Search results for "Cretaceous."

showing 6 items of 166 documents

Students' field research extends knowledge of origin of a UNESCO World Heritage site in Germany

2003

In 1992, as part of field-based course work with the Earth science department of the Universitat Minz, students began to investigate the structures of oil shale basins located in the Sprendlinger Horst, a horst-type block forming the northeastern shoulder of the Tertiary Upper Rhine Graben in southwestern Germany (figure 1). The Sprendlinger Horst is mainly built up by Hercynian or pre-Hercynian basement, Permian sediments, and volcanic rocks, as well as by several Tertiary alkali basalts and rare Cretaceous trachytes. In 1992, it was unknown whether the oil shale basins were of tectonic, volcanic, or even of impact origin.

geographygeography.geographical_feature_categoryPermianGeochemistryCretaceousVolcanic rockGrabenTectonicsBasement (geology)General Earth and Planetary SciencesHorstGeomorphologyOil shaleGeologyEos, Transactions American Geophysical Union
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A possible tsunami deposit around the Jurassic–Cretaceous boundary in the Boulonnais area (northern France)

2005

Abstract An unusual succession of facies locally deposited around the Jurassic–Cretaceous boundary in the Boulonnais (northern France) is attributed to a tsunami event by comparison with recent tsunami deposits. This sedimentary succession includes basal erosion with reworked lithified blocks, soft-sediment deformations, an erosional conglomerate overlain by wood fragments and clays containing continental and marine fossils in one setting and conglomerate with mixed fauna in an other setting. The tsunami probably affected the coast of the Boulonnais area of the London–Brabant Massif. The origin of the event is unknown. It was most probably triggered by an earthquake, but other origins such …

geographygeography.geographical_feature_categoryStratigraphyGeologyLandslideMassifCretaceousConglomeratePaleontologyVolcanoFaciesSedimentary rockGeomorphologyLithificationGeologySedimentary Geology
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Concreções calcárias da formação Santana, bacia do Araripe: uma proposta de classificação.

2007

18 pages; The calcareous concretions of the Santana Formation have been known since 1800 thanks to the work of João da Silva Feijó (1800). Their study was promoted internationally by the report of von Spix and von Martius (1823-1831), and their richness in fossil fishes led Silva Santos to name them “ichthyoliths” in 1950. Here we propose a classification for the various types of calcareous concretions that occurred in the Santana Formation (Late Cretaceous, Araripe Basin). We consider their geographic distribution and we propose a terminological uniformization for the descriptions of that material. This will serve future statistical, geographical, geochemical and taphonomical studies that,…

ichthyolithSantana FormationLate Cretaceousmacrofossils[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphysyngenetic carbonate concretions[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Preliminary study on the unusual properties in the habitat of Ranunculetum baudotii in Central Europe

2011

Abstract The study examines the patches of the saltwater association Ranunculetum baudotii in a new, atypical site; i.e., located more than 400 km away from the Baltic coastal line. They were found in a karst spring, and were the first locality of the community identified in Poland. The water and sediments within the patches were analyzed chemically in the laboratory, but, conductivity, water temperature and O2 content were measured in the field. The spring was determined to be a relatively stable aquatic habitat, with a typical chemical composition of subterranean water (a prevalence of hydro-carbonate, calcium and magnesium ions), and rich, e.g., in nitrogen and phosphorus, and disturbed …

karst springQH301-705.5BiologyGeneral Biochemistry Genetics and Molecular BiologyAquatic plantSpring (hydrology)ecological conditionsKarst springBiology (General)Magnesium ionbiodiversitygeographygeography.geographical_feature_categoryGeneral Immunology and Microbiologybatrachium baudotiiEcologyGeneral NeurosciencePlant communityKarstthreatened plant communitiesCretaceousHabitatphytocoenosesanthropopressureGeneral Agricultural and Biological Sciencesaquatic vegetationOpen Life Sciences
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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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The late Late Albian (Mortoniceras fallax Zone) cephalopod fauna from the Bracquegnies formation at Strépy-Thieu (Hainaut, southern Belgium).

2016

Excavations in 1989-1990 for the construction of a boat lift near the villages of Strépy and Thieu, east of Mons (province of Hainaut, southern Belgium), exposed a 40-metre section of the Bracquegnies Formation (Haine Green Sandstone Group; the ‘Meule de Bracquegnies’ of previous authors). Several hundred well-preserved, silicified cephalopods were collected from between 15 and 35 metres above the base of the sequence temporarily exposed there. The fauna is: Eutrephoceras clementianum (d’Orbigny, 1840), Puzosia (Puzosia) mayoriana (d’Orbigny, 1841), Callihoplites tetragonus (Seeley, 1865), Discohoplites valbonnensis valbonnensis (Hébert & Munier-Chalmas, 1875), Cantabrigites cantabrigense S…

nautiloidstaxonomyAmmonitesAmmonoidea[SDV.BID.SPT] Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyNautiloidea[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAlbiantaxonomy.Cretaceous[ SDV.BID.SPT ] Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomy[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
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