Serpulite Member SKWFF

 

Premise Definition extended after NAM and RGD (1980) . In adjoining Germany referred to as Serpulit (Schott (1951) ; t Hart (1969) ; Kemper (1973) Kemper (1973) ).
Derivatio nominis Named after the village of Weiteveen, municipality of Schoonebeek, in the southeastern part of the province of Drente.
Type section Location map See figure (pdf)
  Well Schoonebeek-197 (pdf)
  Location N 52°38’58.0
E 07°02’34.2
  Depth 1230 to 1330 m
  Length 100 m along hole
  Reference NAM and RGD (1980)
Additional section Location map See figure (pdf)
  Well Ruinen-1 (pdf)
  Location N 52°44’09.8
E 06°27’12.8
  Depth 1046 to 1087 m
  Length 41 m along hole
  Well Exloo Odoorn-2 (pdf)
  Location N 52°54’20.7
E 06°51’57.8
  Depth 1697 to 1708 m
  Length 11 m along hole
  Well De Bente-1 (pdf)
  Location N 52°41’37.8
E 06°46’15.7
  Depth 1174 to 1218 m
  Length 44 m along hole
  Well Oldenzaal-2 (pdf)
  Location N 52°17’18.8
E 06°56’23.8
  Depth 295 to 374 m
  Length 79 m along hole
Definition A bluish grey, limestone-rich claystone interval which is characterised by the dominant occurrence of serpulid fragments. The frequently intercalated microcoquina beds and laminae contain abundant pelecypod and ostracod remains. Anhydritic beds and nodules are abundant.
Upper Boundary Its upper boundary with the Coevorden Claystone Formation is marked by a characteristic wire-line log marker, corresponding to a conspicuous claystone break in a clayey-marly interval with limestones.
Lower Boundary It usually conformably overlies the Upper Marl Member, but locally unconformably overlies the Altena Group or older sediments.
Distribution Dutch part of the Lower Saxony Basin, which reaches the easternmost parts of the Dutch provinces of Groningen, Drente and Overijssel.
Age Late Portlandian - earliest Ryazanian(?) (t Hart (1969) ; Kemper (1973) Kemper (1973) ) The base of the Cretaceous (Ryazanian) is currently placed near the top of the Serpulite Member (Kemper (1973) Kemper (1973) ; Allen, P. and Wimbledon, W.A (1991) : at the base of the Upper Serpulite in Germany, which is absent in the Netherlands). The end of the Portlandian is characterised by a sharp decrease in Classopollis (Burger (1966) , Herngreen et al (1980) ). The member is placed in zone Upper Malm 6 or F of the regional ostracod zonation (Wolburg (1949) ; Sung (1955) ; t Hart (1969) . Ostracods occurring frequently in this member are: Cypridea dunkeri carinata, C. posticalis, C. binodosa and C. fasciculata.
Depositional Setting Lacustrine basin-margin to marginal-marine sub-basin (lagoonal) setting. The dominance of carbonates points to a low input of clastic material.
Sequence Stratigraphy The member mainly represents the Highstand systems tract of sequences LZA 1.4 and 1.5a, as can be seen from the generally funnel-shaped log patterns.
References See References Upper Jurassic/ Lower Cretaceous

Van Adrichem Boogaert, H.A. & Kouwe, W.F.P., 1993-1997. [Stratigraphic unit]. In: Stratigraphic Nomenclature of the Netherlands.
Retrieved [Datum] from [url].