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Reiner Giesler
Researcher at Umeå University
Publications - 110
Citations - 7656
Reiner Giesler is an academic researcher from Umeå University. The author has contributed to research in topics: Soil water & Permafrost. The author has an hindex of 48, co-authored 106 publications receiving 6755 citations. Previous affiliations of Reiner Giesler include Swedish University of Agricultural Sciences.
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Boreal forest plants take up organic nitrogen
TL;DR: The data indicate that organic nitrogen is important for these different plants, even when they are competing with each other and with non-symbiotic microorganisms, which has major implications for the understanding of the effects of nitrogen deposition, global warming and intensified forestry.
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Rock-eating fungi
A.G. Jongmans,N. van Breemen,Ulla S. Lundström,P.A.W. van Hees,Roger D. Finlay,M. Srinivasan,Torgny Unestam,Reiner Giesler,P.-A. Melkerud,Mats Olsson +9 more
TL;DR: In this paper, symbiotic mycorrhizal hyphae translocate dissolved minerals from the isolated micropores directly to their host plants, bypassing competition for nutrient uptake by other organisms.
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Fertilization of boreal forest reduces both autotrophic and heterotrophic soil respiration
TL;DR: In this paper, a large-scale girdling experiment was performed in a long-term nutrient optimization experiment in a 40-year-old stand of Norway spruce in northern Sweden.
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Low molecular weight organic acids and their Al-complexes in soil solution—composition, distribution and seasonal variation in three podzolized soils
TL;DR: Low molecular weight organic acids have been determined qualitatively and quantitatively over a growing season in the soil solution of three podzolized soil profiles as discussed by the authors, and several low molecular weight (LMW) acids such as citric, shikimic, oxalic, fumaric, formic, acetic, malonic, malic, lactic and t-aconitic acids were identified.
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Mycorrhizal weathering: A true case of mineral plant nutrition?
TL;DR: In this article, weatherable minerals in all podzol surface soils and shallow granitic rock under European coniferous forests studied hitherto are crisscrossed by numerous open, tubular pores, 3-10 μm in width.