Research paperFaunal response to transgressive-regressive cycles: example from the Jurassic of western India
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Palaeoecological and palaeoenvironmental analyses of Cenomanian–early Turonian macrobenthic faunas from the northern Eastern Desert of Egypt
2021, Cretaceous ResearchCitation Excerpt :The abundance and environmental distribution of these macrofaunal groups were controlled mainly by several factors that greatly affected the diversity and dominance of species (El-Hedeny and El-Sabbagh, 2005; El-Sabbagh, 2008; Nagm, 2009, 2015; El-Sabbagh et al., 2011, 2015; Abdelhady et al., 2020; Abdel-Raheem et al., 2020). Numerous studies have used sedimentological information along with synecological and taphonomic data for reconstructing Mesozoic marine palaeoenvironments (e.g., Fürsich, 1977, 1984, 1994; Oschmann, 1988; Fürsich et al., 1991, 1995, 2001, 2004; Röhl et al., 2001; Berndt, 2002; Wilmsen et al., 2007; Ayoub-Hannaa and Fürsich, 2012; Abdelhady and Fürsich, 2014; El-Sabbagh et al., 2017). However, no studies have yet treated the Cenomanian–early Turonian palaeoenvironment of the Eastern Desert of Egypt within the framework of sedimentological and palaeoecological relationships.
Middle Jurassic evolution of a northern Tethyan carbonate ramp (Alborz Mountains, Iran)
2021, Sedimentary GeologyUnravelling the paleoecology of flat clams: New insights from an Upper Triassic halobiid bivalve
2020, Global and Planetary ChangeResponses of benthic foraminifera to environmental variability: A case from the Middle Jurassic of the Kachchh Basin (Western India)
2019, Marine MicropaleontologyCitation Excerpt :A sudden regime change is noted since the mid– Middle Callovian (from the base of Obtusicostites Zone; Fig. 2–4), from sand to sandy clay and silt, marked by greenish–yellow gypsiferous shales with thin–bedded siltstones, interspersed with ferruginous and calcareous nodules (Fig. 4). Throughout this gypsiferous unit (gypsum is most likely the oxidation product of pyrite reacting with Ca2+ ions; secondary gypsum), from the base to top, there is a gradual increase in sand content (terrigenous input) and smectite, with occasional levels containing the opportunistic Bositra–dominated low–diversity bivalve faunas (see also Fürsich et al., 1991). In the present study, the opportunistic deep infaunal taxa Reophax metensis dominates this unit and forms a distinct assemblage (Figs. 4–5).