2 edition of Upper Jurassic-Lower Cretaceous dinoflagellate assemblages from Arctic Canada found in the catalog.
Upper Jurassic-Lower Cretaceous dinoflagellate assemblages from Arctic Canada
W. W. Brideaux
|Contributions||Fisher, M. J., Geological Survey of Canada.|
|LC Classifications||QE774D5 B7|
|The Physical Object|
|Pagination||iv, 68,  leaves,  leaves of plates :|
|Number of Pages||68|
At Ocean Drilling Program Hole C in the Southern Indian Ocean, a total of Late Cretaceous dinoflagellate taxa were encountered in 38 productive samples from Cores CR through CR ( mbsf). Four provisional dinoflagellate assemblage zones and five subzones were recognized based on the character of the. Full text of "Bulletin of the British Museum (Natural History) Geology Supplement" See other formats PRESENT TAXONOMIC ATTRIBUTIONS OF THE DINOFLAGELLATE CYSTS AND ACRITARCHS TREATED BY DAVEY, DOWNIE, SARJEANT AND WILLIAMS (, ) BY LINDA ANN KRUKEWICH AND WILLIAM ANTONY SWITHIN SARJEANT (University of Saskatchewan) PP BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) .
Multivariate analysis of Late Cretaceous Kanguk Formation (Arctic Canada) palynomorph assemblages to identify nearshore to distal marine groupings L.V. Hills Department of Geology, University of Calgary and Geophysics, University Drive NW, Calgary, AB T2N 1N4. The described scheme of the Lower Cretaceous (Berriasian-Barremian) stratigraphic subdivisions is elaborated based on palynological study of sections in the Khatanga depression, Ust-Yenisei region, Pur-Taz interfluve, and around the Ob River latitudinal segment, the North Siberia. Stratigraphic distribution of microphytoplankton studied in detail is used to distinguish 10 biostratigraphic.
(). Upper cretaceous dinoflagellate biostratigraphy of the subsurface Atlantic coastal plain of New Jersey and Delaware, U.S.A. Palynology: Vol. 13, No. 1, pp. fields in the Middle Jurassic, Upper Jurassic and Lower Cretaceous (after Brooks et al., ) 3 3 Generalised tectonic phases of the Central and Northern North Sea 4 4 Approximate extent of the ‘Mid-Cimmerian Unconformity’ due to transient domal uplift and .
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Get this from a library. Upper Jurassic-lower Cretaceous dinoflagellate assemblages from Arctic Canada. [W W Brideaux; M J Fisher].
UPPER BARREMIAN TO UPPER ALBIAN (LOWER CRETACEOUS) DINOFLAGELLATE CYST ASSEMBLAGES, CANADIAN ARCTIC ARCHIPELAGO HENRIK N0HR-HANSEN The Geological Survey of Denmark and Greenland Thoravej 8 DK Copenhagen NV Denmark. DAVID J. McINTYRE Underhill Drive N.W Calgary, Alberta T2N 4E9 Canada Abstract.
Jurassic and Lower Cretaceous palynomorph assemblages are described from the Cape Flora Section and compared with assemblages recorded from Svalbard, East Greenland and Arctic Canada. The quantitative distribution of palynomorphs and palynodebris has also been estimated.
Preservation is good, and from the six samples investigated, 41 species of dinoflagellate cysts, acritarchs, pollen. A Preliminary Dinoflagellate Zonation of the Uppermost Jurassic and Lower Part of the Cretaceous, Canadian Arctic, and Possible Correlation in the Western Canada Basin.
Taxonomic investigations of palynomorphs from the Byers Group (Upper Jurassic-Lower Cretaceous), Livingston and Snow islands, Antarctic Peninsula Palynology Palynostratigraphy at the Permian-Triassic boundary of the Amb section, Salt Range, PakistanCited by: 4.
The upper Dongrong Formation, containing Buchia fischeriana and dinoflagellate cyst assemblage Oligosphaeridium pulcherrium, can be correlated approximately with the whole of the Dong’anzhen Formation (Table 1, cols 1–2) since the index species, Buchia fischeriana, is common to both the upper Dongrong and lower Dong’anzhen formations, and the age of dinoflagellate assemblage in the upper.
Two Upper Jurassic–Lower Cretaceous palynological successions from the Qinghai-Xizang Plateau, China, are briefly introduced in this paper. The northern succession, from the Tanggula Mountains area, consists of three assemblage zones whereas the southern comprises two zones.
Upper Jurassic and Lower Cretaceous Existing Late Jurassic stratigraphy was established in when NAM and RGD published the ‘Stratigraphic Nomenclature of the Netherlands’. Van Adrichem Boogaert and Kouwe revised the standard in The palynozonation is primarily based on dinoflagellate cyst and accessory pollen.
The Cretaceous succession is divided into 15 palynozones: seven Lower Cretaceous zones and eight Upper Cretaceous. These were first formally described from the upper Albian of Kansas but have been recorded from the upper Neocomian to the Upper Cretaceous (Singh, ; Harding, ; Batten and Lister, a, b) and in the Eocene of the Mackenzie delta (G.
Dolby, personal observations). In every case, these appear to have occupied fresh to low-salinity. The Oxfordian-Kimmeridgian stage boundary (Upper Jurassic): Dinoflagellate cyst assemblages from the Harome Borehole, North Yorkshire, England ☆ Author links open overlay panel Joanna E.
Thomas Beris M. Cox. Jurassic and Lower Cretaceous palynomorph assemblages from Cape Flora, Franz Josef Land, Arctic, USSR Article (PDF Available) in Norsk Geologisk Tidsskrift January with 68 Reads.
The lower unit ( m– m; ft– ft) consists of mudstone. The upper unit is dominated by siltstone and mudstone with minor sandstone in fining upward cycles 10–15 m thick. A carbonate bed occurs at m ( ft) and carbonate concretions possibly occur. Brideaux, WW and Fisher, MJ () Upper Jurassic-Lower Cretaceous dinoflagellate assemblages from arctic Canada.
Geological Survey of Canada BulletinBøgvad, R and Rosenkrantz, A () Beiträge zur Kenntnis der unteren Kreide Ostgrönlands. Several studies of dinoflagellate cyst assemblages in the Upper Jurassic–Lower Cretaceous successions in Svalbard and from the western Barents Sea have been carried out over the last thirty years (Bjærke, ; Århus, ; Bailey, ; Smelror et al., ; Smelror & Dypvik, ).
This is the first report where informal. Middle Jurassic to Early Cretaceous dinoflagellate assemblage zones in eastern Heilongjiang Province, northeast China Author links open overlay panel Youhua Zhu Chengquan He Show more.
evidence for the Upper Jurassic-Lower Cretaceous age of the succession cropping our along the northeastern shore of Lake Hazen (Fig. The sediments containing age diagnostic dinocysts assemblages, spores and pollen are exposed from Hazen Camp to km southeast along the Hazen Lake shore.
They were studied in three lithological sections. Craspedites canadensis in the Canadian Arctic Arch-ipelago. These assemblages are upper Tithonian in age. It would thus appear that the upper limit of G.
jurassica is probably lower Tithonian. The best exposure of the Pareodinia osming-tonesis zone, where the assemblage could be asso-ciated directly with Buchia fisheriana, was recorded. For example, the only previous records of Jurassic and Cretaceous dinoflagellate cysts from the Qinghai-Xizang (Tibet) Plateau are brief reports by Mao and Bian,Cheng and He, This study is on the dinoflagellate cysts of 14 samples from the Xiali, Suowa and Xueshan formations of the Yanshiping Group (Upper Jurassic–Lower Cretaceous) of the northern Qinghai-Xizang Plateau, China.
Dinoflagellate cyst biostratigraphy, palynofacies, depositional environment and sequence stratigraphy of the Agardhfjellet Formation (Upper Jurassic - Lower Cretaceous) in central Spitsbergen. Dinoflagellate cysts and associated aquatic palynomorphs have been recovered from the dinosaur-bearing Tendaguru Beds (Upper Jurassic–Lower Cretaceous) at Tendaguru, a hill in southeast Tanzania.
Palynofloras from these beds are generally dominated by pollen grains of Mesozoic conifers (mainly Classopollis), but dinoflagellate cysts occur.Jurassic-Lower Cretaceous lithostratigraphic nomenclature for the Danish Central Trough. Danmarks Geol. Undersøgelse, Serie A, 12, 65 pp.
Johannessen, P.N., Sedimentology and sequence stratigraphy of paralic and shallow marine Upper Jurassic sandstones in .V.
A. Zakharov, T. I. Nal'nyaeva, and N. I. Shul'gina, " New Data on Biostratigraphy of the Upper Jurassic– Lower Cretaceous Deposits of the Paksa Peninsula, the Anabar Bay (North Middle Siberia.