Search results for "Facies"

showing 2 items of 232 documents

Formation of microbial organic carbonates during the Late Jurassic from the Northern Tethys (Amu Darya Basin, Uzbekistan): implications for Jurassic …

2020

23 pages; International audience; The Late Jurassic was a period of major global carbon cycle perturbations with episodes of anoxia leading to regional accumulation of organic matter in sediments worldwide. The Tubiegatan section (SW Gissar Mountains, Uzbekistan) located in the Northern Tethys, shows atypical organic-rich limestone and marl deposits (up to 6% of total organic carbon) marked by pronounced negative excursions of δ13Ccarb (amplitude of ca. 12‰) and δ13Corg (amplitude of ca. 4‰) recorded during the Middle Oxfordian (Transversarium Zone). A transdisciplinary approach including sedimentology, palynofacies characterization, mineralogy, organic and inorganic geochemistry was carrie…

microbial/laminated sediments52 anoxia010504 meteorology & atmospheric sciencesGeochemistryLate Jurassic02 engineering and technologyOceanography01 natural scienceschemistry.chemical_compoundAnoxia[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarl0202 electrical engineering electronic engineering information engineeringAmu Darya BasinOrganic matter14. Life underwaterMicrobial mat0105 earth and related environmental sciencesStable isotopesTotal organic carbonSabkhachemistry.chemical_classificationGlobal and Planetary Changegeographygeography.geographical_feature_category020206 networking & telecommunicationsorganic-rich carbonatesstable isotopes 5315. Life on landCretaceousPalynofacieschemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
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An Upper Mississippian echinoderm microfauna from the Genicera Formation of northern León (Carboniferous, Cantabrian Mountains, N Spain)

2020

For the first time an echinoderm microfauna is recorded from the cephalopod limestone facies (‘griotte facies’) of the lower Carboniferous (Mississippian) Genicera Fm. (Alba Fm.). The formation is widespread in the Cantabrian Mountains in NW Spain, but the ossicles are from some sections in the surroundings of the Bernesga valley in northern León. They have been derived from insoluble acetic acid residues from samples of the upper and especially of the uppermost part of the formation (Canalón Mb. and Millaró Beds). The microfauna include taxonomically treated wheel-shaped ossicles, sieve-plates and rods of holothurians, goniodonts of ophiocistioids, and ophiuroid and stenuroid skeletal elem…

viséan serpukhovian cephalopod limestone carbonate microfacies echinoderm ossicles taxonomy.PaleozoicbiologyApodidaPaleontologybiology.organism_classificationQE701-760SerpukhovianPaleontologyEchinodermViséanCarboniferousMicrofaunaOphiocistioideaGeologySpanish Journal of Palaeontology
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