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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.

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