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Temperate and cold temperate waters worldwide.
Scandinavia, eastern Europe, western Siberia, and Alaska harbour the balance of peatlands in the cold temperate region.
For example, wetlands in boreal and cold temperate forests tend to recover more slowly than do warm wetlands.
Lowland tundra animals appear to have evolved in central Eurasia when tundra replaced the cold temperate steppe.
The largest families of orthopterans are worldwide in range, although all have decreased numbers of species in cold temperate zones.
These parameters were studied after simulated and natural runoff at four different sites in Southern Norway with cold temperate climate.
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Assis, J., Lucas, A. V., Bárbara, I. & Serrão, E. Á. Future climate change is predicted to shift long-term persistence zones in the cold-temperate kelp Laminaria hyperborea.
The soils of cold-temperate mountainous forest ecosystems contain large carbon pools that may respond quickly to changes in climate and land use.
The primary objective of this study was to understand the spatial distribution of SOC within a representative mountainous landscape in the cold-temperate zone in Japan.
Cold-temperate transition surfaces in polythermal glaciers and at the permafrost base in their forelands can act as a specific hub between the glacial and periglacial domains.
Estimated temperatures from both proxies coincide, in general terms: cold-temperate conditions during the latest Tortonian (~ 16 °C; cold-temperate climate), dry sub-tropical conditions during the Messinian (16.6 °C 22 °C), and dry sub-tropical conditions during the early Pliocene (16.6 °C 17.2 °C).
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