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John Lindquist's Home Page – Part 2Part 1 is here. |
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More About the Job.Beginning bacteriology lab courses generally confine themselves to the relatively small universe of conveniently easy-to-grow representatives of the chemoorganotrophic bacteria. Much can be learned – and applied to other living things – from this microbial group which does happen to include a lot of important pathogens, food spoilage organisms, general contaminants, and participants in various aspects of biodegradation – basically the "in our face" organisms. As in our previous "Bacteriology 102" course, the new, partly-virtualized Microbiology 102 course encompasses a lot of good things to know about (including anaerobic respiration) and continues to venture beyond chemotrophy into the wonderful world of anoxygenic phototrophy. Indeed, we find that the purple non-sulfur photosynthetic bacteria are a refreshing change of pace and are actually quite easy to isolate, even from hailstones! So, of the five general ways that organisms can generate their energy, we delve into all but oxygenic phototrophy. Along the way we realize that testing and describing organisms regarding their use of any one (or more) of these five catabolic methods is certainly more instructive than getting bogged down with the old-school method (with a thioglycollate and glucose-containing solid medium) of determining "oxygen relationships" which can only be applied productively to the characterization of those aforementioned easy-to-grow chemoorganotrophs and is often a pain for students and instructors to interpret. In fact, it's a redundant and generally ill-taught test which is better used to demonstrate the special growth patterns of microaerophiles and the relative efficiencies of fermentation vs. aerobic respiration as shown for those named in this test system as "facultative anaerobes." Even though I think this test should have died out with the 20th Century or at least with the demolition of Fred Hall, I have a relatively objective treatment of the usual "oxygen relationship test" which explains its usefulness and limitations here. I miss the real good old days back in 5th grade science class when "oxygen relationships" were simply described as whether or not an organism had the capability (for whatever reason) of growing aerobically and/or anaerobically – with the simple use of the terms "aerobe," "anaerobe" and "facultative" [sic]. A beginning lab course (such as ours) should really be spending some time in the fascinating worlds of cyanobacteria and chemolithotrophs. That these organisms tend to be "inconvenient" to work with is no reason to ignore them. Think about where we would be without them. So why just pay lip service to microbial diversity? In the 21st Century we may discover presently unimaginable metabolic processes that energize and fabricate life forms on Mars and elsewhere, and putting more emphasis right now on lithotrophic organisms in general microbiology teaching labs would not be a bad idea. Such has always been highly relevant to microbiology. The late P. W. Wilson made the study of the nitrogen cycle (including nitrification – an important chemolithotrophic process in the soil) a significant part of his introductory micro lab when he was here through the early 1970s.
Certainly microbial consortia are a practical consideration for demonstration and discussion. In my explorations of sandy areas up north, I frequently come across classic examples of cryptobiotic soil – those places where mixtures of chemotrophic and phototrophic microorganisms turn the inorganic into organic and initiate substrates for higher forms of life. These organisms are Nature's Terraformers – important in the early stages of the process wherein sand develops into topsoil. They can appear as clumps of steel wool and as velvety pincushions, and cutting one open reveals a core of sand. Click on the two nearby photos which were taken while visiting the Apostle Islands where there are some restricted areas containing cryptobiotic soil that are marked off as delicate ecosystems. Microscopically one can readily see fungi and also filamentous and unicellular algae and cyanobacteria. I have yet to check out what bacteria may be present. Aside from these "soil lichens," iron bacteria are another mixed group of organisms that I have been treating superficially (so far) on the web. Regarding the webworks, I am still pumping out the not-so-interactive reference material in an attempt to upload what little I know about bacteriology besides what is in the 2006 lab manual cited below. The catabolism page (still on the first page of a Google search for "catabolism" but no longer no. 1) arose out of an attempt to summarize energy/electron/ATP generation in the Farm Microbiology Short Course (a bright spot in the school year – and certainly a place to expand on soil microbiology and lithotrophy) where lecture time is very short indeed. A "whiteboard" presentation developed during a recent lecture on the subject is shown here. It is always best to summarize the basic strategy of any biological process first. For catabolism, then, further details can come along as time and relevancy to the course permit and may include such things as specific intermediates and pathways, the internal electron transfers in fermentation pathways, what photoorganotrophy really amounts to, and the interesting variations of anaerobic respiration presented by methanogenesis and "anammox." (Anammox needs to be included in any discussion of the nitrogen cycle.) Another web effort is the beta-galactosidase page which is hidden away here. More bacteriological concepts whose practical applications and interpretations tend to follow basic patterns include quantitation, media, isolation, identification, and the cycles of elements. These things – as well as proper usage of terms – are gone over in the web pages expanded upon below and also in the 2006 manual. The enteric bacteria are especially suited as practical examples to use in the discussions regarding differential media formulation (see references 3 and 4 below) and genotypic identification, and that is where I tend to concentrate my interest concerning these organisms. When dealing with enterics in the teaching lab over the past several decades, useless memorization of genera and species and their characteristics and habitats have long ago given way to a more practical approach. A handout associated with our enteric experiment (which includes one of our classic "thought questions") is shown here.
One kind of writing course that should be required concerns something I entirely regret not getting the hang of decades ago, and that is taking lecture notes in real-time that are complete, organized, and understandable. Maybe I should have learned stenography in high school. The inability to generate a "things to do" list that is totally inspiring and adhered to has been another problem. Yet when it comes to writing in general – whether it be academic, travel-related, fiction or whatever – who cannot be inspired by the highly-talented likes of a Robert J. Sawyer or Timothy Hallinan? Charles Dickens' contemporary Ned Buntline just may be able to teach us a thing or two; one can imagine the kind of blog that might have come out of him. Getting back to topic, here is a generality that seems to hold up well: All dilution plating problems are basically the same problem but with different variables. The same sort of thing goes when one is interpreting the various pH-based differential media. The solutions to these things need not be made unnecessarily complicated, and each particular medium or dilution problem need not be dealt with from scratch as a special case, for crying out loud. Once we can see the overall framework behind things, perhaps we can find a way to summarize everything such that it can fit on one side of a 5 X 7 note card! No lab protocol is perfect in its content or organization, and there is always a need for improving such things. Students can look at a manual protocol for an upcoming experiment and come up with a clarified flow chart to get the lab done efficiently. Also, with a good command of basic microbiology, any thoughtful instructor or student can come up with some really creative ways of doing and finding out certain things, and it is encouragement of that sort of thing that is behind the thought exercise here. Speaking of creativity, check out the relevant blog entries here. Working with the teaching labs' culture collection over the several decades of my employment here has been quite educational. A few of our stock cultures are descendants of ATCC strains (many generations removed), but the majority of our cultures have been isolated by myself or students and have wound up being "archived" for one reason or another. My "Edwardsiella Isolation Project" introduced a number of enterics into our teaching labs including a strain of the very rare Edwardsiella tarda Biogroup 1 whose origin was a small, warm bay of Lake Superior which harbored a lot of seagull feces and dead fish. Our spectacular Photobacterium was isolated from store-bought shrimp. The strains of E. coli and K. pneumoniae that we use routinely were isolated from pitcher plants, and our Rhodomicrobium came from water trapped by a bromeliad; click here for more about these plant sources. Even though some of our cultures come from well-known, commercial sources, we cannot put any strain number on any of our cultures but our own. No stock culture operation can say that any particular strain has the same exact genotype and phenotype of the isolate or certified strain it may have been descended from – no matter how few generations have transpired. Lyophilization is our ultimate method of storing cultures for indefinite periods and is an ongoing process – when our machine can be MacGyvered to work reliably! We have experienced the loss of some cultures while in refrigerated storage; one lesson from this is never to store Heart Infusion Agar cultures of Edwardsiella tarda (Nutrient Agar being preferred for extended viability). Also, we have seen major characteristics of a few of our refrigerator-stored strains visibly shift during serial subculturing. Some examples follow:
So, what can be a thankless chore can also be a kind of education one cannot pick up from one's usual coursework or laboratory teaching duties. Relevant Publications and Websites.
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So that's the state of the art presently. Time to go outside and lighten up. |
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