Kuznetsov A P, Vinogradov M E
Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117851 Russia.
Izv Akad Nauk Ser Biol. 2002 Nov-Dec(6):714-7.
The scale of production-destruction biotic balance in the Black Sea ecosystem, flows of organic carbon, carbon dioxide, and oxygen, and rate and volume of organic matter input in the Black Sea sediment as a source of formation and accumulation of fossilized hydrocarbon fuel minerals are estimated on the basis of the current concept of efficiency of solar radiation utilization by photosynthesis. The volume of "excessive" oxygen formed in the ecosystem and its contribution to global oxygenation of the atmosphere are shown.
基于当前光合作用利用太阳辐射效率的概念,估算了黑海生态系统中生物生产 - 破坏平衡的规模、有机碳、二氧化碳和氧气的流动,以及作为化石烃燃料矿物形成和积累来源的黑海沉积物中有机质输入的速率和体积。展示了生态系统中形成的“过量”氧气的体积及其对全球大气氧化的贡献。