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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Alps
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Eastern Alps
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Northern Limestone Alps (1)
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Limestone Alps
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Northern Limestone Alps (1)
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Central Europe
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Austria
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Lower Austria (1)
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Northern Limestone Alps (1)
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Western Europe
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United Kingdom
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Great Britain
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England
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Lancashire England (1)
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Yorkshire England (1)
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Scotland
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Aberdeenshire Scotland (2)
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Lewis Creek (1)
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United States
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Arkansas
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Howard County Arkansas (1)
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Kentucky
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Leslie County Kentucky (1)
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fossils
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bacteria (1)
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fungi (4)
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Invertebrata
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Arthropoda
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Mandibulata
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Insecta (1)
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microfossils (3)
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palynomorphs
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miospores
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Classopollis (1)
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Plantae
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algae (1)
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Pteridophyta (1)
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Spermatophyta
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Bennettitales (1)
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Coniferales (1)
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geologic age
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Coal Measures (1)
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Mesozoic
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Cretaceous
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Comanchean
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Trinity Group (1)
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Lower Cretaceous
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Trinity Group (1)
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Triassic
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Upper Triassic
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Carnian (1)
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Paleozoic
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Carboniferous
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Pennsylvanian
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Middle Pennsylvanian
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Breathitt Formation (1)
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Devonian
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Lower Devonian (3)
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Primary terms
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bacteria (1)
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diagenesis (1)
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Europe
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Alps
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Eastern Alps
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Northern Limestone Alps (1)
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Limestone Alps
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Northern Limestone Alps (1)
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-
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Central Europe
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Austria
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Lower Austria (1)
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Northern Limestone Alps (1)
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Western Europe
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United Kingdom
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Great Britain
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England
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Lancashire England (1)
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Yorkshire England (1)
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Scotland
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Aberdeenshire Scotland (2)
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-
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fungi (4)
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Invertebrata
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Arthropoda
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Mandibulata
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Insecta (1)
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Mesozoic
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Cretaceous
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Comanchean
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Trinity Group (1)
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Lower Cretaceous
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Trinity Group (1)
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Triassic
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Upper Triassic
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Carnian (1)
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micropaleontology (1)
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paleoecology (4)
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Paleozoic
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Carboniferous
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Pennsylvanian
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Middle Pennsylvanian
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Breathitt Formation (1)
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Devonian
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Lower Devonian (3)
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palynomorphs
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miospores
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Classopollis (1)
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Plantae
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algae (1)
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Pteridophyta (1)
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Spermatophyta
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Gymnospermae
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Bennettitales (1)
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Coniferales (1)
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United States
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Arkansas
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Howard County Arkansas (1)
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Kentucky
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Leslie County Kentucky (1)
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A fungal reproductive unit from the Lower Devonian Rhynie chert (Aberdeenshire, Scotland) that demonstrates an unusual hyphal investment pattern
REINVESTIGATING CARBONIFEROUS “ACTINOMYCETES”: AUTHIGENIC FORMATION OF BIOMIMETIC CARBONATES PROVIDES INSIGHT INTO EARLY DIAGENESIS OF PERMINERALIZED PLANTS
Microfossils from the Lower Devonian Rhynie Chert with Suggested Affinities to the Peronosporomycetes
THE ADVANTAGE OF THIN SECTION PREPARATIONS OVER ACETATE PEELS IN THE STUDY OF LATE PALEOZOIC FUNGI AND OTHER MICROORGANISMS
PALEOMYCOLOGY: THE REDISCOVERY OF THE OBVIOUS
Fossil Insect Eggs and Ovipositional Damage on Bennettitalean Leaf Cuticles from the Carnian (Upper Triassic) of Austria
Carboniferous
Abstract The Carboniferous (359.2–299 Ma, Gradstein et al. 2004 ) succession of Central Europe records one of the most important time periods with respect to European geology, since it marks the final collision of Gondwana with the northern continent of Laurussia (i.e. Laurentia, Baltica and Avalonia). Oblique convergence resulted in collisional processes which created a mountain belt extending from Russia, through western Europe and into North America. The climax of the Variscan Orogeny was the formation of the supercontinent Pangaea leaving a relict Palaeo-tethys to the east ( Scotese & Langford 1995 ) (Fig. 9.1 ). The Variscan belt is a broad (c. 1000 km) complex curvilinear feature extending across Europe and marking the zones of Variscan-age deformation (Figs 9.2 & 9.3 ). The final phase of Variscan activity was also a period of terrane mobility and tectonic instability in the Central European region with sinistral wrench faulting causing widespread rifting of the northern European crust ( Pegrum 1984 a, b ; Ziegler 1990 ). The Carboniferous succession in Central Europe is generally dominated by marine sediments (both clastic and carbonate) in the lower part of the succession¨ The clastic sediments tend to be deeper-water shelf or turbiditic successions, although in some areas (e.g. Belgium, northern Germany) limestones are locally important or even dominant, particularly during the Tournaisian and Visean. In late Carboniferous times, successions are predominantly continental with some coal-bearing units being deposited (particularly in Westphalian times). An exception to the dominantly sedimentary record is provided