- Title Pages
- [UNTITLED]
- Dedication
- Preface
- Acknowledgments
- Chapter Appendixes
- Figures
- Tables
- Abbreviations and Definitions
-
One Climate Change, Biodiversity, and Ecosystem Health -
Two The Pleistocene Fossils of Porcupine Cave, Colorado -
Three The Modern Environment, Flora, and Vegetation of South Park, Colorado -
Four The Historical Context of Porcupine Cave -
Five The Geology and Speleogenesis of Porcupine Cave -
Six Magnetostratigraphic Constraints on the Age of Pleistocene Fossiliferous Strata in Porcupine Cave’s DMNH Velvet Room Excavation -
Seven Age and Correlation of Key Fossil Sites in Porcupine Cave -
Eight Biology of Wood Rats as Cave Dwellers and Collectors -
Nine Paleopathology and Taphonomic Modification of Mammalian Bones from Porcupine Cave -
Ten : A Summary of Fossilized Species in Porcupine Cave -
Eleven Synopsis of the Herpetofauna from Porcupine Cave -
Twelve The Early and Middle Pleistocene Avifauna from Porcupine Cave -
Thirteen The Carnivora from Porcupine Cave -
Fourteen Middle Pleistocene (Irvingtonian) Ochotona (Lagomorpha: Ochotonidae) from Porcupine Cave -
Fifteen Leporidae of the DMNH Velvet Room Excavations and Mark’s Sink -
Sixteen Identification of Miscellaneous Mammals from the Pit Locality: Including Soricidae, Leporidae, Geomyoidea -
SEVENTEEN Systematics and Faunal Dynamics of Fossil Squirrels from Porcupine Cave -
Eighteen Fossil Wood Rats of Porcupine Cave: Tectonic or Climatic Controls? -
Nineteen Arvicoline Rodents from Porcupine Cave -
Twenty Pliocene and Pleistocene Horses from Porcupine Cave -
Twenty-One Pleistocene (Irvingtonian) Artiodactyla from Porcupine Cave -
Twenty-Two Irvingtonian Mammals from the Badger Room in Porcupine Cave: Age, Taphonomy, Climate, and Ecology -
Twenty-Three Faunal Dynamics of Small Mammals through the Pit Sequence -
Twenty-Four Stable Carbon and Oxygen Isotope Analysis of Marmot Cheek Teeth from the Pit Locality -
Twenty-Five Assessing the Effect of Middle Pleistocene Climate Change on Marmota Populations from the Pit Locality -
Twenty-Six Effect of Climate Change on Terrestrial Vertebrate Biodiversity - Literature Cited
- Contributors
- Index
Irvingtonian Mammals from the Badger Room in Porcupine Cave: Age, Taphonomy, Climate, and Ecology
Irvingtonian Mammals from the Badger Room in Porcupine Cave: Age, Taphonomy, Climate, and Ecology
- Chapter:
- (p.294) (p.295) Twenty-Two Irvingtonian Mammals from the Badger Room in Porcupine Cave: Age, Taphonomy, Climate, and Ecology
- Source:
- Biodiversity Response to Climate Change in the Middle Pleistocene
- Author(s):
Alan B. Shabel
Anthony D. Barnosky
Tonya Van Leuvan
Faysal Bibi
Matthew H. Kaplane
- Publisher:
- University of California Press
This chapter describes fossil deposits of mammals in the Badger Room of Porcupine Cave. The Badger Room is a small chamber in the Porcupine Cave system located approximately 25 m from the modern entrance to the cave. The Badger Room mammal fauna is very diverse; it contains abundant lagomorph, rodent, and carnivore remains. Some of the specimens were used to explore the paleoclimate of the region surrounding the cave. The climate spaces occupied by each species were assumed to encompass the physiological tolerance limits of each taxon with regard to temperature and moisture. The chapter also used autecological estimates for habitat reconstruction and analysis of the community structure of the mammal fauna.
Keywords: mammals, Badger Room, lagomorph, rodent, carnivore, paleoclimate, autecological estimates, habitat reconstruction
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- Title Pages
- [UNTITLED]
- Dedication
- Preface
- Acknowledgments
- Chapter Appendixes
- Figures
- Tables
- Abbreviations and Definitions
-
One Climate Change, Biodiversity, and Ecosystem Health -
Two The Pleistocene Fossils of Porcupine Cave, Colorado -
Three The Modern Environment, Flora, and Vegetation of South Park, Colorado -
Four The Historical Context of Porcupine Cave -
Five The Geology and Speleogenesis of Porcupine Cave -
Six Magnetostratigraphic Constraints on the Age of Pleistocene Fossiliferous Strata in Porcupine Cave’s DMNH Velvet Room Excavation -
Seven Age and Correlation of Key Fossil Sites in Porcupine Cave -
Eight Biology of Wood Rats as Cave Dwellers and Collectors -
Nine Paleopathology and Taphonomic Modification of Mammalian Bones from Porcupine Cave -
Ten : A Summary of Fossilized Species in Porcupine Cave -
Eleven Synopsis of the Herpetofauna from Porcupine Cave -
Twelve The Early and Middle Pleistocene Avifauna from Porcupine Cave -
Thirteen The Carnivora from Porcupine Cave -
Fourteen Middle Pleistocene (Irvingtonian) Ochotona (Lagomorpha: Ochotonidae) from Porcupine Cave -
Fifteen Leporidae of the DMNH Velvet Room Excavations and Mark’s Sink -
Sixteen Identification of Miscellaneous Mammals from the Pit Locality: Including Soricidae, Leporidae, Geomyoidea -
SEVENTEEN Systematics and Faunal Dynamics of Fossil Squirrels from Porcupine Cave -
Eighteen Fossil Wood Rats of Porcupine Cave: Tectonic or Climatic Controls? -
Nineteen Arvicoline Rodents from Porcupine Cave -
Twenty Pliocene and Pleistocene Horses from Porcupine Cave -
Twenty-One Pleistocene (Irvingtonian) Artiodactyla from Porcupine Cave -
Twenty-Two Irvingtonian Mammals from the Badger Room in Porcupine Cave: Age, Taphonomy, Climate, and Ecology -
Twenty-Three Faunal Dynamics of Small Mammals through the Pit Sequence -
Twenty-Four Stable Carbon and Oxygen Isotope Analysis of Marmot Cheek Teeth from the Pit Locality -
Twenty-Five Assessing the Effect of Middle Pleistocene Climate Change on Marmota Populations from the Pit Locality -
Twenty-Six Effect of Climate Change on Terrestrial Vertebrate Biodiversity - Literature Cited
- Contributors
- Index