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| Titel |
Climatic factors and reindeer grazing -- the effects on soil carbon dynamics
in subarctic boreal pine forest. |
| VerfasserIn |
Kajar Köster, Egle Köster, Frank Berninger, Jukka Pumpanen |
| Konferenz |
EGU General Assembly 2016
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| Medientyp |
Artikel
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| Sprache |
en
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 18 (2016) |
| Datensatznummer |
250125869
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| Publikation (Nr.) |
 EGU/EGU2016-5520.pdf |
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| Zusammenfassung |
| Reindeer (Rangifer tarandus L.) are the most important large mammalian herbivores in the
northern ecosystems, affecting plant diversity, soil nutrient cycling and soil organic matter
decomposition. Changes caused by reindeer in vegetation have indirect effects on physical
features of the soil e.g. soil microclimate, root biomass and also on soil carbon
dynamics.
In a field experiment in Finnish Lapland, Värriö Strict Nature Reserve (67˚ 46’ N, 29˚
35’ E) we investigated how the reindeer grazing in subarctic boreal forest combined with
climate (air temperature and precipitation) affects soil temperature, soil water content, and
ultimately the CO2 efflux from forest soils. The study was carried out in the growing seasons
of the years 2013 and 2014, where 2013 was an extremely dry year (specially the summer),
and the year 2014 was a “normal” year in means of precipitations. Our study areas are located
in the northern boreal subarctic coniferous forest at the zone of the last intact forest
landscapes in Fennoscandia, where large areas of relatively undisturbed subarctic Scots pine
(Pinus sylvestris L.) forests can still be found. We established the experiment as a
split plot experiment with 2 blocks and 5 sub-plots per treatment that were divided
into grazed and non-grazed parts, separated with a fence. The sample plots are
located along the borderline between Finland and Russia, where the ungrazed area
was excluded from reindeer already in 1918, to prevent the Finnish reindeer from
going to the Russian side and there are not many reindeer on Russian side of the
area.
Our study showed that in subarctic mature pine forests, soil temperatures were higher, and
soil water content was fluctuating more on grazed areas compared to non-grazed areas in both
years. In both years, the soil water content on the grazed area was highest in June. The
situation changed somewhere in the second half of July when the moisture content in the
non-grazed area was higher. We found significant negative correlation between soil water
content and soil temperature. The soil CO2 effluxes were mostly affected by the year of
measurement, time of measurement (different months through growing season), soil
temperature and also area (grazed or non-grazed). In both years we measured higher CO2
emissions on the grazed areas compared to non-grazed areas but the difference was
not significant. The average soil CO2 efflux values were significantly higher in
year 2014 compared to 2013 mainly due to differences in soil temperature at the
beginning of the season. Soil moisture content was not affecting the soil CO2 efflux. |
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