The Cenomanian/Turonian boundary interval deep-sea deposits in the Zagros Basin (SW Iran): Bioevents, carbon isotope record and palaeoceanographic model
B Kalanat, H Vaziri-Moghaddam - Palaeogeography, palaeoclimatology …, 2019 - Elsevier
Abstract The Cenomanian/Turonian (C/T) boundary interval, spanning the upper part of the
Sarvak Formation in the Zagros Basin (Izeh Zone), has been studied to determine the timing …
Sarvak Formation in the Zagros Basin (Izeh Zone), has been studied to determine the timing …
The 'Black Band': local expression of a global event
MB Hart - Proceedings of the Yorkshire Geological Society, 2019 - lyellcollection.org
The organic-rich, black mudstones that were initially described as the Black Band in
Lincolnshire, Humberside and Yorkshire are known to be a local representation of the …
Lincolnshire, Humberside and Yorkshire are known to be a local representation of the …
Tracking the key parameters stimulating organic carbon productivity, accumulation rate and preservation based on foraminiferal proxies in the subsurface Miocene …
WA Makled, AA Abd El Ghany, SI Soliman - Marine and Petroleum Geology, 2019 - Elsevier
Productivity, redox conditions and sedimentation rate constrain the enrichments of organic
matters and under suitable conditions they can trigger larger enrichments. These …
matters and under suitable conditions they can trigger larger enrichments. These …
[HTML][HTML] Micropaleontology and systematic determination of Miscellaneidae family in the Middle Paleocene–lower Eocene deposits in the north of Zahedan, Padagi …
M Gorgij, S Shahraki Mirzaei - Journal of Stratigraphy and …, 2019 - jssr.ui.ac.ir
Abstratct Miscellaneidae are Paleogene larger index microfossils (Middle Paleocene–Early
Eocene) that are important for biozonation of shallow marine deposits. These large benthic …
Eocene) that are important for biozonation of shallow marine deposits. These large benthic …
Caractérisation géochimique des changements paléoenvironnementaux au cours de l'Évènement Océanique Anoxique 2 (~ 94 Ma) dans le Bassin Vocontien (SE …
J Danzelle - 2019 - theses.hal.science
Le passage Cénomanien-Turonien (~ 94 Ma) au Crétacé supérieur est marqué par une
période de diminution de la quantité d'O2 dans les sédiments et la colonne d'eau et de …
période de diminution de la quantité d'O2 dans les sédiments et la colonne d'eau et de …