Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian …

HC Jenkyns, AJ Dickson, M Ruhl… - …, 2017 - Wiley Online Library
Abstract Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major
palaeoceanographic phenomenon that took place during an interval of extreme global …

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 …

Sea-level change, carbon cycling and palaeoclimate during the Late Cenomanian of northwest Europe; an integrated palaeoenvironmental analysis

S Voigt, AS Gale, T Voigt - Cretaceous research, 2006 - Elsevier
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 …

Assessing the educational potential of geosites: Introducing a method using inquiry-based learning

E Drápela - Resources, 2022 - mdpi.com
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 …

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 …

Intercontinental correlation of organic carbon and carbonate stable isotope records: evidence of climate and sea‐level change during the Turonian (Cretaceous)

I Jarvis, J Trabucho‐Alexandre… - The Depositional …, 2015 - Wiley Online Library
Abstract Carbon (δ13Corg, δ13Ccarb) and oxygen (δ18Ocarb) isotope records are
presented for an expanded Upper Cretaceous (Turonian–Coniacian) hemipelagic …

Calcareous nannofossils of the Cenomanian/Turonian boundary interval from the Boreal Realm (Wunstorf, northwest Germany)

C Linnert, J Mutterlose, J Erbacher - Marine Micropaleontology, 2010 - Elsevier
The Cenomanian/Turonian boundary interval (CTBI) is marked by an intense climatic
warming presumably caused by large magmatic eruptions. This warming was characterised …

Calcareous nannofossils from Eastbourne (southeastern England) and the paleoceanography of the Cenomanian–Turonian boundary interval

C Linnert, J MUTTERLOSE, R Mortimore - Palaios, 2011 - pubs.geoscienceworld.org
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) …

[HTML][HTML] Changes in bivalve assemblages at the onset of the OAE2 event in the Peri-Tethyan area (Bohemian Cretaceous Basin)

L Kunstmüllerová, M Košťák - Cretaceous Research, 2024 - Elsevier
Abstract The Ocean Anoxic Event (OAE2) at the Cenomanian-Turonian boundary presents a
unique record of gradual global warming and its effects on benthic organisms. The present …

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 …