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Are we now living in the Anthropocene
a Department of Geology, University of Leicester, Leicester LE1 7RH, UK
b Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
c Department of Earth Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK
d Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK
e Department of Earth Sciences, University of Liverpool, Liverpool L69 3BX, UK
f Royal Botanic Gardens, Birdwood Avenue, South Yarra, Melbourne, Victoria, Australia
g School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth, Hampshire PO1 3QL, UK, and Department of Palaeontology, Natural History Museum, London SW7 5BD, UK
h Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK
i Petro-Strat Ltd, 33 Royston Road, St. Albans, Herts AL1 5NF, UK, and Department of Palaeontology, Natural History Museum, London SW7 5BD, UK
j Centre for Environmental Magnetism and Palaeomagnetism, Geography Department, Lancaster University, Lancaster LA1 4YB, UK
k School of Earth, Ocean and Planetary Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3YE, UK
l British Geological Survey, Keyworth, Nottinghamshire NG12 5GG, UK
m National Oceanography Centre, University of Southampton, University Road, Southampton SO14 3ZH, UK
n BG Group plc, 100 Thames Valley Park Drive, Reading RG6 1PT, UK
o Scarborough Centre for Environmental and Marine Sciences, University of Hull, Scarborough Campus, Filey Road, Scarborough YO11 3AZ, UK, and Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK
p British Geological Survey, Murchison House, Edinburgh EH9 3LA, UK
The term Anthropocene, proposed and increasingly employed to denote the current interval of anthropogenic global environmental change, may be discussed on stratigraphic grounds. A case can be made for its consideration as a formal epoch in that, since the start of the Industrial Revolution, Earth has endured changes sufficient to leave a global stratigraphic signature distinct from that of the Holocene or of previous Pleistocene interglacial phases, encompassing novel biotic, sedimentary, and geochemical change. These changes, although likely only in their initial phases, are sufficiently distinct and robustly established for suggestions of a Holocene–Anthropocene boundary in the recent historical past to be geologically reasonable. The boundary may be defined either via Global Stratigraphic Section and Point (“golden spike”) locations or by adopting a numerical date. Formal adoption of this term in the near future will largely depend on its utility, particularly to earth scientists working on late Holocene successions. This datum, from the perspective of the far future, will most probably approximate a distinctive stratigraphic boundary.
Received: October 17, 2007; Accepted: November 6, 2007
DOI: 10.1130/GSAT01802A.1
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