2012
DOI: 10.1016/j.palaeo.2012.05.015
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Unraveling the origin of the Late Triassic multitaxic bone accumulation at Krasiejów (S Poland) by diagenetic analysis

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Cited by 46 publications
(51 citation statements)
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“…The region was dominated by low-relief gilgai microrelief, characterized by alternating mounds and depressions, influenced by accidental heavy storm runoffs during wet seasons (Szulc 2005;compare Bilan 1975;Dzik et al 2000;Dzik and Sulej 2007;Bodzioch and Kowal-Linka 2012). Thus, its critical character includes the rapid lateral pinchout of the 0.5-m-thick bone bed in the Krasiejów clay pit (see also borehole data in Bilan 1975), in opposition to the predicted lateral continuity of the given horizon so typical of lacustrine basins (repeatedly asserted since Dzik et al 2000;Sulej 2007, 2016: 805-807).…”
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“…The region was dominated by low-relief gilgai microrelief, characterized by alternating mounds and depressions, influenced by accidental heavy storm runoffs during wet seasons (Szulc 2005;compare Bilan 1975;Dzik et al 2000;Dzik and Sulej 2007;Bodzioch and Kowal-Linka 2012). Thus, its critical character includes the rapid lateral pinchout of the 0.5-m-thick bone bed in the Krasiejów clay pit (see also borehole data in Bilan 1975), in opposition to the predicted lateral continuity of the given horizon so typical of lacustrine basins (repeatedly asserted since Dzik et al 2000;Sulej 2007, 2016: 805-807).…”
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confidence: 99%
“…But what, in this context, can be the meaning of the enigmatic (from a sedimentological viewpoint) phrase "periodic ponding at a lake shore"? The gray, fossil-bearing claystone layer is actually swamp sediment, underbedded by an impermeable vertisol and bounded by elevated ridges (and mostly graded upward into a reddish regolithic soil complex deposited during the next dry period; compare Szulc 2005;Bodzioch and Kowal-Linka 2012).…”
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