Agglutinated foraminifera from the Turonian–Coniacian boundary interval in Europe – paleoenvironmental remarks and stratigraphy [PDF]
Agglutinated foraminiferal assemblages of the Turonian–Coniacian from the GSSP (Global Boundary Stratotype Section and Point) of Salzgitter–Salder (Subhercynian Cretaceous Basin, Germany) and other sections, including Bielefeld–Ostwestfalendamm ...
R. M. Besen +5 more
doaj +1 more source
Late Cretaceous mega-, meso-, and microfloras from Lower Silesia [PDF]
Late Cretaceous plants from the North Sudetic Basin (Lower Silesia, south-western Poland) are reviewed on the basis of megaflora from 17 localities (270 identifiable specimens), mesoflora from two localities, and microflora from four localities.
Adam T. Halamski +4 more
doaj +1 more source
Sedimentary Mercury Enrichments as a Tracer of Large Igneous Province Volcanism
Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Lawrence M. E. Percival +3 more
wiley +2 more sources
Palynological studies on the Upper Cretaceous Wata and Matulla formations in Bakr Oil Field, Gulf of Suez, Egypt [PDF]
Palynological investigation of the subsurface Upper Cretaceous (Turonian-Santonian) Wata and Matulla formations in three wells drilled in the Bakr oilfield, Gulf of Suez area is presented.
Ali Soliman +3 more
doaj +1 more source
Biostratigraphy of Kometan Formation in Khashab Well-1, Hamrin Area, Northeastern Iraq. [PDF]
The present study deals with biostratigraphy of the Kometan from the subsurface section of Khashab well No.1, Hamrin area Northeastern Iraq. Lithologically, the studied Kometan Formation are divided into three units.
Aokab AL-jubory, Majid AL-Mutwali
doaj +1 more source
The Poigny borehole near Provins (Seine-et-Marne) provides the most complete single pristine section through the Upper Cretaceous Chalk of the Paris Basin.
Pearce, Martin A. +5 more
doaj +1 more source
The eastern part of the Sakarya Zone, known as the Eastern Pontides, is represented by a south-facing carbonate platform during the Late Jurassic-Early Cretaceous.
Merve Özyurt +2 more
doaj +1 more source
This study is a reconstruction of the Coniacian palaeogeographic and palaeoenvironmental development in the North Sudetic Basin, a synclinal trough within the Late Cretaceous Central European seaway linking the Boreal and Tethyan marine provinces.
Stanisław Leszczyński, Wojciech Nemec
doaj +1 more source
The evolution of porosity and sequence stratigraphy study of the Khasib Formation (Late Turonian-Coniacian) in two wells, in central Iraq were conducted. In the first well EB-X, the Khasib Formation sequences are confined to a depth of 2182-2285
Ezzat Al-Fandi +2 more
doaj +1 more source
The Turonian-Coniacian deposits of the south-west of the Ulyanovsk-Saratov trough
Integrated study of a series of the Turonian and Coniacian complete geological records has revealed the stratigraphic completeness and specified the faunal contents of the deposits.
E. M. Pervushov +4 more
doaj +1 more source

