FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4366992706> ?p ?o ?g. }

• W4366992706 abstract "Abstract The palaeoenvironments of the upper Palaeozoic succession in the eastern foot slopes of the Northern Galala Plateau, west of the Gulf of Suez, Egypt, are interpreted based on a detailed study of the sequence-stratigraphic framework, sedimentary facies and trace fossils. The upper Carboniferous–lower Permian Aheimer Formation has been studied in its type section exposed in Wadi Aheimer. Three unconformities bound four 3rd-order depositional sequences, including the upper Carboniferous DS NG 1, and the lower Permian DS NG 2‒4. These sequences are correlated with their counterparts on the North African and Arabian plates. The sedimentary facies characteristics indicate palaeoenvironments ranging from fluvial, estuarine, intertidal, shallow subtidal, shoreface to offshore transitional settings. The abundant and diverse ichno-assemblages are composed of horizontal, vertical and sub-vertical traces. At least 26 ichnotaxa have been identified, representing suites of the Glossifungites , proximal Cruziana , and proximal-archetypal Cruziana ichnofacies. Ichnofabric analysis revealed three distinct ichnofabrics: Tisoa , Schaubcylindrichnus and Zoophycos ichnofabrics. The trace and body fossil distribution and trophic structure of some of the recorded faunal assemblages confirm relatively stable and low-stress shallow-marine environments. In contrast, the trophic structure of some other assemblages indicates the influence of particular environmental parameters, including substrate consistency, bathymetry, water energy, productivity, rate of sedimentation, salinity and oxygen availability. The integrated results indicate that the sequences were formed during an interval dominated by different perturbations that resulted in a wide spectrum of depositional features. Moreover, evidence for Carboniferous–Permian glaciation is tentatively established in North Egypt but require further investigations." @default.
• W4366992706 created "2023-04-27" @default.
• W4366992706 creator A5049000262 @default.
• W4366992706 creator A5052439568 @default.
• W4366992706 creator A5081189366 @default.
• W4366992706 creator A5086046723 @default.
• W4366992706 creator A5090557402 @default.
• W4366992706 date "2023-04-01" @default.
• W4366992706 modified "2023-10-11" @default.
• W4366992706 title "Stratigraphical, microfacies, and ichnological characteristics and depositional environments of the Permo‒Carboniferous Aheimer Formation, western side of the Gulf of Suez, Egypt" @default.
• W4366992706 cites W1494761397 @default.
• W4366992706 cites W1508406286 @default.
• W4366992706 cites W1528563603 @default.
• W4366992706 cites W1529976899 @default.
• W4366992706 cites W1538456952 @default.
• W4366992706 cites W1540714975 @default.
• W4366992706 cites W1594515700 @default.
• W4366992706 cites W1674446040 @default.
• W4366992706 cites W1755726326 @default.
• W4366992706 cites W1764022448 @default.
• W4366992706 cites W1909319766 @default.
• W4366992706 cites W1914731816 @default.
• W4366992706 cites W1963643588 @default.
• W4366992706 cites W1964578975 @default.
• W4366992706 cites W1965602831 @default.
• W4366992706 cites W1969199454 @default.
• W4366992706 cites W1969557417 @default.
• W4366992706 cites W1970644949 @default.
• W4366992706 cites W1971690605 @default.
• W4366992706 cites W1973601592 @default.
• W4366992706 cites W1975115126 @default.
• W4366992706 cites W1975433068 @default.
• W4366992706 cites W1976558540 @default.
• W4366992706 cites W1979768410 @default.
• W4366992706 cites W1980058580 @default.
• W4366992706 cites W1980205563 @default.
• W4366992706 cites W1980642926 @default.
• W4366992706 cites W1983589204 @default.
• W4366992706 cites W1985089835 @default.
• W4366992706 cites W1990619084 @default.
• W4366992706 cites W1991754156 @default.
• W4366992706 cites W1993226856 @default.
• W4366992706 cites W1994436705 @default.
• W4366992706 cites W1994865492 @default.
• W4366992706 cites W1996296821 @default.
• W4366992706 cites W1998393286 @default.
• W4366992706 cites W2001210533 @default.
• W4366992706 cites W2008773751 @default.
• W4366992706 cites W2008827854 @default.
• W4366992706 cites W2008975622 @default.
• W4366992706 cites W2010608057 @default.
• W4366992706 cites W2013432809 @default.
• W4366992706 cites W2017280227 @default.
• W4366992706 cites W2020700198 @default.
• W4366992706 cites W2021275366 @default.
• W4366992706 cites W2028773657 @default.
• W4366992706 cites W2030719360 @default.
• W4366992706 cites W2034471984 @default.
• W4366992706 cites W2035856604 @default.
• W4366992706 cites W2040031322 @default.
• W4366992706 cites W2046093084 @default.
• W4366992706 cites W2047961688 @default.
• W4366992706 cites W2049132609 @default.
• W4366992706 cites W2050735490 @default.
• W4366992706 cites W2051162298 @default.
• W4366992706 cites W2054234673 @default.
• W4366992706 cites W2055487844 @default.
• W4366992706 cites W2056670043 @default.
• W4366992706 cites W2057416934 @default.
• W4366992706 cites W2060243557 @default.
• W4366992706 cites W2064121411 @default.
• W4366992706 cites W2064860762 @default.
• W4366992706 cites W2066250998 @default.
• W4366992706 cites W2067628429 @default.
• W4366992706 cites W2071064541 @default.
• W4366992706 cites W2074055256 @default.
• W4366992706 cites W2075089399 @default.
• W4366992706 cites W2079431706 @default.
• W4366992706 cites W2082318604 @default.
• W4366992706 cites W2082440975 @default.
• W4366992706 cites W2084651298 @default.
• W4366992706 cites W2087772250 @default.
• W4366992706 cites W2089539728 @default.
• W4366992706 cites W2092093635 @default.
• W4366992706 cites W2093879665 @default.
• W4366992706 cites W2104764232 @default.
• W4366992706 cites W2109178298 @default.
• W4366992706 cites W2109913185 @default.
• W4366992706 cites W2117891866 @default.
• W4366992706 cites W2121255113 @default.
• W4366992706 cites W2122748668 @default.
• W4366992706 cites W2127091558 @default.
• W4366992706 cites W2127342021 @default.
• W4366992706 cites W2138666479 @default.
• W4366992706 cites W2139326036 @default.
• W4366992706 cites W2144336460 @default.
• W4366992706 cites W2144414810 @default.
• W4366992706 cites W2150291090 @default.
• W4366992706 cites W2156022682 @default.
• W4366992706 cites W2162913303 @default.

• next