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  • 1
    Publication Date: 2004-10-02
    Description: One of the great debates about extinction is whether humans or climatic change caused the demise of the Pleistocene megafauna. Evidence from paleontology, climatology, archaeology, and ecology now supports the idea that humans contributed to extinction on some continents, but human hunting was not solely responsible for the pattern of extinction everywhere. Instead, evidence suggests that the intersection of human impacts with pronounced climatic change drove the precise timing and geography of extinction in the Northern Hemisphere. The story from the Southern Hemisphere is still unfolding. New evidence from Australia supports the view that humans helped cause extinctions there, but the correlation with climate is weak or contested. Firmer chronologies, more realistic ecological models, and regional paleoecological insights still are needed to understand details of the worldwide extinction pattern and the population dynamics of the species involved.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Barnosky, Anthony D -- Koch, Paul L -- Feranec, Robert S -- Wing, Scott L -- Shabel, Alan B -- New York, N.Y. -- Science. 2004 Oct 1;306(5693):70-5.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Integrative Biology and Museums of Paleontology and Vertebrate Zoology, University of California, Berkeley, CA 94720, USA. barnosky@socrates.berkeley.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/15459379" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Archaeology ; Climate ; Conservation of Natural Resources ; *Ecosystem ; Human Activities ; Humans ; *Paleontology ; *Population Dynamics ; Predatory Behavior ; Time
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2011-03-04
    Description: Palaeontologists characterize mass extinctions as times when the Earth loses more than three-quarters of its species in a geologically short interval, as has happened only five times in the past 540 million years or so. Biologists now suggest that a sixth mass extinction may be under way, given the known species losses over the past few centuries and millennia. Here we review how differences between fossil and modern data and the addition of recently available palaeontological information influence our understanding of the current extinction crisis. Our results confirm that current extinction rates are higher than would be expected from the fossil record, highlighting the need for effective conservation measures.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Barnosky, Anthony D -- Matzke, Nicholas -- Tomiya, Susumu -- Wogan, Guinevere O U -- Swartz, Brian -- Quental, Tiago B -- Marshall, Charles -- McGuire, Jenny L -- Lindsey, Emily L -- Maguire, Kaitlin C -- Mersey, Ben -- Ferrer, Elizabeth A -- R01 GM069801/GM/NIGMS NIH HHS/ -- England -- Nature. 2011 Mar 3;471(7336):51-7. doi: 10.1038/nature09678.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Integrative Biology, University of California, Berkeley, California 94720, USA. barnosky@berkeley.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21368823" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Biodiversity ; Conservation of Natural Resources/methods/trends ; Earth (Planet) ; Endangered Species/history/*statistics & numerical data/trends ; *Extinction, Biological ; Fossils ; History, 21st Century ; History, Ancient ; Human Activities ; Humans
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2012-06-09
    Description: Localized ecological systems are known to shift abruptly and irreversibly from one state to another when they are forced across critical thresholds. Here we review evidence that the global ecosystem as a whole can react in the same way and is approaching a planetary-scale critical transition as a result of human influence. The plausibility of a planetary-scale 'tipping point' highlights the need to improve biological forecasting by detecting early warning signs of critical transitions on global as well as local scales, and by detecting feedbacks that promote such transitions. It is also necessary to address root causes of how humans are forcing biological changes.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Barnosky, Anthony D -- Hadly, Elizabeth A -- Bascompte, Jordi -- Berlow, Eric L -- Brown, James H -- Fortelius, Mikael -- Getz, Wayne M -- Harte, John -- Hastings, Alan -- Marquet, Pablo A -- Martinez, Neo D -- Mooers, Arne -- Roopnarine, Peter -- Vermeij, Geerat -- Williams, John W -- Gillespie, Rosemary -- Kitzes, Justin -- Marshall, Charles -- Matzke, Nicholas -- Mindell, David P -- Revilla, Eloy -- Smith, Adam B -- R01 GM069801/GM/NIGMS NIH HHS/ -- England -- Nature. 2012 Jun 6;486(7401):52-8. doi: 10.1038/nature11018.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Integrative Biology, University of California, Berkeley, California 94720, USA. barnosky@berkeley.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22678279" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Climate Change/*statistics & numerical data ; *Earth (Planet) ; *Ecosystem ; Environmental Monitoring ; Forecasting ; Human Activities ; Humans ; *Models, Theoretical
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 1996-06-14
    Description: Analyses of fossil mammal faunas from 2945 localities in the United States demonstrate that the geographic ranges of individual species shifted at different times, in different directions, and at different rates in response to late Quaternary environmental fluctuations. The geographic pattern of faunal provinces was similar for the late Pleistocene and late Holocene, but differing environmental gradients resulted in dissimilar species composition for these biogeographic regions. Modern community patterns emerged only in the last few thousand years, and many late Pleistocene communities do not have modern analogs. Faunal heterogeneity was greater in the late Pleistocene.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Graham -- Lundelius Jr -- Schroeder -- Toomey III -- Anderson -- Barnosky -- Burns -- Churcher -- Grayson -- Guthrie -- Harington -- Jefferson -- Martin -- McDonald -- Morlan -- Semken Jr -- Webb -- Werdelin -- Wilson -- New York, N.Y. -- Science. 1996 Jun 14;272(5268):1601-6.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉R. W. Graham, M. A. Graham, E. K. Schroeder, and R. S. Toomey III are at Research and Collections Center, Illinois State Museum, 1011 East Ash, Springfield, IL 62703, USA. E. L. Lundelius Jr., Department of Geological Sciences, University of Texas, Austin, TX 78712, USA. E. Anderson, Denver Museum of Natural History, Denver, CO 80205, USA. A. D. Barnosky, Mountain Research Center, Montana State University, Bozeman, MT 59715, USA. J. A. Burns, Provincial Museum of Alberta, Edmonton, Alberta, Canada T5N 0M6. C. S. Churcher, Department of Zoology, University of Toronto, Toronto, Ontario, Canada M5S 1A1. D. K. Grayson, Department of Anthropology, University of Washington, Seattle, WA 98195, USA. R. D. Guthrie, Department of Biology, University of Alaska, Fairbanks, AK 99701, USA. C. R. Harington, Earth Sciences Section (Paleobiology), Canadian Museum of Nature, Ottawa, Ontario, Canada K1P 6P4. G. T. Jefferson, Anza-Borrego Desert State Park, 200 Palm Canyon Drive, Borrego Springs, CA 92004, USA. L. D. Martin, Museum of Natural History, University of Kansas, Lawrence, KS 66045, USA. H. G. McDonald, Hagerman Fossil Beds National Monument, Post Office Box 570, Hagerman, ID 83332, USA. R. E. Morlan, Canadian Museum of Civilization, Post Office Box 3100 Station B, Hull, Quebec, Canada J8X 4H2. H. A. Semken Jr., Department of Geology, University of Iowa, Iowa City, IA 52242, USA. S. D. Webb, Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA. L. Werdelin, Department of Paleozoology, Swedish Museum, Box 50007, S-104 05 Stockholm, Sweden. M. C. Wilson, Department of Archaeology, Simon Fraser University, Burnaby, BC, Canada V5A 1S6.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/8662471" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 2016-01-09
    Description: Human activity is leaving a pervasive and persistent signature on Earth. Vigorous debate continues about whether this warrants recognition as a new geologic time unit known as the Anthropocene. We review anthropogenic markers of functional changes in the Earth system through the stratigraphic record. The appearance of manufactured materials in sediments, including aluminum, plastics, and concrete, coincides with global spikes in fallout radionuclides and particulates from fossil fuel combustion. Carbon, nitrogen, and phosphorus cycles have been substantially modified over the past century. Rates of sea-level rise and the extent of human perturbation of the climate system exceed Late Holocene changes. Biotic changes include species invasions worldwide and accelerating rates of extinction. These combined signals render the Anthropocene stratigraphically distinct from the Holocene and earlier epochs.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Waters, Colin N -- Zalasiewicz, Jan -- Summerhayes, Colin -- Barnosky, Anthony D -- Poirier, Clement -- Galuszka, Agnieszka -- Cearreta, Alejandro -- Edgeworth, Matt -- Ellis, Erle C -- Ellis, Michael -- Jeandel, Catherine -- Leinfelder, Reinhold -- McNeill, J R -- Richter, Daniel deB -- Steffen, Will -- Syvitski, James -- Vidas, Davor -- Wagreich, Michael -- Williams, Mark -- Zhisheng, An -- Grinevald, Jacques -- Odada, Eric -- Oreskes, Naomi -- Wolfe, Alexander P -- New York, N.Y. -- Science. 2016 Jan 8;351(6269):aad2622. doi: 10.1126/science.aad2622.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉British Geological Survey, Keyworth, Nottingham NG12 5GG, UK. ; Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK. ; Scott Polar Research Institute, Cambridge University, Lensfield Road, Cambridge CB2 1ER, UK. ; Department of Integrative Biology, Museum of Paleontology, and Museum of Vertebrate Zoology, University of California-Berkeley, Berkeley, CA 94720, USA. ; Morphodynamique Continentale et Cotiere, Universite de Caen Normandie, Centre National de la Recherche Scientifique (CNRS), 24 Rue des Tilleuls, F-14000 Caen, France. ; Geochemistry and the Environment Division, Institute of Chemistry, Jan Kochanowski University, 15G Swietokrzyska Street, 25-406 Kielce, Poland. ; Departamento de Estratigrafia y Paleontologia, Facultad de Ciencia y Tecnologia, Universidad del Pais Vasco/Euskal Herriko Unibertsitatea, Apartado 644, 48080 Bilbao, Spain. ; School of Archaeology and Ancient History, University of Leicester, University Road, Leicester LE1 7RH, UK. ; Department of Geography and Environmental Systems, University of Maryland-Baltimore County, Baltimore, MD 21250, USA. ; Laboratoire d'Etudes en Geophysique et Oceanographie Spatiales (CNRS, Centre National d'Etudes Spatiales, Institut de Recherche pour le Developpement, Universite Paul Sabatier), 14 Avenue Edouard Belin, 31400 Toulouse, France. ; Department of Geological Sciences, Freie Universitat Berlin, Malteserstrasse 74-100/D, 12249 Berlin, Germany. ; Georgetown University, Washington, DC, USA. ; Nicholas School of the Environment, Duke University, Box 90233, Durham, NC 27516, USA. ; The Australian National University, Canberra, Australian Capital Territory 0200, Australia. ; Department of Geological Sciences, University of Colorado-Boulder, Box 545, Boulder, CO 80309-0545, USA. ; Marine Affairs and Law of the Sea Programme, The Fridtjof Nansen Institute, Lysaker, Norway. ; Department of Geodynamics and Sedimentology, University of Vienna, A-1090 Vienna, Austria. ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, Beijing Normal University, Beijing 100875, China. ; Institut de Hautes Etudes Internationales et du Developpement, Chemin Eugene Rigot 2, 1211 Geneve 11, Switzerland. ; Department of Geology, University of Nairobi, Nairobi, Kenya. ; Department of the History of Science, Harvard University, Cambridge, MA 02138, USA. ; Department of Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9, Canada.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26744408" target="_blank"〉PubMed〈/a〉
    Keywords: Aluminum/analysis ; *Biota ; Carbon Cycle ; Climate ; Construction Materials/analysis ; *Earth (Planet) ; Fossil Fuels/adverse effects ; Geologic Sediments/*chemistry ; *Human Activities ; Humans ; Ice/analysis ; Introduced Species ; Plastics/analysis ; Radioactive Fallout/analysis ; Radioisotopes/analysis
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 1982-04-09
    Description: The locomotion of proscalopid moles, an extinct group restricted to North America, differed from that of other animals. Analysis of a newly discovered and relatively complete and articulated skeleton shows that the digging technique of proscalopids involved a combination of motions that has not been observed in modern fossorial insectivores. The many anatomical peculiarities of proscalopids are related to their specialized digging technique and justify their assignment to a new family of insectivores, the Proscalopidae.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Barnosky, A D -- New York, N.Y. -- Science. 1982 Apr 9;216(4542):183-5.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17736251" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
    Publication Date: 1985-04-19
    Description: Fossils of the late Pleistocene elk Megaloceros giganteus from Ballybetagh bog, near Dublin, Ireland, indicate that males segregated from females during winters. The segregation implies seasonal rutting and polygynous mating and is consistent with the idea that large antlers functioned for social display. Within male groups, winterkill was the chief cause of death and was highest among juveniles and small adults with small antlers. There is no evidence to support the popular conception that heavy antlers caused animals to drown or become mired.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Barnosky, A D -- New York, N.Y. -- Science. 1985 Apr 19;228(4697):340-4.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17790237" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 8
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 17 (1989), S. 413-436 
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 9
  • 10
    Publication Date: 2008-08-11
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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