Salthill Quarry, Clitheroe: A resource revitalised

Stephen K Donovan (The Netherlands), Paul Kabrna (UK) and Pelham H Donovan (The Netherlands) A while ago, SKD published a critique of the poor geoconservation practices on one of England’s most productive Sites of Special Scientific Interest (SSSI) of Mississippian age – the so-called scraped surface at Salthill Quarry, Clitheroe, Lancashire (Grayson, 1981; Bowden et al., 1997; Kabrna, 2011, locality 4; see also Salthill Quarry, Clitheroe: A resource degraded) (Fig. 1; and see also Donovan, 2011). The locality is one of the best sites for Mississippian (Lower Carboniferous) echinoderms in northern Europe. It is particularly good for crinoids, but also for rarer blastoids and, if you are willing to process bulk samples, the spines and plates of echinoids (Donovan et al., 2003; Donovan & Lewis, 2011; Donovan, in press). However, when it was visited by SKD in 2010, the geological features were being overgrown by grasses and other plants; that is, the geological SSSI was being transformed, passively, into a botanical nature reserve. Fig. 1. The crinoid bank (locality 4 of Kabrna, 2011) as it was in 2010, largely obscured by grass (after Donovan, 2011, fig. 1). Collectors (left and middle) approximately define the poor exposure of bedded limestone at that time, which extended a little way past the bush in the centre. The best collecting was along this line and lower, where crinoid debris accumulated as a fossil-enriched gravel. For an earlier view of this slope, see Donovan (2012, fig. 3A, B). This situation persisted until recently. In April … Read More

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