Netherlands Annual Ecology Meeting 2018 – day 1

February 13, 2018

Today the Dutch ecological community has convened at the Netherlands Annual Ecology Meeting (NEAM) in the forest near Lunteren. The meeting was kicked off by plenary lectures by Trisha Atwood and Han Olff who talked to the theme of “Ecosystem functioning in a changing world”. Trisha highlighted the importance of animals in modifying plant communities and their consequent importance for understanding changes in carbon storage. Han illustrated the complexity of ecological networks and posed the significant challenge of understanding changes in competing networks. Following the plenaries I chose two sessions to follow. The first on “Plant Ecology” and the second on “Ecosystem Resilience”. There were many exciting talks in both sessions, two of which grabbed my attention. Mara Baudena (Utrecht University) highlighted the complexity of modelling forest-grassland interactions in Africa, while Sofia Gomes (Naturalis Biodiversity Centre) showed surprising (to me) variation in mychorizal fungi across the globe.Furthermore four talks were presented by researchs at my home, the Institute for Biodiversity & Ecosystem Dynamics (University of Amsterdam):

  • Crystal McMichael “Ancient human disturbances may be skewing our understanding of Amazonian ecology”
  • Milan Teunissen van Manan “Species specific responses in leaf wax n-alkane composition from six tropical tree species”
  • Kenneth Rijsdijk “Assessing the resiliance of insular species to past climate change”
  • Seringe Huisman “Characterization of phytoliths in premontance western Amazonian forests”

So an exciting day, now for food and beer, and back on it tomorrow! Follow live on Twitter 

A sociometabolic reading of the Anthropocene

March 28, 2014


Human impacts on environments

Human impact on environments takes many forms and varies in space and time

Phil Jardine on:

Fischer-Kowalski, M., Krausmann, F. & Pallua, I. (2014) A sociometabolic reading of the Anthropocene: Modes of subsistence, population size and human impact on Earth. The Anthropocene Review, 1(1), 8 – 33.

Regardless of whether it’s worthwhile designating the “Anthropocene” as a new geological epoch (I have my doubts), determining the trajectory of human impact upon the Earth system is important. It provides context for how people see their relationship with natural systems and resources, and can help shape environmental policy and its acceptance by the public. But where to put the onset of this impact – where does the Anthropocene start? The authors of this paper belong to the Institute of Social Ecology at Klagenfurt University, Austria, and take a social sciences approach to the problem. Rather than focusing on physical evidence in the environment, as a geologist might do to delimit a geological epoch, Fischer-Kowalski et al. use a model where human impact is measured as the product of population size, affluence (= energy available per person) and technology, summed over three modes of subsistence: hunter-gatherers, agrarian and industrial. This avoids problems of time lags between human activity and the signature it leaves, and allows the authors to pull apart different driving factors across different societal types.

Using this approach shows a definite shift at around AD 1500: human impact was gradually increasing prior to this, but there is a sharp upturn at ~AD 1500, energy use becomes more important for amplifying the impact of population growth, and a shift from biomass to fossil fuel driven energies enhances this further. While there are problems with this approach – determining energy throughput for long-dead societies will always involve a lot of extrapolation from modern patterns – the authors are careful in stating their assumptions, and going through possible issues with the model itself. It would have been nice to see a comparison between the model output and the empirical evidence though, to help bridge the gap between these two different takes on the same question.

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