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Last millennium Northern Hemisphere summer temperatures from tree rings: Part II, spatially resolved reconstructionsClimate field reconstructions from networks of tree-ring proxy data can be used to characterize

English. Read and Discuss: Forestry = Английский язык. Читаем и обсуждаем: лесное хозяйство

Features of the development stability of tree plantations of large city industrial zones an assessment of the stability of the development of tree plantations growing in the zone of influence

Temperature change as a driver of spatial patterns and long-term trends in chironomid (Insecta: Diptera) diversity increases in colder regions such as the Arctic under sustained global warming, but with complex

History of East European chernozem soil degradation; protection and restoration by tree windbreaks in the russian steppeHistory of East European chernozem soil degradation; protection and restoration by tree windbreaks

Genetic structure of coast redwood (Sequoia sempervirens [D. Don] Endl.) populations in and outside of the natural distribution range based on nuclear and chloroplast microsatellite markers is one of the few conifer tree species that are polyploid. Despite its unique ecological and economic

Imperatives of sustainable development in the shadow and in the light of the pandemic, environmentally responsible, biologically safe, institutionally oriented to the interests of the majority

Carbon dioxide sequestration as a climate mitigation strategy criterion in tropical forests (Case study from central african region) of the Global Carbon Cycles in Atmosphere-Plants – Soil System (APS) represent the response of vegetation

Long-term warming and elevated CO2 increase ammonia-oxidizing microbial communities and accelerate nitrification in paddy soil resilient in response to individual and interactive impacts of warming and elevated CO2. Consequently

Long-term warming and elevated CO2 increase ammonia-oxidizing microbial communities and accelerate nitrification in paddy soil resilient in response to individual and interactive impacts of warming and elevated CO2. Consequently

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