Manndraperelv Member: This member is the youngest member of this formation, and is roughly 190 metres (620ft) at its thickest, and mainly consists of coarse-grained, red quartzitesandstones and conglomerate, which is interbedded with greywacke and mudstone. The lower strata of this member contains occasional Ichnotaxon, which have been noted to be similar to Planolites, and also contains the agglutinated organism, Palaeopascichnus.[2][3]
Innerelv Member; This member is the middle member of this formation, and is the largest member in terms of thickness, coming in at around 275–300 metres (902–984ft) thick. Near the base of this member, it mainly consists of green to red shales, which contain occasional interbedded fine-grained, red sandstones. Towards and into the middle, the shales become a more greenish-grey colour, with fine-grained cross-laminated sandstones. At the top of the member, the fine-grained sandstones give way to much thicker interbedded medium to coarse, parallel-laminated sandstone. In exposed areas, the sandstone features rippled tops, and their orientation suggest a southwestern palaeocurrent at the time of deposition. In non-exposed areas, this layer is overlain by a top-most layer of greenish-grey, parallel-laminated siltstones, which are interbedded with fine-grained, ripple-marked sandstone.[2] This is also the main fossiliferous member of the whole formation, containing a wide range of discoidal forms.[2]
Lillevatn Member: This member is the oldest member of this formation, and is also the smallest, only being 40 metres (130ft) at its thickest. It mainly consists of a quartz conglomerate, which are overlain by medium-grained, gray sandstones.[2]
Using Rubidium–strontium dating on samples collected within the Stappogiedde Formation and other formations within the area, a minimum age of 530±0Ma had been recovered from samples collected at the top of the formation, dating part of the Manndraperelv member to within the early Cambrian period, and is inline with previous Rb-Sr dating studies.[4] The maximum age of 560±0Ma had been recovered from the base of the formation, reaffirming assumptions that the majority of the formation is Ediacaran in age.[1]
The Stappogiedde Formation contains a myriad of discoidal forms, from Cyclomedusa being the most common form, to others like Ediacaria and Nimbia occlusa.[2]
Genera that are not found within the main fossiliferous Innerelv member will be noted as such.
12Gorokhov, I. M.; Siedlecka, A.; Roberts, D.; Melnikov, N. N.; Turchenko, T. L. (September 2001). "Rb–Sr dating of diagenetic illite in Neoproterozoic shales, Varanger Peninsula, northern Norway". Geological Magazine. 138 (5): 541–562. doi:10.1017/S001675680100574X.
1234567891011121314Farmer, J.; Vidal, G.; Moczydłowska, M.; Strauss, H.; Ahlberg, P.; Siedlecka, A. (March 1992). "Ediacaran fossils from the Innerelv Member (late Proterozoic) of the Tanafjorden area, northeastern Finnmark". Geological Magazine. 129 (2): 181–195. doi:10.1017/S001675680000827X.
123Crimes, T. P.; McILROY, D. (November 1999). "A biota of Ediacaran aspect from lower Cambrian strata on the Digermul Peninsula, Arctic Norway". Geological Magazine. 136 (6): 633–642. doi:10.1017/S0016756899003179.
↑Pringle, I. R. (November 1972). "Rb-Sr age determinations on shales associated with the Varanger Ice Age". Geological Magazine. 109 (6): 465–472. doi:10.1017/S0016756800042734.
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