Author: Spencer G. LucasPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 185
Book Description
Carboniferous-Permian Transition in the Robledo Mountains, Southern New Mexico
Author: Spencer G. LucasPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 185
Book Description
Carboniferous-Permian Transition at Carrizo Arroyo, Central New Mexico
Author: Spencer G. LucasPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 309
Book Description
The Carboniferous-Permian Transition in Central New Mexico
Author: Spencer G. LucasPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Science
Languages : en
Pages : 398
Book Description
The Carboniferous-Permian Transition
Author: Spencer G. LucasPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 481
Book Description
Carboniferous-Permian transition in Socorro County, New Mexico
Author: Spencer G. LucasPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Geology
Languages : en
Pages : 362
Book Description
The Carboniferous Timescale
Author: S.G. LucasPublisher: Geological Society of London
ISBN: 1786205424
Category : Science
Languages : en
Pages : 1012
Book Description
The print edition is published as 2 hardback volumes, parts A and B, and sold as a set. The Carboniferous was the time of the assembly of Pangaea by the collision of the Gondwanan and Larussian supercontinents, and the principal interval of the late Paleozoic ice ages. These tectonic and climatic events caused dramatic sea-level fluctuations and climate changes and produced a Carboniferous world that was diverse topographically and climatologically, perhaps only rivalled in that diversity by the late Cenozoic world. Furthermore, the Carboniferous was a time of the accumulation of vast coal deposits of great economic and societal significance. The temporal ordering of geological and biotic events during Carboniferous time thus is critical to the interpretation of some unique and pivotal events in Earth history. This temporal ordering is based on the Carboniferous timescale, which has been developed and refined for nearly two centuries. This book reviews the history of the development of the Carboniferous chronostratigraphic scale and includes comprehensive analyses of Carboniferous radioisotopic ages, magnetostratigraphy, isotope-based correlations, cyclostratigraphy and timescale-relevant marine and non-marine biostratigraphy and biochronology.
Carboniferous-Permian Transition in Cañon del Cobre, northern New Mexico
Author: Spencer G. LucasPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Cañon del Cobre (N.M.).
Languages : en
Pages : 238
Book Description
THE PENNSYLVANIAN SECTION AT BISHOP CAP AND THE HORQUILLA SEAWAY IN THE SOUTHWESTERN USA-NORTHERN MEXICO
Author: SPENCER G. LUCASPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Science
Languages : en
Pages : 85
Book Description
The Trace-Fossil Record of Major Evolutionary Events
Author: M. Gabriela MánganoPublisher: Springer
ISBN: 9401796009
Category : Science
Languages : en
Pages : 372
Book Description
This volume addresses major evolutionary changes that took place during the Ediacaran and the Paleozoic. These include discussions on the nature of Ediacaran ecosystems, as well as the ichnologic signature of evolutionary radiations, such as the Cambrian explosion and the Great Ordovician biodiversification event, the invasion of the land, and the end-Permian mass extinction. This volume set provides innovative reviews of the major evolutionary events in the history of life from an ichnologic perspective. Because the long temporal range of trace fossils has been commonly emphasized, biogenic structures have been traditionally overlooked in macroevolution. However, comparisons of ichnofaunas through geologic time do reveal the changing ecology of organism-substrate interactions. The use of trace fossils in evolutionary paleoecology represents a new trend that is opening a window for our understanding of major evolutionary radiations and mass extinctions. Trace fossils provide crucial evidence for the recognition of spatial and temporal patterns and processes associated with paleoecologic breakthroughs.
LATE CRETACEOUS (CAMPANIAN-MAASTRICHTIAN) AMMONITES FROM THE PIERRE SHALE, RATON BASIN, NORTHEASTERN NEW MEXICO AND SOUTHEASTERN COLORADO
Author: PAUL L. SEALEYPublisher: New Mexico Museum of Natural History and Science
ISBN:
Category : Science
Languages : en
Pages : 195
Book Description