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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Antarctica
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Transantarctic Mountains
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Queen Alexandra Range (1)
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Victoria Land (1)
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Europe
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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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polar regions (1)
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United States
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Illinois (1)
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Kentucky
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Leslie County Kentucky (1)
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elements, isotopes
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carbon
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C-13/C-12 (1)
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isotope ratios (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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fossils
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bacteria (1)
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burrows (1)
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fungi (4)
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ichnofossils
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Planolites (1)
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Skolithos (1)
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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 (5)
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palynomorphs
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miospores (1)
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Plantae
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algae (1)
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Bryophyta
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Musci
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Sphagnum (1)
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Pteridophyta
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Filicopsida (1)
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Equisetales (1)
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Spermatophyta
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Gymnospermae
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Coniferales
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Cycadales (1)
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Glossopteridales
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Glossopteris (1)
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Pteridospermae (1)
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geologic age
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Coal Measures (1)
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Fremouw Formation (2)
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Paleozoic
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Mississippian
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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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Ordovician (1)
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Permian
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Upper Permian (1)
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Phanerozoic (1)
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Primary terms
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Antarctica
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Transantarctic Mountains
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Queen Alexandra Range (1)
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Victoria Land (1)
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bacteria (1)
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carbon
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C-13/C-12 (1)
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diagenesis (1)
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electron microscopy (2)
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Europe
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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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fungi (4)
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ichnofossils
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Planolites (1)
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Skolithos (1)
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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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-
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isotopes
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stable isotopes
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C-13/C-12 (1)
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Mesozoic
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Cretaceous (1)
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Jurassic (1)
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Triassic
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Fremouw Formation (2)
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Middle Triassic (1)
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micropaleontology (1)
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paleobotany (1)
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paleoclimatology (2)
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paleoecology (6)
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paleontology (1)
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Paleozoic
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Carboniferous
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Mississippian
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Middle Mississippian (1)
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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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Ordovician (1)
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Permian
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Upper Permian (1)
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palynology (2)
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palynomorphs
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miospores (1)
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Phanerozoic (1)
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Plantae
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algae (1)
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Bryophyta
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Musci
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Sphagnum (1)
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-
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Pteridophyta
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Filicopsida (1)
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Sphenopsida
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Equisetales (1)
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Spermatophyta
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Gymnospermae
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Coniferales
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Picea (1)
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Cycadales (1)
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Ginkgoales (1)
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Glossopteridales
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Glossopteris (1)
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Pteridospermae (1)
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United States
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Illinois (1)
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Kentucky
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Leslie County Kentucky (1)
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sedimentary structures
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burrows (1)
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soils
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paleosols (1)
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A fungal reproductive unit from the Lower Devonian Rhynie chert (Aberdeenshire, Scotland) that demonstrates an unusual hyphal investment pattern
Leaf habit of Late Permian Glossopteris trees from high-palaeolatitude forests
REINVESTIGATING CARBONIFEROUS “ACTINOMYCETES”: AUTHIGENIC FORMATION OF BIOMIMETIC CARBONATES PROVIDES INSIGHT INTO EARLY DIAGENESIS OF PERMINERALIZED PLANTS
Paleozoic mosses: Small, but no longer inconspicuous
Microfossils from the Lower Devonian Rhynie Chert with Suggested Affinities to the Peronosporomycetes
TRIASSIC FLORAS OF ANTARCTICA: PLANT DIVERSITY AND DISTRIBUTION IN HIGH PALEOLATITUDE COMMUNITIES
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
MATONIACEOUS FERNS (GLEICHENIALES) FROM THE MIDDLE TRIASSIC OF ANTARCTICA
The ichnologic record of the continental invertebrate invasion; evolutionary trends in environmental expansion, ecospace utilization, and behavioral complexity
Fredda D. Reed was one of the first students of Adolph Noé and was responsible for some of the early work on Carboniferous coal-ball plants in North America. As a faculty member for 35 years at Mount Holyoke College, she touched the lives of generations of students through her strong work ethic, tenacity for detail, and unending sense of humor.
Plant megafossils are described and illustrated from several localities and stratigraphic levels within the Ellsworth Mountains. The flora is dominated by various species of Glossopteris foliage and also includes sphenophyte stems and leaf sheaths, glossopterid reproductive organs, Gangamopteris leaves, and Vertebraria -type axes. The plants are preserved as impressions in fine-grained shale within the Polarstar Formation. Based on comparisons with other Antarctic and Gondwana floras, a Middle to Late Permian age is suggested.