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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Primary terms
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carbon
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Cenozoic
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Quaternary
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upper Pleistocene
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Weichselian
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upper Weichselian
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Younger Dryas (1)
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Tertiary
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lower Tertiary (1)
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Paleogene
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Paleocene
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Reptilia
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Abstract Our paper presents the first draft of a geomorphological map of the German North Sea and Baltic Sea. The inspiration for this map comes from the international collaboration of marine researchers within the European EMODnet Geology Project ( https://www.emodnet-geology.eu/ ). The current climate change intensifies the natural processes of change in nature. Within the framework of various nature conservation projects, the importance of marine sediment structures on marine fauna and their reproductive cycles, sedimentation conditions, currents, etc. has been investigated. In order to be able to make statements for the German seas and document changes, the current state must first be recorded.
The Carboniferous conodont Lochriea commutata (Branson and Mehl, 1941), the type species of Lochriea Scott, 1942: nomenclatural history, apparatus composition and effects on Lochriea species
Origin, migration pathways, and prediction of high carbon dioxide accumulations in the Lower Saxony Basin (northwestern Germany): Part I
Origin, migration pathways, and prediction of high carbon dioxide accumulations in the Lower Saxony Basin (northwestern Germany): Part II
3D ground-penetrating radar attributes to generate classified facies models: A case study from a dune island
Improved hydrogeophysical imaging by structural coupling of 2D magnetic resonance and electrical resistivity tomography
Magnetic resonance tomography constrained by ground-penetrating radar for improved hydrogeophysical characterization
Abstract Cretaceous sandstones occur mainly in the north and NE of Germany. Some of them have been quarried for more than a thousand years and they have been transported to other regions, even abroad, from as early as medieval times. These are the Elbe Sandstones in Saxony, the Wealden Sandstones and the Bentheimer Sandstone in Lower Saxony and the Baumberger Sandstone in North Rhein-Westfalia. All of these are still quarried, and all can be used as building stone as well as for sculptures. They are introduced with their special features and their use over the centuries.