  We present high spatial resolution observations of short lived transients,
ribbon and jets like events above a pore in Ca II H images where fine structure
like umbral dots, lightbridge and penumbral micro filaments are present in the
underlying photosphere. We found that current layers are formed at the edges of
convective fine structure due to the shear between their horizontal field and
the ambient vertical field. High vertical electric current density patches are
observed in the photosphere around these events which indicates the formation
of a current sheet at the reconnection site. In the framework of past studies,
low altitude reconnection could be the mechanism that produces such events. The
reconnection is caused by an opposite polarity field produced by the bending of
field lines by convective downflows at the edge of the pore fine structures.
