Temat: miospores - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Remarks on palynostratigraphy of the Namurian Wałbrzych Formation in the northern part of the Intrasudetic Basin (SW Poland)
Autorzy:: Górecka-Nowak, A.
Majewska, M.
Powiązania:: https://bibliotekanauki.pl/articles/2059926.pdf
Data publikacji:: 2002
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Instrasudetic Basin
Namurian
palynostratigraphy
miospores
Opis:: Rich assemblages of the Namurian miospores were recorded in the deposits of the Wałbrzych Formation from the northern part of the Intrasudetic Basin. One hundred twenty five miospore taxa were determined and two miospore zones were distinguished. Deposits from Konradów and Biały Kamień belong to the Stenozonotriletes triangulus-Rotaspora knoxi (TK) Zone, correlated to the middle Namurian A. Deposits from Szczawno Zdrój appeared to be younger, because they represents the Lycospora subtriquetra-Kraeuselisporites ornatus (SO) Zone (late Namurian A).
Źródło:: Geological Quarterly; 2002, 46, 2; 101-116
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Age revision of Carboniferous rocks in the northern part of the Intra-Sudetic Basin (SW Poland) based on miospore data
Autorzy:: Górecka-Nowak, Anna
Jankowska, Adrianna
Muszer, Jolanta
Powiązania:: https://bibliotekanauki.pl/articles/2058777.pdf
Data publikacji:: 2021
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: miospores
palynostratigraphy
Serpukhovian
Bashkirian
Namurian
Intra-Sudetic Basin
Opis:: Palynostratigraphic studies of the Carboniferous strata of the Szczawno and Wałbrzych formations, outcropping in the vicinity of Wałbrzych in the northern part of the Intra-Sudetic Basin, are reported. Rocks of the Szczawno Formation in a section near Konradów had earlier been assigned to the Upper Visean, while rocks of the Wałbrzych Formation in the Biały Kamień section were included to the Lower Namurian [the Stenozonotriletes triangulus–Rotaspora knoxi (TK) Miospore Zone]. This study describes abundant palynological material with many taxonomically diverse miospore assemblages from these rocks, allowing precise palynostratigraphic conclusions. These showed that the rocks of the Szczawno Formation studied should be referred to the lower part of the Serpukhovian [Verrucosisporites morulatus (Vm) Subzone], correlated with the lowest Namurian, while rocks of the Wałbrzych Formation from Biały Kamień belong to the Lower Bashkirian [Lycospora subtriquetra–Cirratriradites rarus (SR) Subzone], correlated with the Upper Namurian A. These results indicate that the rocks from both sections studied are younger than they were earlier believed. This revises the age of the Szczawno and Wałbrzych formations in the northern part of the Intra-Sudetic Basin which belong to four miospore zones, from Vm to SR, corresponding to the Serpukhovian and lowermost Bashkirian (Namurian A corresponding to the Pendleian to Alportian of British chronostratigraphy).
Źródło:: Geological Quarterly; 2021, 65, 1; 8
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: A record of climatic changes in the Triassic palynological spectra from Poland
Autorzy:: Fijałkowska-Mader, A.
Powiązania:: https://bibliotekanauki.pl/articles/2059985.pdf
Data publikacji:: 2015
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: miospores
climate
Triassic
palyno-palaeoclimatic model
PPC
Opis:: Based on quantitative and qualitative analyses of the Triassic miospores assemblages from different regions of Poland climatic changes have been documented. Analyzed material came from the published and archival works of Orłowska-Zwolińska and author and comprised ten palynological zones distinguished in the Triassic of Poland. Two different palynological methods were applied in this study – PPC model and SEG model – to obtain palaeoclimatic and palaeoenvironmetal data. Xerophytic elements (spores and pollen grains of xerophytic plants), reflecting mainly dry climate conditions, dominated in the palynomorph spectra of the Triassic deposits from Poland. Significant numbers of hygrophytic elements indicating temporary more humid phases occurred in the late Olenekian, Ladinian, the middle Carnian, late Norian and the Rhaetian.
Źródło:: Geological Quarterly; 2015, 59, 4; 615--653
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Palynostratigraphy of the Culm deposits of the Moravian-Silesian zone (Poland) at Toszek Castle Hill
Autorzy:: Trzepierczyńska, A.
Powiązania:: https://bibliotekanauki.pl/articles/2058834.pdf
Data publikacji:: 2003
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Moravian–Silesian zone
Culm
flysch
palynostratigraphy
miospores
Serpukhovian
Opis:: The Early Carboniferous age of the flysch succession in the Moravian-Silesian zone has been based principally on lithological correlations with the stratotype goniatite-bearing section. Its uppermost part-the Kyjovice Formation in the region of Toszek (Poland)-has been studied palynologically for the first time. Miospore assemblages of the upper part of the Western European nitidus-carnosus (NC) miospore Zone of the early Serpukhovian have been distinguished. This agrees well with a general stratigraphic range of the Kyjovice Formation within the Go-E1a goniatite zones.
Źródło:: Geological Quarterly; 2003, 47, 4; 373-380
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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