developed by Lin Chao. He notes that life has the ability to evolve when exposed to new environments. He suggests successively transferring the putative life forms to a new nutrient batch and observing whether or not they become more efficient at utilizing the nutrients, in essence a test to see if they undergo natural selection and Darwinian evolution [17],[18]. If microbes were present in the Martian soil, why did the GCMS not detect the required organic compounds? Recent experiments show that millions of microbes per gram could be contained in soil without the Viking GCMS being able to detect them: State-of-the-art instruments for detecting extraterrestrial life. "The possible presence of organic compounds on Mars is also uncertain. Using a pyrolysis procedure, in combination with a gas chromatograph/mass spectrometer (GCMS), Viking did not detect any organic compounds above a level of a few parts per billion in near surface samples at two different landing sites. However, it is now apparent that the Viking pyrolysis GCMS instruments would not have detected the presence of millions of bacterial cells in 1 g of soil. In addition, oxidation reactions involving organic compounds on the Martian surface would likely produce nonvolatile products that also would not have been detected by the Viking GCMS."[19] In addition to this, there may have been another factor operating: the GCMS may not have received samples of sufficient size to register a response. The GCMS as designed was supposed to give a signal indicating that full samples were delivered. This signal was never received [20],[21]: ON MARS. Ch. 11-5 SCIENCE ON MARS. "The first soil samples were acquired on sol 8, 28 July. Four samples were dug, with the first being deposited into the biology instrument distributor assembly, the next two into the GCMS processor, and the fourth into the funnel of the x-ray fluorescence spectrometer. All the commands were successfully executed, but there was no positive indication that the gas chromatograph-mass spectrometer processor had been properly filled. A second acquisition attempt still did not provide a "sample level detector `full' indication". The sampler system, having completed its programmed sequences in a normal manner, parked the boom as planned. On Earth, the lander performance specialists began to analyze the possible causes of the anomaly: (1) insufficient sample acquired in the collector head because the same sample collection site had also been used for the biology sample; (2) insufficient time allowed for the sample to pass from the funnel through the sample grinding section and then through the fine (300-micrometer) sieve into the metering cavity of the instrument; (3) grinder stirring spring not contacting the sieve; or (4) sample-level-detector circuit faulty. Since the "level-full" detector consisted of a very fine wire stretched across the cavity to which the sample material was delivered, it was also possible that it had broken when the soil was dropped into the funnel."[20] and The Search for Organic Substances and Inorganic Volatile Compounds in the Surface of Mars. "The are two positions to which any of the ovens can be moved in any sequence. The load position is directly under the sampling system, which delivers about 1-2 cm^3 of surface material that after having been ground is passed through a 0.3 mm sieve. A mechanical poker pushes the material through a funnel into the oven. This operation is timed in such a manner that the filling of the oven is complete with any of the terrestrial test soils (including finely ground basalt, commonly referred to as 'lunar nominal'). However, there is no sensor measuring the final level or completeness of the fulling operation. Thus one has to assume that the oven is filled to capacity, i.e., approximately 60 mm^3 of surface material is being analyzed."[21] So it is possible the GCMS only got a partial sample delivered. This obviously could effect the "no organics on Mars" conclusion from the GCMS experiment. In contrast, the biology experiments, which used the same delivery system as the GCMS, did get their sample "full" indications. It turns out that the GCMS used a much smaller sieving grid for its samples then the biology experiments. Then a possible explanation is that some grain sizes were larger than the grid for the GCMS which caused it too clog. An additional factor is the electrostatic charging that should take place in the dry thin atmosphere on Mars, which could have caused particles to adhere to the grid. In fact the Pathfinder mission found electrostatic adhesion of the magnetic dust on Mars to the Sojourner wheels. An experiment I would like to see performed would be to see if using Mars soil simulants in dry, low pressure, cold conditions as on Mars if only small amounts of sample are passed through because of electrostatic adhesion. Mars scientists in examining the GCMS results came to the conclusion that samples were delivered because water was detected in the experiment. However, it is impossible to know the size of the samples delivered. It could still be that the samples were so small that organics in the sample did not register. This is important because the amount of water assumed to be in the Martian soil is based on this measurement. However, two separate measurement techniques suggest this amount is too low, one from Earth-bound infrared spectra of Mars, the other from the gamma-ray spectrometer experiment on Mars Odyssey. The first comes from a paper [22] that shows there is a discrepancy between the water content of the Martian soil as determined by the GCMS and determined by other Earth-based and orbiter observations, perhaps by a factor of 1 to 2 orders of magnitude. The second is from the GRS measurements showing large amounts of water in the Martian surface [23]: Mars Water, Odd Surface Features Tied to Life. "Data gleaned by Odyssey has shown tremendous water ice deposits, Boynton said. "It really is changing the way we think of how the ice formed," Boynton told SPACE.com . The idea that water vapor eked down to depths deep enough and cold enough to condense out does not seem to account for the vast amounts of water ice detected, he said. "There's no telling how deep the ice might extend just below surface on Mars, Boynton said. It could be several hundreds of feet to well over a mile in depth. "All of a sudden you're starting to talk about a pretty significant amount of water," Boynton said. "It looks like the Viking 2 landing site was actually right on top of this ice. If its robot arm had dug just a little bit deeper they would have found it,' he said."[23] Boynton assumes here that the discrepancy was due to the Viking sample arm not going deep enough, but actually it may be because the Viking measurement was off. Bob Clark 1.)Proceedings of Spie, SPIE-The International Society for Optical Engineering, "Instruments, Methods, and Missions for the Investigation of Extraterrestrial Microorganisms." 29 July-1 August 1997, San Diego, California The Viking Labeled Release Experiment and Life on Mars Gilbert V. Levin Biospherics Incorporated http://mars.spherix.com/spie/spiehtml.htm 2.)Liquid water and life on Mars. Gilbert V. Levin and Ron L. Levin http://mars.spherix.com/spie2/spie98.htm 3.)Mars : the living planet. Barry DiGregorio; Gilbert V Levin; Patricia Ann Straat Publisher: Berkeley, Calif. : Frog, c1997. http://www.amazon.com/exec/obidos/ISBN=1883319587/ 4.)Evidence That the Reactivity of the Martian Soil Is Due to Superoxide Ions. A. S. Yen, S. S. Kim, M. H. Hecht, M. S. Frant, B. Murray Science, Vol 289, Issue 5486, 1909-1912 , 15 September 2000 http://www.sciencemag.org/cgi/conten.../289/5486/1909 5.)SP-4212 On Mars: Exploration of the Red Planet. 1958-1978. SCIENCE ON MARS. http://www.hq.nasa.gov/office/pao/Hi...12/ch11-5.html 6.)The search for life on Mars : evolution of an idea. Henry S. F. Cooper, Jr. New York : Holt, Rinehart and Winston, c1980. http://www.amazon.com/exec/obidos/ISBN=0030461669/ 7.)Presto! Bacteria Turn Toxic Wastes into Salt Component and Oxygen. http://www.microbe.org/news/perchlorate_microbe.asp 8.)Newly Discovered Bacteria Can Generate Oxygen. http://www.siu.edu/backissues/001004/ 9.)BENZENE BUSTERS http://www.siu.edu/~perspect/01_fall/benzene.html 10.)BREATH OF LIFE. http://www.siu.edu/worda/persp/f98/Breath.html 11.)Mars-Like Soils in the Atacama Desert, Chile, and the Dry Limit of Microbial Life. Science, Vol 302, Issue 5647, 1018-1021 , 7 November 2003 http://www.sciencemag.org/cgi/conten.../302/5647/1018 12.)Ubiquity and Diversity of Dissimilatory (Per)chlorate-Reducing Bacteria. Applied and Environmental Microbiology, December 1999, p. 5234-5241, Vol. 65, No. 12 http://aem.asm.org/cgi/content/full/65/12/5234 13.)Anaerobic benzene oxidation coupled to nitrate reduction in pure culture by two strains of Dechloromonas. NATURE |VOL 411 | 28 JUNE 2001 |1039-1043 http://www.nature.com/nature/journal...df/4111039.pdf 14.)Laurie A. Achenbach Research Interests. Genetic Regulation of Perchlorate Reduction. http://www.science.siu.edu/microbiology/achenbach/ 15.)Universal Immunoprobe for (Per)Chlorate-Reducing Bacteria. Applied and Environmental Microbiology, June 2002, p. 3108-3113, Vol. 68, No. 6 http://aem.asm.org/cgi/content/full/68/6/3108 16.)Sequencing and Transcriptional Analysis of the Chlorite Dismutase Gene of Dechloromonas agitata and Its Use as a Metabolic Probe. Applied and Environmental Microbiology, October 2002, p. 4820-4826, Vol. 68, No. 10 http://aem.asm.org/cgi/content/full/68/10/4820 17.)Defining Life by Bruce Moomaw Cameron Park - April 28, 2000 http://spacedaily.com/news/life-00w4.html 18.)The Meaning of Life. by Lin Chao BioScience, March 2000, Vol. 50, No. 3, p. 245-250. http://ibscore.dbs.umt.edu/biol223/B...eads/Chao2.pdf 19.)State-of-the-art instruments for detecting extraterrestrial life. Jeffrey L. Bada PNAS | January 30, 2001 | vol. 98 | no. 3 | 797-800 http://www.pnas.org/cgi/content/full/98/3/797 20.)ON MARS. Ch. 11-5 SCIENCE ON MARS http://www.hq.nasa.gov/office/pao/Hi...12/ch11-5.html 21.)The Search for Organic Substances and Inorganic Volatile Compounds in the Surface of Mars, Jour. Geophys. Res., vol. 82, no. 28, September 30, 1977, p. 4642. 22.)Water content of the Martian soil: Laboratory simulations of reflectance spectra, Authors: YEN, A. S.; MURRAY, B. C.; ROSSMAN, G. R., Journal: Journal of Geophysical Research, v. 103, No. E5, p. 11,125 (1998). http://www.gps.caltech.edu/~marssurf/waterice/soilh2o/ 23.)Mars Water, Odd Surface Features Tied to Life. By Leonard David Senior Space Writer 28 March 2003 http://space.com/scienceastronomy/ma...ks_030328.html |