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Pacific Ocean Mega Ecotone of Northern Eurasia - An Evolutionary Model of a Continental Biosphere (Hardcover)
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Pacific Ocean Mega Ecotone of Northern Eurasia - An Evolutionary Model of a Continental Biosphere (Hardcover)
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The monograph presents the results of studies of the organization
of terrestrial geo (eco-) systems in the Pacific mobile belt - the
tectonically and climatically active zone of contact between the
mainland and the ocean, creating new land areas. A detailed
evolutionary landscape-ecological concept based on a discrete
empirical-statistical modeling of forest natural complexes at
various stages of the geological history of the formation of the
continental biosphere in the Northwest Pacific is presented. Based
on the materials of large-scale landscape surveys conducted at
experimental ranges, three spatiotemporal sections are described
with a common trajectory of subaerial landscape genesis: 1)
neo-specific, progressive - the stage of nucleation and upward
evolution of volcanogenic island-arc geosystems of the
Neogene-Quaternary age in the ocean environment, with the formation
at the local level of the beginnings of zonal types of geographical
environment and with the emergence of "climate unjustified" highly
productive forests due to geothermal th power of active volcanoes;
2) subpacific marginal continental - the stage of their subsequent
continental development as a young (Mesozoic) mountain-valley
morphostructure, with the formation of buffer forest communities of
evolutionary menopause; 3) subpacific regressive - the final stage
of decaying evolution, due to the fragmentation and sinking of the
marginal parts of the material, with the advent of continental
islands with a "decrepit" denudation relief, active exogenous
morpholithogenesis and a simplified structure of the forest cover.
The climatic-genetic mechanisms of evolutionary
landscape-ecological processes in various sectors of the Pacific
megaecoton are described using simulation of these processes
according to landscape forecasts for the next 100-200 years.
According to the stability parameters of forest communities,
chronological regularities of climatogenic phytocenotic
transformations in the island-arc and marginal continental
landscapes are revealed.
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