scholarly journals The Mygoora Local Fauna: a late Quaternary vertebrate assemblage from central Australia

2002 ◽  
Vol 18 ◽  
pp. 77-93
Author(s):  
Dirk Megirian ◽  
Peter Murray ◽  
Peter K Latz ◽  
Ken A Johnson
Keyword(s):  
Late Quaternary ◽  
Local Fauna ◽  
Central Australia ◽  
Vertebrate Assemblage

Vertebrate paleontology, stratigraphy, and paleohydrology of Tule Springs Fossil Beds National Monument, Nevada (USA)

2017 ◽  
Vol 4 ◽  
pp. 55-98
Author(s):  
Kathleen Springer ◽  
Jeffrey Pigati ◽  
Eric Scott
Keyword(s):  
Las Vegas ◽  
Late Quaternary ◽  
Plant Macrofossils ◽  
Distinct Species ◽  
American Southwest ◽  
Local Fauna ◽  
Climatic Oscillations ◽  
Las Vegas Valley ◽  
National Monument ◽  
Desert Wetlands

Tule Springs Fossil Beds National Monument (TUSK) preserves 22,650 acres of the upper Las Vegas Wash in the northern Las Vegas Valley (Nevada, USA). TUSK is home to extensive and stratigraphically complex groundwater discharge (GWD) deposits, called the Las Vegas Formation, which represent springs and desert wetlands that covered much of the valley during the late Quaternary. The GWD deposits record hydrologic changes that occurred here in a dynamic and temporally congruent response to abrupt climatic oscillations over the last ~300 ka (thousands of years). The deposits also entomb the Tule Springs Local Fauna (TSLF), one of the most significant late Pleistocene (Rancholabrean) vertebrate assemblages in the American Southwest. The TSLF is both prolific and diverse, and includes a large mammal assemblage dominated by Mammuthus columbi and Camelops hesternus. Two (and possibly three) distinct species of Equus, two species of Bison, Panthera atrox, Smilodon fatalis, Canis dirus, Megalonyx jeffersonii, and Nothrotheriops shastensis are also present, and newly recognized faunal components include micromammals, amphibians, snakes, and birds. Invertebrates, plant macrofossils, and pollen also occur in the deposits and provide important and complementary paleoenvironmental information. This field compendium highlights the faunal assemblage in the classic stratigraphic sequences of the Las Vegas Formation within TUSK, emphasizes the significant hydrologic changes that occurred in the area during the recent geologic past, and examines the subsequent and repeated effect of rapid climate change on the local desert wetland ecosystem.

scholarly journals Alluvial evidence for major climate and flow regime changes during the middle and late Quaternary in eastern central Australia

Geomorphology ◽  
2008 ◽  
Vol 101 (1-2) ◽  
pp. 109-129 ◽  
Author(s):  
Gerald C. Nanson ◽  
David M. Price ◽  
Brian G. Jones ◽  
Jerry C. Maroulis ◽  
Maria Coleman ◽  
...  
Keyword(s):  
Flow Regime ◽  
Late Quaternary ◽  
Regime Changes ◽  
Central Australia

scholarly journals Vertebrate paleontology, stratigraphy, and paleohydrology of Tule Springs Fossil Beds National Monument, Nevada (USA)

2017 ◽  
Vol 4 ◽  
pp. 55-98
Author(s):  
Kathleen B. Springer ◽  
Jeffrey S. Pigati ◽  
Eric Scott
Keyword(s):  
Las Vegas ◽  
Late Quaternary ◽  
Plant Macrofossils ◽  
Distinct Species ◽  
American Southwest ◽  
Local Fauna ◽  
Climatic Oscillations ◽  
Las Vegas Valley ◽  
National Monument ◽  
Desert Wetlands

Tule Springs Fossil Beds National Monument (TUSK) preserves 22,650 acres of the upper Las Vegas Wash in the northern Las Vegas Valley (Nevada, USA). TUSK is home to extensive and stratigraphically complex groundwater discharge (GWD) deposits, called the Las Vegas Formation, which represent springs and desert wetlands that covered much of the valley during the late Quaternary. The GWD deposits record hydrologic changes that occurred here in a dynamic and temporally congruent response to abrupt climatic oscillations over the last ~300 ka (thousands of years). The deposits also entomb the Tule Springs Local Fauna (TSLF), one of the most significant late Pleistocene (Rancholabrean) vertebrate assemblages in the American Southwest. The TSLF is both prolific and diverse, and includes a large mammal assemblage dominated by Mammuthus columbi and Camelops hesternus. Two (and possibly three) distinct species of Equus, two species of Bison, Panthera atrox, Smilodon fatalis, Canis dirus, Megalonyx jeffersonii, and Nothrotheriops shastensis are also present, and newly recognized faunal components include micromammals, amphibians, snakes, and birds. Invertebrates, plant macrofossils, and pollen also occur in the deposits and provide important and complementary paleoenvironmental information. This field compendium highlights the faunal assemblage in the classic stratigraphic sequences of the Las Vegas Formation within TUSK, emphasizes the significant hydrologic changes that occurred in the area during the recent geologic past, and examines the subsequent and repeated effect of rapid climate change on the local desert wetland ecosystem.

scholarly journals The vertebrate fossil collection record from the Chinchilla Sand, South–East Queensland, 1844-2021

2021 ◽  
Vol 63 ◽  
pp. 11-25
Author(s):  
Joanne E. Wilkinson ◽  
◽  
Kristen D. Spring ◽  
T.L. Dunn ◽  
Gilbert J. Price ◽  
...  
Keyword(s):  
Spatial Information ◽  
Local Fauna ◽  
Digital Map ◽  
Queensland Museum ◽  
Collection Record ◽  
The Future ◽  
Field Notes ◽  
Fossil Vertebrate ◽  
Vertebrate Assemblage ◽  
Systematic Framework

Since the mid-1840s a diverse fossil vertebrate assemblage, referred to as the Chinchilla Local Fauna, has been collected from the Pliocene deposits of the Chinchilla Sand on the western Darling Downs of South-East Queensland. In large part because of this long history and the numerous collectors who have worked fossil deposits in the area, much ambiguity regarding site and locality names and their specific coordinates exists. Here, we review the vertebrate fossil collection records in the Queensland Museum Fossil, Donor, Collector and Locality Registers, correspondence, and field notes in an effort to pinpoint the location of each named locality and site and develop a digital map which highlights the historical collecting sites at one significant locality in the Chinchilla area. To ensure that a systematic framework for all future collecting from the main collecting area (Chinchilla Rifle Range) is maintained, we recommend the use of consistent nomenclature for sites so that spatial information of the highest possible quality is captured into the future. We recommend future collections include detailed recordings of stratigraphic contexts as well as GPS coordinates.

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