STRATI 2013 pp 909-914 | Cite as

The Anthropocene: A Geomorphological and Sedimentary View

  • Antony G. Brown
Conference paper
Part of the Springer Geology book series (SPRINGERGEOL)

Abstract

The “Anthropocene”, as used to describe the interval of recent Earth history during which humans have had an “overwhelming” effect on the Earth system, is now being formally considered as a possible new geological Epoch. Such a new geological time interval (possibly equivalent to the Pleistocene Epoch) requires both theoretical justification as well as empirical evidence preserved within the geological record. Since the geological record is driven by geomorphological processes, geomorphology has to be an integral part of this consideration given that it is Earth-surface processes that produce terrestrial and near-shore stratigraphy. This paper sets a priori considerations concerning the possible formalisation of the Anthropocene from a geomorphological perspective, including the recognition of human dominance in sedimentary transport systems, the boundary problem, and the spatial diachrony of “anthropogenic geomorphology”.

Keywords

Earth-surface processes Sediment transport Fluvial geomorphology Alluviation 

References

  1. Brown, A. G. (2008). Geoarchaeology, the four dimensional (4D) fluvial matrix and climatic causality. Geomorphology, 101, 278–297.CrossRefGoogle Scholar
  2. Chiverrell, R. C. (2006). Past and future perspectives upon landscape instability in Cumbria, northwest England. Regional Environmental Change, 6, 101–114.CrossRefGoogle Scholar
  3. Church, M. (2010). The trajectory of geomorphology. Progress in Physical Geography, 34, 265.CrossRefGoogle Scholar
  4. Certini, G., & Scalenghe, R. (2011). Anthropogenic soils are the golden spikes for the Anthropocene. The Holocene, 21, 847–852.CrossRefGoogle Scholar
  5. Dearing, J., & Jones, R. T. (2003). Coupling temporal and spatial dimensions of global sediment flux through lake and marine sediment records. Global and Planetary Change, 39, 147–168.CrossRefGoogle Scholar
  6. Fanning, P. (1994). Long-term contemporary erosion rates in an arid rangelands environment in western New South Wales, Australia. Journal of Arid Environments, 28, 173–187.CrossRefGoogle Scholar
  7. Gale, S. J., & Hoare, P. G. (2012). The stratigraphic status of the Anthropocene. The Holocene. doi: 10.1177/0959683612449764.
  8. Gilbert, G. K. (1877). Report on the Geology of the Henry Mountains. Washington, DC: United States Geological and Geographical Survey Rocky Mountains Region, General Printing Office.Google Scholar
  9. Haff, P. K. (2010). Hillslopes, rivers, plows, and trucks: mass transport on Earth’s surface by natural and technological processes. Earth Surface Processes and Landforms, 35, 1157–1166.CrossRefGoogle Scholar
  10. Happ, S. C., Rittenhopuse, G., & Dobson, G. C. (1940). Some principles of accelerated stream and valley sedimentation. United States Department of Agriculture Technical Bulletin 695.Google Scholar
  11. Hoffmann, T., Thorndycraft, V. R., Brown, A. G., Coulthard, T. J., Damnati, B., Kale, V. S., et al. (2010). Human impact on fluvial regimes and sediment flux during the Holocene: Review and future research agenda. Global and Planetary Change, 72, 87–98.CrossRefGoogle Scholar
  12. Hooke, R Le B. (1994). On the history of humans as geomorphic agents. Geology, 28, 843–846.CrossRefGoogle Scholar
  13. Jablonski, D. (2004). Extinction: past and present. Nature, 427, 589.Google Scholar
  14. Lespez, L., Drezen, Y Le, Garnier, A., Rasse, M., Eichorn, B., Ozainne, S., et al. (2011). High-resolution fluvial records of Holocene environmental changes in the Sahel: The Yamé River at Ounjougou (mali, West Africa). Quaternary Science Reviews, 30, 737–756.CrossRefGoogle Scholar
  15. Marsh, G. P. (1874). The Earth as modified by human actions. New York: C. Scribner’s Sons.Google Scholar
  16. Montgomery, D. (2007). Dirt: The erosion of civilizations. Berkeley, California: University of California Press. 295p.Google Scholar
  17. Natermann, E. (1941). Das Sinken der Wasserstände der Weser und ihr Zusammenhang mit der Auelehmbildung des Wesertales. Arch. Landes- u. Volkskde. Niedersachsens 9, 288–309. Oldenburg.Google Scholar
  18. Nilsson, T. (1983). The Pleistocene. Dordrecht, Holland: D. Reidel Publishers. 651p.Google Scholar
  19. Rustomji, P., & Pietsch, T. (2007). Alluvial sedimentation rates from south eastern Australia indicate post-European settlement landscape recovery. Geomorphology, 90, 73–90.CrossRefGoogle Scholar
  20. Rose, J. (2010). The Quaternary of the British Isles: Factors forcing environmental change. Journal of Quaternary Science, 25, 399–418.CrossRefGoogle Scholar
  21. Sauer, C. O. (1938). Destructive exploitation in modern colonial expansion. International geographical congress Amsterdam, III, sect. IIc, pp. 494–499.Google Scholar
  22. Shotton, F. W. (1978). Archaeological inferences from the study of alluvium in the lower Severn–Avon valleys. In S. Limbrey & J. G. Evans (Eds.), The effect of man on the landscape: The Lowland Zone. CBA Research Report 21 (pp. 27–32). London: Council for British Archaeology.Google Scholar
  23. Steffen, W., Crutzen, P. J., & McNeill, J. R. (2007). The Anthropocene: Are humans now overwhelming the great forces of Nature? Ambio, 36, 614–621.CrossRefGoogle Scholar
  24. Syvitski, J. P. M., Peckham, S. D., Hilberman, R., & Mulder, T. (2003). Predicting the terrestrial flux of sediment to the global ocean: a planetary perspective, Science, 162, 5–24.Google Scholar
  25. Sylvitski, J. P. M., Vörösmart, C. J., Kettner, A. J., & Green, P. (2005). Impact of humans on the flux of terrestrial sediment to the Global coastal ocean. Science, 308, 376–380.CrossRefGoogle Scholar
  26. Trimble, S. (1981). Changes in sediment storage in Coon Creek basin, Driftless Area, Wisconsin, 1853–1975. Science, 214, 181–183.CrossRefGoogle Scholar
  27. Wainwright, J., & Thornes, J. B. (2004). Environmental issues in the Mediterranean: Processes and perspectives from the past and present. London: Routledge.Google Scholar
  28. Walker, et al. (2009). Formal definition and dating of the Global Stratotype Section and Point (GSSP) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records. Journal of Quaternary Science, 24, 3–17.CrossRefGoogle Scholar
  29. Walter, R. C., & Merritts, D. J. (2008). Natural streams and the legacy of water-powered mills. Science, 319, 299–304.CrossRefGoogle Scholar
  30. Wilkinson, B. H. (2005). Humans as geologic agents: A deep-time perspective. Geology, 33, 161–164.CrossRefGoogle Scholar
  31. Wolman, M. G., & Schick, A. P. (1967). Effects of construction on fluvial sediment: Urban and suburban areas of Maryland. Water Resources Research, 3, 451–462.CrossRefGoogle Scholar
  32. Zalasiewicz, J., Williams, M., Steffen, W., & Crutzen, P. (2010). The new world of the Anthropocene. Environmental Science and Technology, 44, 2228–2231.CrossRefGoogle Scholar
  33. Zalasiewicz, J., Williams, M., Fortey, R., Smith, A., Barry, T. L., Coe, A. L., et al. (2011). Stratigraphy of the Anthropocene. Philosophical Transactions of the Royal Society A, 369, 1036–1055.CrossRefGoogle Scholar

Copyright information

© Springer International Publishing Switzerland 2014

Authors and Affiliations

  • Antony G. Brown
    • 1
  1. 1.Palaeoenvironmental Laboratory University of SouthamptonSouthamptonUK

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