The structure of ferrocene was famously analysed by Woodward and Wilkinson in 1952[cite]10.1021/ja01128a527[/cite],[cite]10.1016/S0022-328X(00)88947-0[/cite], symmetrically straddled in history by Pauling (1951) and Watson and Crick (1953). Quite a trio of Nobel-prize winning molecular structural analyses, all based on a large dose of intuition. The structures of both proteins and DNA succumbed to models built from simple Lewis-type molecules with covalent (and hydrogen) bonds; ferrocene is intriguingly similar and yet different. Similar because