Upper Silurian microplankton of the Leintwardine Group, Ludlow Series, in the type Ludlow area and adjacent regions

The acritarchs and prasinophyte algae from the Upper Bringewood, Lower Leintwardine, Upper Leintwardine and Lower Whitcliffe formations of the Ludlow type area and surrounding regions are described. The following new taxa are proposed: Cymatiosphaera pumila sp. nov., Melikeriopalla pustula sp. nov., Cheleutochroa beechenbankensis sp. nov., Cymbosphaeridium molyneuxii sp. nov., Flammulasphaera bella gen. et sp. nov., Percultisphaera incompta sp. nov., Salopidium aldridgei sp. nov. and Umbellasphaeridium? wicanderi sp. nov. A holotype is defined for Lophosphaeridium galeatum Hill and a further 34 new taxa are described under open nomenclature. Two biozones, identified by the first appearance of the zone taxon, are defined in the Sunnyhill section, Ludlow [Global Stratotype Section and Point (GSSP) for the base of the Ludfordian Stage, Ludlow Series]. The base of the Leoniella vilis Biozone is identified at 4.52m below the top of the Upper Bringewood Formation at Beechenbank, Aymestrey. The base of the Triangulina sanpetrensis Biozone is identified at 15.49m above the base of the Lower Leintwardine Formation and Ludfordian Stage at the Sunnyhill section. These biozones allow correlation with sections in north–west Spain, Podolia and Gotland. The possibility of using Visbysphaera whitcliffense and U.? wicanderi as biozonal indicators is suggested.     

Early Ludlow monograptids with Devonian morphological affinities

Nilssoni–scanicus Zone deposits (Silurian, early Ludlow) from the Leintwardine and Long Mountain districts of Britain, and the Clrasi Borehole, Moesian Platform of Romania, have yielded a species of monograptid which, whilst resembling rare Ludlow Monoclimacis species, has strong morphological affinities with Devonian monograptids such as Monograptus ramstalensis Jaeger. Because of the occurrence of such structures at a surprisingly low horizon the writers urge caution in identifying age from monotypic assemblages. The difficulties surrounding the affinities of the low Ludlow species necessitates a provisional open nomenclature as Monograptus sp. The possible evolutionary significance is discussed.     

The environmental significance of Lingula in the Ludlow Series of the Welsh Borderland and Wales

Cherns. Lesley 1979 01 15: The environmental significance of Lingula in the Ludlow Series of the Welsh Borderland and Wales. Lethaia . Vol. 12. pp. 35–46, Oslo. ISSN 0024–1164.
The inarticulate brachiopod Lingula is commonly regarded as an indicator of very nearshore environments, particularly when found in monospecific assemblages. However, neither of the two common species in the Lower Leintwardine Beds, L. lewisii and L. lata . which occur commonly in such associations, have distributions indicative of such an environment. Their Occurrence correlates closely with the Leintwardinian palaeogeography. The former species is concentrated in shelf areas, the latter is confined to the basin; the two distributions overlap little. Individuals of both species are found articulated and perpendicular to the bedding, apparently in situ . Hence, the species may be inferred to have equivalent, infaunal modes of life comparable to living representatives of the family. The basinal distribution of L. lara is an original feature. The depth of the actively subsiding basin was relatively great, judging from sedimentological and palaeogeographical evidence. Therefore, L. lata was a species adapted to 'deep-water' environments. The lingulid distributions, reviewed against the concept of brachiopod depth-related communities previously defined for the Ludlow show the latter to be inapplicable in the Leintwardinian. The depth significance postulated for the recurrent species associations typical of the shelf sequences cannot be accepted.