This feature occurs in Katian / Hirnantian transition strata in West Wales - in laminated hemi-pelagite. It is about 200mm high and 100mm across. There are a number of similar features in the strata 25m or so below this one (it occurs at least 8 times with varying details of morphology. Much of the rock below this level is full of Chondrites style burrows. Looks to me like some form of infilled Dominichnial shaft between surface and deep burrows...any further thoughts?