[3] This unit outcrops in central Skane on a few isolated exposures, being traditionally subdivided into the lower “millstone” (“kvarnstenen”) and the upper “buildingstone”.

[5][6] It has been assumed to be limited to Hettangian-Sinemurian layers, yet recent palynological analysis suggest the uppermost section is of Pliensbachian age, underlying and maybe interacting with the younger volcanic deposits.

[1] The Höör sandstone represents a mostly fluvial unit with a rich collection of fossil plants, yet also includes brackish bivalves in some layers, pointing to marine ingressions locally.

[7] This member represents the older layers of the formation, being exposed in the abandoned stanstorpsgraven quarry and in the Vittseröd area.

[8] The presence of silt and mature quartz arenites, well sorted and fairly well rounded derived from strongly altered feldspars, shows that this member hosted a high-energy environment, one where tidal currents have been invoked for the modification of fine-grained sandstones, linked with the changes of the Laurasian Seaway.

[9] The upper parts of this unit are influenced by the initial pulse of the Pliensbachian coeval vulcanism with heavy volcanic minerals in the uppermost layers.

This faunal aggrupation occurs together with abundant foliar remains and are equivalent to the Brandsberga erratics, which was closer to the mouth of the bay developed in the region, as it proves the find on its sandstone of more clear marine fauna.

This fragment has been considered to be a Limulus or Mesolimulus prosomal shield, but due to the limited and fragmentary nature some authors referred to it as ?Chelicerata incertae sedis.

Wielandiella may be regarded as a fossil taxon characterized by bennettitalean shrubs with branched stems and a divaricate architecture Pterophyllum[16][19] Vittseröd Member Affinities with Williamsoniaceae inside Bennettitales.

In the uppermost layers is the dominant macroflora outside Pelmastermales Anomozamites[16][19] Vittseröd Member Affinities with Williamsoniaceae inside Bennettitales.