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Schilfsandstein

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Journal Article
Published: 04 October 2018
Journal of the Geological Society (2019) 176 (1): 133–148.
...M. Franz; E. Kustatscher; C. Heunisch; S. Niegel; H.-G. Röhling Abstract Recently intensified research on the mid-Carnian episode stimulated discussions about the mid-Carnian climate and a supposed humid climate shift. This basin-scale study on the Schilfsandstein, the type-example of the mid...
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<span class="search-highlight">Schilfsandstein</span> palaeosols in the North German Basin, for the example of th...
Published: 04 October 2018
Fig. 6. Schilfsandstein palaeosols in the North German Basin, for the example of the Morsleben 52A well. Floodplain fines material of stacked sheetsands was modified to spodosols and calcic–gypsic vertisols in the Lower Schilfsandstein and spodosols, calcisols and gypsisols in the Upper
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Overview of palaeosol classes of the <span class="search-highlight">Schilfsandstein</span> in the Central Europea...
Published: 04 October 2018
Table 1. Overview of palaeosol classes of the Schilfsandstein in the Central European Basin. South Germany emended after Nitsch (2005) .
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Outcrop example of Upper <span class="search-highlight">Schilfsandstein</span> palaeosols at Gispersleben (Thurin...
Published: 04 October 2018
Fig. 4. Outcrop example of Upper Schilfsandstein palaeosols at Gispersleben (Thuringia). ( a ) Overview with litholog showing stacked sheetsands with protosols in the lower part and mature vertisols above. In the upper part (above 50 cm), individual palaeosols were initially formed as gleysols
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Outcrop and core examples of <span class="search-highlight">Schilfsandstein</span> palaeosols. ( a ) Calcisol at ...
Published: 04 October 2018
Fig. 5. Outcrop and core examples of Schilfsandstein palaeosols. ( a ) Calcisol at Altengottern (Thuringia, Upper Schilfsandstein) with vertical columnar carbonate nodules (arrows) and large horizontal carbonate nodules (encircled) in destratified shales; hammer marks the palaeosol top; scale bar
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Plant macrofossils of the <span class="search-highlight">Schilfsandstein</span> flora; scale bars represent 1 cm ...
Published: 04 October 2018
Fig. 7. Plant macrofossils of the Schilfsandstein flora; scale bars represent 1 cm for all figures. ( a ) Sporophyll of Lepacyclotes , Korber Korb (SMNS Pb645). ( b ) Apical axis fragment of Equisetites , Stuttgart (SMNS P.563). ( c ) Axis with elongate microphylls of Neocalamites , Stuttgart
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Quantitative composition of the <span class="search-highlight">Schilfsandstein</span> macroflora: 15 localities o...
Published: 04 October 2018
Fig. 8. Quantitative composition of the Schilfsandstein macroflora: 15 localities of South and Central Germany (for locations see Fig. 1 ).
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Macroplant Eco Groups (MEG) of the <span class="search-highlight">Schilfsandstein</span> macroflora: 16 localitie...
Published: 04 October 2018
Fig. 9. Macroplant Eco Groups (MEG) of the Schilfsandstein macroflora: 16 localities of South and central Germany (for locations see Fig. 1 ).
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<span class="search-highlight">Schilfsandstein</span> palynoflora. 1–16, Obernsees 1 well: 1, 2,  Anapiculatispor...
Published: 04 October 2018
Fig. 11. Schilfsandstein palynoflora. 1–16, Obernsees 1 well: 1, 2, Anapiculatisporites spp., P80644. 3, Leschikisporis aduncus , P80644. 4, Lycospora sp., P80644. 5, Kraeuselisporites spp., P80643. 6–8, Aratrisporites spp., P80643. 9, 10, Aulisporites astigmosus , P 80643, P80644. 11
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP469.1
EISBN: 9781786203885
... in the established Buntsandstein fairway but also in Rogenstein oolites and Muschelkalk carbonates. In addition, sand-prone sections in the Late Triassic, such as the Schilfsandstein, have the potential to be hydrocarbon reservoirs. Several Triassic intervals are now the focus for developing geothermal projects...
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Palynomorph Eco Groups (PEG) and palynomorph associations of the Schilfsand...
Published: 04 October 2018
Fig. 10. Palynomorph Eco Groups (PEG) and palynomorph associations of the Schilfsandstein. O, Ovalipollis association; I, inland sea palynomorph association; L, Leschikisporis association; A, Aulisporites association; T, trilete laevigate spores association, *redrawn from Visscher et al
Journal Article
Journal: Clay Minerals
Published: 01 September 2014
Clay Minerals (2014) 49 (4): 569–594.
... of palinostratigraphic data ( Orlowska-Zwolińska, 1983 ; Szulc et al. , 2006 ): Ladinian Grenzdolomite and Carnian Lower Gipskeuper (“dry” intervals: sabkha/playa sediments), followed by Carnian Schilfsandstein fluvial clastic (“wet” interval: braided/anastomosing river sediments), Carnian/Norian Upper Gipskeuper...
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Journal Article
Published: 01 April 1990
Journal of the Geological Society (1990) 147 (2): 321–327.
..., Palaeoecology 1989 70 29 51 Hahn G. Paläomagnetische Untersuchungen im Schilfsandstein (Trias, Km 2), Westeuropas Geologische Rundschau 1984 73 499 516 Hallam A. The end-Triassic bivalve extinction event Palaeogeography, Palaeoclimatology, Palaeoecology 1981 39 1 44...
Journal Article
Published: 12 July 2018
Journal of the Geological Society (2018) 175 (6): 1004–1011.
...) to early late Carnian (early Tuvalian), sometimes referred to as ‘middle Carnian’ (e.g. Hornung et al. 2007 ; Rigo et al. 2007 ; Dal Corso et al. 2015 ). In the Germanic basin, the Stuttgart Formation (Schilfsandstein) of the German Keuper is the principal non-marine record of the Carnian wet...
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Journal Article
Published: 08 October 2018
Journal of the Geological Society (2019) 176 (1): 149–166.
... the Dunscombe Mudstone Formation ( Porter & Gallois 2008 ; Ruffell et al. 2016 ). This facies change is also expressed in the Keuper Group in the Germanic Basin, where red playa lake deposits were temporarily interrupted by sandy fluvial channel and overbank deposits of the Schilfsandstein (Stuttgart...
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Journal Article
Published: 21 December 2018
Journal of the Geological Society (2019) 176 (1): 129–131.
...) was based on observations, mostly of the palynofacies, in the Shilfsandstein in the Germanic Basin. After more than 20 years, the palaeoclimatic significance of the Schilfsandstein is still a matter of debate. Most of the uncertainty is related to the ambiguity of the palynological record...
Journal Article
Published: 03 August 2015
Geological Magazine (2016) 153 (2): 271–284.
... eloquently by Shukla, Bachmann & Singh ( 2010 ) for the same stratigraphic unit, the Schilfsandstein (syn. = Stuttgart Formation) and its regional equivalents, that were discussed by both Visscher et al. ( 1994 ) and us (Simms & Ruffell, 1989 , 1990 ). In summary...
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Journal Article
Published: 01 September 2006
Environmental Geosciences (2006) 13 (3): 145–161.
..., and finally ceased with the deposition of the shallow-marine Exter Formation (Rhätkeuper) sandstones ( Reinhardt and Ricken, 2000 ). The incised-valley sandstones of the Stuttgart Formation (formerly termed Schilfsandstein) occur basinwide but display variable thickness. These sandstones consist...
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Journal Article
Published: 31 October 2018
Journal of the Geological Society (2018) 175 (6): 986–988.
... . The Schilfsandstein and its flora; arguments for a humid mid-Carnian episode? Journal of the Geological Society, London , https://doi.org/10.1144/jgs2018-053 Gianolla , P. , Ragazzi , E. , Roghi , G. , 1998 . Upper Triassic amber from the Dolomites (northern Italy) . A paleoclimatic indicator...
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Detrital mineralogy revealing low compositional maturity of the Schilfsands...
Published: 04 October 2018
Fig. 3. Detrital mineralogy revealing low compositional maturity of the Schilfsandstein. ( a ) Ternary plot ( McBride 1963 ) of 98 samples investigated herein in comparison to previously published examples; Q, mono- and polycrystalline quartz and chert; F, feldspar; L, lithic fragments (unstable