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  • 1
    Call number: 9/M 07.0421(395) ; https://doi.org/10.1144/SP395
    In: Geological Society special publication
    Description / Table of Contents: Humankind has pervasively influenced the Earth's atmosphere, biosphere, geosphere, hydrosphere and cryosphere, arguably to the point of fashioning a new geological epoch, the Anthropocene. To constrain the Anthropocene as a potential formal unit within the Geological Time Scale, a spectrum of indicators of anthropogenically-induced environmental change is considered, and shown as stratigraphical signals that may be used to characterize an Anthropocene unit, and to recognize its base. This volume describes a range of evidence that may help to define this potential new time unit and details key signatures that could be used in its definition. These signatures include lithostratigraphical (novel deposits, minerals and mineral magnetism), biostratigraphical (macro- and micro-palaeontological successions and human-induced trace fossils) and chemostratigraphical (organic, inorganic and radiogenic signatures in deposits, speleothems and ice and volcanic eruptions). We include, finally, the suggestion that humans have created a further sphere, the technosphere, that drives global change.
    Type of Medium: Monograph available for loan
    Pages: 393 Seiten , Illustrationen, Diagramme
    ISBN: 9781862396289
    Series Statement: Geological Society special publication 395
    Classification:
    Historical Geology
    Note: TABLE OF CONTENTS An introduction to the Anthropocene: case for and against a new epoch A stratigraphical basis for the Anthropocene? / Colin N. Waters, Jan A. Zalasiewicz, Mark Williams, Michael A. Ellis and Andrea M. Snelling / Geological Society, London, Special Publications, 395, 1-21, 24 March 2014, https://doi.org/10.1144/SP395.18 The ‘Anthropocene’ as a ratified unit in the ICS International Chronostratigraphic Chart: fundamental issues that must be addressed by the Task Group / S. C. Finney / Geological Society, London, Special Publications, 395, 23-28, 24 October 2013, https://doi.org/10.1144/SP395.9 The term ‘Anthropocene’ in the context of formal geological classification / P. L. Gibbard and M. J. C. Walker / Geological Society, London, Special Publications, 395, 29-37, 25 October 2013, https://doi.org/10.1144/SP395.1 Can an Anthropocene Series be defined and recognized? / Jan Zalasiewicz, Mark Williams and Colin N. Waters / Geological Society, London, Special Publications, 395, 39-53, 10 March 2014, https://doi.org/10.1144/SP395.16 The nature of anthropogenic deposits and landscape modification An assessment of lithostratigraphy for anthropogenic deposits / J. R. Ford, S. J. Price, A. H. Cooper and C. N. Waters / Geological Society, London, Special Publications, 395, 55-89, 8 April 2014, https://doi.org/10.1144/SP395.12 The relationship between archaeological stratigraphy and artificial ground and its significance in the Anthropocene / M. Edgeworth / Geological Society, London, Special Publications, 395, 91-108, 25 October 2013, https://doi.org/10.1144/SP395.3 The mineral signature of the Anthropocene in its deep-time context / Jan Zalasiewicz, Ryszard Kryza and Mark Williams / Geological Society, London, Special Publications, 395, 109-117, 19 December 2013, https://doi.org/10.1144/SP395.2 Geomagnetic and mineral magnetic characterization of the Anthropocene / Ian Snowball, Mark W. Hounslow and Andreas Nilsson / Geological Society, London, Special Publications, 395, 119-141, 19 December 2013, https://doi.org/10.1144/SP395.13 A biostratigraphical signature for the Anthropocene Is the fossil record of complex animal behaviour a stratigraphical analogue for the Anthropocene? / M. Williams, J. A. Zalasiewicz, C. N. Waters and E. Landing / Geological Society, London, Special Publications, 395, 143-148, 25 October 2013, https://doi.org/10.1144/SP395.8 Palaeontological evidence for defining the Anthropocene / Anthony D. Barnosky / Geological Society, London, Special Publications, 395, 149-165, 24 October 2013, https://doi.org/10.1144/SP395.6 Coral reefs in the Anthropocene: persistence or the end of the line? / O. Hoegh-Guldberg / Geological Society, London, Special Publications, 395, 167-183, 20 March 2014, https://doi.org/10.1144/SP395.17 Microbiotic signatures of the Anthropocene in marginal marine and freshwater palaeoenvironments / I. P. Wilkinson, C. Poirier, M. J. Head, C. D. Sayer and J. Tibby / Geological Society, London, Special Publications, 395, 185-219, 31 January 2014, https://doi.org/10.1144/SP395.14 Geochemical signatures and catastrophic events Assessing the Anthropocene with geochemical methods / Agnieszka Gałuszka, Zdzisław M. Migaszewski and Jan Zalasiewicz / Geological Society, London, Special Publications, 395, 221-238, 24 October 2013, https://doi.org/10.1144/SP395.5 Definition of the Anthropocene: a view from the underworld / Ian J. Fairchild and Silvia Frisia / Geological Society, London, Special Publications, 395, 239-254, 24 October 2013, https://doi.org/10.1144/SP395.7 Ice Sheets and the Anthropocene / Eric W. Wolff / Geological Society, London, Special Publications, 395, 255-263, 25 November 2013, https://doi.org/10.1144/SP395.10 The release and persistence of radioactive anthropogenic nuclides / Gary J. Hancock, Stephen G. Tims, L. Keith Fifield and Ian T. Webster / Geological Society, London, Special Publications, 395, 265-281, 28 February 2014, https://doi.org/10.1144/SP395.15 Volcanic markers for dating the onset of the Anthropocene / Victoria C. Smith / Geological Society, London, Special Publications, 395, 283-299, 21 November 2013, https://doi.org/10.1144/SP395.11 The technosphere concept Technology as a geological phenomenon: implications for human well-being / P. K. Haff / Geological Society, London, Special Publications, 395, 301-309, 24 October 2013, https://doi.org/10.1144/SP395.4
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    Branch Library: GFZ Library
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  • 2
    Keywords: Anthropocene ; stratigraphy
    Description / Table of Contents: An introduction to the Anthropocene: case for and against a new epoch --- A stratigraphical basis for the Anthropocene? / Colin N. Waters, Jan A. Zalasiewicz, Mark Williams, Michael A. Ellis and Andrea M. Snelling / Geological Society, London, Special Publications, 395, 1-21, 24 March 2014, https://doi.org/10.1144/SP395.18 --- The ‘Anthropocene’ as a ratified unit in the ICS International Chronostratigraphic Chart: fundamental issues that must be addressed by the Task Group / S. C. Finney / Geological Society, London, Special Publications, 395, 23-28, 24 October 2013, https://doi.org/10.1144/SP395.9 --- The term ‘Anthropocene’ in the context of formal geological classification / P. L. Gibbard and M. J. C. Walker / Geological Society, London, Special Publications, 395, 29-37, 25 October 2013, https://doi.org/10.1144/SP395.1 --- Can an Anthropocene Series be defined and recognized? / Jan Zalasiewicz, Mark Williams and Colin N. Waters / Geological Society, London, Special Publications, 395, 39-53, 10 March 2014, https://doi.org/10.1144/SP395.16 --- The nature of anthropogenic deposits and landscape modification --- An assessment of lithostratigraphy for anthropogenic deposits / J. R. Ford, S. J. Price, A. H. Cooper and C. N. Waters / Geological Society, London, Special Publications, 395, 55-89, 8 April 2014, https://doi.org/10.1144/SP395.12 --- The relationship between archaeological stratigraphy and artificial ground and its significance in the Anthropocene / M. Edgeworth / Geological Society, London, Special Publications, 395, 91-108, 25 October 2013, https://doi.org/10.1144/SP395.3 --- The mineral signature of the Anthropocene in its deep-time context / Jan Zalasiewicz, Ryszard Kryza and Mark Williams / Geological Society, London, Special Publications, 395, 109-117, 19 December 2013, https://doi.org/10.1144/SP395.2 --- Geomagnetic and mineral magnetic characterization of the Anthropocene / Ian Snowball, Mark W. Hounslow and Andreas Nilsson / Geological Society, London, Special Publications, 395, 119-141, 19 December 2013, https://doi.org/10.1144/SP395.13 --- A biostratigraphical signature for the Anthropocene --- Is the fossil record of complex animal behaviour a stratigraphical analogue for the Anthropocene? / M. Williams, J. A. Zalasiewicz, C. N. Waters and E. Landing / Geological Society, London, Special Publications, 395, 143-148, 25 October 2013, https://doi.org/10.1144/SP395.8 --- Palaeontological evidence for defining the Anthropocene / Anthony D. Barnosky / Geological Society, London, Special Publications, 395, 149-165, 24 October 2013, https://doi.org/10.1144/SP395.6 --- Coral reefs in the Anthropocene: persistence or the end of the line? / O. Hoegh-Guldberg / Geological Society, London, Special Publications, 395, 167-183, 20 March 2014, https://doi.org/10.1144/SP395.17 --- Microbiotic signatures of the Anthropocene in marginal marine and freshwater palaeoenvironments / I. P. Wilkinson, C. Poirier, M. J. Head, C. D. Sayer and J. Tibby / Geological Society, London, Special Publications, 395, 185-219, 31 January 2014, https://doi.org/10.1144/SP395.14 --- Geochemical signatures and catastrophic events --- Assessing the Anthropocene with geochemical methods / Agnieszka Gałuszka, Zdzisław M. Migaszewski and Jan Zalasiewicz / Geological Society, London, Special Publications, 395, 221-238, 24 October 2013, https://doi.org/10.1144/SP395.5 --- Definition of the Anthropocene: a view from the underworld / Ian J. Fairchild and Silvia Frisia / Geological Society, London, Special Publications, 395, 239-254, 24 October 2013, https://doi.org/10.1144/SP395.7 --- Ice Sheets and the Anthropocene / Eric W. Wolff / Geological Society, London, Special Publications, 395, 255-263, 25 November 2013, https://doi.org/10.1144/SP395.10 --- The release and persistence of radioactive anthropogenic nuclides / Gary J. Hancock, Stephen G. Tims, L. Keith Fifield and Ian T. Webster / Geological Society, London, Special Publications, 395, 265-281, 28 February 2014, https://doi.org/10.1144/SP395.15 --- Volcanic markers for dating the onset of the Anthropocene / Victoria C. Smith / Geological Society, London, Special Publications, 395, 283-299, 21 November 2013, https://doi.org/10.1144/SP395.11 --- The technosphere concept --- Technology as a geological phenomenon: implications for human well-being / P. K. Haff / Geological Society, London, Special Publications, 395, 301-309, 24 October 2013, https://doi.org/10.1144/SP395.4
    Pages: Online-Ressource (VI, 321 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862396715
    Language: English
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  • 3
    Publication Date: 2016-07-21
    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-20 th 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 towards 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.
    Electronic ISSN: 2328-4277
    Topics: Geosciences
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  • 4
    Publication Date: 2018
    Description: The Anthropocene Review, Ahead of Print. 〈br/〉
    Print ISSN: 2053-0196
    Electronic ISSN: 2053-020X
    Topics: Geography
    Published by Sage
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  • 5
    Publication Date: 2018
    Description: The Anthropocene Review, Volume 5, Issue 3, Page 222-229, December 2018. 〈br/〉
    Print ISSN: 2053-0196
    Electronic ISSN: 2053-020X
    Topics: Geography
    Published by Sage
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  • 6
    Publication Date: 2016-02-04
    Description: Biospheric relationships between production and consumption of biomass have been resilient to changes in the Earth system over billions of years. This relationship has increased in its complexity, from localised ecosystems predicated on anaerobic microbial production and consumption, to a global biosphere founded on primary production from oxygenic photoautotrophs, through the evolution of Eukarya, metazoans, and the complexly networked ecosystems of microbes, animals, fungi and plants that characterise the Phanerozoic Eon (the last ~541 million years of Earth history). At present, one species, Homo sapiens , is refashioning this relationship between consumption and production in the biosphere with unknown consequences. This has left a distinctive stratigraphy of the production and consumption of biomass, of natural resources, and of produced goods. This can be traced through stone tool technologies and geochemical signals, later unfolding into a diachronous signal of technofossils and human bioturbation across the planet, leading to stratigraphically almost isochronous signals developing by the mid-20 th century. These latter signals may provide an invaluable resource for informing and constraining a formal Anthropocene chronostratigraphy, but are perhaps yet more important as tracers of a biosphere state that is characterised by a geologically unprecedented pattern of global energy flow that is now pervasively influenced and mediated by humans, and which is necessary for maintaining the complexity of modern human societies.
    Electronic ISSN: 2328-4277
    Topics: Geosciences
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  • 7
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  • 9
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    American Association for the Advancement of Science (AAAS)
    In: Science
    Publication Date: 2016-08-16
    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. Authors: Colin N. Waters, Jan Zalasiewicz, Colin Summerhayes, Anthony D. Barnosky, Clément Poirier, Agnieszka Gałuszka, Alejandro Cearreta, Matt Edgeworth, Erle C. Ellis, Michael Ellis, Catherine Jeandel, Reinhold Leinfelder, J. R. McNeill, Daniel deB. Richter, Will Steffen, James Syvitski, Davor Vidas, Michael Wagreich, Mark Williams, An Zhisheng, Jacques Grinevald, Eric Odada, Naomi Oreskes, Alexander P. Wolfe
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Geosciences , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 10
    Publication Date: 2016-03-01
    Description: Progradational fluvio-deltaic systems tend towards but cannot reach equilibrium, a state in which the longitudinal profile does not change shape and all sediment is bypassed beyond the shoreline. They cannot reach equilibrium because progradation of the shoreline requires aggradation along the longitudinal profile. Therefore progradation provides a negative feedback, unless relative sea level falls at a sufficient rate to cause non-aggradational extension of the longitudinal profile. How closely fluvio-deltaic systems approach equilibrium is dependent on their progradation rate, which is controlled by water depth and downstream allogenic controls, and governs sediment partitioning between the fluvial, deltaic, and marine domains. Here, six analogue models of coastal fluvio-deltaic systems and small prograding shelf margins are examined to better understand the effect of water depth, subsidence, and relative sea-level variations upon longitudinal patterns of sediment partitioning and grain-size distribution that eventually determine large-scale stratigraphic architecture. Fluvio-deltaic systems prograding in relatively deep-water environments are characterized by relatively low progradation rates compared to shallow-water systems. This allows these deeper water systems to approach equilibrium more closely, enabling them to construct less concave and steeper longitudinal profiles that provide low accommodation to fluvial systems. Glacio-eustatic sea-level variations and subsidence modulate the effects of water depth on the longitudinal profile. Systems are closest to equilibrium during falling relative sea level and early lowstand, resulting in efficient sediment transport towards the shoreline at those times. Additionally, the strength of the response to relative sea-level fall differs depending on water depth. In systems prograding into deep water, relative sea-level fall causes higher sediment bypass rates and generates significantly stronger erosion than in shallow-water systems, which increases the probability of incised-valley formation. Water depth in the receiving basin thus forms a first-order control on the sediment partitioning along the longitudinal profile of fluvio-deltaic systems and the shelf clinoform style. It also forms a control on the availability of sand-grade sediment at the shoreline that can potentially be remobilized and redistributed into deeper marine environments. Key findings are subsequently applied to the literature of selected shelf clinoform successions.
    Print ISSN: 1527-1404
    Electronic ISSN: 1938-3681
    Topics: Geosciences
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