2018
DOI: 10.1016/j.cretres.2017.05.002
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Upper Cretaceous shallow-marine deposits of the southwestern Münsterland (northwest Germany) influenced by synsedimentary tectonics

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Cited by 12 publications
(7 citation statements)
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“…The two cores were chosen for this study because of an already existing detailed biostratigraphic framework, the presence of chemostratigraphic data (carbonate content, δ 13 C values) and excellent core recovery in both cases. For lithostratigraphic and biostratigraphic details see Berensmeier et al (2018), Dölling et al (2018), and Püttmann et al (2018).Additionally, four samples from the chalk facies (Seaford Head) were provided by Prof. Ian Jarvis (Kingston University London) for calcareous nannofossil analysis. The material was correlated based on biostratigraphic and chemostratigraphic data from Jarvis et al (2006) and Hampton et al (2007).…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The two cores were chosen for this study because of an already existing detailed biostratigraphic framework, the presence of chemostratigraphic data (carbonate content, δ 13 C values) and excellent core recovery in both cases. For lithostratigraphic and biostratigraphic details see Berensmeier et al (2018), Dölling et al (2018), and Püttmann et al (2018).Additionally, four samples from the chalk facies (Seaford Head) were provided by Prof. Ian Jarvis (Kingston University London) for calcareous nannofossil analysis. The material was correlated based on biostratigraphic and chemostratigraphic data from Jarvis et al (2006) and Hampton et al (2007).…”
Section: Methodsmentioning
confidence: 99%
“…During a recent drilling campaign in northwestern Germany, Cenomanian to lower Campanian strata (100‐81 Ma) have been cored in 13 wells (Dölling et al., 2018). The cores recovered glauconite‐rich marls, which were deposited about 0–10 km north off the former coast, under shallow‐marine conditions.…”
Section: Introductionmentioning
confidence: 99%
“…Dölling et al . () proposed that this member should be transferred into the newly established Duisburg Formation, a move accepted by the German Subcommission of Cretaceous Stratigraphy in the autumn of 2017 (Dölling ). A rich phosphatized fauna, which may be partly reworked from older strata, occurs near the base of the Soest Greensand Member.…”
Section: Geological Settingmentioning
confidence: 99%
“…This extensive transgression was followed by a regression that entailed a hiatus, which includes the middle Turonian (Phase 8), and resulted in the deposition of the Soest Greensand Member of the Oerlinghausen Formation (Phase 9) ). Dölling et al (2017) proposed that this member should be transferred into the newly established Duisburg Formation, a move accepted by the German Subcommission of Cretaceous Stratigraphy in the autumn of 2017 (Dölling 2018). A rich phosphatized fauna, which may be partly reworked from older strata, occurs near the base of the Soest Greensand Member.…”
Section: Geological Settingmentioning
confidence: 99%
“…The red rectangles show the sections presented in Figure 5: l., lower; mid., middle; up., upper; Sald., Salder; Er., Erwitte; Coe., Coesfeld; Bau., Baumberg; lim., limestones. Source: Modified after Hiss and Mutterlose (2010) and Dölling et al (2018). [Colour figure can be viewed at wileyonlinelibrary.com]…”
Section: Introductionmentioning
confidence: 99%