A total of 24 benthic samples were collected from the low-tide mark along an 800 m transect, using a standard corer methodology46 , from marine sandy beach substrata in Prestwick (three every 100 m between 55°30.481′N, 4°37.489′W and 55°30.194′N, 4°37.368′W) and a further three from Littlehampton (50°48.021′N, 00°32.530′W), UK, during the summer of 2007. The latter sampling site was used as a geographically disparate out-group comparison. For the sequencing analysis, each biological sample comprised three pooled 44 mm diameter×100 mm benthic samples taken approximately 10 m apart. An additional core was taken for sediment analysis. All samples were immediately fixed in 500 ml storage pots containing 300 ml of DESS (20% DMSO and 0.25 M disodium EDTA, saturated with NaCl, pH 8.0)47 .
The meiofaunal size fraction was mechanically separated from the sand and concentrated by decanting five times with filtered tap water through a 45 μm filter. Subsequent separation from fine silt was achieved by repetitive centrifugation in 1.16 specific gravity LUDOX-TM solution48 . Following centrifugation, each sample was retained on a distinct mesh sieve, which was then folded, sliced and placed in a 15 ml falcon tube and kept at −80 °C until DNA extraction. Samples were lysed overnight at 55 °C in lysis buffer (100 mM Tris–HCl, pH7.5; 100 mM NaCl; 100 mM EDTA; 1% SDS, 500 μg ml−1 proteinase K), assisted by spinning wheel mixing, and DNA extracted with the QIAamp DNA Blood Maxi Kit (Qiagen) following the manufacturer's protocol.