Results 11 to 20 of about 149 (137)
The Neogene series of Samos Island show a complex succession of continental depositional environments. Saline lakes suggest episodic ingressions of marine‐related water or groundwater inflows. Climate is the main controlling factor on the depositional record of Samos and neighbouring regions.
Youri Hamon +8 more
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Middle Jurassic multi‐scale transgressive–regressive cycles: An example from the Lusitanian Basin
Middle Jurassic multi‐scale transgressive–regressive cycles were recognised in the Central Lusitanian Basin, Portugal. New data from calcareous nannofossils and dinoflagellate assemblages constrained the Bathonian–early Callovian age for the studied interval, thus filling the gap of the Middle Jurassic in the Central Lusitanian Basin. Using descriptive
Antonio J. C. Magalhães +15 more
wiley +1 more source
Palaeoenvironmental study and sequence stratigraphy of Sanghaneh Formation in Qalehjegh section (North of Bojnord) using organic matter contents of the rock unit [PDF]
Introduction Kopeh-Dagh basin is located northeast of Iran and in this basin the sedimentary beds began from middle Jurassic. The Sanghaneh Formation is one of the lower Cretaceous rock units in sections.
Hossein Kazemi, Ebrahim Ghasemi-Nejad
doaj +1 more source
The focus of this contribution is on laminated microbial deposits in fluvial and lacustrine carbonate environments, in particular stromatolites and oncolites, and their relationships with other lithofacies, as tools to gather varied information, primarily environmental (i.e.
Concha Arenas‐Abad
wiley +1 more source
The Lapis Tiburtinus travertine developed in a system of sub‐basins with subaqueous conditions interconnected by a hydrographic network controlled through time by fluctuations of the Aniene River base level Abstract 3D modelling is a fundamental tool to visualize and understand the history of sedimentary basin filling and to reconstruct the geobody ...
Alessandro Mancini +3 more
wiley +1 more source
ABSTRACT Marine Oxygen Isotope Stage 11 (MIS 11, Hoxnian Interglacial) is an important interval for understanding both climate change in an interglacial partially analogous to the Holocene and the response of geomorphic processes, biotic systems, and hominin populations to these changes. In Britain, many sites correlated to MIS 11 have not been studied
J. E. Sherriff +4 more
wiley +1 more source
The aim of this study was to propose an integrated workflow to quantify detrital input into autochthonous lacustrine deposits in terms of regional extent and total organic carbon (TOC) content. This workflow includes (a) organic geochemical data such as Rock Eval data together with quantitative palynofacies assessment and (b) palaeogeographical maps ...
Françoise Behar +2 more
wiley +1 more source
A study method based on characterization of palynofacies (organic matter, palynomorphs) preserved in sediments was applied to obtain information about past environments of Sardinian sites. Organic matter (OM) was classified in ten categories according to
PAOLA PITTAU +2 more
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The cuttings from the Jurassic Naokelekan Formation have been studied in the oil exploratory Binari-Serwan-1 Well in Dokan Town, Iraqi Kurdistan Region, NE Iraq.
Rzger A. Abdula +4 more
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Late Paleocene CO2 drawdown, climatic cooling and terrestrial denudation in the southwest Pacific [PDF]
Late Paleocene deposition of an organic-rich sedimentary facies on the continental shelf and slope of New Zealand and eastern Australia has been linked to short-lived climatic cooling and terrestrial denudation following sea level fall.
C. J. Hollis +11 more
doaj +1 more source

