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A suite of early Eocene (～ 55 Ma) climate model boundary conditions
model boundary conditions early Eocene
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2014/12/19
We describe a set of early Eocene (～ 55 Ma)
climate model boundary conditions constructed in a selfconsistent reference frame and incorporating recent data and
methodologies. Given the growing need ...
A Paleoclimate Modeling Experiment to Calculate the Soil Carbon Respiration Flux for the Paleocene-Eocene Thermal Maximum
A Paleoclimate Modeling Experiment Calculate the Soil Carbon Respiration Flux the Paleocene-Eocene Thermal Maximum
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2014/10/21
The Paleocene-Eocene Thermal Maximum (PETM) (55 million years ago) stands as the largest in a series of extreme warming (hyperthermal) climatic events, which are analogous to the modern day increase i...
Mineralogic Characterization and Petroleum Potential of Clays (Shales) of the N’Kappa Formation (Paléocene-Eocene) in the Douala Sedimentary Sub-basin (South-West Cameroon)
Mineralogy Organic Matter Petroleum Potential
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2013/3/11
The aim of this research work was to report a facies analysis of the N’Kappa formation, identified the clay minerals present in those facies and evaluate their oil potential. For that to be done, Lith...
Foraminiferal Biostratigraphy and Palaeoenvironmental Reconstruction of the Paleocene–Eocene Transition at the Kharrouba Section, Tunisia (Southern Tethys Margin)
benthic foraminifera palaeobathymetry Paleocene-Eocene agglutinated Southern Tethys margin
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2010/10/14
At Kharrouba (near Tunis City in northern Tunisia), on the southern margin of the Tethyan realm, the Paleocene-Eocene (P-E) transition interval deposition is continuous and complete. Based on high-res...
Stratigraphy and Larger Foraminifera of the Eocene Shallow-marine and Olistostromal Units of the Southern Part of the Thrace Basin, NW Turkey
southern Thrace benthic foraminifera biometry taxonomy biostratigraphy
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2010/10/14
The Eocene marine sequence in the southern part of the Thrace Basin (NW Turkey) involves a variety of platform and deep-marine olistostromal units, the stratigraphy of which have been vigorously debat...
Basement Types, Lower Eocene Series, Upper Eocene Olistostromes and the Initiation of the Southern Thrace Basin, NW Turkey
Thrace Basin Circum-Rhodope belt olistostrome mass flows ophiolitic mélange
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2010/10/14
The Eocene sequence of the southern Thrace Basin unconformably overlies two types of basement: (1) Slate, limestone and phyllite crop out in small inliers under the Upper Eocene conglomerates and lime...
Campanian–Early Eocene Stratigraphy of the Southern Galala Plateau,Eastern Desert,Egypt
Larger foraminifera Campanian–Early Eocene Southern Galala Plateau Eastern Desert Egypt
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2009/12/8
Several species of larger foraminifera have been recorded in the Campanian–Early Eocene succession of the Southern Galala Plateau. These species include Orbitoides media (ARCHIAC), Omphalocyclus macro...
Decastronema barattoloi (DE CASTRO),characteristic fossil of the Palaeocene and the Eocene peritidal sediments from the Adriatic carbonate platform
Decastronema barattoloi Adriatic Carbonate Platform Palaeocene Eocene peritidal environment
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2009/12/7
The renewed deposition in the Palaeogene and the oldest part of the non-interrupted Palaeocene succession is characterized by the presence of Decastronema barattoloi (DE CASTRO), cyanobacterial tubes ...
Subduction-related Eocene shoshonites from the Cenozoic Urumieh-Dokhrat magmatic arc (Qaleh-Khargooshi area,West of the Yazd province,Iran)
shoshonite Eocene Urumieh-Dokhtar Qaleh-Khargooshi Iran
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2010/1/11
The fifth phase of Eocene volcanism in the central part of the Urumieh-Dokhtar magmatic arc (UDMA), comprises lavas with shoshonitic characteristics, ranging from trachybasalt to trachydacite. In shos...