TY - JOUR A1 - Khaled, Mohamed Ismail T1 - Nomes of Lower Egypt in the early Fifth Dynasty JF - E&G Quaternary Science Journal N2 - Having control over the landscape played an important role in the geography and economy of Egypt from the predynastic period onwards. Especially from the beginning of the Old Kingdom, we have evidence that kings created new places (funerary domains) called (centers) and (Ezbah) for the equipment of the building projects of the royal tomb and the funerary cult of the king, as well as to ensure the eternal life of both kings and individuals. Kings used these localities in order to do so, and they oftentimes expanded the border of an existing nome and created new establishments. Consequently, these establishments were united or divided into new nomes. The paper discusses the geography of Lower Egypt and the associated royal domains in the early Fifth Dynasty based on the new discoveries from the causeway of Sahura at Abusir. N2 - Die geographische Unterteilung des Landes als Voraussetzung des Zugriff auf die Ressourcen des Landes spielte für die Wirtschaft Ägyptens und königliche Bauprojekte seit der prädynastischen Zeit eine wichtige Rolle. Um die landwirtschaftliche Nutzung des Landes auszuweiten und diesen Zugriff gleichzeitig zu sichern, begründeten die ägyptischen Könige Wirtschaftsanlagen (Grabdomänen) an schon bestehenden oder neu geschaffenen Siedlungen. Da sich der größte Teil der agrarisch nutzbaren Fläche im Delta befand, wurde im Laufe der Zeit auch das bestehende Gausystem dieses Gebietes mehrfach verändert. Das Papier erörtert die Geographie des Deltas in der frühen fünften Dynastie auf der Grundlage neuer Entdeckungen vom Aufweg des Pyramidenbezirkes des Sahure in Abusir (Abstract was translated by Eva Lange-Athinodorou.). KW - nomes KW - Egypt KW - Fifth Dynasty Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-230350 VL - 70 IS - 1 ER - TY - JOUR A1 - Abdelhafez, Omnia Hesham A1 - Fawzy, Michael Atef A1 - Fahim, John Refaat A1 - Desoukey, Samar Yehia A1 - Krischke, Markus A1 - Mueller, Martin J. A1 - Abdelmohsen, Usama Ramadan T1 - Hepatoprotective potential of Malvaviscus arboreus against carbon tetrachloride-induced liver injury in rats JF - PLoS ONE N2 - Malvaviscus arboreus Cav. is a medicinal plant belonging to family Malvaceae with both ethnomedical and culinary value; however, its phytochemical and biological profiles have been scarcely studied. Accordingly, this work was designed to explore the chemical composition and the hepatoprotective potential of M. arboreus against carbon tetrachloride (CCl\(_4\))-induced hepatotoxicity. The total extract of the aerial parts and its derived fractions (petroleum ether, dichloromethane, ethyl acetate, and aqueous) were orally administered to rats for six consecutive days, followed by injection of CCl\(_4\) (1:1 v/v, in olive oil, 1.5 ml/kg, i.p.) on the next day. Results showed that the ethyl acetate and dichloromethane fractions significantly alleviated liver injury in rats as indicated by the reduced levels of alanine transaminase (ALT), aspartate transaminase (AST), alkaline phosphatase (ALP), total bilirubin (TB), and malondialdehyde (MDA), along with enhancement of the total antioxidant capacities of their livers, with the maximum effects were recorded by the ethyl acetate fraction. Moreover, the protective actions of both fractions were comparable to those of silymarin (100 mg/kg), and have been also substantiated by histopathological evaluations. On the other hand, liquid chromatography-high resolution electrospray ionization mass spectrometry (LC‒HR‒ESI‒MS) metabolomic profiling of the crude extract of M. arboreus aerial parts showed the presence of a variety of phytochemicals, mostly phenolics, whereas the detailed chemical analysis of the most active fraction (i.e. ethyl acetate) resulted in the isolation and identification of six compounds for the first time in the genus, comprising four phenolic acids; β-resorcylic, caffeic, protocatechuic, and 4-hydroxyphenylacetic acids, in addition to two flavonoids; trifolin and astragalin. Such phenolic principles, together with their probable synergistic antioxidant and liver-protecting properties, seem to contribute to the observed hepatoprotective potential of M. arboreus. KW - high performance liquid chromatography KW - phenols KW - phytochemicals KW - antioxidants KW - metabolomics KW - medicinal plants KW - Egypt KW - xenobiotic metabolism KW - Malvaviscus arboreus Y1 - 2018 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-177243 VL - 13 IS - 8 ER - TY - THES A1 - Nagm, Emad Hamdy Mahmoud T1 - Integrated stratigraphy, palaeontology and facies analysis of the Cenomanian – Turonian (Upper Cretaceous) Galala and Maghra El Hadida formations of the western Wadi Araba, Eastern Desert, Egypt T1 - Integrierte Stratigraphie, Paläontologie und Faziesanalyse der Galala- und Maghra El Hadida Formationen (Cenoman – Turon, Oberkreide) im westlichen Wadi Araba, Eastern Desert, Ägypten N2 - Four sections of the Galala and Maghra El Hadida formations on the footwalls of the slopes of the northern and southern Galala plateaus in Wadi Araba (Eastern Desert) have been measured and sampled in great detail. The Galala Formation is ranging in thickness from 55 to 95 meters. It unconformably overlies the Malha Formation which forms the base of the studied sections. The upper boundary of the Galala Formation is characterized by a major unconformity which separates it from the overlying the Maghra El Hadida Formation. The Galala Formation can be subdivided into five shallowing-upward cycles, each cycle starting with deep-lagoonal, marly-silty deposits at the base and grading into highly fossiliferous shallow-lagoonal limestones at the top. Only the basal part of the Galala Formation consists of unfossiliferous, greenish sandy siltstones intercalated with thin cross-bedded, bioturbated, fine- to medium-grained sandstones. Despite the lack of biostratigraphic markers in that lower part, its age can be assigned to the late Middle Cenomanian, since the conformably overlying strata contain the ammonite Neolobites vibrayeanus (D’ORBIGNY), the index marker of the early Upper Cenomanian which extends into the top of the formation. The measured thickness of the overlying Maghra El Hadida Formation is ranging from 59 to 118 meters. This formation starts with the Ghonima Member, introduced in this work to distinguish a brown, fine- to medium-grained calcareous sandstone unit in its lower part. The Ghonima Member is erosionally incised into the Galala Formation, explaining its strong lateral variability in thickness, ranging from 3 to 21 meters. It is mostly unfossiliferous except for irregular bioturbation in its upper part. The Ghonima Member is assigned to the middle Upper Cenomanian, based on its stratigraphic position between the lower Upper Cenomanian Neolobites vibrayeanus Zone and the overlying upper Upper Cenomanian Metoicoceras geslinianum and Vascoceras cauvini zones. This means that the lower part of the Maghra El Hadida Formation, about 20 – 30 m thick, accumulated during the latest Cenomanian and that the base of the formation does not coincide with the base of the Turonian as commonly believed. The overlying succession of the Maghra El Hadida Formation is characterized by an increase of carbonate content, represented by yellow, soft marls intercalated with fine-grained wacke- to packstones containing a highly fossiliferous ammonite assemblage of the upper Upper Cenomanian and Lower Turonian (zones of Vascoceras proprium, Choffaticeras spp., and Wrightoceras munieri). The Middle Turonian part of the Maghra El Hadida Formation consists of poorly fossiliferous, thick-bedded yellowish marls with upward-increasing silt content, showing occasional intercalations of medium- to coarse-grained sandstones with hummocky cross-stratification. The topmost part of the Maghra El Hadida Formation consists of brownish, medium-grained sandstones topped by fossiliferous marly limestones yielding the Upper Turonian zonal ammonite Coilopoceras requienianum (D’ORBIGNY). Based on sequence stratigraphic analyses, four complete 3rd order depositional sequences and the lower part of a fifth one, each bounded by major unconformities, can be recognized: depositional sequence DS WA 1 (upper Middle – lower Upper Cenomanian) includes the entire Galala Formation, while the Maghra El Hadida Formation comprises all the overlying depositional sequences: DS WA 2 (upper Upper Cenomanian – Lower Turonian) reaches from the base of the Metoicoceras geslinianum Zone to the top of Wrightoceras munieri Zone, DS WA 3 and DS WA 4 comprise the Middle Turonian, while Upper Turonian sequence DS WA 5 is not complete. The stratigraphic positions of the recognized sequence 2 boundaries SB WA 1 to SB WA 5 match well with contemporaneous sequence boundaries known from Europe and elsewhere. The stacking pattern of the basic cycles and bundles of the Galala Formation (5:1) and the Maghra El Hadida Formation (4:1) strongly suggest an orbital forcing by MILANKOVITCH periodicities. The Galala Formation is composed of five 5th-order bundles which equal to ~500 kyr, each bundle equals to ~100 kyr (short eccentricity). Every bundle has five basic (6th-order) cycles, each one representing ~20 kyr (precession). Based on this precession-short eccentricity syndrome, the accumulation rate of the Galala Formation therefore accounts for about 19 cm/kyr. The rate of sea-level fall at sequence boundary SB WA 2 (equivalent to the quasi-global mid-Late Cenomanian SB Ce V) estimated is with 35 cm/kyr which can be explained only by glacio-eustasy. The Upper Cenomanian and Lower Turonian part of the Maghra El Hadida Formation is considered to equal to ~1200 kyr, based on the existence of three 4th-order bundles with an inferred duration of ~400 kyr for each bundle (long eccentricity of the MILANKOVITCH Band). Every bundle consists of four basic cycles with a duration of ~100 kyr. This means that the upper Cenomanian part of the Maghra El Hadida Formation is equivalent to ~400 kyr, while the Lower Turonian (consisting of the two upper bundles) lasted 800 kyr. This matches well with the recently proposed 785 kyr duration of the Early Turonian (SAGEMAN et al., 2006; VOIGT et al., 2008) and contradicts the 1300 kyr according to the standard time scale of GRADSTEIN et al. (2004). According to this temporal constrains, the accumulation rate of the Maghra El Hadida Formation is about 4.25 cm/kyr. In addition, based on the cyclostratigraphic analysis, the range of the Early Turonian genus Choffaticeras (HYATT) is equivalent to ~325 kyr and morphological changes within its lineage can be quantified. The macrobenthos (bivalves, gastropods, echinoids) and cephalopods of the Galala and Maghra El Hadida formations were identified and illustrated in 24 figures. The ammonite taxonomy and palaeobiogeographic distribution is discussed in detail. Four genera and eight ammonite species are recorded from Egypt for the first time. The microfloral and -faunal assemblage identified in thin sections revealed two species of dasycladalean algae, two species of udoteacean algae, five species of benthic foraminifera, and two species of crustacean microcoprolites. The six facies types of the upper Middle – Upper Cenomanian Galala Formation document largely open-lagoonal, warm water conditions, while the depositional environment of the Upper Cenomanian – Turonian Maghra El Hadida Formation (16 facies types) is suggested to range from a deep-subtidal to intertidal. KW - Oberkreide KW - inegrierte Stratigraphie KW - Makrobenthos KW - Ammoniten KW - Faziesanalyse KW - Ägypten KW - Oberkreide KW - inegrierte Stratigraphie KW - Makrobenthos KW - Ammoniten KW - Faziesanalyse KW - Ägypten KW - Upper Cretaceous KW - integrated stratigraphy KW - macrobenthos KW - ammonites KW - facies analysis KW - Egypt Y1 - 2009 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-39881 ER -