The concept of the "magnetic polarity time scale" refers to the record of the Earth's magnetic field reversals as captured over geological time in oceanic basalt formations. The term "chron" refers to a time period during which the Earth's magnetic field maintains a stable polarity. The present-day epoch's magnetic polarity is known by a specific name.
Let's evaluate the given options to identify the correct name for the current magnetic polarity epoch:
Based on the above explanations, the correct answer to the question is the Bruhnes chron, as it is the current magnetic polarity epoch. The Bruhnes chron is associated with a normal or 'normal' magnetic polarity, meaning the magnetic north pole is near the geographic north pole.