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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Antarctica (1)
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Arctic Ocean
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Alpha Cordillera (2)
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Amerasia Basin (1)
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Invertebrata
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Spermatophyta
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Mesozoic
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Primary terms
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Tertiary
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Invertebrata
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Porifera
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Protista
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Neogloboquadrina
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isotopes
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Mesozoic
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Permian
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Northern Greenland
Metamorphism obscures primary taphonomic pathways in the early Cambrian Sirius Passet Lagerstätte, North Greenland
Lower Cambrian (Series 2) small shelly fossils from along Nares Strait (Nunavut and Greenland; Laurentia)
An outer shelf shelly fauna from Cambrian Series 2 (Stage 4) of North Greenland (Laurentia)
Elrathia hensonensis nomen novum, new replacement name for Elrathia groenlandica Geyer and Peel, 2017 (Trilobita, Ptychopariacea)
Glomulina oculus , New Calcareous Foraminiferal Species from the High Arctic: A Potential Indicator of a Nearby Marine-Terminating Glacier
Constraints from cosmogenic nuclides on the glaciation and erosion history of Dove Bugt, northeast Greenland
Polypleuraspis (Arthropoda, Trilobita) from the middle Cambrian (Miaolingian Series) around Kane Basin (Nunavut and Greenland)
The Sirius Passet Lagerstätte of North Greenland: a remote window on the Cambrian Explosion
The Smithian–Spathian boundary in North Greenland: implications for extreme global climate changes
The timing of fjord formation and early glaciations in North and Northeast Greenland
Tarimspira from the Cambrian (Series 2, Stage 4) of Laurentia (Greenland): extending the skeletal record of paraconodontid vertebrates
Characterization of kerogenous films and taphonomic modes of the Sirius Passet Lagerstätte, Greenland
Tectonic implications of the lithospheric structure across the Barents and Kara shelves
Abstract This paper considers the lithospheric structure and evolution of the wider Barents–Kara Sea region based on the compilation and integration of geophysical and geological data. Regional transects are constructed at both crustal and lithospheric scales based on the available data and a regional three-dimensional model. The transects, which extend onshore and into the deep oceanic basins, are used to link deep and shallow structures and processes, as well as to link offshore and onshore areas. The study area has been affected by numerous orogenic events in the Precambrian–Cambrian (Timanian), Silurian–Devonian (Caledonian), latest Devonian–earliest Carboniferous (Ellesmerian–svalbardian), Carboniferous–Permian (Uralian), Late Triassic (Taimyr, Pai Khoi and Novaya Zemlya) and Palaeogene (Spitsbergen–Eurekan). It has also been affected by at least three episodes of regional-scale magmatism, the so-called large igneous provinces: the Siberian Traps (Permian–Triassic transition), the High Arctic Large Igneous Province (Early Cretaceous) and the North Atlantic (Paleocene–Eocene transition). Additional magmatic events occurred in parts of the study area in Devonian and Late Cretaceous times. Within this geological framework, we integrate basin development with regional tectonic events and summarize the stages in basin evolution. We further discuss the timing, causes and implications of basin evolution. Fault activity is related to regional stress regimes and the reactivation of pre-existing basement structures. Regional uplift/subsidence events are discussed in a source-to-sink context and are related to their regional tectonic and palaeogeographical settings.