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WELCOME TO THE ANTHROPOCENE
     The geolog y of humanity




     ICT for Life Sciences Forum
     MELBOURNE, 6 DECEMBER 2012                                    OWEN GAFFNEY
     Adapted for the web 7 December 2012                    Director of Communications
                                         International Geosphere-Biosphere Programme

  Image: Globaia



2012 © Owen Gaffney
ANTHROPOCENE
  •  Earth is moving out of its current
     geological epoch, the Holocene
  •  Humanity is largely responsible for this exit
  •  Humanity has become a global geological
     force – since the 1950s
  •  Adapt our worldviews accordingly



The Anthropocene: conceptual and historical perspectives. Phil Trans A Steffen et al 2011


2012 © Owen Gaffney                           Image: NASA, released 5 Dec 2012
Insert data visualization from
    Anthropocene.info
    Welcome to the Anthropocene
    http://vimeo.com/39048998




2012 © Owen Gaffney                  Credit: Globaia/IGBP
www.anthropocene.info
   The world’s first website dedicated to the concept of the
   Anthropocene




2012 © Owen Gaffney       Credit: Globaia/IGBP/CSIRO/Stockholm Resilience Centre
www.anthropocene.info




2012 © Owen Gaffney         Credit: Globaia/IGBP/CSIRO/Stockholm Resilience Centre
The Great Acceleration




2012 © Owen Gaffney
Population




                                          US	
  Bureau	
  of	
  the	
  Census	
  (2000)	
  Interna5onal	
  database	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Total real GDP




                         Nordhaus	
  (1997)	
  The	
  economics	
  of	
  new	
  goods.	
  University	
  of	
  Chicago	
  Press	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Foreign direct investment




                                                             World	
  Bank	
  (2002)	
  data	
  and	
  sta5s5cs	
  
                          IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Damming of rivers




                                                           World	
  Commission	
  on	
  Dams	
  (2000)	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Water use




                                                   Shiklomanov	
  (1990)	
  Global	
  Water	
  Resources	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Fertiliser consumption




                                                Interna5onal	
  Fer5lizer	
  Industry	
  Associa5on	
  (2002)	
  
                        IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Urban population




                                                          The	
  State	
  of	
  the	
  World’s	
  Ci5es	
  (2001)	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Paper consumption




                                                            Pulp	
  and	
  paper	
  interna5onal	
  (1993)	
  
                       IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Motor vehicles




                                                          Global	
  environmental	
  outlook	
  (2000)	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Telephones




                      Canning	
  (2001)	
  A	
  database	
  of	
  world	
  infrastructure	
  stocks,	
  1950-­‐95	
  World	
  Bank	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
International tourism




                                        World	
  Tourism	
  Organiza5on	
  (2001)	
  Tourism	
  industry	
  trends	
  
                        IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Fisheries exploitation




                      Percentage of global fisheries either fully exploited, overfished or collapsed. Source:
                                                                      FAOSTAT (2002) Statistical databases
2012 © Owen Gaffney            IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Shrimp farm production




                      IAnnual shrimp production as a proxy for coastal zone alteration. Sources: WRI
                                                      (2003) A guide to world resources, 2002-2004
2012 © Owen Gaffney        IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Domesticated land




             Amount of land converted to pasture and cropland. Source: Klein Goldewijk and Battjes (1997)
                    National Institute for Public Health and the Environment (RIVM). Bilthoven, Netherlands
2012 © Owen Gaffney                IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Planetary response




2012 © Owen Gaffney            Image: NASA, released 5 Dec 2012
Atmospheric CO2 concentration




                                                    Etheridge	
  et	
  al.	
  Geophys	
  Res	
  101:	
  4115-­‐4128	
  
                       IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Atmospheric N2O concentration




                                                    Machida	
  et	
  al	
  Geophys	
  Res	
  Le	
  22:2921-­‐2925	
  
                        IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Atmospheric CH4 concentration




                                                       Blunier	
  et	
  al	
  J	
  Geophy	
  Res	
  20:	
  2219-­‐2222	
  
                       IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Northern hemisphere average surface
                     temperature




                                                    Mann	
  et	
  al	
  Geophys	
  Res	
  Le	
  26(6):	
  759-­‐762	
  
                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Ozone depletion




                      percentage total column ozone loss over Antarctica, using the average annual total
                           column ozone, 330, as a base. Image: J.D. Shanklin, British Antarctic Survey
2012 © Owen Gaffney            IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Tropical rainforest and woodland loss




        Loss of tropical rainforest and woodland, as estimated for tropical Africa, Latin America and South and
         Southeast Asia. Sources: Richards (1990) In: The Earth as transformed by human action, Cambridge
2012 © Owen Gaffney University Press IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Natural climatic disasters




 Decadal frequency of great floods (one-in-100-year events) after 1860 for basins larger than 200 000 km2 with
      observations that span at least 30 years. Source: Milly et al. (2002) Nature 415:514-517 IGBP synthesis:
2012 © Owen Gaffney                                   Global Change and the Earth System, Steffen et al 2004
Coastal zone nitrogen flux




         Model-calculated partitioning of the human-induced nitrogen perturbation fluxes in the global coastal
               margin for the period since 1850. Source: Mackenzie et al. (2002) Chem. Geology 190:13-32
2012 © Owen Gaffney                 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Biodiversity loss




    Mathematically calculated rate of extinction. Source: Wilson (1992) The diversity of life, the Penguin Press.
                                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
2012 © Owen Gaffney
Great acceleration




                      IGBP synthesis: Global Change and the Earth System, Steffen et al 2004

2012 © Owen Gaffney
Great Acceleration




                       IGBP synthesis: Global Change and the Earth System, Steffen et al 2004

2012 © Owen Gaffney
“Our	
  foot	
  is	
  stuck	
  	
  
                      on	
  the	
  ACCELERATOR	
  
                      	
  and	
  we	
  are	
  heading	
  
                      towards	
  an	
  ABYSS.”	
  
                      	
  
                             	
  	
  	
  	
  UN	
  Secretary	
  General	
  
                                       Ban	
  Ki-­‐Moon,	
  2009	
  	
  	
  	
  	
  	
  	
  	
     	
  	
  




2012 © Owen Gaffney
This is our life support system
                        Water             Atmosphere




2012 © Owen Gaffney                           Credit: Adam Nieman
Does Earth have a pulse?


2012 © Owen Gaffney   Credit: Tomas Oneborg / SvD / SCANPIX
Modern humans appear in Africa


 Carbon
 dioxide

Temperature


 Methane




                      Adapted by IGBP from:
                      Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008.
2012 © Owen Gaffney   Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
Beyond natural boundaries


                      Adapted by IGBP from:
                      Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008.
2012 © Owen Gaffney   Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
World Bank Report, November 2012




2012 © Owen Gaffney
2011-2012 Fossil and Cement Emissions
•  Projection for, 58% over 1990




 •  Uncertainty is ±5% for one standard
    deviation (IPCC “likely” range)
 •    Source: Peters et al. 2012a; Le Quéré et al. 2012; CDIAC Data; Global Carbon Project 2012
2012 © Owen Gaffney
2012 Global Carbon Budget
                                                                                       30
                                                                                                                                                               RCP8.5
                                                                                              Historical
                                                                                                                                                               4.0−6.1°C
                                                                                              2012 Estimate
                                                                                              RCP8.5              RCP4.5
                  Fossil-fuel, cement production, and gas flaring emissions (PgC/yr)
                                                                                       25     RCP6                RCP3-PD
                                                                                              Historical uncertainty
                                                                                              Earlier scenarios

                                                                                       20




                                                                                       15
                                                                                                                                                               RCP6
                                                                                                                                                               2.6−3.7°C


                                                                                       10




                                                                                        5                                                                      RCP4.5
                                                                                                                                                               2.0−3.0°C


                                                                                                                                          RCP3-PD: 1.3−1.9°C
                                                                                        0
                                                                                       1980    2000           2020          2040   2060      2080            2100
Peters GP, Global Carbon Project 2012, Nature Climate Change



2012 © Owen Gaffney
Dams built 1800-2009




2012 © Owen Gaffney               James Syvitski, CSDMS
2012 © Owen Gaffney   Credit: NASA LandSat
2012 © Owen Gaffney   Credit: NASA LandSat
Pearl River Delta, China


  24 OF 33 MAJOR DELTAS ARE SINKING
  500 MILLION PEOPLE LIVE ON DELTAS
  85% HIT BY SEVERE FLOODING RECENTLY
  Parts of Jakarta have sunk 4 metres since 1974




2012 © Owen Gaffney   Credit: NASA LandSat   Syvitski 2009, Nature Geoscience
Dubai




2012 © Owen Gaffney           Credit: NASA LandSat
Dubai




2012 © Owen Gaffney           Credit: NASA LandSat
Las Vegas




2012 © Owen Gaffney               Credit: NASA LandSat
Las Vegas




2012 © Owen Gaffney               Credit: NASA LandSat
“WE WILL BUILD MORE
                      URBAN AREAS
                      IN THE 1ST 3 DECADES
                      OF THE 21ST CENTURY
                      THAN ALL OF HISTORY

                      COMBINED.”
                      PROFESSOR KAREN SETO, YALE




2012 © Owen Gaffney
Deforestation in the Bolivian rainforest




  Credit: NASA/USGS
2012 © Owen Gaffney
We use an area the size of South America to grow our crops
    And an area the size of Africa for our livestock.




2012 © Owen Gaffney                           Ellis 2010
90%	
  of	
  total	
  
   mammalian	
  biomass	
               …	
  up	
  from	
  
     is	
  made	
  up	
  of	
           0.1%	
  10,000	
  
      humans	
  and	
                   years	
  ago…	
  
     domesNcated	
                                  	
  
           animals.	
  


2012 © Owen Gaffney               Science, 7 Oct 2011
2012 © Owen Gaffney
Paul Crutzen
   Nobel laureate
   Former IGBP Vice
   Chair

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                                                                                                                                                                        Envir ill, J. R.
                                                                                                                                                                                                ridg e Earth
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2012 © Owen Gaffney
                                                                                                                                                chlo                      ghto          , Ne             of th           der         e                an
                                                                                                            e be                                                                n,             wY               eT            the , 1990
                                                                                                                  com re now Antar ro- C he Scienti J. T. et al. ork, 200 wentieth Sun: An ).
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                                                                                                                                  ch w lated c Berg bridge, 2 Basis (C ds) Clima
                                                                                               002
                                                                                                    Mac                                                                                                                              tury
                                                                                                          mil
                                                                                                              la                         o           ).              e             0               am             te                        Wor
2000. IGBP Scientific Committee meeting, Cuernavaca, Mexico

  “Stop	
  using	
  the	
  word	
  Holocene.	
  
  We’re	
  not	
  in	
  the	
  Holocene	
  any	
  
  more.	
  We’re	
  in	
  the…the…	
  




                  ...ANTHROPOCENE”
         “It	
  was	
  quiet	
  in	
  the	
  room	
  for	
  a	
  while.”	
  

2012 © Owen Gaffney
1992: New York Times journalist Andrew Revkin’s book - Global
                 Change mentions the Anthrocene




                                “We	
  are	
  entering	
  an	
  age	
  that	
  might	
  
                                someday	
  be	
  referred	
  to	
  as,	
  say,	
  the	
  
                                Anthrocene	
  [sic].	
  AYer	
  all,	
  it	
  is	
  a	
  
                                geological	
  age	
  of	
  our	
  own	
  making.”



2012 © Owen Gaffney
1989: U.S writer and activist Bill McKibben publishes the End of Nature




2012 © Owen Gaffney
1980s: U.S. biologist Eugene Stoermer’s
      (1934-2012) lectures mention the Anthropocene




2012 © Owen Gaffney
Sixties space exploration and the 1972 United Nations
       summit on the environment gave people a new
       perspective




NASA Earth rise


2012 © Owen Gaffney
Vladimir Verdansky (1963-1945)

                          •  Life is a geological
                             force
                          •  Noösphere – the
                             world of thought
                             driving
                             environmental
                             change
                           Image; Memorial Office Museum of
                           Academician VI Verdansky Moscow.




2012 © Owen Gaffney
George Perkins Marsh (1801-1882)
                       Man	
  and	
  Nature	
  (1864)	
  
                       	
  
                       The	
  Earth	
  as	
  Modified	
  by	
  
                       Human	
  AcNon:	
  Man	
  and	
  
                       Nature.	
  (1874)	
  




                        George P. Marsh, photographed by Mathew B.
                        Brady between 1855 and 1865. Brady-Handy
                        Collection (Library of Congress). [call number:
                        BH8201-4981; reproduction number: LC-
                        BH8201-4981 DLC (b&w film copy neg.)




2012 © Owen Gaffney
Edward Seuss (1831-1914)



                                 Developed the concept
                                 of the biosphere.



                             Image: Eigenes Foto einer
                             Originallithographie in eigenem
                             Besitz




2012 © Owen Gaffney
Antonio Stoppani (1824-1891)

                                  Humanity is a
                                  “new telluric
                                  force, which in
                                  power and
                                  universality may
                                  be compared to
                                  the greater
                                  forces of earth.”
                                  Corso di geologia
                                  1873.
      ‘Anthropozoic era’         Image: Paleontologica
                                 Lombarda



2012 © Owen Gaffney
When did the Anthropocene start? Start of large-scale
      hunting? Dawn of agriculture? Industrial revolution?
      1950?
                    Fire Hunting Agriculture Industrial
                                             revolution
                                                    Digital age




2012 © Owen Gaffney
Who decides?




2012 © Owen Gaffney
2012 © Owen Gaffney   Credit 1996 macrae@geo.ucalgary.ca
But the rest of the world is not
                 waiting…




2012 © Owen Gaffney
2012 © Owen Gaffney
2012 © Owen Gaffney
2012 © Owen Gaffney
Credit: BBC



2012 © Owen Gaffney
“The concept of the
  ANTHROPOCENE
  heralds a profound
  shift in PERCEPTION
  of our place in the
   WORLD.”
  Nobel Laureate Elinor Ostrom
  (1933-2012)
  Planet Under Pressure




 Photo credit: Chris Meyer



2012 © Owen Gaffney
Centuries from now,
the defining event of the
20th century may not be the
Great Wars, the battle of ideologies,
or even the Industrial Revolution per se.
It may well be the ascendency of a
single species to become the
dominant geological force –
in a single human lifetime.




2012 © Owen Gaffney            Image: NASA, released 5 Dec 2012
…Where are we going?
The role of ICT in changing the narrative




2012 © Owen Gaffney           Image: NASA, released 5 Dec 2012
The industrialization of friendship
                The globalization of small talk



2012 © Owen Gaffney
2011        Global connectivity has moved into hyperdrive




2.3 billion internet users (30% of population)
6 billion mobile phone subscriptions
By 2015, 60% of world population will be online


                                        Data: ITU Measuring the Information Society (2012)
                                        Pic credit: Paul Butler, visualizing friendship




2012 © Owen Gaffney
Image: Steve Song. Copyright CC-BY




2012 © Owen Gaffney
Within a decade A L L but the
      most marginalised in societies
      will be C O N N E C T E D in new
      and p r ofou nd w ays.
                        Pic credit: Paul Butler, visualizing friendship




2012 © Owen Gaffney
Arab Spring




   “The regimes thought the youth were divorced
   from politics. They didn’t notice that young
   people were connected among themselves.”
   Syrian activist “Khaled”, Financial Times, Dec 2011.



2012 © Owen Gaffney
Arab Spring

 Defining features
 •  Complex causes but
    social media has
    defining role
 •  Heightened
    awareness of equality
    and fairness
 •  Social media exposes
    extent of distrust




2012 © Owen Gaffney
Occupy movement

 Defining features
 •  Social media has
    defining role
 •  Demanding openness
    and transparency
 •  Heightened
    awareness of equality
    and fairness




2012 © Owen Gaffney
“Discontinuities are…
                      precisely what you would
                      expect if you consider
                      today’s societies from a
                      complex-systems
                      perspective.”

                      “Social media…have the
                      potential to facilitate
                      qualitatively new collective
                      behaviours.”
                      Ball P. Nature
                      21 December 2011




2012 © Owen Gaffney
“Isolated, anonymous
  individuals overharvest
  common-pool resources.”
  BUT…



  Nobel Laureate Elinor Ostrom
  (1933-2012)




 Photo credit: Chris Meyer



2012 © Owen Gaffney
“Simply allowing
  COMMUNICATION, or
  “CHEAP TALK,” enables
  participants to reduce
  overharvesting. ”



  Nobel Laureate Elinor Ostrom
  (1933-2012)



 Photo credit: Chris Meyer



2012 © Owen Gaffney
•  Reliable knowledge
  •  Individuals like to see how
     sustainability benefits whole
     group
  •  Trust others to keep promises


  Nobel Laureate Elinor Ostrom
  (1933-2012)




 Photo credit: Chris Meyer



2012 © Owen Gaffney
Social networking is a keystone innovation




2012 © Owen Gaffney
“There is a direct link from more precise
 gossip at the watercooler to better
 decisions.”
 Nobel Laureate Daniel Kahneman
 Thinking, fast and slow, 2011

   With social networking we
   have a global watercooler


   Photo: Jon Roemer




2012 © Owen Gaffney
Sustainable Development Goals:
        Include ICT access for all




2012 © Owen Gaffney
Conclusions
 •  In one lifetime humanity has become a global
    geological force – the Great Acceleration
 •  Earth is moving out of its current geological
    epoch, the Holocene – the Anthropocene
 •  Action on global sustainability essential
 •  Change in WORLDVIEW required. Could social
    media be a keystone innovation?




2012 © Owen Gaffney            Image: NASA, released 5 Dec 2012
D	
   N	
   A
               Like
                          	
  DNA,             the         word
               ANTHROPOCENE
               is destined to leap from the world of science into the

               GLOBAL LEXICON

2012 © Owen Gaffney
www.anthropocene.info
     www.anthropocenejournal.com
     www.igbp.net

2012 © Owen Gaffney
WELCOME TO THE ANTHROPOCENE
The geology of humanity
MELBOURNE, December 2012


 Thank you!
 @owengaffney
 #anthropocene

 WEB
 www.anthropocene.info
 www.anthropocenejournal.com
 www.igbp.net

 EMAIL
 Owen.gaffney@igbp.kva.se


2012 © Owen Gaffney

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Welcome to the Anthropocene: the geology of humanity

  • 1. WELCOME TO THE ANTHROPOCENE The geolog y of humanity ICT for Life Sciences Forum MELBOURNE, 6 DECEMBER 2012 OWEN GAFFNEY Adapted for the web 7 December 2012 Director of Communications International Geosphere-Biosphere Programme Image: Globaia 2012 © Owen Gaffney
  • 2. ANTHROPOCENE •  Earth is moving out of its current geological epoch, the Holocene •  Humanity is largely responsible for this exit •  Humanity has become a global geological force – since the 1950s •  Adapt our worldviews accordingly The Anthropocene: conceptual and historical perspectives. Phil Trans A Steffen et al 2011 2012 © Owen Gaffney Image: NASA, released 5 Dec 2012
  • 3. Insert data visualization from Anthropocene.info Welcome to the Anthropocene http://vimeo.com/39048998 2012 © Owen Gaffney Credit: Globaia/IGBP
  • 4. www.anthropocene.info The world’s first website dedicated to the concept of the Anthropocene 2012 © Owen Gaffney Credit: Globaia/IGBP/CSIRO/Stockholm Resilience Centre
  • 5. www.anthropocene.info 2012 © Owen Gaffney Credit: Globaia/IGBP/CSIRO/Stockholm Resilience Centre
  • 6. The Great Acceleration 2012 © Owen Gaffney
  • 7. Population US  Bureau  of  the  Census  (2000)  Interna5onal  database   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 8. Total real GDP Nordhaus  (1997)  The  economics  of  new  goods.  University  of  Chicago  Press   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 9. Foreign direct investment World  Bank  (2002)  data  and  sta5s5cs   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 10. Damming of rivers World  Commission  on  Dams  (2000)   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 11. Water use Shiklomanov  (1990)  Global  Water  Resources   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 12. Fertiliser consumption Interna5onal  Fer5lizer  Industry  Associa5on  (2002)   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 13. Urban population The  State  of  the  World’s  Ci5es  (2001)   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 14. Paper consumption Pulp  and  paper  interna5onal  (1993)   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 15. Motor vehicles Global  environmental  outlook  (2000)   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 16. Telephones Canning  (2001)  A  database  of  world  infrastructure  stocks,  1950-­‐95  World  Bank   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 17. International tourism World  Tourism  Organiza5on  (2001)  Tourism  industry  trends   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 18. Fisheries exploitation Percentage of global fisheries either fully exploited, overfished or collapsed. Source: FAOSTAT (2002) Statistical databases 2012 © Owen Gaffney IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 19. Shrimp farm production IAnnual shrimp production as a proxy for coastal zone alteration. Sources: WRI (2003) A guide to world resources, 2002-2004 2012 © Owen Gaffney IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 20. Domesticated land Amount of land converted to pasture and cropland. Source: Klein Goldewijk and Battjes (1997) National Institute for Public Health and the Environment (RIVM). Bilthoven, Netherlands 2012 © Owen Gaffney IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 21. Planetary response 2012 © Owen Gaffney Image: NASA, released 5 Dec 2012
  • 22. Atmospheric CO2 concentration Etheridge  et  al.  Geophys  Res  101:  4115-­‐4128   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 23. Atmospheric N2O concentration Machida  et  al  Geophys  Res  Le  22:2921-­‐2925   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 24. Atmospheric CH4 concentration Blunier  et  al  J  Geophy  Res  20:  2219-­‐2222   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 25. Northern hemisphere average surface temperature Mann  et  al  Geophys  Res  Le  26(6):  759-­‐762   IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 26. Ozone depletion percentage total column ozone loss over Antarctica, using the average annual total column ozone, 330, as a base. Image: J.D. Shanklin, British Antarctic Survey 2012 © Owen Gaffney IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 27. Tropical rainforest and woodland loss Loss of tropical rainforest and woodland, as estimated for tropical Africa, Latin America and South and Southeast Asia. Sources: Richards (1990) In: The Earth as transformed by human action, Cambridge 2012 © Owen Gaffney University Press IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 28. Natural climatic disasters Decadal frequency of great floods (one-in-100-year events) after 1860 for basins larger than 200 000 km2 with observations that span at least 30 years. Source: Milly et al. (2002) Nature 415:514-517 IGBP synthesis: 2012 © Owen Gaffney Global Change and the Earth System, Steffen et al 2004
  • 29. Coastal zone nitrogen flux Model-calculated partitioning of the human-induced nitrogen perturbation fluxes in the global coastal margin for the period since 1850. Source: Mackenzie et al. (2002) Chem. Geology 190:13-32 2012 © Owen Gaffney IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 30. Biodiversity loss Mathematically calculated rate of extinction. Source: Wilson (1992) The diversity of life, the Penguin Press. IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 31. Great acceleration IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 32. Great Acceleration IGBP synthesis: Global Change and the Earth System, Steffen et al 2004 2012 © Owen Gaffney
  • 33. “Our  foot  is  stuck     on  the  ACCELERATOR    and  we  are  heading   towards  an  ABYSS.”            UN  Secretary  General   Ban  Ki-­‐Moon,  2009                     2012 © Owen Gaffney
  • 34. This is our life support system Water Atmosphere 2012 © Owen Gaffney Credit: Adam Nieman
  • 35. Does Earth have a pulse? 2012 © Owen Gaffney Credit: Tomas Oneborg / SvD / SCANPIX
  • 36. Modern humans appear in Africa Carbon dioxide Temperature Methane Adapted by IGBP from: Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008. 2012 © Owen Gaffney Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
  • 37. Beyond natural boundaries Adapted by IGBP from: Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008. 2012 © Owen Gaffney Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
  • 38. World Bank Report, November 2012 2012 © Owen Gaffney
  • 39. 2011-2012 Fossil and Cement Emissions •  Projection for, 58% over 1990 •  Uncertainty is ±5% for one standard deviation (IPCC “likely” range) •  Source: Peters et al. 2012a; Le Quéré et al. 2012; CDIAC Data; Global Carbon Project 2012 2012 © Owen Gaffney
  • 40. 2012 Global Carbon Budget 30 RCP8.5 Historical 4.0−6.1°C 2012 Estimate RCP8.5 RCP4.5 Fossil-fuel, cement production, and gas flaring emissions (PgC/yr) 25 RCP6 RCP3-PD Historical uncertainty Earlier scenarios 20 15 RCP6 2.6−3.7°C 10 5 RCP4.5 2.0−3.0°C RCP3-PD: 1.3−1.9°C 0 1980 2000 2020 2040 2060 2080 2100 Peters GP, Global Carbon Project 2012, Nature Climate Change 2012 © Owen Gaffney
  • 41. Dams built 1800-2009 2012 © Owen Gaffney James Syvitski, CSDMS
  • 42. 2012 © Owen Gaffney Credit: NASA LandSat
  • 43. 2012 © Owen Gaffney Credit: NASA LandSat
  • 44. Pearl River Delta, China 24 OF 33 MAJOR DELTAS ARE SINKING 500 MILLION PEOPLE LIVE ON DELTAS 85% HIT BY SEVERE FLOODING RECENTLY Parts of Jakarta have sunk 4 metres since 1974 2012 © Owen Gaffney Credit: NASA LandSat Syvitski 2009, Nature Geoscience
  • 45. Dubai 2012 © Owen Gaffney Credit: NASA LandSat
  • 46. Dubai 2012 © Owen Gaffney Credit: NASA LandSat
  • 47. Las Vegas 2012 © Owen Gaffney Credit: NASA LandSat
  • 48. Las Vegas 2012 © Owen Gaffney Credit: NASA LandSat
  • 49. “WE WILL BUILD MORE URBAN AREAS IN THE 1ST 3 DECADES OF THE 21ST CENTURY THAN ALL OF HISTORY COMBINED.” PROFESSOR KAREN SETO, YALE 2012 © Owen Gaffney
  • 50. Deforestation in the Bolivian rainforest Credit: NASA/USGS 2012 © Owen Gaffney
  • 51. We use an area the size of South America to grow our crops And an area the size of Africa for our livestock. 2012 © Owen Gaffney Ellis 2010
  • 52. 90%  of  total   mammalian  biomass   …  up  from   is  made  up  of   0.1%  10,000   humans  and   years  ago…   domesNcated     animals.   2012 © Owen Gaffney Science, 7 Oct 2011
  • 53. 2012 © Owen Gaffney
  • 54. Paul Crutzen Nobel laureate Former IGBP Vice Chair Geo log y of ma Pau F l J. C ru nkin or th tze n of h e past um thr d pog have es ans on ee centu enic cala clim em ted. the glo ries, th refe natu ate m issions Becaus bal env e effec in ring r a o ir com ral beh y dep f carbo e of thes onme ts th 1926, to the term e. It se aviour art sig n dioxid e anthr t dir incre V. I. “anthro n e The con cep way ‘Anth ems for ma nific antl e, glo o- mu ectio asing Vern p ads ozoic Anth ropo s r ap b n in im sup huma opocen propria ny mil y fro al co st pro which pact o ky ack era”. A p n m ns ce perio lemen -domine’ to the te to a lennia f no c en th n The ting hav ciousn ed, nam e proc mankin wledge d A Anth d of ated prese ssign to in e e hav nthropo th the t ,g e nt, whe e latter ne cou 10–12 ne — al epoc y ‘w rnadsky gs.” T greate ught, th in th ropoce e pas Holoc eologic in man e Ve round ater an d tho wards f evoluti he sur g gre ss an ely to sses o d: “T d in d incr on cen e sta ert tury ed in th could cen e ld th o r a eas , wh b shown analy part o be sa millen e war h, ro rld of used th eilhard influen nd fo ing in p olar en a e late e e said ed ses f the id to nia. m le o thou e ter de ce o rms ice naly ighte to con centr the be of air eighte have s The own f hum ght’ m ‘n Cha n th grow sho ses enth — o rd eir in meth atio ginn trapp enth tarted T futu a re an n brain to ma öspher in and carb g glob wed th of air tr with ane. T ns of ing of ed in centur num he rap d env -pow rk the e’ — th on d al c onc e be app h in 1 James is date carbo growin polar ic y, Ea bers id e iron e ioxid ginn ed 784 Watt a n e rth a xp men r in sh growin e ozo e an entrati ing M . ’s de lso hap diox g globa Dur ’s res nd per ansion t. apin g its g n g e n e - de s t dm o etha ns of of envir ankin sign p id l onm d’s g of th ens to c e and pop ing the ources capita of ma s If it have b oying r ne. 187 e ste oinc ulati past h e nkin e p 3 en row am e ide than on thr as co xploit d in chemhad tu en stud roperti Stop , when t was r ing in ngin lion 6 billio has inc ee centu ntinue ation r wo ically ned o ied sin es of e whic pani sp the Ita cogniz fluence e ing in this n and is reased ries, th d apac f ro uld by like b ut that ce the the ha o com h in p oke ab lian g ed as lo on th c Abo attle po century expecte tenfold e huma e. of nd ph then h romin chlorin id-19 lo- u m pare o ou eo n e e 7 d to wer an t a “ne logist g ago a is ut 30 pulati . The d to r to m n by the An enome ave be , the o e beha 0s. the d un w tell Anton s d exploit –50% o on has metha each 10 ore w ta no en z ve grea ivers uric io isap ed b f th rise n e-p bil- not isdom rctic sp n, no a glo one ho d diox pear a y hum e plan n to 1 rodu de v , b ter a forc lity ma force elop this ca ring. M t just al, yea le es o f ea be y exti ide an t a fast ans. Tr et’s lan .4 billio c- m Unless . tast o a rop re by lu n even - r n o e rth,” sion ction. d stron pace, pical r d surfa n. de teorite there is hic situ ck tha t r a c half have be Dam b gly in eleasin infores e en mic — impac a glob atio n didn man of a ll a com uild e co ing crea sing g ca r bo ts viro nm man t, a w al cata da kin or st of th kind. F ccessib mmon and riv specie n en unting ental fo d wil ld war rophe — le l ocea e primisheries fresh place. M er dive s m gineers task lie rce for remain or a p a e m con n regio ary p remov water is ore tha r- th ntally to guid s ahead any m a m an- ti r e e e a 16-fo nental ns and oducti more used b n re era o sustain societ for scie illennia jor o th q a y caus ld du shelf. 35% in n in u an 25 y sc uire ap f the ble ma towar ntists . A % ale An ds an sulp ing 160 ring thEnergy the te pwellin p acce s, and ropriate thropo agemen enviro d n hur milli e tw use mpe g pted may cene t du n- than dio on e ha ra jec , w hu m . r Mor twice thxide em tonne ntieth s grow te th ts, for large-s ell invo an beha This ing is in c w agric e nitr e sum ission s of atm centur n tre stage stance ale geo lve inte viour a ill o s r terr ulture gen fe of its n per y ospher y, Pa ading o , howe to ‘op -engine nation t all e e ti ucti strial than is rtilizer atural e ar, mo ic Ch l J. 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  • 55. 2000. IGBP Scientific Committee meeting, Cuernavaca, Mexico “Stop  using  the  word  Holocene.   We’re  not  in  the  Holocene  any   more.  We’re  in  the…the…   ...ANTHROPOCENE” “It  was  quiet  in  the  room  for  a  while.”   2012 © Owen Gaffney
  • 56. 1992: New York Times journalist Andrew Revkin’s book - Global Change mentions the Anthrocene “We  are  entering  an  age  that  might   someday  be  referred  to  as,  say,  the   Anthrocene  [sic].  AYer  all,  it  is  a   geological  age  of  our  own  making.” 2012 © Owen Gaffney
  • 57. 1989: U.S writer and activist Bill McKibben publishes the End of Nature 2012 © Owen Gaffney
  • 58. 1980s: U.S. biologist Eugene Stoermer’s (1934-2012) lectures mention the Anthropocene 2012 © Owen Gaffney
  • 59. Sixties space exploration and the 1972 United Nations summit on the environment gave people a new perspective NASA Earth rise 2012 © Owen Gaffney
  • 60. Vladimir Verdansky (1963-1945) •  Life is a geological force •  Noösphere – the world of thought driving environmental change Image; Memorial Office Museum of Academician VI Verdansky Moscow. 2012 © Owen Gaffney
  • 61. George Perkins Marsh (1801-1882) Man  and  Nature  (1864)     The  Earth  as  Modified  by   Human  AcNon:  Man  and   Nature.  (1874)   George P. Marsh, photographed by Mathew B. Brady between 1855 and 1865. Brady-Handy Collection (Library of Congress). [call number: BH8201-4981; reproduction number: LC- BH8201-4981 DLC (b&w film copy neg.) 2012 © Owen Gaffney
  • 62. Edward Seuss (1831-1914) Developed the concept of the biosphere. Image: Eigenes Foto einer Originallithographie in eigenem Besitz 2012 © Owen Gaffney
  • 63. Antonio Stoppani (1824-1891) Humanity is a “new telluric force, which in power and universality may be compared to the greater forces of earth.” Corso di geologia 1873. ‘Anthropozoic era’ Image: Paleontologica Lombarda 2012 © Owen Gaffney
  • 64. When did the Anthropocene start? Start of large-scale hunting? Dawn of agriculture? Industrial revolution? 1950? Fire Hunting Agriculture Industrial revolution Digital age 2012 © Owen Gaffney
  • 65. Who decides? 2012 © Owen Gaffney
  • 66. 2012 © Owen Gaffney Credit 1996 macrae@geo.ucalgary.ca
  • 67. But the rest of the world is not waiting… 2012 © Owen Gaffney
  • 68. 2012 © Owen Gaffney
  • 69. 2012 © Owen Gaffney
  • 70. 2012 © Owen Gaffney
  • 71. Credit: BBC 2012 © Owen Gaffney
  • 72. “The concept of the ANTHROPOCENE heralds a profound shift in PERCEPTION of our place in the WORLD.” Nobel Laureate Elinor Ostrom (1933-2012) Planet Under Pressure Photo credit: Chris Meyer 2012 © Owen Gaffney
  • 73. Centuries from now, the defining event of the 20th century may not be the Great Wars, the battle of ideologies, or even the Industrial Revolution per se. It may well be the ascendency of a single species to become the dominant geological force – in a single human lifetime. 2012 © Owen Gaffney Image: NASA, released 5 Dec 2012
  • 74. …Where are we going? The role of ICT in changing the narrative 2012 © Owen Gaffney Image: NASA, released 5 Dec 2012
  • 75. The industrialization of friendship The globalization of small talk 2012 © Owen Gaffney
  • 76. 2011 Global connectivity has moved into hyperdrive 2.3 billion internet users (30% of population) 6 billion mobile phone subscriptions By 2015, 60% of world population will be online Data: ITU Measuring the Information Society (2012) Pic credit: Paul Butler, visualizing friendship 2012 © Owen Gaffney
  • 77. Image: Steve Song. Copyright CC-BY 2012 © Owen Gaffney
  • 78. Within a decade A L L but the most marginalised in societies will be C O N N E C T E D in new and p r ofou nd w ays. Pic credit: Paul Butler, visualizing friendship 2012 © Owen Gaffney
  • 79. Arab Spring “The regimes thought the youth were divorced from politics. They didn’t notice that young people were connected among themselves.” Syrian activist “Khaled”, Financial Times, Dec 2011. 2012 © Owen Gaffney
  • 80. Arab Spring Defining features •  Complex causes but social media has defining role •  Heightened awareness of equality and fairness •  Social media exposes extent of distrust 2012 © Owen Gaffney
  • 81. Occupy movement Defining features •  Social media has defining role •  Demanding openness and transparency •  Heightened awareness of equality and fairness 2012 © Owen Gaffney
  • 82. “Discontinuities are… precisely what you would expect if you consider today’s societies from a complex-systems perspective.” “Social media…have the potential to facilitate qualitatively new collective behaviours.” Ball P. Nature 21 December 2011 2012 © Owen Gaffney
  • 83. “Isolated, anonymous individuals overharvest common-pool resources.” BUT… Nobel Laureate Elinor Ostrom (1933-2012) Photo credit: Chris Meyer 2012 © Owen Gaffney
  • 84. “Simply allowing COMMUNICATION, or “CHEAP TALK,” enables participants to reduce overharvesting. ” Nobel Laureate Elinor Ostrom (1933-2012) Photo credit: Chris Meyer 2012 © Owen Gaffney
  • 85. •  Reliable knowledge •  Individuals like to see how sustainability benefits whole group •  Trust others to keep promises Nobel Laureate Elinor Ostrom (1933-2012) Photo credit: Chris Meyer 2012 © Owen Gaffney
  • 86. Social networking is a keystone innovation 2012 © Owen Gaffney
  • 87. “There is a direct link from more precise gossip at the watercooler to better decisions.” Nobel Laureate Daniel Kahneman Thinking, fast and slow, 2011 With social networking we have a global watercooler Photo: Jon Roemer 2012 © Owen Gaffney
  • 88. Sustainable Development Goals: Include ICT access for all 2012 © Owen Gaffney
  • 89. Conclusions •  In one lifetime humanity has become a global geological force – the Great Acceleration •  Earth is moving out of its current geological epoch, the Holocene – the Anthropocene •  Action on global sustainability essential •  Change in WORLDVIEW required. Could social media be a keystone innovation? 2012 © Owen Gaffney Image: NASA, released 5 Dec 2012
  • 90. D   N   A Like  DNA, the word ANTHROPOCENE is destined to leap from the world of science into the GLOBAL LEXICON 2012 © Owen Gaffney
  • 91. www.anthropocene.info www.anthropocenejournal.com www.igbp.net 2012 © Owen Gaffney
  • 92. WELCOME TO THE ANTHROPOCENE The geology of humanity MELBOURNE, December 2012 Thank you! @owengaffney #anthropocene WEB www.anthropocene.info www.anthropocenejournal.com www.igbp.net EMAIL Owen.gaffney@igbp.kva.se 2012 © Owen Gaffney