[Hat Tip: Genomicron]
Yesterday's molecule was the type II reaction center from the photosynthetic purple bacterium Rhodobacter spaeroides. 
Your task for today is to identify the molecules with the question marks and explain (briefly) what's going on. Your task for today is to identify the molecules with the question marks and explain (briefly) what's going on. [Hat Tip: Jennifer Smith who found the original video, made for a Tommy Douglas tribute at the 2006 NDP Convention. Does this mean that Jack Bauer is a commie?
1. On the other hand, after 40-odd years I've accumulated a long list of things NOT to get her.
Razib Khan of Gene Expression has a list [States which do well educationally, blame Canada!]. 
There's always been a healthy debate about the role of an undergraduate education. Some view it as primarily a way of preparing for a job after graduation. At most universities we have undergraduate programs that do just that—engineering, and management studies are prime examples.Leshner said the goal of undergraduate education should be to give students a "fundamental knowledge of what science is, and what it is not, along with some key concepts." He also cautioned the conference participants not to fall into the trap of shifting the goal toward developing a scientific workforce, but, rather, remaining concerned with science for all undergraduates.I agree with Leshner. We should not fall into the trap of turning a university education into a job training program.
I know it's unfair to jump on one sentence, but after that point, all I could think about, is that the man must be completely clueless and out of touch with the reality of both the needs of students and the life science industry. Statements that imply that workforce doesn't matter and that biology educators should avoid "falling into the trap" also imply that biology is only for those wealthy students that won't need to find jobs after college.This seems way over the top to me. Of course a good biology education will expose students to lab skills and practical aspects of biology. That's not being questioned.
I have heard this from other college faculty before. Apparently you shouldn't consider a college education, and certainly, not an education in life science to be some kind of ticket to employment. SCIENCE (all of you fall down on your hands and knees, okay?) is only for those with independent means or those who plan to go to medical school.
I mean, it must be nice to just go to school and not be concerned about learning any sort of marketable skill. Unfortunately, while Leshner compliments college biology teachers for ignoring notions about job preparation, students are the ones who will pay the price. Even those who go on to graduate school, eventually have to learn bench skills.
The technique you are referring to is partition chromatography. The sample is spotted at one end of the immobile phase and a liquid mobile phase is allowed to adsorb along the phase, often in an enclosed container, which is an necessity if the mobile phase is a mixture of volatile liquid. Because different molecules have varying affinities for the solid and mobile phases (their partition coefficient) they are carried along the direction of the flow of the mobile phase at different rates giving their Rf value. The immobile phase can be paper, thin layers of different compounds like silica gel, or ion exchange resins. It is also used in Gas Liquid and Gas Solid chromatography as well where the mobile phase is a gas.The Nobel Laureates are Martin and Synge for inventing partition chromatography. The winner is Maria Altshuler of the University of Toronto. Congratulations Maria, you beat out a dozen others who had the right answer!
Today's "molecule" isn't a molecule. I'm looking for the technique that's illustrated by the example shown here. Describe the technique and identify the Nobel Laureates who discovered it.The image is taken from this website on paper chromatography.
J. William Schopf is a paleontologist at the University of California, Los Angeles (USA). He became famous in the 1990s for his studies of the Apec chert—ancient rocks in the northern part of Western Australia near the town of Marble Bar. Parts of these rocks have been reliably dated to 3.465 billion years ago. 
Eleven taxa (including eight heretofore undescribed species) of cellularly preserved filamentous microbes, among the oldest fossils known, have been discovered in a bedded chert unit of the Early Archean Apex Basalt of northwestern Western Australia. This prokaryotic assemblage establishes that trichomic cyanobacterium-like microorganisms were extant and morphologically diverse at least as early as approximately 3465 million years ago and suggests that oxygen-producing photoautotrophy may have already evolved by this early stage in biotic history.The data were immediately challenged. There were two problems, First, many paleonotologists questioned whether the "fossils" were really fossils. They suggested that the structures could easily be inorganic in nature and not remnants of living organisms. Secondly, the presence of cyanobacteria—among the most complex bacteria—is inconsistent with molecular data. Even though the early tree of life is complicated, the available evidence indicates that cyanobacteria arose late in the evolution of bacterial taxa. It's very unlikely that the earliest forms of life could be cyanobacteria, or even photosynthetic bacteria.
Over the years, the challengers became more and more emboldened. In 2002 Martin Brasier published a re-analysis of Schopf's original fossils and noticed that the published images were not as complete as they could be. In the figure shown here, Brasier et al. (2002) compare Schopf's original images ("b" and "c") with a larger view of the same material. The textbooks say that oxygen-producing microorganisms evolved some 3.5 billion years ago. But as that claim and its author come under attack, the history of life on Earth may have to be rewritten...A similar piece in Science helps drive the point home (Kerr, 2002).
Supporters and critics of Schopf alike describe him as a driven and tenacious character — nicknamed 'Bull' Schopf by some — whose energy and enthusiasm has done much to raise the profile of micropalaeontology, and to draw funding into the field. "He has a driving ambition to be in the limelight, and he doesn't like to admit he's wrong," says one former colleague. But these traits have led Schopf into conflict with his collaborators on at least one previous occasion.
The search for fossils in rocks formed before the Cambrian explosion of life 540 million years ago "has been plagued by misinterpretation and questionable results," leading paleontologist William Schopf of the University of California, Los Angeles (UCLA), once noted. Now Schopf's own claim for the oldest known fossils--fossils that have entered textbooks as the oldest ever found--is under attack as a misinterpretation of intriguingly shaped but purely lifeless minerals.The latest paper by Pinti et al. (2009) extends earlier observations of the Apex chert that re-interpret it as a hydrothermal vent. Temperatures reached 250° during formation of the vent and the alternation between molten and cooler forms of material was not conducive to life. Furthermore, deposits of iron oxides and clay minerals could be mistaken for microfossils .
A paper in this week's issue of Nature argues that the microscopic squiggles in a 3.5-billion-year-old Australian chert are not fossilized bacteria, as Schopf claimed in a 1993 Science paper (30 April 1993, p. 640), but the curiously formed dregs of ancient hot-spring chemistry. "There's a continuum [of putative microfossils] from the almost plausible to the completely ridiculous," says lead author Martin Brasier, a micropaleontologist at the University of Oxford, U.K. "Our explanation is that they are all abiogenic artifacts."
If true, the analysis calls into question the fossil record of life's first billion years. It would also raise doubts about the judgment of Schopf, the man chosen by NASA to set the standard for distinguishing signs of life from nonlife at the press conference unveiling martian meteorite ALH84001 (Science, 16 August 1996, p. 864). But Schopf says that such speculation is unwarranted. "I would beg to differ" with Brasier's interpretation, he says. "They're certainly good fossils."
This persuasive discovery seems an almost inevitable, yet highly problematic, consequence to the increasing scientific doubts about the original claim. We may well ask what exactly was the material originally analysed and reported? What was the apatite grain with supposed graphite inclusions that figured on the covers of learned and popular journals soon after the discovery? These questions must surely be answered and, if necessary, lessons learned for the more effective checking and duplication of spectacular scientific claims from the outset.There's another, potentially more serious, problem with using isotope ratios as evidence of early life. Gérard et al. (2009) have recently documented the presence of modern bacteria in drillcore samples of rocks that are 2.7 billion years old. They detected trace amounts of ribosomal RNA that were sufficient to identify more that ten diverse species of bacteria living in these subsurface formations.
To my regret, the ancient Greenland rocks have not yet produced any compelling evidence for the existence of life by 3.8 billion years ago. The reader is reminded that another debate on early life is currently in progress on 3.5-billion-year-old rocks in Western Australia, where chains of cell-like structures, long identified as genuine fossils10, have recently been downgraded by some workers11 to the status of artefacts produced by entirely non-biological processes. To have a chance of success, it seems that the search for remnants of earliest life must be carried out on sedimentary rocks that are as old, unmetamorphosed, unmetasomatized and undeformed as possible. That remains easier said than done. For the time being, the many claims for life in the first 2.0–2.5 billion years of Earth's history are once again being vigorously debated: true consensus for life's existence seems to be reached only with the bacterial fossils of the 1.9-billion-year-old Gunflint Formation of Ontario12.
Our results strongly suggest that contemporary bacteria inhabit what are generally considered exceptionally well-preserved subsurface Archaean fossil stromatolites of the Hamersley Basin, Western Australia. They are possibly in very low numbers, their distribution confined to microfractures where water may circulate (perhaps only intermittently), and their metabolic activities might be extremely low. However, upon geological timescales spanning 2.7 Gy, even such low cell numbers must have contributed significantly to the pool of biogenic signatures associated to these rocks, including microfossils, biological isotopic fractionation and lipid biomarkers. Although our results do not necessarily invalidate previous analyses, they cautiously question the interpretation of ancient biomarkers or other life traces associated to old rocks, even pristine, as syngenetic biogenic remains when bulk analyses are carried out.What does all this tell us about early life? It tells us that the evidence for life before 3 billion years ago is being challenged in the scientific literature. You can no longer assume that life existed that early in the history of Earth. It may have, but it would be irresponsible to put such a claim in the textbooks without a note of caution.
Brasier, M.D., Green, O.R., Jephcoat, A.P., Kleppe, A.K., Van Kranendonk, M.J., Lindsay, J.F., Steele, A., and Grassineau, N.V. (2002) Questioning the evidence for Earth's oldest fossils. Nature 416::76-81. [PubMed]
Dalton, R. (2002) Microfossils: Squaring up over ancient life. Nature 417:782-784. [doi:10.1038/417782a]
Fedo, C.M., Whitehouse, M.J. and Kamber, B.S. (2006) Geological constraints on detecting the earliest life on Earth: a perspective from the Early Archaean (older than 3.7 Gyr) of southwest Greenland. Phil. Trans. R. Soc. B 361:851-867. [doi: 10.1098/rstb.2006.1836]
Gérard, E., Moreira, D., Philippot, P., Van Kranendonk, M.J., and López-García, P. (2009) Modern Subsurface Bacteria in Pristine 2.7 Ga-Old Fossil Stromatolite Drillcore Samples from the Fortescue Group, Western Australia. PLoS ONE 4: e5298. [doi:10.1371/journal.pone.0005298]
Pinti, F.L., Mineau, R., and Clement, V. (2009) Hydrothermal alteration and microfossil artefacts of the 3,465-million-year-old Apex chert. Nature Geoscience 2:640-643. [doi: 10.1038/ngeo601]
Schopf, J.W. (1993) Microfossils of the Early Archean Apex chert: new evidence of the antiquity of life. Science 260:640-646. [PubMed]
Gérard, E., Moreira, D., Philippot, P., Van Kranendonk, M., & López-García, P. (2009). Modern Subsurface Bacteria in Pristine 2.7 Ga-Old Fossil Stromatolite Drillcore Samples from the Fortescue Group, Western Australia PLoS ONE, 4 (4) DOI: 10.1371/journal.pone.0005298
Pinti, D., Mineau, R., & Clement, V. (2009). Hydrothermal alteration and microfossil artefacts of the 3,465-million-year-old Apex chert Nature Geoscience, 2 (9), 640-643 DOI: 10.1038/ngeo601
One thing men are really good at is making mistakes—just ask any woman. When it comes to mutations we are ten times better than women at ensuring the evolution of the species. Alleles can be fixed by natural selection or by random genetic drift. If most are fixed by natural selection (adaptation) then you'll learn very little about the overall mutation rate aside from a minimum estimate. That's because you don't know the fitness of every allele and how fast it became fixed in the population and you don't know how many mutations were detrimental or neutral, and what happened to them.1. This isn't strictly correct but you can ignore the small regions where recombination is possible.
Britten, R.J. (2002) Divergence between samples of chimpanzee and human DNA sequences is 5%, counting indels. Proc. Nat. Acad. Sci. USA 99:13633-13635. [doi: 10.1073/pnas.172510699]
Nachman, M.W. (2004) Haldane and the first estimates of the human mutation rate. J Genet. 83:231-233. [PubMed]
Xue, Y., Wang, Q., Long, Q., Ng, B.L., Swerdlow, H., Burton, J., Skuce, C., Taylor, R., Abdellah, Z., Zhao, Y.; Asan, Macarthur, D.G., Quail, M.A., Carter, N.P., Yang, H., Tyler-Smith, C. (2009) Human Y Chromosome Base-Substitution Mutation Rate Measured by Direct Sequencing in a Deep-Rooting Pedigree. Curr Biol. Aug 26. [Epub ahead of print] [doi: 10.1016/j.cub.2009.07.032]
Xue, Y., Wang, Q., Long, Q., Ng, B., Swerdlow, H., Burton, J., Skuce, C., Taylor, R., Abdellah, Z., & Zhao, Y. (2009). Human Y Chromosome Base-Substitution Mutation Rate Measured by Direct Sequencing in a Deep-Rooting Pedigree Current Biology DOI: 10.1016/j.cub.2009.07.032
1. Thank-you.
Today's "molecule" isn't a molecule. I'm looking for the technique that's illustrated by the example shown here. Describe the technique and identify the Nobel Laureates who discovered it.The image is taken from this website on paper chromatography.
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