Showing posts with label biol275. Show all posts
Showing posts with label biol275. Show all posts

Wednesday, December 3, 2008

The role mtDNA plays in the evolutionary differentiation of species

Bob Koons shares his reflections on a Biogeography class discussion from some weeks ago. I've been unable to upload many student submissions to this blog due to severe tendonitis which limited my computer use for some time, but I'm beginning to catch up and hope to have the remaining student submissions uploaded before the semester ends!



Neotropical diversification of montane populations have been studied mainly in the lowlands of geographical regions simply due to the fact that there is a much larger diversity of species inhabiting the lowlands compared to the highlands. Studies use multiple approaches of statistical methods to get their data to agree. Which test is the best one depends upon the question being asked?



Species can be traced back to their origins using mtDNA, which is directly passed down from the mother. A species that has genetic ties to an ancestor and all its descendant taxa is called monophyletic and a species that has an ancestral taxon and some, but not all, of its descendant taxa; an artificial taxon. (Lomolino et al 2006) Geography plays a role in how a species diversifies over time as was demonstrated by the Finch scenario. The finches migrated south from Mexico to the Northern Andes Mountains of South America. Some finches traversed the Andes and migrated south along the east side of the Andes. The geographic isolation separating the two groups allows for natural selection to run its course allowing for the distinct differences we see in the finches today.



So does this apply to humans also? Can human mtDNA show this geographical divergence differentiating our species? An article entitled, “Geographic origin of human mitochondrial DNA: Accommodating phylogenetic uncertainty and model comparison” by John Huelsenbeck and Nikita Imennov compare the two main theories of the origin of the humans, which are the “out of Africa” and the “regional continuity hypothesis. The “out of Africa” hypothesis relates that modern humans all came from a common ancestor in Africa. Humans spread from there to all parts of the globe, and subsequently wiping out other “homos” that were encountered. The “regional continuity hypothesis” says a single species of homo originated throughout the old world connected through gene flow, after any migration from Africa occurred. Statistics using mtDNA show that the out of Africa scenario is the most possible origin for modern humans. A Bayesian inference statistical analysis was used to accommodate phylogenetic uncertainty from all trees then comparing the probabilities. Bayesian statistics is defined as, “Of or pertaining to statistical methods that regard parameters of a population as random variables having known probability distributions.”In their article Huelsenbeck and Imennov 2002 state, “In this study, we point out how Bayesian inference can be used to accommodate phylogenetic uncertainty when comparing five different models for the origin of modern human mtDNA.” 200 sequences of mtDNA were analyzed, each sequence was 428 sites long, from the hypervariable region I (HVRI) of the mitochondrial region of modern humans and an out group sequence from Neanderthal mtDNA. They used 40 sequences from each geographical region of the globe in their analysis; Africa, Europe, Asia, Americas, and Australia were represented. As discussed in class, and in this paper, a statistical analysis can be modified in many ways. This study used a uniform prior on all possible trees, another way to analyze the data would be to perform a coalescence prior, or to chose another method reconstructing the ancestral geographic area of human mtDNA. Another way of statistical modifications could include a stochastic two-stage model or a coalescence process with different populations connected by variable levels of migration. Still other ways exist that can modify an analysis; the trees could be reconstructed using a molecular clock restraint and incorporated into a Bayesian or maximum likelihood framework. (Huelsenbeck and Imennov 2002) A DNA sequence from Neanderthals may give a clearer answer to the out of Africa hypothesis. MtDNA can be useful to determine human geographic origin after all. Whew! From this we can clearly see that data can and is modified in many different ways to suit a desired outcome.



References:

Huelsenbeck, J. and Imennov, N., 2002. Geographic origin of human mitochondrial DNA: Accommodating phylogenetic uncertainty and model comparison. In Systematic Biology Vol. 51, No 1 pp.155-165.

Lomolino, M.V et al. 2006. Biogeography. MA: Sinauer Associates.

Dictionary.com, Bayesian Statistics. Retrieved October 5,2008.


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Wednesday, October 1, 2008

Zotero: an open source alternative to Endnote

If you haven't tried the campus site-licensed Endnote software to manage your reference collection yet - (or perhaps because you have and didn't like it) and if you'd prefer an open-source alternative with some apparently nifty online features (esp. for firefox users), consider Kevin Zelnio's advice: Screw EndNote, Try Zotero. You can download it here.



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Sunday, September 7, 2008

Life, The Universe, and Everything Else...

ResearchBlogging.orgJennie Talbot shares her musings following the class discussion last week in Biogeography (Biol 275).

In class we discussed the idea that niches are places that supply a particular organism with all of the resources required for it to thrive. The discussion led to questions regarding how much the niche impacted the species and, in turn, how much the species impacted the niche. For example, a plant species may thrive on the side of a mountain because it is here that the plant can find soil with good nutrients, adequate sun light, and reasonable temperatures. However, as more and more plants colonize the side of the mountain, transpiration will occur at a higher rate, which will produce more moisture in the air and, ultimately cause more rain to fall. The plant’s root system will hold the nutrient-rich soil despite all of the rain. Animals may come and feed on the well-nourished plants and, in turn defecate onto the soil, adding more nutrients for the plants to use. As more and more plants grow in this favorable environment, it is likely that the side of the mountain will get more rain then it did before the plants migrated to this location. Likewise, the side of the mountain may have better soil because of the wildlife that eat the plants. In fact, the wildlife may migrate to this newly colonized region on the mountainside because of the resources available. Therefore, the cycle will continue with more rain, better soil nutrients, healthier plants, and new wildlife. In this way, the side of the mountain, which may at one point have been completely void of life, has become a bustling habitat for multiple species.



So then I have to ask the question, “Was earth created for life or did life mold the earth into what it is today?” Of course, people may say, “Yes, the earth was created for life.” Well, Harold C. Urey submits that the earliest atmosphere of earth was composed mostly of hydrogen, methane, and nitrogen with only trace amounts of other elements such as carbon and oxygen. Over time a bunch of chemical reactions occurred (if you want to know all of the reactions, read Urey’s paper) and the earth’s atmosphere changed from being predominantly hydrogen and methane based to being highly oxidized with a lot of free energy created from oxidation reactions. The available free energy made it possible for a few primitive organisms to thrive. From here on out, those small organisms began to colonize earth. Current literature suggests that heterotrophic cells evolved 3.5 billion years ago followed by autotrophic cells (somewhere around 2.7 billion years ago), eukaryotes (2 billion years ago) and then multicellular organisms (Kardong, 2005). Because of the newly formed organisms on the planet, compounds that the earth had not seen yet (like isotopes of sulfur) were made and the compounds that were available already could be molded into something that could be used by another organism (Urey, 1952; Kasting, 1993).


So what does all of that mean? It seems to me that when the earth was created, it was completely uninhabitable. Which may mean the earth was not created for life and it is because of life, that the earth is habitable now. When the earth first came to be, there were atmospheric elements that began to interact with one another. From this energy was released, organic molecules were formed and the genesis of life began. At this point in the story, organisms have done nothing to alter the earth. However, with the birth of the first autotrophic cells (and the use of photosynthesis), living organisms began to transform the earth into something that could sustain life. Since then life has molded the planet into what it is today. Of course, it is likely that life has not molded the entire planet (as in, I am not sure that living organisms have any impact on the core of the planet itself…but this is science, so you never know, something could be discovered ☺) and who knows about our impact on the entire solar system. Nevertheless, in terms of niches within our range of exploration on the surface of the earth, it seems that living organisms can have a drastic, sometimes detrimental, impact on their habitats. Image what the world would look like if there was no deforestation or animal poaching. Imagine if the mosquitoes that bite us incessantly were not provided with stagnant water supplies in the rims of old tires and so could not reproduce in new habitats and spread deadly diseases to the inhabitants of those places. What if plumes of dinoflagellates did not blanket the ocean and poison thousands of fish each year. What if asparagus seeds did not float on water? What if fungus did not decompose leaf litter on the forest floor? What would the world look like without millions of species changing the world into a place called home?


Okay, so the end of that paragraph was a little cheesy. But truly, without life shaping the planet what would the planet look like? From these thoughts, I believe, at least for now, that living organisms have morphed the earth into what we know today. Without life on this planet, the earth would look completely different.

Sources


Kardong, Kenneth V. 2007. An Introduction to Biological Evolution. 2nd ed. Boston: McGraw-Hill Companies, Inc., 49-54.


J. Kasting (1993). Earth's early atmosphere Science, 259 (5097), 920-926 DOI: 10.1126/science.11536547


Harold C. Urey (1952). On the Early Chemical History of the Earth and the Origin of Life Proceedings of the National Academy of Sciences, 38 (4), 351-363



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