Results 11 to 20 of about 2,224 (123)
Dinosaur footprints in the Upper Turonian-Coniacian limestone in the Krnica Bay (NE Istria, Croatia)
Geologija, 2003 Three isolated footprints and one trackway that can be attributed to bipedal dinosaur, from a limestone bed in vicinity of Požara promontory, Krnica Bay, are described. According to the stratigraphic position the footprints are late Turonian to Coniacian
Alenka Mauko, Borut Florjančič
doaj +1 more source
Palynostratigraphy of the late Cretaceous (Coniacian) magothy formation of Delaware and Maryland
, 2022 McLaughlin, Peter P., Jr.This study examines the palynostratigraphy of the Magothy Formation in the Northern Delmarva Peninsula with the objectives of correlation with the Magothy Formation of New Jersey; documentation of palynomorphs within this ...
Norville, Robert Caleb
core +1 more source
Acta Palaeobotanica, 2019 The Ul’ya flora comes from the Amka Formation of the Ul’ya Depression, located in the Okhotsk–Chukotka volcanic belt (North-East Russia). This flora includes ~50 species, among which conifers predominate. Ferns and angiosperms are also diverse. The Ul’ya
VYACHESLAV V. AKININ +5 more
doaj +1 more source
BSGF - Earth Sciences Bulletin, 2020 Many Cretaceous asymmetrical rhynchonellid brachiopods (Brachiopoda, Rhynchonellida) have long been considered as Rhynchonella difformis (Valenciennes in Lamarck, 1819).
Gaspard Danièle, Charbonnier Sylvain
doaj +1 more source
Lithostratigraphy, depositional history and sea level changes of the Cauvery Basin, southern India [PDF]
Geološki Anali Balkanskoga Poluostrva, 2003 The sedimentary sequence exposed in the erstwhile Tiruchirapalli district hosts a more or less complete geological record of the Upper Cretaceous-Tertiary period.
Muthuvairvasamy Ramkumar +2 more
doaj +1 more source
Rivista Italiana di Paleontologia e Stratigrafia, 2017 The Cenomanian-Coniacian units of the Capriolo - Corno Pendita area belong to the eastern margin of the Lombardy Basin. The Coniacian turbidite sandstone lithosome (Arenarie di Sarnico) unconformably overlies the Cenomanian-Turonian units.
R. BERSEZIO, L. MENSINI
doaj +1 more source
"OAE 3" – regional Atlantic organic carbon burial during the Coniacian–Santonian [PDF]
Climate of the Past, 2012 The Coniacian–Santonian time interval is the inferred time of oceanic anoxic event 3 (OAE 3), the last of the Cretaceous OAEs. A detailed look on the temporal and spatial distribution of organic-rich deposits attributed to OAE 3 suggests that black shale
M. Wagreich
doaj +1 more source
Biostratigraphy, microfacies, sedimentary environments of the Gurpi and Amiran formations in the Gerdbisheh section, High Zagros [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2023 Biostratigraphy, microfacies and depositional environments of the Upper Cretaceous deposits (Gurpi and Amiran formations) were carried out in the Gerdbisheh section.
Yadolah Ezampanah +2 more
doaj +1 more source
Turonian-Coniacian (Upper Cretaceous) of the Babadag Basin (North Dobrogea, Romania) : integrated biostratigraphy and microfacies succession [PDF]
, 2019 The Upper Turonian to Middle Coniacian (Upper Cretaceous) succession of the Babadag Basin (North Dobrogea, Romania) constitutes an apparently continuous fossiliferous carbonate succession.
Lodowski, Damian +4 more
core +1 more source
Journal of Hydrology: Regional Studies, 2018 Study region: The Turonian-Coniacian aquifer system in the North of the Coastal Sedimentary Basin, southern Benin, West Africa. Study focus: The Turonian-Coniacian aquifer is the major aquifer in southern Benin and is the main source of water supply for ...
Kodjo Apelete Raoul Kpegli +4 more
doaj +1 more source