“…Because this dine appeared to have been stable for several years and the two inland sites had essentially the same proportions of cyanogenic plants, in spite of being topographically very different, Ellis et a!., (1977) sought those environmental factors common to the inland sites by which they differed from the cliff site. They determined that the distribution of molluscs known to graze the acyanogenic form preferentially (Jones, 1966, Crawford-Sidebotham, 1972, together with "exposure" to wind and salt spray from the sea, were the principal factors involved.…”