A preliminary survey of the flora of Bamhameross Common

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Suffolk Natural History, Vol. 32

A PRELIMINARY SURVEY OF THE FLORA OF BARNHAMCROSS COMMON MIKE CREWE In May 1994 I first visited Barnhamcross Common, an area of grassland and scrub immediately south of Thetford and bisected by the AI34, Thetford to Bury St Edmunds road. The common is in the parish of Thetford and thus lies in the administrative county of Norfolk. However, being south and west of the Little Ouse river, it lies within the borders of Vice County 26, West Suffolk. The site is owned by Thetford Town Council and is a Registered Common. Barnhamcross Common is a designated Site of Special Scientific Interest (SSSI) and is managed for its wildlife value by a Local Management Group which organises and oversees any work that is carried out by the Barnhamcross Common Conservation Volunteers (BCCCV). The group produces a newsletter, issue number 2 (April 1993) of which carries an informal checklist of the plant taxa identified on the site in recent times, prepared by Nick Gibbons. It was clear to me from this checklist (of some 250 plant taxa) that information had been gathered piecemeal and that no complete survey of the whole site had been carried out. The most intensive botanical survey to date of Breckland (Trist, 1979) appears to have only given the site a cursory look for any of the rarer species. This is presumably because the common was not in one of the 1km squares selected for intensive coverage by that survey. It seems perhaps remarkable (but by no means unique!) that a SSSI has received such scant attention. The accompanying map, supplied by members of BCCCV, details the sections and areas referred to throughout this paper. All plant Classification and nomenclature follows Stace (1992).

Soil and Topography The unique topography of Breckland has been amply covered elsewhere (e.g. Simpson, 1982; Trist, 1979). Barnhamcross Common lies in the heart of Breckland and shows many of the features that were typical of the whole area before cultivation by Man. The underlying chalk is covered with a layer of acid sands which vary in depth to a remarkable degree. Changes from one to the other can be very abrupt and complex mosaics of acid and alkaline areas make mapping of soil types almost impossible beyond a basic generalisation. On the west side of the common (E5) there is an excellent example of 'stone-striping', a geological feature which was formed in the last ice-age when glacial action resulted in regulär bands of gravels and chalk, with the dips in between becoming infilled with wind-blown sand. This produced alternating strips of acid and calcareous soils which are reflected in the Vegetation present. In general, the bulk of the sandy, acid areas lie to the east of the AI34 (A, B and C) with another area extending as a narrow band from the south end of D l and the north end of E l into E4 and E2. There is a remarkably clear line visible in the change of Vegetation where the acid soil gives way to calcareous ground in E4. The main calcareous areas occur in Sections D and E, to the west of the road. There is also a strip of more or less neutral soil running northsouth through the centre of the common, roughly following the course of the road.

Trans. Suffolk Nat. Soc. 32 (1996)


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