WebThis spore assemblage data shows that the age is TC zone, and from the upper part of that zone. Correlation with the British Carboniferous stages (Riley 1993) indicates an Asbian age. Palaeoenvironment. The significant characteristic of the Fife 1 assemblage is the overwhelming abundance of Lycospora pusilla microspores. http://earthwise.bgs.ac.uk/index.php/Southern_%E2%80%98Dinantian%E2%80%99_successions,_Carboniferous,_Northern_England
TER CARBONIFEROUS (LATE VISEAN) CYCLICITY IN SOUTHERN …
WebThe age of the clastic rocks immediately below the rock-head at 37′ 8″ (11·5 m) was indeterminable, but in the interval below, down to 752′ (229 m), lower Namurian rocks (E1, Pendleian) were determined (including the Blae Pot Limestone and the upper part of the Catsbit Limestone). Web(3) Upper Asbian terraced limestone unit with minor shallowing-upward cycles of poorly bedded Kamaenella-rich limestone with shell bands and palaeokarst features. This unit is very similar to other cyclic sequences of late Asbian age in southern Ireland and western Europe, suggesting a glacio-eustatic origin for this fourth-order cyclicity. my health credit valley
Lithostratigraphy and biostratigraphy of the Lower Carboniferous ...
WebRegionally, the group name is used to unify all equivalent, locally named, thick carbonate platform successions of Dinantian and earliest Namurian age in the north of England (P916068). The greatest exposed thickness is seen in Ravenstonedale where about 800 m of strata range from Chadian up to Asbian in age. WebBivalve and brachiopod faunas indicate an Asbian (D1Subzone) age ~*2(Bracewell 1925), although palynological evidence (Turner et al.1995) suggests an Asbian to early Brigantian age. Web1 gen 2005 · Asbian age (upper Cf6 Subzone) is assigned to. the succession, from approximately the middle (second) S. junceum band to the top of the for-mation in the Ballymote Syncline, and from the. myhealth cranbourne logo