Pleistocene Overkill and North American Mammalian Extinctions
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Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 99, NUMBER 4 A CHECK-LIST OF THE FOSSIL BIRDS OF NORTH AMERICA BY ALEXANDER WETMORE Assistant Secretary, Smithsonian Institution (Publication 3587) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JUNE 18, 1940 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 99, NUMBER 4 A CHECK-LIST OF THE FOSSIL BIRDS OF NORTH AMERICA BY ALEXANDER WETMORE Assistant Secretary, Smithsonian Institution (Publication 3587) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JUNE 18, 1940 Z^t £ovi) i^a{fttnore (pnea BALTIMORE, MD., U. 8. A. A CHECK-LIST OF THE FOSSIL BIRDS OF NORTH AMERICA By ALEXANDER WETMORE Assistant Secretary, Smithsonian Institution Since publication of the last complete list of the fossil birds of North America, which appeared in the Fourth Edition of the Check- list of North American Birds of the American Ornithologists' Union in October 1931, there have been many changes and additions, both in species found only in fossil state and in modern forms recorded from Pleistocene and (rarely) earUer deposits. This information is widely scattered so that it seems pertinent now to gather it together and to present the entire list again for the use of all who may be interested. The material that follows is complete so far as records have come to attention to January 1940. In preparing this paper every species included has been checked carefully against the original records, and data pertaining to geologic distribution have been revised. As in the fourth edition of the A. O. U. Check-list, all modern forms for which there are fossil records have been included. -
Additions to the Late Pleistocene Vertebrate Paleontology of the Las
Additions to the Late Pleistocene Vertebrate Paleontology of ABSTRACT the Las Vegas Formation, Clark County, Nevada DISCUSSION Studies from the 1930s through the 1960s documented one of the most significant late The detailed mapping of over 500 vertebrate paleontologic localities Pleistocene faunas from the Mojave Desert in the Tule Springs area of North Las Vegas. in the upper Las Vegas Wash proved to be an interesting challenge in Recent field investigations in North Las Vegas by the San Bernardino County Museum Kathleen Springer, J. Christopher Sagebiel, Eric Scott, Craig Manker and Chris Austin terms of discerning the stratigraphy. Very little geologic have broadened our knowledge of this fauna across the Las Vegas Wash.Seven units, investigation had been performed in this region since the 1967 work designated A through G, have been defined in the section of the Las Vegas Wash near Division of Geological Sciences, San Bernardino County Museum, Redlands, California of Haynes. That very detailed study was geographically limited to Tule Springs State Park. Units B, D, and E have proven fossiliferous in the area of the the Tule Springs archaeologic investigation and the very near Tule Springs State Park, and date to>40,000 ybp, approximately 25,500 ybp, and about environs at a reconnaissance level. Our study area, falling mostly 14,500 to 9,300 ybp,respectively. Research across the Las Vegas Wash has resulted in within the Gass Peak S.W. 7.5’ U.S.G.S. topographic sheet, had not the discovery of several hundred new fossil localities. In describing the geology at these BACKGROUND been mapped. -
Late Quaternary Extinctions on California's
Flightless ducks, giant mice and pygmy mammoths: Late Quaternary extinctions on California’s Channel Islands Torben C. Rick, Courtney A. Hofman, Todd J. Braje, Jesu´ s E. Maldonado, T. Scott Sillett, Kevin Danchisko and Jon M. Erlandson Abstract Explanations for the extinction of Late Quaternary megafauna are heavily debated, ranging from human overkill to climate change, disease and extraterrestrial impacts. Synthesis and analysis of Late Quaternary animal extinctions on California’s Channel Islands suggest that, despite supporting Native American populations for some 13,000 years, few mammal, bird or other species are known to have gone extinct during the prehistoric human era, and most of these coexisted with humans for several millennia. Our analysis provides insight into the nature and variability of Quaternary extinctions on islands and a broader context for understanding ancient extinctions in North America. Keywords Megafauna; island ecology; human-environmental interactions; overkill; climate change. Downloaded by [Torben C. Rick] at 03:56 22 February 2012 Introduction In earth’s history there have been five mass extinctions – the Ordovician, Devonian, Permian, Triassic and Cretaceous events – characterized by a loss of over 75 per cent of species in a short geological time period (e.g. 2 million years or less: Barnosky et al. 2011). Although not a mass extinction, one of the most heavily debated extinction events is the Late Quaternary extinction of megafauna, when some two-thirds of large terrestrial mammalian genera (444kg) worldwide went extinct (Barnosky et al. 2004). Explanations for this event include climate change, as the planet went from a glacial to interglacial World Archaeology Vol. -
Verification and Reverification: Problems in Archaeofaunal Studies
J. Ethnobiol. 6(1):9-18 Sunnner 1986 VERIFICATION AND REVERIFICATION: PROBLEMS IN ARCHAEOFAUNAL STUDIES AMADEO M. REA Curator of Birds and Mammals Natural History Museum Post Office Box 1390 San Diego, CA 92112 ABSTRACT.-Biological materials from archaeological excavations, particularly faunal remains, are of most lasting scientific value if they are properly handled, individually numbered, and adequately reported in published accounts. Archaeologists are urged never to put bones in plastic bags. Authors of faunal accounts are encouraged to publish reasons for their determinations, to mention comparative materials used, and to give individual identifying numbers and element descriptions with their proveniences to aid subsequent study and reverification. Knowledge of the local fauna enhances the validity of interpreta tions. Better appreciation of the culture and its particular technology would improve biologists' accounts. Archaeological bones have been used in reconstruction of past diets and environments. They are of use to both paleontologists and neontologists. A signifi cant contribution of biological materials is the demonstration of human-wrought modifica tions (particularly insular extinctions and extirpations) in species densities. Existing com parative osteological collections are weak in quantity and sometimes poor in quality; 820/0 of the world's ca. 9,000 bird species are represented by ten or fewer skeletons in museums worldwide. INTRODUCTION The very basis of science is empirical evidence. The taxonomic disciplines are based on specimen documentation, publicly available, subject to reverification. Ethnobiological studies are no exception. The biological specimens that a native consultant associates with her or his ethnotaxonomic identifications (voucher specimens, see Bye 1986),together with that person's critical comments, should be available to future workers once the research is published. -
Overkill, Glacial History, and the Extinction of North America's Ice Age Megafauna
PERSPECTIVE Overkill, glacial history, and the extinction of North America’s Ice Age megafauna PERSPECTIVE David J. Meltzera,1 Edited by Richard G. Klein, Stanford University, Stanford, CA, and approved September 23, 2020 (received for review July 21, 2020) The end of the Pleistocene in North America saw the extinction of 38 genera of mostly large mammals. As their disappearance seemingly coincided with the arrival of people in the Americas, their extinction is often attributed to human overkill, notwithstanding a dearth of archaeological evidence of human predation. Moreover, this period saw the extinction of other species, along with significant changes in many surviving taxa, suggesting a broader cause, notably, the ecological upheaval that occurred as Earth shifted from a glacial to an interglacial climate. But, overkill advocates ask, if extinctions were due to climate changes, why did these large mammals survive previous glacial−interglacial transitions, only to vanish at the one when human hunters were present? This question rests on two assumptions: that pre- vious glacial−interglacial transitions were similar to the end of the Pleistocene, and that the large mammal genera survived unchanged over multiple such cycles. Neither is demonstrably correct. Resolving the cause of large mammal extinctions requires greater knowledge of individual species’ histories and their adaptive tolerances, a fuller understanding of how past climatic and ecological changes impacted those animals and their biotic communities, and what changes occurred at the Pleistocene−Holocene boundary that might have led to those genera going extinct at that time. Then we will be able to ascertain whether the sole ecologically significant difference between previous glacial−interglacial transitions and the very last one was a human presence. -
Mitogenomics Supports an Unexpected Taxonomic Relationship for the Extinct Diving Duck Chendytes Lawi and Definitively Places the Extinct Labrador Duck ⁎ Janet C
Buckner, et al. Published in Molecular Phylogeny and Evolution, 122:102-109. 2018 Mitogenomics supports an unexpected taxonomic relationship for the extinct diving duck Chendytes lawi and definitively places the extinct Labrador Duck ⁎ Janet C. Bucknera, Ryan Ellingsona, David A. Goldb, Terry L. Jonesc, David K. Jacobsa, a Department of Ecology and Evolutionary Biology, University of California, Los Angeles, CA 90095, United States b Division of Biology and Biological Engineering, California Institute of Technology, Pasadena, CA 91125, United States c Department of Social Sciences, California Polytechnic State University, San Luis Obispo, CA 9340, United States ARTICLE INFO ABSTRACT Keywords: Chendytes lawi, an extinct flightless diving anseriform from coastal California, was traditionally classified as a sea Biodiversity duck, tribe Mergini, based on similarities in osteological characters. We recover and analyze mitochondrial Anatidae genomes of C. lawi and five additional Mergini species, including the extinct Labrador Duck, Camptorhynchus Ancient DNA labradorius. Despite its diving morphology, C. lawi is reconstructed as an ancient relictual lineage basal to the Labrador duck dabbling ducks (tribe Anatini), revealing an additional example of convergent evolution of characters related to Mitochondrial genome feeding behavior among ducks. The Labrador Duck is sister to Steller’s Eider which may provide insights into the California paleontology Duck evolution evolution and ecology of this poorly known extinct species. Our results demonstrate that inclusion of full length mitogenomes, from taxonomically distributed ancient and modern sources can improve phylogeny reconstruc- tion of groups previously assessed with shorter single-gene mitochondrial sequences. 1. Introduction an extended study by Livezey (1993) suggested placement in the eider genus Somateria. -
Pliocene and Early Pleistocene) Faunas from New Mexico
Chapter 12 Mammalian Biochronology of Blancan and Irvingtonian (Pliocene and Early Pleistocene) Faunas from New Mexico GARY S. MORGAN1 AND SPENCER G. LUCAS2 ABSTRACT Signi®cant mammalian faunas of Pliocene (Blancan) and early Pleistocene (early and medial Irvingtonian) age are known from the Rio Grande and Gila River valleys of New Mexico. Fossiliferous exposures of the Santa Fe Group in the Rio Grande Valley, extending from the EspanÄola basin in northern New Mexico to the Mesilla basin in southernmost New Mexico, have produced 21 Blancan and 6 Irvingtonian vertebrate assemblages; three Blancan faunas occur in the Gila River Valley in the Mangas and Duncan basins in southwestern New Mexico. More than half of these faunas contain ®ve or more species of mammals, and many have associated radioisotopic dates and/or magnetostratigraphy, allowing for correlation with the North American land-mammal biochronology. Two diverse early Blancan (4.5±3.6 Ma) faunas are known from New Mexico, the Truth or Consequences Local Fauna (LF) from the Palomas basin and the Buckhorn LF from the Mangas basin. The former contains ®ve species of mammals indicative of the early Blancan: Borophagus cf. B. hilli, Notolagus lepusculus, Neo- toma quadriplicata, Jacobsomys sp., and Odocoileus brachyodontus. Associated magnetostra- tigraphic data suggest correlation with either the Nunivak or Cochiti Subchrons of the Gilbert Chron (4.6±4.2 Ma), which is in accord with the early Blancan age indicated by the mam- malian biochronology. The Truth or Consequences LF is similar in age to the Verde LF from Arizona, and slightly older than the Rexroad 3 and Fox Canyon faunas from Kansas. -
A New Anseriform Genus and Species from the Nebraska Pliocene
A NEW ANSERIFORM GENUS AND SPECIES FROM THE NEBRASKA PLIOCENE LESTER L. SHORT AMONGavian fossilson loan to me from the University of Nebraska State Museumis the tarsometatarsusof a goose-likeanseriform bird from the early Plioceneof Nebraska. The tarsometatarsushas somefeatures of geeseand swans,and of the anatinetribe Tadornini,but it alsotends somewhattoward the Cairinini in someof its features. Comparisonwith extant and fossilAnseriformes in the American Museum of Natural History and the United States National Museum and a study of the literature have convincedme that this tarsometatarsusrepresents an undescribed speciesthat is sufficientlydistinct to warrant placementin a new genus. I thank the authoritiesof the above-mentionedmuseum for their help in conductingmy studies.I am gratefulto CharlesG. Sibley,who originally borrowedthe fossil,for permissionto studyit. It is a pleasureto acknowl- edgethe aid of C. B. Schultzfor the loan of the material, and H. B. Gundersonof the Universityof NebraskaState Museumfor usefulinfor- mationconcerning the fossil. The use and potential importance of stereophotographyin avian paleontologyhas beendiscussed by Cracraft (1968: 3-4). I hope the stereophotographsreproduced here will facilitatecomparisons by avian paleontologists. Heteroehen, new genus Type of genus.--Heterochenpratensis, new species. Diagnosis.--Anseriformtarsometatarsus, near the size of Anser anser, and characterizedby: trochleaenot spreadgreatly as in modern swans, geeseand sheldrakes;outer surfacegently curving toward distal end -
A Giant Anseriformes of the Neogene of The
Downloaded from http://rsos.royalsocietypublishing.org/ on January 11, 2017 The extreme insular adaptation of Garganornis rsos.royalsocietypublishing.org ballmanni Meijer, 2014: a Research giant Anseriformes of the Cite this article: Pavia M, Meijer HJM, Rossi Neogene of the MA, Göhlich UB. 2017 The extreme insular adaptation of Garganornis ballmanni Meijer, 2014: a giant Anseriformes of the Neogene of Mediterranean Basin the Mediterranean Basin. R. Soc. open sci. 1 2 4: 160722. Marco Pavia , Hanneke J. M. Meijer , Maria Adelaide http://dx.doi.org/10.1098/rsos.160722 Rossi3 and Ursula B. Göhlich4 1Dipartimento di Scienze della Terra, Museo di Geologia e Paleontologia, Università degli Studi di Torino, Via Valperga Caluso 35, 10125 Torino, Italy Received: 20 September 2016 2Department of Natural History, University Museum, University of Bergen, Postboks Accepted: 5 December 2016 7800, 5007 Bergen, Norway 3Soprintendenza archeologia, belle arti e paesaggio dell’Abruzzo, Via degli Agostiniani 14, 66100 Chieti, Italy 4Department of Geology and Paleontology, Natural History Museum Vienna, Subject Category: Burgring 7, 1010 Vienna, Austria Earth science MP, 0000-0002-5188-4155 Subject Areas: palaeontology New skeletal elements of the recently described endemic giant anseriform Garganornis ballmanni Meijer, 2014 are presented, coming from the type-area of the Gargano and from Scontrone, Keywords: southern and central Italy, respectively. The new remains fossil bird, Anseriformes, flightlessness, represent the first bird remains found at Scontrone so far, and insular gigantism, Miocene, Italy another shared element between these two localities, both part of the Apulia-Abruzzi Palaeobioprovince. The presence of a very reduced carpometacarpus confirms its flightlessness, only previously supposed on the basis of the very large size, while Author for correspondence: the morphologies of tarsometatarsus and posterior phalanges Marco Pavia clearly indicate the adaptation of G. -
Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the Use of Paleobiology for Natural Resource Management Policy Jeffrey M
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2014 Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy Jeffrey M. Martin East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Natural Resources and Conservation Commons, Natural Resources Management and Policy Commons, Paleobiology Commons, and the Paleontology Commons Recommended Citation Martin, Jeffrey M., "Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy" (2014). Electronic Theses and Dissertations. Paper 2360. https://dc.etsu.edu/ etd/2360 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy ______________________ A thesis presented to the faculty of the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences ______________________ by Jeff M. Martin May 2014 ______________________ Jim I. Mead, Chair Blaine W. Schubert Steven C. Wallace Keywords: Bison, Grand Canyon, Paleontology, Conservation, Geospatial, Paleobiology 1 ABSTRACT Late Pleistocene and Holocene Bison of Grand Canyon and Colorado Plateau: Implications from the use of Paleobiology for Natural Resource Management Policy by Jeff M. -
The Dynamic Geomorphic Setting of the Late Pleistocene Hartley Mammoth Site
University of New Mexico UNM Digital Repository Earth and Planetary Sciences ETDs Electronic Theses and Dissertations Spring 3-2-2017 THE DYNAMIC GEOMORPHIC SETTING OF THE LATE PLEISTOCENE HARTLEY MAMMOTH SITE: BURIAL AND SKELETAL PRESERVATION IN A SLUMP-BLOCK DEPRESSION NEAR ABIQUIU, NEW MEXICO Jennifer K. Muus University of New Mexico Follow this and additional works at: https://digitalrepository.unm.edu/eps_etds Part of the Geology Commons, and the Geomorphology Commons Recommended Citation Muus, Jennifer K.. "THE DYNAMIC GEOMORPHIC SETTING OF THE LATE PLEISTOCENE HARTLEY MAMMOTH SITE: BURIAL AND SKELETAL PRESERVATION IN A SLUMP-BLOCK DEPRESSION NEAR ABIQUIU, NEW MEXICO." (2017). https://digitalrepository.unm.edu/eps_etds/189 This Thesis is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. i Jennifer Muus ______________________________ Candidate Earth and Planetary Sciences __________________ Department This thesis is approved, and it is acceptable in quality and form for publication: Approved by the Thesis Committee: Dr. Grant Meyer, Chairperson ___________________________________ Dr. Leslie McFadden Dr. Bruce Huckell _____________________________________________ ii THE DYNAMIC GEOMORPHIC SETTING OF THE LATE PLEISTOCENE HARTLEY MAMMOTH SITE: BURIAL AND SKELETAL PRESERVATION IN A SLUMP-BLOCK DEPRESSION NEAR ABIQUIU, NEW MEXICO BY JENNIFER KRISTINE MUUS B.A. GEOLOGY, WESTERN WASHINGTON UNIVERSITY, 2010 B.SC. HONOURS PHYSICAL GEOGRAPHY, VICTORIA UNIVERSITY OF WELLINGTON, 2012 THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science Earth and Planetary Sciences The University of New Mexico Albuquerque, New Mexico May, 2017 iii ACKNOWLEDGEMENTS I would like to thank my advisor and committee chair, Dr. -
Domesticated Megafauna of Americas: Needs, Possibilities and Results
Interdisciplinary Description of Complex Systems 18(2-A), 72-84, 2020 DOMESTICATED MEGAFAUNA OF AMERICAS: NEEDS, POSSIBILITIES AND RESULTS Dragica Šalamon*, Luana Velagić, Bernard Kuhar and Alen Džidić University of Zagreb – Faculty of Agriculture Zagreb, Croatia DOI: 10.7906/indecs.18.2.1 Received: 15 May 2019. Review article Accepted: 25 February 2020. ABSTRACT The article aims to determine why so few domestic animals originated in American domestication centres. The knowledge has been gathered from interdisciplinary sources taking into account recent archaeogenomic and spatial analysis research. The process of domestication is described, and different domestication centres are compared to the domestication needs and opportunities on the American continents. Human colonization of the American continent is considered. Important domestication centres on the North and South American continent are described. Dogs that colonized the American continents together with people and horses that arrived during the European colonization are also considered. The analysis of the American megafauna that lived on the continent during the first colonization of Homo sapiens showed that the big extinction occurred due to climate change and overhunting. Comparing the evolutionary process of domestication between Afro-Eurasia and America we found that there was no intentional domestication in areas peripheral to the original domestication centres in the Americas. Also, diversification of the domesticated animal purpose in the Americas is limited to dogs. KEY WORDS North America, South America, domestication, animals, megafauna CLASSIFICATION JEL: N50 *Corresponding author, : [email protected]; -; *Faculty of Agriculture, Svetošimunska cesta 25, HR – 10 000 Zagreb, Croatia Domesticated megafauna of Americas: needs, possibilities and results INTRODUCTION Anatomically modern human (Homo sapiens) evolved in Africa around 300 000 years ago [1].