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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Central Asia
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Kazakhstan (2)
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Omsk Russian Federation (1)
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Siberia (2)
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Atlantic Ocean
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Commonwealth of Independent States
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Europe
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elements, isotopes
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carbon
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isotope ratios (1)
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fossils
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Protista
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geochronology methods
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geologic age
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Cenozoic
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Paleogene
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igneous rocks
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igneous rocks
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volcanic rocks (1)
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Primary terms
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Asia
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Central Asia
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Kazakhstan (2)
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Omsk Russian Federation (1)
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Siberia (2)
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Atlantic Ocean
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North Atlantic
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North Sea (1)
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Australasia
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New Zealand (1)
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biogeography (1)
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carbon
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C-13/C-12 (1)
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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lower Eocene
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Ypresian (1)
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upper Paleocene (3)
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climate change (1)
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Europe
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Central Europe
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Austria
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Salzburg State Austria (2)
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Jutland (1)
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Pechora Basin (1)
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Western Europe
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Scandinavia
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Denmark (1)
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igneous rocks
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volcanic rocks (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Ostracoda (1)
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isotopes
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paleoclimatology (1)
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paleomagnetism (1)
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palynomorphs
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Plantae
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algae
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diatoms (1)
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sedimentary rocks (1)
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sedimentary rocks
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sedimentary rocks (1)
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Early and middle Eocene dinoflagellate cysts from the Aktulagay section, Kazakhstan
Eocene dinoflagellate cyst biostratigraphy of research borehole 011-BP, Omsk Region, southwestern Siberia
WILSONIDIUM PECHORICUM NEW SPECIES—A NEW DINOFLAGELLATE SPECIES WITH UNUSUAL ASYMMETRY FROM THE PALEOCENE/EOCENE TRANSITION
DINOFLAGELLATE CYSTS FROM THE MIDDLE EOCENE TO ?LOWERMOST OLIGOCENE SUCCESSION IN THE KYSING RESEARCH BOREHOLE, CENTRAL DANISH BASIN
The Dababiya Quarry Section: Lithostratigraphy, clay mineralogy, geochemistry and paleontology
Chronostratigraphic terminology at the Paleocene/Eocene boundary
Global dinoflagellate event associated with the late Paleocene thermal maximum
The Paleocene/Eocene-boundary interval of a Tethyan deep-sea section (Austria) and its correlation with the North Sea basin
Abstract The Cenozoic evolution of the epicontinental North Sea Basin is described on the basis of sequence stratigraphy, comprising analyses of seismic sections, petrophysical logs and biostratigraphic studies of foraminifera, dinoflagellates and calcareous nannofossils. Stratigraphic, palaeogeographic and palaeoecological information from the Danish onshore area is integrated in the study. The deposits are subdivided into 21 sequences, which group into seven informal major units. The sequence boundaries are identified by differences in seismic facies and by seismic onlap, toplap and truncation features. The maximum flooding surfaces are placed at internal downlap surfaces which correlate with high values on the gamma-ray logs. The source of sediments and the direction of sediment transport changed several times during Cenozoic deposition. Transport was mainly from the north during the Late Paleocene and Early Eocene, from the west during the Middle and Late Eocene and from the north and northeast during the Oligocene to Quaternary times. The depocenters of the seven major units are generally located marginally, apparently adjoining the source areas. There is only minor evidence for changes in subsidence rates in the basin. A constant rate is assumed from Paleocene to mid Middle Miocene time. For the remaining part of the Cenozoic time an increased rate is indicated. A tentative relative sea-level curve for the North Sea Basin is proposed. The overall trends of the curve are broadly comparable with the global sea-level curve of Haq et al. (1988). Discrepancies may be caused by differences in the biostratigraphic calibrations. The most pronounced Oligocene sea-level fall is dated as latest Oligocene.