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Foraminiferal proliferations in the Alborz Basin (northern Iran): global responses to Early Carboniferous glaciations
Abadi M., Kulagina E., Voeten D.
shift of subtropical and temperate taxa to tropical latitudes in response to the glaciations
Sedimentologic and paleoclimatic reconstructions of carbonate factory evolution in the Alborz Basin (northern Iran) indicate a global response to Early Carboniferous (Tournaisian) glaciations
Sardar Abadi M., Kulagina E., Voeten D., Boulvain F., Da Silva A.
© 2016 Elsevier B.V.The Lower Carboniferous Mobarak Formation records the development of a storm
Foraminiferal proliferations in the Alborz Basin (northern Iran): global responses to Early Carboniferous glaciations
Abadi M., Kulagina E., Voeten D.
shift of subtropical and temperate taxa to tropical latitudes in response to the glaciations
Sedimentologic and paleoclimatic reconstructions of carbonate factory evolution in the Alborz Basin (northern Iran) indicate a global response to Early Carboniferous (Tournaisian) glaciations
Sardar Abadi M., Kulagina E., Voeten D., Boulvain F., Da Silva A.
© 2016 Elsevier B.V.The Lower Carboniferous Mobarak Formation records the development of a storm
Scarce ctenacanthiform sharks from the Mississippian of Austria with an analysis of Carboniferous elasmobranch diversity in response to climatic and environmental changes
Feichtinger I., Ivanov A.O., Winkler V., Dojen C., Kindlimann R., Kriwet J., Pfaff C., Schraut G., Stumpf S.
The Carboniferous is characterized by drastic climatic and environmental fluctuations, which
The formation of the Alleghenian Isthmus triggered the Bashkirian glaciation: Constraints from warm-water benthic foraminifera
Davydov V., Cózar P.
and the onset of the Bashkirian glaciation.
Palaeobiogeography and diversification of Tournaisian-Viséan bryozoans (lower-middle Mississippian, Carboniferous) from Eurasia
Tolokonnikova Z., Ernst A., Wyse Jackson P.
, Carboniferous) from Eurasia
The Dzerzhinka Section (eastern slope of the South Urals): An overview of the fauna and facies around the Devonian-Carboniferous boundary
Gatovsky Y., Nikolaeva S., Gorozhanina E., Kulagina E., Gorozhanin V., Alekseev A., Mizens A., Mizens L.
TheDevonian-Carboniferous boundary section near the village of Dzerzhinka (vicinity of
Paleogeographic causes of the formation of mineral deposits on the east of the East European platform in the Permian period
Khasanov R., Balabanov Y.
of ore and nonmetallic minerals are global climatic changes caused by Carboniferous-Permian glaciation.
Oldest known naiaditid bivalve from the high-latitude Late Devonian (Famennian) of South Africa offers clues to survival strategies following the Hangenberg mass extinction
Scholze F., Gess R.
Supergroup) was studied and compared with known Carboniferous examples. For the first time, Devonian bivalves

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