Results 31 to 40 of about 3,719 (167)
Upper cretaceous magmatic suites of the Timok magmatic complex [PDF]
Geološki Anali Balkanskoga Poluostrva, 2010 The Upper Cretaceous Timok Magmatic Complex (TMC) developed on a continental crust composed of different types of Proterozoic to Lower Cretaceous rocks. The TMC consists of the magmatic suites: Timok andesite (AT) - Turonian-Santonian, Metovnica
Banješević Miodrag
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Neomeris mokragorensis sp. Nov. (Calcareous alga, Dasycladales) from the cretaceous of Serbia, Montenegro and the Northern calcareous Alps, (Gosau group, Austria) [PDF]
Geološki Anali Balkanskoga Poluostrva, 2007 The new species of the genus Neomeris - Neomeris mokragorensis sp. nov. described in this paper from western Serbia originates: from the Albian of Mokra Gora (the succession transgrading on the serpentinite) and from the Turonian of the Skrapež-Kosjerić ...
Radoičić Rajka, Schlagintweit Felix
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, 2023 The Oceanic Anoxic Event 3 (Coniacian-Santonian): paleoceanographic changes and plankton response - Miniati F.
IODP-ITALIA Commissione IODP-Italia - Commissione per il coordinamento della partecipazione italiana all'International Ocean Discovery Program (IODP) (3130239)
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Acta Palaeontologica Polonica25 years ago, a diverse vertebrate assemblage was discovered at the famous Santonian (Upper Cretaceous) Iharkút fossil locality (Bakony Mts, western Hungary). Fishes, among them members of the order Pycnodontiformes have been important components of this
Márton Szabó, John J. Cawley
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Geologica Acta, 2020 The Llert syncline is located in the South-central Pyrenees, between the eastern termination of the EW-trending Cotiella Basin and the north-western limb of the NS-trending Turbón-Serrado fold system.
A. Ramos +4 more
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Chukhonastovka – the reference section of the Turonian-Lower Santonian from the Volga-Ilovlya interfluve (the Volga right bank area near Volgograd). Paper 2. Characteristics of the Oryctocomplexes [PDF]
Известия Саратовского университета. Новая серия: Серия Науки о ЗемлеA representative complex of the Turonian-Santonian carbonate-producing invertebrates has been revealed. It comprised benthic foraminifers, diverse echinoderms, brachiopods, calcareous and siliceous sponges.
Pervushov, Evgeniy Mikhaylovich +4 more
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"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
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The Anatomical Record, EarlyView.Abstract Studies investigating paleopathologies in sauropods remain scarce despite their relative abundance in the fossil record. In this study we report new occurrence of paleopathological features, corresponding to a neoplasm found in a middle caudal vertebra (MCT.R.2120) of an advanced titanosaur from the Presidente Prudente Formation (Bauru Basin ...
Maria Luiza Peres Bertolossi +5 more
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(Appendix A) Carbon chemistry for Albian-Santonian black shale sequences at ODP Site 207-1258
, 2006 (Appendix A) Carbon chemistry for Albian-Santonian black shale sequences at ODP Site 207 ...
Forster, Astrid +5 more
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Integrative Zoology, EarlyView.This study reports two isolated feather fossils from the Lower Cretaceous Dabeigou Formation in northeastern China. Morphological analyses identified them as the earliest known feathered theropods (potentially including avian) in the Jehol Biota. This finding reveals a complex ecosystem at the dawn of the Jehol Biota, bridging the temporal and faunal ...
Qian Wu +2 more
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