2020
DOI: 10.1016/j.agrformet.2020.108040
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Impact of Climate Change and Adaptive Genetic Potential of Norway Spruce at the South–eastern Range of Species Distribution

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Cited by 19 publications
(7 citation statements)
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“…In Romania, local provenances are, generally, less performing than some provenances from other regions [65]. Furthermore, a significant site effect was detected, suggesting that phenotypic plasticity rather than local adaptation explains phenotypic differences among provenances [66][67][68]. Similar results were also observed in other geographical regions of Europe [69][70][71].…”
Section: Discussionsupporting
confidence: 57%
“…In Romania, local provenances are, generally, less performing than some provenances from other regions [65]. Furthermore, a significant site effect was detected, suggesting that phenotypic plasticity rather than local adaptation explains phenotypic differences among provenances [66][67][68]. Similar results were also observed in other geographical regions of Europe [69][70][71].…”
Section: Discussionsupporting
confidence: 57%
“…Considering that drought events will become more frequent and intense in the near future, the strategies to cope with climate change have to prepare forests by increasing the adaptive capacity of tree populations [35]. Recent research shows that selecting and transferring forest reproductive material adapted to the new environmental conditions of the planting site could increase genetic diversity in those areas and could facilitate the adaptation of forest species [36][37][38]. Therefore, assessment of intraspecific genetic variation and identifying populations expected to be best adapted to the future climate conditions is essential for increasing forest productivity and adaptability in the context of climate changes.…”
Section: Introductionmentioning
confidence: 99%
“…The +2°C and +3°C MAAT isotherms appear to rise statistically significant over 1961–2010 period, suggesting a potential expansion of the areas of climate‐favourable physiologically conditions for the development of forest vegetation (Mihai et al , 2018a, 2018b, 2020) but also a likely decrease in the periglacial processes dynamics at the lower boundary of the periglacial belt. The largest upslope shifts were estimated for the +3°C MAAT in the E Carpathians (225 m/50 years) (Figure 8).…”
Section: Resultsmentioning
confidence: 98%