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Articles 1 - 10 of 10

Full-Text Articles in Paleontology

Cenozoic Paleoceanography 1986: An Introduction, W. H. Berger, Larry A. Mayer Dec 1987

Cenozoic Paleoceanography 1986: An Introduction, W. H. Berger, Larry A. Mayer

Affiliate Scholarship

New developments in Cenozoic paleoceanography include the application of climate models and atmospheric general circulation models to questions of climate reconstruction, the refinement of conceptual models for interpretation of the carbon isotope record in terms of carbon mass balance, paleocirculation, paleoproductivity, and the regional mapping of paleoceanographic events by acoustic stratigraphy. Sea level change emerges as a master variable to which changes in the ocean environment must be traced in many cases, and tests of the onlap-offlap paradigm therefore are of crucial importance.


Geology Of Selected Sites Near The Republican River In Franklin County, Nebraska, Roger K. Pabian Jul 1987

Geology Of Selected Sites Near The Republican River In Franklin County, Nebraska, Roger K. Pabian

Conservation and Survey Division

No abstract provided.


Groundwater Levels In Nebraska, 1986, Michael J. Ellis, Vincent H. Dreeszen Jul 1987

Groundwater Levels In Nebraska, 1986, Michael J. Ellis, Vincent H. Dreeszen

Conservation and Survey Division

No abstract provided.


Late Paleozoic Sea Levels And Depositional Sequences, Charles A. Ross, June R. P. Ross Jan 1987

Late Paleozoic Sea Levels And Depositional Sequences, Charles A. Ross, June R. P. Ross

Geology Faculty Publications

Cyclic sea level charts for the Lower Carboniferous (Mississippian), Middle and Upper Carboniferous (Pennsylvanian), and Permian show considerable variability in the duration and magnitude of third-order depositional sequences, and also in the position of general sea level as represented by second-order sea level. Transgressive and highstand system tracts are numerous on the cratonic shelves of the late Paleozoic continents. Shelf margin wedges are less well represented except at times of general lower sea levels. Most low stand wedges and all low stand fan systems are structurally deformed and make up many of the accretionary wedges and displaced terranes that lie …


Resource Notes-Fall/Winter 1986-87 Jan 1987

Resource Notes-Fall/Winter 1986-87

Conservation and Survey Division

No abstract provided.


Resource Notes-Spring/Summer 1987 Jan 1987

Resource Notes-Spring/Summer 1987

Conservation and Survey Division

No abstract provided.


Nebraska Mineral Operations Review, 1986, Raymond R. Burchett, Duane A. Eversoll Jan 1987

Nebraska Mineral Operations Review, 1986, Raymond R. Burchett, Duane A. Eversoll

Conservation and Survey Division

No abstract provided.


Conservation And Survey Division. 1987. Significant Rises And Declines In Nebraska Groundwater Levels (From Pre-Development As Of Fall 1985)/Registered Irrigation Wells In Nebraska (As Of January 1, 1986), Conservation Survey Division, U.S. Geological Survey Jan 1987

Conservation And Survey Division. 1987. Significant Rises And Declines In Nebraska Groundwater Levels (From Pre-Development As Of Fall 1985)/Registered Irrigation Wells In Nebraska (As Of January 1, 1986), Conservation Survey Division, U.S. Geological Survey

Conservation and Survey Division

No abstract provided.


Significant Rises And Declines In Nebraska Groundwater Levels (From Pre-Development As Of Fall 1985)/Registered Irrigation Wells In Nebraska (As Of January 1, 1986), Conservation Survey Division, U.S. Geological Survey Jan 1987

Significant Rises And Declines In Nebraska Groundwater Levels (From Pre-Development As Of Fall 1985)/Registered Irrigation Wells In Nebraska (As Of January 1, 1986), Conservation Survey Division, U.S. Geological Survey

Conservation and Survey Division

No abstract provided.


Biostratigraphic Zonation Of Late Paleozoic Depositional Sequences, Charles A. Ross, June R. P. Ross Jan 1987

Biostratigraphic Zonation Of Late Paleozoic Depositional Sequences, Charles A. Ross, June R. P. Ross

Geology Faculty Publications

Correlation of more than seventy third-order depositional sequences in Carboniferous and Permian strata uses assemblage zones of warm water benthic and nektonic shelf faunas. These include calcareous foraminifers, bryozoans, conodonts, and ammonoids and represent tropical, subtropical, and warm temperate water faunas from carbonate shelves and adjacent cratonic basins.

After the Early Carboniferous faunal zonation was highly provincial and worldwide correlations of depositional sequences are based on interpretations of evolutionary lineages and depositional patterns in each province and in identifying times of limited dispersals between provinces.

Associated with these faunal zones there were times of expanded or reduced faunal diversities and …