Species-specific indication of 13 tree species growth on climate warming in temperate forest community of northeast China

Temperate forests in northeast Asia are crucial to maintaining biodiversity conservation and ecological security. Under the background of global warming and drought, it is of great significance to study the special indicator effect of tree growth on climate change. Dendrochronological analysis of di...

Full description

Bibliographic Details
Main Authors: Cherubini, P. (Author), Li, Z. (Author), Wang, X. (Author), Yuan, D. (Author), Zhang, Y. (Author), Zhu, L. (Author)
Format: Article
Language:English
Published: Elsevier B.V. 2021
Subjects:
Online Access:View Fulltext in Publisher
LEADER 04295nam a2200709Ia 4500
001 10.1016-j.ecolind.2021.108389
008 220427s2021 CNT 000 0 und d
020 |a 1470160X (ISSN) 
245 1 0 |a Species-specific indication of 13 tree species growth on climate warming in temperate forest community of northeast China 
260 0 |b Elsevier B.V.  |c 2021 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1016/j.ecolind.2021.108389 
520 3 |a Temperate forests in northeast Asia are crucial to maintaining biodiversity conservation and ecological security. Under the background of global warming and drought, it is of great significance to study the special indicator effect of tree growth on climate change. Dendrochronological analysis of different tree species in the same community under climate change can provide valuable information for the adaptive potential of tree species and the species-specific growth indications. Here, we compared the radial growth patterns of 13 co-occurring tree species in a temperate forest community in northeast China. Pearson correlation and moving interval analysis were used to reveal the key climate factors affecting radial growth and the temporal stability of growth-climate relationships, respectively. Results showed that temperature and moisture played a key role in the radial growth of the 13 co-occurring tree species in northeast China. The radial growth of Pinus sylvestris var. mongolica, Picea koraiensis, and Ulmus davidiana increased significantly after rapid warming (around the 1980s), while the radial growth of Pinus koraiensis, Acer mono, and Betula platyphylla decreased slightly. The radial growth of almost all tree species (except P. koraiensis, A. mono, and B. platyphylla) had a positive indication of temperature, especially Juglans mandshurica, Fraxinus mandshurica, and U. davidiana. The precipitation in the early growing season (May to June) and the relative humidity in the growing season were positively correlated with the growth of most species. Coniferous and diffuse-porous tree species were more resistant and recovery to extreme droughts than semi-ring-porous and ring-porous species (except U. davidiana). The 13 co-occurring tree species, especially conifers, showed low resistance and high recovery to extreme temperature. The differences in the growth-climate relationships among different species may be related to wood properties and ecological habits. If the climate continues to warm, coniferous trees will suffer the most serious impact, so they need protection most. Our results highlight that differentiated strategies are needed for the management and restoration of different tree species due to the species-specific indications of climate warming. © 2021 The Authors 
650 0 4 |a Acer mono 
650 0 4 |a Asia 
650 0 4 |a Betula platyphylla 
650 0 4 |a biodiversity 
650 0 4 |a Biodiversity 
650 0 4 |a China 
650 0 4 |a climate change 
650 0 4 |a Climate warming 
650 0 4 |a Coniferophyta 
650 0 4 |a Conservation 
650 0 4 |a Co-occurring community 
650 0 4 |a Co-occurring community 
650 0 4 |a Correlation methods 
650 0 4 |a Drought 
650 0 4 |a Ecology 
650 0 4 |a Forestry 
650 0 4 |a Fraxinus mandshurica 
650 0 4 |a global warming 
650 0 4 |a Global warming 
650 0 4 |a growing season 
650 0 4 |a Indicator indicator 
650 0 4 |a Juglans mandshurica 
650 0 4 |a Northeast China 
650 0 4 |a Picea koraiensis 
650 0 4 |a Pinus koraiensis 
650 0 4 |a Pinus sylvestris 
650 0 4 |a Radial-growth 
650 0 4 |a Rapid warming 
650 0 4 |a Rapid warming 
650 0 4 |a Recovery 
650 0 4 |a Recovery 
650 0 4 |a relative humidity 
650 0 4 |a Resistance 
650 0 4 |a Resistance 
650 0 4 |a Species specifics 
650 0 4 |a temperate forest 
650 0 4 |a Temperate forest 
650 0 4 |a Temperate forests 
650 0 4 |a tree 
650 0 4 |a Tree growth 
650 0 4 |a Tree growth 
650 0 4 |a Tree species 
650 0 4 |a Ulmus davidiana 
700 1 |a Cherubini, P.  |e author 
700 1 |a Li, Z.  |e author 
700 1 |a Wang, X.  |e author 
700 1 |a Yuan, D.  |e author 
700 1 |a Zhang, Y.  |e author 
700 1 |a Zhu, L.  |e author 
773 |t Ecological Indicators