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  • 1
    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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  • 2
    Publication Date: 2013-10-26
    Description: Anthropogenic chemical contamination is one of the most evident signals of human influence on the environment. The large amounts of industrially produced pollutants that have been introduced, over decades, into air, soil and water have caused modifications to natural elemental cycling. Anthropogenic contamination usually leads to enrichment in many elements, particularly in industrial areas. Thus, certain elements and their isotopes can be used as geochemical tracers of anthropogenic impact. Some human-induced changes in the environment may be regarded as a secondary effect of pollution, such as acidification, which causes increased geochemical mobility of several trace elements in surficial deposits. Methods used by geochemists to assess the scale of anthropogenic influence on the environment include calculations of anthropogenic influence on the environment via enrichment and contamination factors, geoaccumulation index and pollution load index. The use of geochemical background levels for delineating between natural and anthropogenic pollution is important. A historical perspective of anthropogenic contamination, allied with isotopic and geochemical signatures in dated sediment cores, may be applied to help define the Anthropocene.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 3
    Publication Date: 2016-09-06
    Print ISSN: 1735-1472
    Electronic ISSN: 1735-2630
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 4
    Publication Date: 2014-11-25
    Print ISSN: 1735-1472
    Electronic ISSN: 1735-2630
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 5
    Publication Date: 2022-03-21
    Description: Stratigraphy provides insights into the evolution and dynamics of the Earth System over its long history. With recent developments in Earth System science, changes in Earth System dynamics can now be observed directly and projected into the near future. An integration of the two approaches provides powerful insights into the nature and significance of contemporary changes to Earth. From both perspectives, the Earth has been pushed out of the Holocene Epoch by human activities, with the mid‐20th century a strong candidate for the start date of the Anthropocene, the proposed new epoch in Earth history. Here we explore two contrasting scenarios for the future of the Anthropocene, recognizing that the Earth System has already undergone a substantial transition away from the Holocene state. A rapid shift of societies toward the UN Sustainable Development Goals could stabilize the Earth System in a state with more intense interglacial conditions than in the late Quaternary climate regime and with little further biospheric change. In contrast, a continuation of the present Anthropocene trajectory of growing human pressures will likely lead to biotic impoverishment and a much warmer climate with a significant loss of polar ice.
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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