2.
Many
New
England forests have been harvested at intervals of 70-80 years for
over 200 years. The following graph shows general living biomass trends for
such a forest over this time period, with four logging episodes.
You can think of this curve as showing the accumulation of
NPP --
the excess of GPP over respiration and decay, accumulating as biomass
(or as carbon). The
sharply descending parts of the curve show removal of biomass (wood)
in logging. Describe
any other patterns or trends you see over the several cycles of
logging and regrowth. Offer a
hypothesis explaining the dominant patterns in terms of ecosystem
processes; use terms
and concepts from
ecosystem ecology (e.g., you
might need to refer to gross and/or net production, respiration,
limiting resources,...). There's an appearance of
unsustainability here; offer two
possibilities (derived from your hypothesis) for ‘improving’ the
situation; how might
you change things to keep the biomass available for harvest from
becoming less each time?
3. Human burning of fossil fuels injects large amounts of carbon dioxide into the atmosphere. CO2 is, of course, the source of carbon for photosynthesis and so an essential resource for primary production (by photosynthetic autotrophs). It has been suggested that added CO2 should, therefore, act as a fertilizer, increasing plant growth and NPP. If this were the case, there is the potential that ecosystems would become 'carbon sinks', removing (some of) the excess CO2 from the atmosphere and sequestering it in added biomass, thus reducing the rate at which this most important 'greenhouse gas' builds up in the atmosphere. This would be a desirable thing. However, as we have seen, the regulation of ecosystem productivity is complex, and this outcome depends on several other things. Describe at least one assumption -- in terms of ecosystem process and properties -- of this hypothesis; that is, what would have to be true before this CO2 fertilization effect (increased NPP resulting in increased sequestration of carbon) could take place? Imagine you were in charge of things; think of some practices you could implement to INCREASE the likelihood that vegetation would take up more CO2 as it became available through increased rates of NPP.
AND TWO of these THREE ABOUT SUCCESSION
4. We have discussed some of the trends one might expect in successional dynamics, particularly in terms of changes in importance of 'life-history' types (for example, 'r-selected' opportunists are particularly well adapted for dispersal and for rapid exploitation of abundant resources; 'K-selected' competitors may grow and disperse more slowly, but have high competitive ability).. Taking all of this into account, discuss how you would expect SPECIES DIVERSITY (considered simply as the number of different species present in a community -- also called 'species richness') to change over ‘successional time’ – that is, over the years following a major disturbance? TO MAKE THIS EASIER (maybe), assume that this happens in a habitat where late-successional communities are closed FORESTS (like most of our local landscape). Sketch a graph showing, generally, how you think species diversity would be related to time since disturbance (don't worry about actual numbers; focus on shape -- trends and slopes), and explain why you predict this pattern. Use appropriate concepts and terminology about competition and niche dynamics.
5. Review the case
study of the Boundary Waters Canoe Area, from which Heinselman
developed the 'shifting mosaic' model of landscape dynamics. Suppose climate change caused a decrease in the frequency of fires such that return time increased from around 100 years to, perhaps, 150-200 years, with other factors staying much the same. Predict how the properties of the 'landscape mosaic' might change. What
changes would you predict if return time DECREASED
significantly? Comment specifically on how these changes might
affect overall diversity.