Palaeoclimate perturbations before the Sheinwoodian glaciation: A trigger for extinctions during the 'Ireviken Event'

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F10%3A00000355" target="_blank" >RIV/00025798:_____/10:00000355 - isvavai.cz</a>
Alternative codes found
RIV/60460709:41330/10:47494
Result on the web
—
DOI - Digital Object Identifier
—

Result language
angličtina
Original language name
Palaeoclimate perturbations before the Sheinwoodian glaciation: A trigger for extinctions during the 'Ireviken Event'
Original language description
Our data suggest that faunal extinctions are connected to time intervals of warming before the establishment of more stable and cooler conditions during the main Sheinwoodian glacial. The most severe extinctions and faunal turnovers at datum points 2 and4 occurred during the early, warmer interval of the event. After the shift into the Sheinwoodian icehouse in the Lower Kockelella ranuliformis Zone, reflected by rapidly decreasing sea?water temperatures, faunas restabilized and reefal communities started to flourish. Sedimentary evidence for the glaciation is discussed for different palaeolatitudes.
Czech name
—
Czech description
—

Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
—

Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2010
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Similar results(10)