Results 91 to 100 of about 2,731 (208)

Frasnian-Famennian low resolution organic carbon isotope data from Poland, Kowala section

open access: yes, 2017
Frasnian-Famennian low resolution organic carbon isotope data from Poland, Kowala ...
Day, James E   +15 more
core   +1 more source

Frasnian-Famennian organic carbon isotope data from Iowa, H-32 drill core

open access: yes, 2017
Frasnian-Famennian organic carbon isotope data from Iowa, H-32 drill ...
Day, James E   +15 more
core   +1 more source

Stages of development of the Middle-Late Devonian ICHTHYOFAUNA (Placodermi: Antiarchi) from the northern Eurasia

open access: yesИзвестия высших учебных заведений: Геология и разведка, 2019
Three stages, namely Middle Devonian (I), Early Late Devonian (II) and Late Late Devonian (III), are distin-guished in the evolution of antiarchs (Placodermi, Antiarchi) in the Middle-Late Devonian of Northern Eurasia.
S. V. Moloshnikov
doaj   +1 more source

Frasnian-Famennian high resolution carbon isotope data from South China, Fuhe section

open access: yes, 2017
Frasnian-Famennian high resolution carbon isotope data from South China, Fuhe ...
Day, James E   +15 more
core   +1 more source

Frasnian-Famennian high resolution carbon isotope data from Poland, Kowala section

open access: yes, 2017
Frasnian-Famennian high resolution carbon isotope data from Poland, Kowala ...
Day, James E   +15 more
core   +1 more source

Famennian (Upper Devonian) stromatolite reefs at Shatang, Guilin, Guangxi, South China

open access: yes, 2004
Stromatolites occurred in many reef complexes throughout the Phanerozoic, and microbial communities played an important role in both ancient and modern stromatolite reefs.
Webb, GE   +5 more
core   +1 more source

Late Famennian Stromatoporoids from Dębnik Anticline, Southern Poland [PDF]

open access: yesActa Palaeontologica Polonica, 2009
Famennian Stromatoporoidea from the Quasiendothyra communis Foraminiferal Zone and slightly younger strata from the Debnik anticline, southern Poland, form a succession of three consecutive assemblages. Assemblages 1 and 3 consist of representatives of the order Clathrodictyida, while assemblage 2 is dominated by the order Labechiida.
openaire   +2 more sources

Lower and Middle Famennian (Upper Devonian) conodont biostratigraphy from Compte section (Central Pyrenees, Spain) [PDF]

open access: yes
A detailed analysis of the conodont sequence in the Compte section, located in the Spanish Central Pyrenees, demonstrates an almost continuous biostratigraphical record for the Famennian sequence studied.
Valenzuela Ríos, José Ignacio   +5 more
core   +1 more source

The Frasnian-Famennian boundary in the Southern Urals [PDF]

open access: yes, 2004
On the western slope of the Southern Urals, a continuous conodont zone sequence within different facies of the Frasnian-Famennian (F-F) boundary beds is documented.
Abramova, A. N., Artyushkova, O. V.
core  

THE CAUSE OF BIOMASS EXTINCTION AT THE FRASNIAN-FAMENNIAN BOUNDARY, THE KERMAN PROVINCE SOUTHEASTERN, CENTRAL IRAN [PDF]

open access: yesJournal of Sciences, Islamic Republic of Iran, 2002
About 35 samples were collected from lower and upper parts of the proposed Frasnianamennian boundary in three sections of Upper Devonian marine sediments of the Kerman province.
doaj  

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