N A T U R E C O N S E R V A T I O N IN T H E C H U R C H Y A R D F . J. BINGLEY
Introduction: In many parishes the churchyard constitutes the last relic of ancient pasture, one of the richest grassland habitats in this country, and one which is disappearing fast under the pressures of modern farming methods. When grass is laid down by a farmer it usually contains two or three grass species, and perhaps clover. After a few years other species of plant slowly invade so that in maybe seven or eight years there could be about a dozen species in the turf. As time passes the number slowly increases and this is why ancient pasture, untouched perhaps for centuries, is so rieh in species. However, its food value for stock is low and that is why so much has been ploughed up by farmers and resown with highly nutritive cultivated strains of grasses. There are 10,500 medieval churches in England; if we include the post-reformation churches there could be as much as 20,000 acres of ancient pasture in our churchyards—a very valuable resource which should be safeguarded for posterity. Shape, size and siting: Churchyards are usually oblong in shape—a round one may indicate a very early site, potentially of great interest. Almost all those measured to date are between one and two acres in area. There are exceptions; Long Melford and Leiston in Suffolk are over two acres. They occupy well-drained sites, often two to three feet above the level of the surrounding land. This may possibly be attributed to the thousands of burials in the churchyard over the centuries; there have probably been twenty or thirty times as many burials in the average village churchyard as the present number of tombstones would lead one to expect. The churchyard may be bounded on one or two sides by a ditch, which may itself be of historical and/or archaeological interest, and may provide an additional habitat favoured by water-loving plants and animals. Soil: The soil of the churchyard varies with that of the district but tends to be neutral to alkaline; bone fragments will add calcium and phosphate and this will be supplemented by limestone and mortar rubble from the decay of tombstones and building materials. This tendency is reflected in the