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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Arabian Peninsula
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Oman (2)
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Saudi Arabia (2)
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China
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Primary terms
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Asia
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Oman (2)
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carbon
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Europe
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Austria
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Southern Europe
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Italy
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Sicily Italy
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Catania Italy (1)
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Invertebrata
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Myodocopida (1)
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Podocopida
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Cavellinidae (1)
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Brachiopoda (2)
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Mollusca
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Ammonoidea (1)
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Protista
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Foraminifera
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Fusulinidae (1)
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Vermes
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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Mesozoic
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Triassic
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Lower Triassic
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Permian-Triassic boundary (3)
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Middle Triassic
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Upper Triassic
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North America
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oxygen
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Paleozoic
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Upper Devonian (1)
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Permian
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Guadalupian
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Khuff Formation (4)
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Lower Permian
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Artinskian (1)
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Middle Permian (2)
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Upper Permian
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Permian-Triassic boundary (3)
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upper Paleozoic (1)
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sedimentary structures
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sedimentary structures (1)
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Late Triassic (Tuvalian – Carnian, Tropites subbullatus/Anatropites spinosus zones) ostracods from Monte Gambanera (Castel di Iudica, Central-Eastern Sicily, Italy)
COMMENT TO LEHRMANN ET AL. NEW SECTIONS AND OBSERVATIONS FROM THE NANPANJIANG BASIN, SOUTH CHINA
Deep-water ostracods from the Middle Anisian (Reifling Formation) of the Northern Calcareous Alps (Austria)
Late Scythian–Anisian ostracods (Crustacea) from the Meged-2 borehole, central Israel
Erosional truncation of uppermost Permian shallow-marine carbonates and implications for Permian-Triassic boundary events: Comment
Kempfia , A New Name for the Genus Bairdiacratia Crasquin, 2008, Non Jiang, 1983
Permian and Triassic radiolarians from northern Tibet: correlation between radiolarian and conodont biozones
Latest Permian deep-water ostracods from southwestern Guangxi, South China
Ostracods of the Permian-Triassic Khuff Formation, Saudi Arabia: palaeoecology and palaeobiogeography
The Permian-Triassic Khuff Formation of central Saudi Arabia
Palaeocopida (Ostracoda) across the Permian–Triassic events: new data from southwestern Taurus (Turkey)
A new ostracode fauna from the Permian-Triassic boundary in Turkey (Taurus, Antalya Nappes)
ABSTRACT Along the western flank of the Haushi-Huqf Upift in Oman, the upper Palaeozoic succession consists of (from oldest to youngest): (1) glaciogenic Upper Carboniferous-Lower Permian Al Khlata Formation; (2) marine Lower Permian Saiwan Formation (= Lower Gharif Member of subsurface Oman); (3) continental Lower and Middle Permian redefined Gharif Formation (= Middle and Upper Gharif members of subsurface Oman); and (4) lower part of the Middle Permian marine Khuff Formation. The succession overlies lower Palaeozoic-Proterozoic rocks, and the Khuff Formation is truncated by Triassic and younger unconformities. The Al Khlata Formation is about 100 m (328 ft) thick, and consists of a succession of diamictite, sandstone enclosing pebbles to boulders of sandstone, dolomite, black chert and pink granite clasts (ranging in diametre from a few centimetres to a metre). The overlying Saiwan Formation comprises two bioclastic units: lower ‘Bellerophon Limestone’ (10-18 m, 33-59 ft thick) and the upper ‘Metalegoceras Limestone’ (35-40 m, 115-131 ft thick). A basal Pachycyrtella Bed of the Saiwan Formation yielded Pachycyrtella omanensis associated with subordinate specimens of the genus Strophalosia indicating a mid-Sakmarian age. Brachiopod, ammonoid and bivalve assemblages in the main part of the Saiwan indicate a late Sakmarian age. The Saiwan Formation contains (5 metres above its base in the type section) Arabian Plate Maximum Flooding Surface MFS P10 of late Sakmarian age, and based on the latest Permian time scale is recalibrated at about 284 Ma (previously 272 Ma).The redefined Gharif Formation (70-100 m; 230-328 ft) lies unconformably above the Saiwan Formation, and consists of shale and sandstone deposited in floodplain and ephemeral shallow-lake environments. Uppermost Gharif ‘estuarine’ subunit B lies conformably below the first marine Khuff deposits, and contains a rich macroflora that is not diagnostic of a precise age, but is considered ?Roadian-?early Wordian. The incomplete Khuff Formation (30 m, 98 ft) consists of three informal members (1-3 from base up). The transition from Gharif subunit B to lowermost Khuff member 1 represents an environmental change from a distal fluviatile/estuarine system bordering a coastal plain, to a clastic transgressive shoal/barrier environment. Khuff members 2 and 3 reflect a carbonate shelf environment. The lower sequence boundary of the Khuff transgression is interpreted to be at the base of Gharif subunit B. Marine fauna in the Khuff Formation includes cephalopods, brachiopods, conodonts, ostracods and bivalves, which indicate a Middle Permian Wordian age. Conodont fauna from the uppermost levels of Khuff member 3 suggests a late Wordian age. The foraminifera indicate a Middle Permian age (Wordian and Capitanian).