What happens during a brain tsunamis?
The brain looks like a complex tapestry of neurons that communicate with each other using both a chemical and an electrical language. Each neuron responds to a balanced cocktail of chemical and electrical signals coming from neighbouring neurons. During spreading depolarization, this “cocktail” is disrupted, and the neurons become less able to function properly. It's comparable to how a tsunami can disrupt the normal functioning of the regions it hits.
Spreading depolarizations have a very low frequency below 0.1 Hz, meaning that they spread slowly. The frequency is significantly lower compared to gamma waves (typical of information processing, 30 Hz), beta waves (problem solving, 14-30 Hz), alpha waves (wakeful relaxation, 8-13 Hz), theta waves (light sleep, 4-8 Hz) and delta waves (deep sleep, 0.5-4 Hz). Research on spreading depolarizations is still ongoing, and its precise functions and implications are not yet fully understood.
How can brain tsunamis be recorded?
Glass microelectrodes, also called pipettes, have long been a fundamental tool in the field of electrophysiology. However, they are limited to measure brain electrical signals in one or a few points. To cover a larger area of the brain, Graphene Flagship researchers have developed flexible graphene field-effect transistors (FETs) and depth neural probes. They have used graphene depth neural probes to study the brain activity of awake rodents suffering from epilepsy. They tested the long-term functionality of these devices by implanting them in rats for 10 weeks. During this time, they were able to record patterns of brain activity seen in certain types of epilepsy and the associated slow brain waves (infraslow oscillations).
Read the original article on Graphene Flagship.
