posted on 2017-02-08, 05:05authored byCaitlin Elise Moore
Tree-grass savanna
ecosystems are a widespread terrestrial biome and are highly valued for their
ecosystem services. They support one fifth of the global human population
through food and timber production and are a key biome for biodiversity, the
water cycle and carbon sequestration. At the global scale, savannas account for
25 % of terrestrial carbon uptake, which is a product of the interplay between
trees and grasses and is maintained through interactions with climate and
disturbance (fire, herbivory, land use change). As the climate changes into the
21st century, the future of savannas in their current form is uncertain.
Modifications to the timing and amount of rainfall delivered to savanna
ecosystems will have implications for species phenology and current structural
(i.e. tree-grass) dynamics. Therefore, it is important to separate the savanna
tree and grass components to understand what governs these dynamics over time
to determine if there is a differential response of trees and grasses to
climate change.
This thesis explores tree and grass dynamics in detail for an
Australian tropical savanna. The eddy covariance technique was employed to
monitor fluxes of carbon, water and energy between the savanna ecosystem and
the atmosphere at the Howard Springs OzFlux site. An understory tower was
utilised to separate the overstory (i.e. tree) and understory (i.e. grass)
contributions into ecosystem fluxes, with particular attention paid to the
gross primary productivity (GPP) component. The partitioned fluxes showed that
the understory was more seasonally dynamic than the overstory, contributing 40
% to ecosystem GPP in the wet season and only 18 % in the dry season.
Understory GPP did not completely cease in the dry season due to contributions
from woody species that occupy 20 % of the understory biomass. To capture the
different phenological signals displayed by the overstory and understory, a
suite of time-lapse cameras (i.e. phenocams) were also installed, where colour
indices were calculated from each camera image to provide a time series of in
situ variability in vegetation greenness. The greenness data closely tracked
GPP over time, and when used in a light use efficiency (LUE) model, tree and
grass GPP estimates from the model were improved. This result reinforces the importance
of vegetation phenology for determining variability in savanna productivity.
The Howard Springs flux site has been in continuous operation
since 2001 and this 15-year flux record was partitioned into overstory and
understory contributions. The partitioned dataset was used to explore whether
the tree-grass ratio had changed over the 15-year period and what the main
meteorological drivers were over time. For the wet season, productivity at
Howard Springs was light limited due to increased cloud cover during the summer
monsoon. In contrast, productivity in the dry season was water limited due to
depletion of soil water stores. Inter-annually, productivity was determined by
soil moisture availability linked with annual rainfall and rainy season length,
and the tree-grass ratio varied in line with changes in the Southern
Oscillation Index (SOI). This research has provided a missing link in our
understanding of tree-grass dynamics in Australian savannas, which is vital if
savanna ecosystems are to be successfully managed in the coming century.