Magnetic reconnection flares in the protoplanetary nebula and the possible origin of meteorite chondrules

A possible episodic heating mechanism that could account for chondrule formation is discussed. The mechanism involves the transient release of energy as a result of magnetic flares in the corona of the protosolar nebula. The possible magnetic behavior of the protosolar nebula is outlined, based on meteorite paleomagnetic evidence about the magnetic field of the protoplanetary nebula and observations of the behavior of magnetic fields. The thermal balance in the melting of a chondrule precursor dust ball is examined. Observational evidence supporting the proposed heating mechanism is presented.