Titlebook: Ecology of Meromictic Lakes; Ramesh D. Gulati,Egor S. Zadereev,Andrei G. Degerm Book 2017 Springer International Publishing AG 2017 Climat

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https://doi.org/10.1007/978-3-642-22015-9radiance levels create conditions that are rarely manifested in temperate lakes. For example, while in temperate lakes the absence of vertical mixing (meromixis) requires a strong salinity gradient to stabilize the water column against thermal convection, deep tropical lakes may remain stable withou

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https://doi.org/10.1007/978-1-0716-0480-9oluble reactive phosphorus, and variable inorganic nitrogen levels. Most of the 16S rRNA gene sequences of microbes are in five major lineages: α- and γ-., ., high G+C Gram positive (.), and low G+C Gram positive (./.). The phytoplankton have large seasonal variations in abundance with maxima in ear

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Ajebbar Omar,Elqorachi Elhoucienic lakes has considerably advanced. Physical processes support the difference in water density between deep (monimolimnion) and surface (mixolimnion) waters in meromictic lakes; such lakes reveal complex biogeochemical interactions that contribute to the maintenance of meromixis. This Conclusion cha

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Introduction: Meromictic Lakes, Their Terminology and Geographic Distribution, monimolimnion, mixolimnion and some other terms related to meromixis. The definition of Hutchinson for meromictic lakes holds for more than 60 years while some modification is required. We differentiate between a meromictic lake and a non-meromictic ones, despite the fact that for deep waters the p

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Chemical Setting and Biogeochemical Reactions in Meromictic Lakeso very high (>300 g L.), i.e. saturated with respect to particular salts. pH varies from acidic (<3) to alkaline (>10), and redox conditions range from well oxygenated and dominated by high concentrations of dissolved ferric iron (Eh about 600 mV in iron-rich acidic pit lakes) to strongly reduced (E

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