Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian …
Abstract Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major
palaeoceanographic phenomenon that took place during an interval of extreme global …
palaeoceanographic phenomenon that took place during an interval of extreme global …
Sea-level change, carbon cycling and palaeoclimate during the Late Cenomanian of northwest Europe; an integrated palaeoenvironmental analysis
A new high resolution sea-level curve for the Late Cenomanian M. geslinianum Zone has
been generated using sequence stratigraphic analysis on transects through the margins of …
been generated using sequence stratigraphic analysis on transects through the margins of …
[HTML][HTML] Assessing the educational potential of geosites: Introducing a method using inquiry-based learning
Geosites are suitable locations for field teaching of Earth sciences. However, their
educational potential does not always correlate with the scientific significance of geosites, as …
educational potential does not always correlate with the scientific significance of geosites, as …
Cretaceous
S Voigt, M Wagreich, F Surlyk, I Walaszczyk, D Uličný… - 2008 - pubs.geoscienceworld.org
Abstract During the Cretaceous (145.5-65.5 Ma; Gradstein et al. 2004). Central Europe was
part of the European continental plate, which was bordered by the North Atlantic ocean and …
part of the European continental plate, which was bordered by the North Atlantic ocean and …
Intercontinental correlation of organic carbon and carbonate stable isotope records: evidence of climate and sea‐level change during the Turonian (Cretaceous)
Abstract Carbon (δ13Corg, δ13Ccarb) and oxygen (δ18Ocarb) isotope records are
presented for an expanded Upper Cretaceous (Turonian–Coniacian) hemipelagic …
presented for an expanded Upper Cretaceous (Turonian–Coniacian) hemipelagic …
The geology of central Europe: Mesozoic and Cenozoic
T McCann - 2008 - books.google.com
Volume 2 provides an overview of the Mesozoic and Cenozoic evolution of Central Europe.
This period commenced with the destruction of Pangaea and ended with the formation of the …
This period commenced with the destruction of Pangaea and ended with the formation of the …
Calcareous nannofossils of the Cenomanian/Turonian boundary interval from the Boreal Realm (Wunstorf, northwest Germany)
The Cenomanian/Turonian boundary interval (CTBI) is marked by an intense climatic
warming presumably caused by large magmatic eruptions. This warming was characterised …
warming presumably caused by large magmatic eruptions. This warming was characterised …
Ammonites, inoceramids and stable carbon isotopes of the Cenomanian–Turonian OAE2 interval in central Europe: Pecínov quarry, Bohemian Cretaceous Basin …
M Košťák, S Čech, D Uličný, J Sklenář, B Ekrt… - Cretaceous …, 2018 - Elsevier
In a well-exposed succession of Cenomanian through lower Turonian strata at Pecínov
(Bohemian Cretaceous Basin, Czech Republic), a detailed study of ammonite and …
(Bohemian Cretaceous Basin, Czech Republic), a detailed study of ammonite and …
Palaeogeography and stratigraphy of the Bohemian Cretaceous Basin (Czech Republic)–an overview
S Čech - Geologické výzkumy (na Moravě a ve Slezsku), 2011 - journals.muni.cz
Palaeogeographically, the area of the present day Bohemian Cretaceous Basin (BCB)
formed a narrow Seaway between the North Sea Basin and the Tethys Ocean during the …
formed a narrow Seaway between the North Sea Basin and the Tethys Ocean during the …
Calcareous nannofossils from Eastbourne (southeastern England) and the paleoceanography of the Cenomanian–Turonian boundary interval
Abstract The Cenomanian–Turonian (C–T) boundary interval is marked by one of the most
prominent perturbations of the Mesozoic carbon cycle, Oceanic Anoxic Event 2 (OAE2) …
prominent perturbations of the Mesozoic carbon cycle, Oceanic Anoxic Event 2 (OAE2) …