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A. B. Herman 《Stratigraphy and Geological Correlation》2007,15(4):373-384
The Albian-Paleocene phytostratigraphic scheme suggested in this work for the North Alaska Subregion of the North Pacific differs from the previous ones and includes three phytostratigraphic horizons of subregional extent and four plant-bearing beds. The scheme is based on distinguished successive stages in flora evolution, being substantiated by comprehensive data on the described floral (plant macrofossils) assemblages. As is established, sedimentation environments gradually changed during the Albian-Paleogene from the west of the subregion to the east so that the marine sedimentation and accumulation of sediments in general terminated in eastern areas later than western ones. 相似文献
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A. B. Herman 《Stratigraphy and Geological Correlation》2007,15(5):516-524
Floras characterizing comparable evolutionary stages in the Anadyr-Koryak and North Alaska subregions of the North Pacific show some essential distinctions despite their similarity in general. Factors responsible for appearance of their distinctive features were most likely the paleoclimatic difference between the subregions and the constrained or even interrupted trans-Beringia migration of plants in particular intervals of geological history. Floras of both subregions survived the Cretaceous-Paleogene boundary crisis without essential consequences for their evolution, and amplitude of floristic changes across the boundary was not greater than by evolutionary changes in the crisis-free Late Cretaceous. Evolution of the North Pacific floras near this boundary has been likely controlled by the long-term paleogeographic and paleoclimatic changes and by plants evolution and migration. 相似文献
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N. K. Mogutcheva 《Stratigraphy and Geological Correlation》2009,17(3):283-290
Paleofloral and palynological records of Lower Jurassic sediments in West Siberia, Kuznetsk (Kuzbass), and Kansk-Achinsk basins and their correlation are discussed. In a number of recent papers dedicated to the Jurassic stratigraphy of Siberia this problem is ambiguously treated. The reference palynological scale has been developed for the Jurassic West Siberian sediments and an uninterrupted succession of floral assemblages associated with it and with regional stratigraphic units has been recognized. On this basis the scheme of the correlation between the Lower Jurassic sediments of the Kansk-Achinsk and Kuznetsk basins and West Siberia permitting a better age estimate of coal-bearing deposits, is proposed. 相似文献
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A. B. Herman 《Stratigraphy and Geological Correlation》2007,15(3):321-332
A high-resolution phytostratigraphic scheme based on plant macrofossils is suggested for the first time for the Albian and Upper Cretaceous of the Anadyr-Koryak Subregion of the North Pacific. Seven phytostratigraphic horizons of the subregion are distinguished based on successive stages in flora evolution substantiated by comprehensive data on described floral assemblages. 相似文献
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V. F. Belyi 《Stratigraphy and Geological Correlation》2008,16(6):639-649
The working stratigraphic chart accepted for the Okhotsk-Chukotsk Volcanogenic Belt (OCVB) at the 3rd Interdepartmental Regional Stratigraphic Conference (IRSC) integrated data of the medium-scale geological survey, the established succession of endemic floras of the developing volcanic highland, and the results of palynological and magnetostratigraphic study (Resolutions of the 3rd…, 2003). The OCVB was formed during the middle Albian-Santonian (and initial Campanian probably). Sequences of the belt are attributed to the Buor-Kemyus (early-middle Albian), Arman (late Albian), Amka (Cenomanian), and Arkagala (Turonian-Santonian) phytostratigraphic horizons. The lack of data on relations between the horizons and fauna-bearing marine deposits is a serious obstacle for correlation of regional subdivisions with the general stratigraphic scale. The problem can be solved using geological methods of palynological and tephrochronological research. Isotopic ages of the OCVB rocks were determined applying the K-Ar and Rb-Sr isotopic dating in the early period and the Ar-Ar and U-Pb (SHRIMP) methods in recent years. The subdivision scheme of the OCVB volcanics based on the K-Ar relict and Rb-Sr isochron dates, which is accepted as addendum to the working stratigraphic chart, confirms in general the geological inferences concerning the OCVB age. The Ar-Ar and U-Pb dates (less than 100 determinations in total) obtained for the Okhotsk, Central Chukotsk, and Anadyr sectors of the OCVB external zone provoked opinions that the belt age should be radically revised. Analysis of new isotopic dates showed that they contradict in variable extent to geological data on the Okhotsk and Central Chukotsk sectors, whereas there is no significant discordance between isotopic and geological data on the Anadyr sector. Consequently, it can be empirically concluded that geological factors influenced the isotopic systems (“clock”). There is also a considerable discordance between the Ar-Ar and U-Pb isotopic dates. These uncertainties of the isotopic dating imply prematurity of idea to revise age of the OCVB. 相似文献
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