Global Change Abstracts The Swiss Contribution - SCNAT
Global Change Abstracts The Swiss Contribution - SCNAT
Global Change Abstracts The Swiss Contribution - SCNAT
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100<br />
ing geographic distance among parcels, and a<br />
differentiation among grazed and mown parcels,<br />
and among sexually and vegetatively reproducing<br />
populations. Band richness of sampled plants per<br />
village was higher for villages where parcels represented<br />
more different land-use types. Within<br />
populations, microsatellite band diversity was<br />
higher in grazed than in mown parcels. Conclusions<br />
<strong>The</strong> diversity of human land use in the Alps<br />
was associated with genetic diversity of P. alpina.<br />
<strong>The</strong>refore, the ongoing socio-economically motivated<br />
land-use changes, which reduce the number<br />
of different land-use types, will affect the genetic<br />
diversity of P. alpina negatively.<br />
Annals of Botany, 2007, V100, N6, NOV, pp<br />
1249-1258.<br />
08.1-164<br />
Recent decline in precipitation and tree<br />
growth in the eastern Mediterranean<br />
Sarris D, Christodoulakis D, Körner C<br />
Greece, Switzerland<br />
Meteorology & Atmospheric Sciences , Plant Sciences<br />
, Forestry<br />
We present evidence of a recent drying in the<br />
eastern Mediterranean, based on weather and<br />
tree-ring data for Samos, an island of the eastern<br />
Aegean Sea. Rainfall declined rapidly after the<br />
late 1970s following trends for the entire Mediterranean<br />
and was associated with reduced tree-ring<br />
width in Pinus brutia. <strong>The</strong> most recent decline<br />
led to the lowest annual radial stem increment<br />
after the last 100 years (as far as records reach).<br />
As moisture availability decreased best correlations<br />
of tree growth with rainfall were obtained<br />
for progressively longer integration periods (1-2<br />
years in moister periods, 5-6 years during the severe<br />
dryness of 20th century’s last decades), suggesting<br />
increasing dependency in deep soil water.<br />
Such long-term integration periods of tree-growth<br />
responses to precipitation have not been reported<br />
before. <strong>The</strong>y may reflect a tree- rooting pattern<br />
adapted to cope with even several successive dry<br />
years. In late summer 2000, moisture reserves became<br />
exhausted, however, and a substantial fraction<br />
of low altitude pines died, including some<br />
80-year-old trees, which underlines the exceptional<br />
extent this trend had reached. Our findings<br />
provide empirical support for Intergovernmental<br />
Panel on Climate <strong>Change</strong> projections derived<br />
from global circulation models that the Mediterranean,<br />
its eastern basin in particular, should become<br />
drier as temperature rises, as was the case in<br />
the recent past.<br />
<strong>Global</strong> <strong>Change</strong> Biology, 2007, V13, N6, JUN, pp<br />
1187-1200.<br />
<strong>Global</strong> <strong>Change</strong> <strong>Abstracts</strong> – <strong>The</strong> <strong>Swiss</strong> <strong>Contribution</strong> | Terrestrial Ecosystems<br />
08.1-165<br />
Modeling the forest transition: Forest scarcity<br />
and ecosystem service hypotheses<br />
Satake A, Rudel T K<br />
Switzerland, USA<br />
Modelling , Forestry , Social Sciences , Ecology ,<br />
Economics<br />
An historical generalization about forest cover<br />
change in which rapid deforestation gives way<br />
over time to forest restoration is called “the forest<br />
transition.” Prior research on the forest transition<br />
leaves three important questions unanswered:<br />
(1) How does forest loss influence an individual<br />
landowner’s incentives to reforest? (2) How does<br />
the forest recovery rate affect the likelihood of<br />
forest transition? (3) What happens after the forest<br />
transition occurs? <strong>The</strong> purpose of this paper is<br />
to develop a minimum model of the forest transition<br />
to answer these questions. We assume that<br />
deforestation caused by landowners’ decisions<br />
and forest regeneration initiated by agricultural<br />
abandonment have aggregated effects that characterize<br />
entire landscapes. <strong>The</strong>se effects include<br />
feedback mechanisms called the “forest scarcity”<br />
and “ecosystem service” hypotheses. In the forest<br />
scarcity hypothesis, forest losses make forest products<br />
scarcer, which increases the economic value<br />
of forests. In the ecosystem service hypothesis, the<br />
environmental degradation that accompanies the<br />
loss of forests causes the value of ecosystem services<br />
provided by forests to decline. We examined the<br />
impact of each mechanism on the likelihood of<br />
forest transition through an investigation of the<br />
equilibrium and stability of landscape dynamics.<br />
We found that the forest transition occurs only<br />
when landowners employ a low rate of future discounting.<br />
After the forest transition, regenerated<br />
forests are protected in a sustainable way if forests<br />
regenerate slowly. When forests regenerate rapidly,<br />
the forest scarcity hypothesis expects instability<br />
in which cycles of large- scale deforestation<br />
followed by forest regeneration repeatedly characterize<br />
the landscape. In contrast, the ecosystem<br />
service hypothesis predicts a catastrophic shift<br />
from a forested to an abandoned landscape when<br />
the amount of deforestation exceeds the critical<br />
level, which can lead to a resource degrading<br />
poverty trap. <strong>The</strong>se findings imply that incentives<br />
for forest conservation seem stronger in settings<br />
where forests regenerate slowly as well as when<br />
decision makers value the future.<br />
Ecological Applications, 2007, V17, N7, OCT, pp<br />
2024-2036.