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Titlebook: Biosphere Origin and Evolution; Nikolay Dobretsov,Nikolay Kolchanov,Georgy Zavarzi Book 2008 Springer-Verlag US 2008 Biom.Evolution.Seen.b

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51#
發(fā)表于 2025-3-30 12:05:08 | 只看該作者
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發(fā)表于 2025-3-30 12:43:10 | 只看該作者
53#
發(fā)表于 2025-3-30 16:56:08 | 只看該作者
54#
發(fā)表于 2025-3-30 23:07:01 | 只看該作者
On the concept for the Organization of the Modern Biosphere in the Terrestrial Subsurfacebiosphere in the terrestrial subsurface into three zones. The zone of the hydrocarbon-oxidizing bacterial filter is situated at depths of up to 1000 m. The biota of this zone utilizes methane and other hydrocarbons. The zone of the carbon dioxide–hydrogen bacterial filter is situated at even greater
55#
發(fā)表于 2025-3-31 03:55:14 | 只看該作者
Biomineralization and Evolution. Coevolution of Mineral and Biological Worldserent origin resulting from the exchange of the matter, energy, and information is applicable to a broad range of processes in nature. This chapter considers biomineralization, one of the fundamental biospheric phenomena, as an example of coevolution of the biological and mineralogical worlds.
56#
發(fā)表于 2025-3-31 07:06:47 | 只看該作者
Visualization of the Silicon Biomineralization in Cyanobacteria, Sponges and Diatoms the biosphere. At present, only diatoms retain this leading position. Using microscopy techniques, we studied mineralization of Si by these organisms. Analysis of silicateins-proteins, which take part in condensation of silica in sponges – helped to establish phylogeny of sponges of Lake Baikal. Th
57#
發(fā)表于 2025-3-31 12:04:27 | 只看該作者
On Important Stages of Geosphere and Biosphere Evolutioneffusive material and the “plume dropper,” which changes the oceanic-to-continental area ratio and the mantle-to-island-arc volcanism intensity ratio every 30 Myr. The World Ocean operates as a homeostatic system: it tempers climates, distributes biogene concentrations evenly over the globe and prov
58#
發(fā)表于 2025-3-31 13:52:48 | 只看該作者
59#
發(fā)表于 2025-3-31 20:47:55 | 只看該作者
60#
發(fā)表于 2025-4-1 01:04:57 | 只看該作者
The Prebiotic Phase of the Origin of Life as Seen by a Physical Chemistxide. One can expect that the Formosa reaction could initiate the above-mentioned prebiological evolution resulting in appearance of ribose which is known as a key element of both RNA and DNA molecules.
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