I. INTRODUCTION
Natural phenomena signals, such as in medicine, seismology, astrophysics, geophysics, acoustics and vibrations, despite of their growing diversity, remain essentially analog, weak in magnitude, superimposed to high common-mode voltages and usually corrupted by noise. They also share common features, such as frequency components in Hertz/sub-Hertz range. To process such stringent signals, their dc component has to be initially filtered out, which is challenging to accomplish on a fully integrated form due to very-large time constants involved.