Details
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 58-65 |
| Seitenumfang | 9 |
| Fachzeitschrift | Biology Bulletin |
| Jahrgang | 36 |
| Publikationsstatus | Veröffentlicht - 4 Feb. 2009 |
Abstract
Changes in the composition of wood organic matter in dead-standing spruce and larch trees depending on the period after their death have been studied in the north of Central Siberia. The period after tree death has been estimated by means of cross-dating. The results show that changes in the composition of wood organic matter in 63% of cases are contingent on tree species. Wood decomposition in dead-standing trees is accompanied by an increase in the contents of alkali-soluble organic compounds. Lignin oxidation in larch begins approximately 80 years after tree death, whereas its transformation in spruce begins not earlier than after 100 years. In the forest-tundra of Central Siberia, the rate of wood organic matter transformation in dead-standing trees is one to two orders of magnitude lower than in fallen wood, which accounts for their role as a long-term store of carbon and mineral elements in these ecosystems.
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in: Biology Bulletin, Jahrgang 36, 04.02.2009, S. 58-65.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - Wood Transformation in Dead-Standing Trees in the Forest–Tundra of Central Siberia
AU - Mukhortova, L. V.
AU - Kirdianov, A. V.
AU - Myglan, V. S.
AU - Guggenberger, G.
PY - 2009/2/4
Y1 - 2009/2/4
N2 - Changes in the composition of wood organic matter in dead-standing spruce and larch trees depending on the period after their death have been studied in the north of Central Siberia. The period after tree death has been estimated by means of cross-dating. The results show that changes in the composition of wood organic matter in 63% of cases are contingent on tree species. Wood decomposition in dead-standing trees is accompanied by an increase in the contents of alkali-soluble organic compounds. Lignin oxidation in larch begins approximately 80 years after tree death, whereas its transformation in spruce begins not earlier than after 100 years. In the forest-tundra of Central Siberia, the rate of wood organic matter transformation in dead-standing trees is one to two orders of magnitude lower than in fallen wood, which accounts for their role as a long-term store of carbon and mineral elements in these ecosystems.
AB - Changes in the composition of wood organic matter in dead-standing spruce and larch trees depending on the period after their death have been studied in the north of Central Siberia. The period after tree death has been estimated by means of cross-dating. The results show that changes in the composition of wood organic matter in 63% of cases are contingent on tree species. Wood decomposition in dead-standing trees is accompanied by an increase in the contents of alkali-soluble organic compounds. Lignin oxidation in larch begins approximately 80 years after tree death, whereas its transformation in spruce begins not earlier than after 100 years. In the forest-tundra of Central Siberia, the rate of wood organic matter transformation in dead-standing trees is one to two orders of magnitude lower than in fallen wood, which accounts for their role as a long-term store of carbon and mineral elements in these ecosystems.
UR - http://www.scopus.com/inward/record.url?scp=63249123966&partnerID=8YFLogxK
U2 - 10.1134/S1062359009010099
DO - 10.1134/S1062359009010099
M3 - Article
C2 - 19239115
VL - 36
SP - 58
EP - 65
JO - Biology Bulletin
JF - Biology Bulletin
SN - 1062-3590
ER -