Results 131 to 140 of about 351 (171)
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Palaeoworld, 2009
Abstract The Afanasievo Quarry, approximately 90 km southeast of Moscow and about 5 km southwest of Voskresensk, starts with Late Moscovian limestone of the Peski Formation, which is overlain by shallow-water carbonates of the Krevyakinian Horizon (Substage) (Suvorovo and Voskresensk formations) and the lower part of the Khamovnikian Horizon ...
Alexander S Alekseev
exaly +2 more sources
Abstract The Afanasievo Quarry, approximately 90 km southeast of Moscow and about 5 km southwest of Voskresensk, starts with Late Moscovian limestone of the Peski Formation, which is overlain by shallow-water carbonates of the Krevyakinian Horizon (Substage) (Suvorovo and Voskresensk formations) and the lower part of the Khamovnikian Horizon ...
Alexander S Alekseev
exaly +2 more sources
Brachiopods of the family Linoproductidae from the Kasimovian Stage of the Moscow Region
Paleontological Journal, 2008Brachiopods from the Kasimovian Stage of the Moscow Region that for more than 70 years were referred to the genus Linoproductus (family Linoproductidae) are revised and redescribed. New characters connected with the ornamentation and inner structure of the dorsal valve are used for the first time in the analysis of the taxonomic structure of the group.
S S Lazarev
exaly +2 more sources
“Sub-Triticites Beds” of the Donskaya Luka and lower boundary of the Kasimovian Stage
Stratigraphy and Geological Correlation, 2009Micro- and macrofauna remains were studied from transitional deposits of Moscovian and Kasimovian Stages in the Donskaya Luka (Volgograd Region). The preliminary analysis of microfauna showed that “sub-Triticites Beds” of the Donskaya Luka contain fusulinid and conodont assemblages enabling correlation of the Middle and Upper Carboniferous deposits in ...
A S Alekseev, Alekseev A S
exaly +2 more sources
Kasimovian floristic change in tropical wetlands and the Middle–Late Pennsylvanian Boundary Event
Geological Society Special Publication, 2023Abstract A threshold-like vegetational change in tropical wetlands occurred in the early Kasimovian (the US Desmoinesian–Missourian boundary) – Event 3. Two earlier significant changes occurred, first in the mid-Moscovian (Atokan–Desmoinesian; ∼Bolsovian–Asturian) – Event 1, and the second in the late Moscovian (mid-Desmoinesian; mid-Asturian)
William A Dimichele +2 more
exaly +2 more sources
New conodont species from the Kasimovian Stage (Upper Carboniferous) of Moscow and Moscow Basin
Paleontological Journal, 2006Three new conodont species, Streptognathodus neverovensis, S. isakovae, and Idiognathodus mestsherensis, which are widespread in the Kasimovian Stage of central Russia, are described.
A S Alekseev, Alekseev A S
exaly +2 more sources
Journal of Foraminiferal Research, 2000
The upper part of the Las Llacerias section shows an exceptionally complete sequence of Upper Moscovian (Myachkovsky) and Kasimovian (Krevyakinsky-Khamovnichesky) strata which yielded fusulinacean foraminifera from numerous beds throughout the succession.
Elisa Villa
exaly +2 more sources
The upper part of the Las Llacerias section shows an exceptionally complete sequence of Upper Moscovian (Myachkovsky) and Kasimovian (Krevyakinsky-Khamovnichesky) strata which yielded fusulinacean foraminifera from numerous beds throughout the succession.
Elisa Villa
exaly +2 more sources
Facies, 2003
The type upper Moscovian-basal Kasimovian argillaceous-carbonate succession of central European Russia contains regionally traced cyclothem-bounded subaerial exposure horizons (geosols) represented mainly by rendzina-type palaeosols. Palaeokarst profiles occurrarely and grade laterally to palaeosols.
Pavel Kabanov
exaly +2 more sources
The type upper Moscovian-basal Kasimovian argillaceous-carbonate succession of central European Russia contains regionally traced cyclothem-bounded subaerial exposure horizons (geosols) represented mainly by rendzina-type palaeosols. Palaeokarst profiles occurrarely and grade laterally to palaeosols.
Pavel Kabanov
exaly +2 more sources
Limuloid tracks into the Meledis Fm. (Upper Carboniferous, Kasimovian) of the Carnic Alps
The work describes the first clear evidence of Limuloid tracks discovered in Italy. The trails are impressed in a Kasimovian terrigenous sequences (Upper Carboniferous) of the Carnic Alps (Meledis Fm., Auernig Group) consisting of fine silicioclastic beds stored up in a shallow marine environment representing an outer delta front.
CONTI, Maria Alessandra +3 more
openaire +2 more sources
Moscovian–Kasimovian boundary conodont assemblages from the Kalinovo section, Donets Basin, Ukraine
Palaontologische Zeitschrift, 2022Tamara I Nemyrovska
exaly +2 more sources
A NEW GENUS AND SPECIES OF LARGE MACRODONT ACTINOPTERYGIAN FROM THE PENNSYLVANIAN (KASIMOVIAN/MISSOURIAN) ATRASADO FORMATION OF NEW MEXICO [PDF]
http://deepblue.lib.umich.edu/bitstream/2027.42/195964/1/ContributionsVol36No2_High res.pdf ; Description of ContributionsVol36No2_High res.pdf : Main ...
Friedman, Matt +6 more
openaire +3 more sources

