The recent descriptions of the crystal structure of the molybdenum-iron protein and the iron protein of Azotobacter vinelandii nitrogenase [ 11 and of Clostridium pasteurianum nitrogenase [2] have been exciting and frustrating, exciting because the structures have been sought for more than 30 years, and frustrating because the structures do not obviously reveal the active site, nor do they really imply a specific active site.This has not prevented speculation and calculation to determine how nitrogenase actually works [3, 41. Simple speculation is easier, but should always attempt to remain consistent with the great deal we do know about the process of biological nitrogen fixation. Calculation is more dangerous. In the past, theoreticians have paid relatively little attention to chemical facts, and relied upon their imagination. The results of the calculations may indeed indicate a preferred pathway among those considered. However, there is no guarantee that the pathways considered include the one that nitrogenase uses. We are limited by our imagination and our knowledge. Consequently, it behoves us, when considering a mechanism, to use all the data we can. This short review is designed to do just that.The structure of the metal clusters at the core of the molybdenum-iron protein in both A. vinelandii [l] and C. pasteurianum [2] are shown in Fig. 1. The smaller eight-iron system, which is believed to act as an electron-transfer agent to the ironmolybdenum cofactor/cluster (FeMoco), is not believed to be involved directly with binding and reducing dinitrogen. There are at least three genetically distinct kinds of nitrogenase [5] based on iron and molybdenum, iron and vanadium, and iron and no other evident metal. These three nitrogenases, with a common iron constituent, have belled the speculation that iron, and not molybdenum or vanadium, is at the active site of nitrogenase [6]. Currently, there is no definitive answer to this problem, but this has not curbed inventive minds.As an example, there have been at least three sets of calculations performed investigating the ways in which dinitrogen might bind to the seven-iron residue of the FeMoco. One 131 was a bit previous, in that the residue initially not identified, but labelled Y, was postulated to be N,. Now, the consensus appears to be that Y is actually sulfur [7]. Another two calculations discuss N, binding to iron clusters [4, 81.