Archive for March, 2010

Light As A Neuronal Switch

March 29th, 2010

Dr. Christine Jurasinski
LabLearner Staff Scientist


How can you control brain activity?  It’s a question that has fascinated us for centuries.  Now, new research suggests that one way may lie with a strategy called optogenetics- the combination of optical and genetics techniques.

Neuroengineer Edward Boyden and his colleagues at MIT have recently discovered a way to use optogenetics to turn neurons within the brain on and off by simply exposing them to a certain wavelength of light.  Their research has far reaching implications for the treatment of conditions such as epilepsy, chronic pain and post-traumatic stress disorder as well as providing a new way for understanding and studying cognition, emotion and other functions of the brain.

Boyden and his collaborators discovered a protein found in a special type of bacteria called archeabacteria that inhabits the Dead Sea. Archeabacteria are a type of bacteria that tend to inhabit extreme environments like hot springs, arctic environment, sulfurous springs or the high salt concentration of the Dead Sea.

The protein they discovered acts as a pump in cells, moving protons out of the cells when active.  They also discovered that this protein, called the Arch protein, can be activated or turned on by light of yellow/green wavelength. Because protons carry a single positive charge, the movement of protons out of a cell changes the voltage within the cell.  The inside of the cell becomes more negative as compared to the outside of the cell.  As neurons work in part through electrical signals, changes in voltage are key to controlling their activity and their ability to fire and signal other neurons.

But, it’s what came next that illustrates that controlling the brain through light may not be as far off in the future as it seems.  These researchers engineered the neurons of mice to produce the Arch protein.  They then implanted a light source in the brain of the mice and found that when the Arch protein was activated in the neurons by the yellow/green light, it pumped protons outside the cells.  As a result the voltage inside the neurons dropped and stopped them from firing! In essence the researchers were able to use light to stop neurons within the brain from firing, silencing an area of the brain.

Once the light was turned off, the Arch protein turned off and “reset” itself.  Within seconds it was able to be activated by light again.  Thus, a combination of yellow/green light and the Arch protein, acted as an “electrical switch” for neurons controlling their active and inactive state.

In addition to the Arch protein, Boyden and his colleagues have found several other proton pumps that respond to other wavelengths of light including those in the red and blue ends of the spectrum.  What they hope is that by combining the different proteins and wavelengths of light different neurons and different areas of the brain could be controlled simultaneously.

How does this related to LabLearner students? Students in the LabLearner Program spend time in 4th and 6th grade studying the properties of light including how absorption and transmission of different wavelengths of light affect our perception of color and control biological processes such as photosynthesis.  This new research shows that understanding light and its properties may be just as important in uncovering the processes of cognition, emotion and in treating brain disorders and diseases.

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Thinking About Evolution? Think Lizards!

March 29th, 2010

Dr. Christine Jurasinski
LabLearner Staff Scientist


Mutation, allele, gene.  What do you think of when you hear these words?  Perhaps DNA comes to mind or disease or the workings of a cell.  But what about evolution?  For many, evolution brings to mind words like Darwin, finches, beaks, and fossils rather than mutations, alleles and genes.

But what about LabLearner students?  While they may begin their exploration of evolution, adaptation, mutations and natural selection by focusing on each of these topics in discrete CELLs such as Ecosystems and Adaptation,  Inheritance and Adaptation, and Genes and Proteins, they have the opportunity to combine all of this knowledge into a more complex and more scientifically “real” concept in the 7th grade CELL Adaptation: a CELL that sets them up for understanding some of the latest research into the molecular mechanisms for how species adapt and evolve.

This newest research comes out of the lab of Dr. Erica Rosenblum of the University of Idaho.  She and her colleagues have uncovered some intriguing information about the genetic process of evolution.  Their research is centered around three species of lizards. Each of these three species exist with dark skin in many areas around the world but have evolved a white skinned variation in the White Sands of New Mexico.  And what strikes the researchers as amazing is that in two of the species, it was accomplished by DIFFERENT MUTATIONS in the SAME GENE.  Even more interesting is that one mutation is DOMINANT while the other is RECESSIVE.

As fifth grade LabLearner students learn, many organisms have two copies of each gene.  One copy on one chromosome.  The other on the other chromosome.  The two copies of the gene are called alleles.  In one of the simplest examples of inheritance of traits, one allele is dominant the other is recessive.  Organisms with two dominant alleles will show the dominant version of a trait such as brown fur.  Organisms with one dominant and one recessive allele will also have the dominant brown fur trait.  However, organisms with two recessive alleles will have the recessive trait of white fur.

What Dr. Rosenblum discovered was that in one species of lizard, the white skin was the result of a dominant allele but in the other species of lizard, the white skin was the result of a recessive allele.  In both cases, the lizards evolved from having brown skin, but it was through different methods of inheritance.

How did this happen?  The answer involves selection pressure and mutations.  About 5000 to 7000 years ago, evaporating lakes in that area of New Mexico left behind huge deposits of gypsum which eroded away leaving an entirely white area of desert in what had once been a brown area.  Lizards which had been living there were brown skinned, which served as excellent camouflage from aerial predators.  However, as the terrain began to change, brown skin against and increasingly white background no longer served to camouflage the lizards, making them easy prey.

What scientists believe happened is that a mutation, a change in the DNA in the gene that controls the color of pigment in the lizards’ skin occurred.  This mutation may have occurred before but would not have likely been retained in the lizard population because white skinned lizards in a brown desert would have been an easy target for predators.  However, a mutation that occurred when the sands were white would have produced white skinned lizards that blended in with their surroundings.  These lizards would have been more likely than the brown skinned lizards to survive to produce offspring.  These offspring would have the mutated gene for producing white skin.  Thus, more and more lizards with allele for white skin would be born because the white sands now “selected for” this allele.

In one species of lizard, the mutation was dominant meaning the trait produced by the gene required only one copy of the gene in order for the skin to be white. The gene on only one chromosome had to be present. In the other species of the lizard, the mutation was recessive.  In other words, in order for the skin to be white, both copies of the mutated gene (one on each chromosome) had to be present.

For 7th grade LabLearner students, this real life example with the lizards epitomizes the concepts they have learned in the Adaptation and Genes and Proteins CELLs.  Evolution and natural selection occur because of changes in DNA.  Changes in DNA can result in differences in proteins and thus traits produced in an organism.  These types of changes can be seen by looking at the frequency of alleles for a trait.  If one trait is selected over another than the allele which produces that trait will appear more frequently in the population.  This is what Dr. Rosenblum and her colleagues would expect to see when comparing the alleles for skin color in lizards in the White Sands area to those same species of lizards in other areas of the world with a brown habitat.

For LabLearner students, the next question would be:

Which species of lizard would you expect to evolve faster, the ones with the dominant or recessive allele?

Based on what they know about modes of inheritance, those 7th grades and even 5th graders should predict—lizards with the dominant allele.  It’s what Dr. Rosenblum predicts and what she and her colleagues will continue to explore.

From her research and those of so many others we see that evolution and our study of it continues. What makes it different from Darwin’s time is that we now have the molecular tools to better understand how and why.

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Uncovering the Principles Behind the Chilean Earthquake and Tsunamis

March 1st, 2010


Dr. Christine Jurasinski
LabLearner Staff Scientist

On Saturday February 27th, the world was once again reminded of the awesome forces that are at work on our planet as an earthquake awakened Chileans in the early morning. The earthquake, which was centered just off the coast of Chile, measured an 8.8 on the Richter scale and generated enough force to generate tsunamis across the Pacific Ocean. The quake came only a day after a 7.0 earthquake in Ryukyu, Japan and a month and a half after the 7.0 earthquake that devastated Haiti.

What is happening here? Are we experiencing more earthquakes than in previous periods of history? While the answer is likely “No, we just are a more populated and therefore a more aware, more affected and more technologically savvy planet than in the past.” these are questions that scientists are actively researching. Their research takes them into the fields not only of geology, but also physics, fields that LabLearner students explore as they investigate principles in CELLs such as Forms of Energy, Earth’s Forces, Potential and Kinetic Energy, and Sound Waves and Pressure and in GAP Units such as Earth’s Changing Surface, The Changing Earth, and Geologic Time.

The earthquake that struck Chile occurred along the boundary that separates two tectonic plates: the Nazca Plate and the South American Plate.

As LabLearner students learn in the The Changing Earth GAP, this is a type of convergent boundary known as a subduction zone. In this particular boundary the Nazca plate moves below or beneath the South American Plate at a rate of 8.9 cm per year.

As this occurs, there are places in which the plates encounter resistance and get stuck. Tension builds between the plates until it becomes so great that the plates “rupture.” To understand rupture, think of a safety pin with the needle of the pin tucked safely under the protective casing. When the needle is depressed and moved out of the area of the casing, it springs open. There is a recoil associated with the release of the needle. This is similar to what happened on Saturday. The two plates were stuck and the tension was so great that the crust on the South American plate suddenly “sprung” above the Nazca plate. As a result, the Earth’s crust was lifted and then settled. This type of movement is called elastic rebound and results, as you can imagine, in the displacement of the Earth’s surface.

However, what seems relatively mild in description produces devastating results. Much of the damage in an earthquake is due to this elastic rebound. However, seismic waves, which are generated as the rupture occurs, also contribute to the devastation. Seismic waves are essentially sound waves that originate from the earth as the rupture is occurring. As the rupture occurs, the waves move the particles of earth in different directions. P waves are seismic longitudinal waves that alternately compress and expand particles of the solid and liquid portion of the Earth through which they move. LabLearner students studying the Sound Waves and Pressure CELL should be familiar with these types of waves as longitudinal waves are responsible for the generation of sound in solids, liquids and gases. In addition to P waves, the rupture causes another type of deep wave within the Earth’s surface called S waves and two types of waves on the surface of the Earth. It is the surface waves that cause additional horizontal and vertical movement of the Earth’s crust and much of the damage from an earthquake.

But as illustrated by Saturday’s event in Chile, the damage caused by the earthquake itself may not be the only concern. Often earthquakes can set off tsunamis- huge masses of moving water that when coming ashore produce their own destruction to both coast and inland areas. Tsunamis occur when there is a significant enough displacement of water to generate waves that have incredibly long wavelengths. They can be caused by earthquakes such as the one in Chile, by volcanic eruptions, and by landslides. Much of what is understood about tsunamis is still evolving.

One of the most devastating tsunamis occurred on December 26, 2004 off the coast of Sumatra and much of what we understand and how we predict tsunamis has come from that event. Luckily the tsunamis that resulted from Chilean earthquake on February 27th were nowhere near the same power. So, how were the tsunamis this past weekend generated?

Again, imagine the events that happened between the two converging plates. The build up of tension resulted in the plates that were “stuck” to suddenly move. In doing this, the South American plate was vaulted upward momentarily and then came back down. What then happened was the column of water above the plate was also pushed upward and then pulled back down by gravity. The result was a wave with a crest and trough that then spread outward like a ripple in a pond creating multiple waves extending from the epicenter of the quake. The energy that drove those waves came from the potential energy of the water as it was lifted. As gravity acted on the uplifted water, the gravitational potential energy was transferred into the kinetic energy of a moving wave. The higher the lift, the greater the potential energy and the greater the kinetic energy of the wave, a concept that LabLearner students explore in the Forms of Energy and Kinetic and Potential Energy CELLs.

What makes tsunami waves different from other types of ocean waves are their potentially crippling power. This power stems in part from their incredibly long wavelengths. As students learn in the Sound Waves and Pressure CELL, the wavelength is the distance between the crest or trough of one wave to the crest or trough of another. The ocean waves generated by wind that we are used to seeing have wavelengths of about 150 m. Tsunami waves are longitudinal waves that have wavelengths of 100 km. This means that normal ocean waves occur with a wave passing approximately every 10 seconds where as the time between successive waves in a tsunami can be more on the order of one every hour. In addition, tsunami waves move at incredible speeds such as 700 km/hr, which means they can travel huge distances across an ocean without losing much energy.

But one of the most intriguing things about tsunamis is the relationship between the height of the wave, its wavelength and the depth of the water. Tsunami waves generated in deep water tend to have relatively small amplitudes (heights) and long wavelengths. This is because the mass and energy of the wave is spread over a large and deep column of water. Thus, when these waves are in the open ocean they are only a few centimeters high and not easily detected by ships or cameras. As a result, tsunami waves are considered shallow water waves. As the tsunami wave moves closer to shore, the rising land of the continental slope or shore decrease the depth of water. Because of the Law of Conservation of Energy, the wavelength of the wave decreases and the height or amplitude of the wave increases. Although the wave slows from 700 km/hr (500 mph) to 50 km/hr (30 mph) as a result of friction with the land and as a result of a decrease in water depth, the incredible energy of the wave is “compacted” into a series of waves closer together and with much greater heights. Waves that impact the shore can be up to 9 meters (30 ft) in height. Thus, these waves can contain an enormous amount of energy and may move water inland for miles with great force. In addition, tsunami waves often do not break like normal ocean waves and dissipate energy. Rather, they move in like tides as great walls of water.

The tsunamis of December 26, 2004 were such waves. Luckily, the tsunamis of February 2010 were not. Tsunamis did reach Hawaii, Japan, the Philippines and the west coast of the United States. However, the amplitude of the waves as the reached shore ranged from several centimeters to approximately 1.8 meters (6 feet). Why these tsunamis differed from those that occurred in Sumatra will be heavily investigated for months to come.

However, what is becoming clear is that at this time in our species history, we can benefit from engaging our students’ interest in the forces that drive and govern our planet. Enhancing their understanding of the geology, physics, chemistry and biology of our planet can ultimately lead to better predictive models, warning systems, preparedness and even solutions in our planet’s future.

Find out more about both earthquakes and tsunamis by investigating the links below.

Tsunamis

http://walrus.wr.usgs.gov/tsunami/basics.html
http://www.ess.washington.edu/tsunami/index.html
http://www.pbs.org/wgbh/nova/tsunami/anatomy.html
http://www.tsunami.noaa.gov/
http://www.tsunami.noaa.gov/tsunami_story.html
http://www.pbs.org/wnet/savageearth/tsunami/index.html
http://faculty.gvsu.edu/videticp/waves.htm

Earthquakes

http://www.pbs.org/wnet/savageearth/index.html
http://www.seismo.unr.edu/ftp/pub/louie/class/100/seismic-waves.html
http://www.geo.mtu.edu/UPSeis/waves.html
http://pubs.usgs.gov/gip/dynamic/dynamic.html

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