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(Table 2) Major elements glass chemistry of the three tephra layers recognise...
Chemistry of tephra layers at 310-315 and 896-897 cm were obtained using SEM-EDS analyses (Scanning Electron Microscopy - Energy Dispersive Spectroscopy), while EPMA-WDS... -
Susceptibility of sediment core Lz1120
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Fig. 4 Sedimentology of core Lz1084 from the central lake basin
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Fig. 6 Radionuclides and total incorangic carbon in sediment core OHR02-1
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Total incorganic carbon content in sediment core OHR03-2
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Total incorganic carbon content in sediment core OHR03-1
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Fig. 7.1 Susceptibility of sediment core Lz1120
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Fig. 7.2 Susceptibility of sediment core Lz1083
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Total incorganic carbon content in sediment core Lz1085
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Fig. 7.4 Susceptibility of sediment core Lz1084
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Total incorganic carbon content in sediment core Lz1083
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Fig. 7.5 Susceptibility of sediment core Lz1085
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Total incorganic carbon content in sediment core Lz1120
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Fig. 7.8 Susceptibility of sediment core Lz1086
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Total incorganic carbon content in sediment core Lz1086
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Geochemistry on various tephrostratigraphic records
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Fig. 3. Lithology and sedimentology on profile Lz1020
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(Table 3) Identified diatoms in sediments of Terrasovoje, Radok and Beaver la...
P = present, P(S) = only singe valves were observed, P(E) = endemic to the Antarctic region, - = not observed. -
(Table 2) Water chemistry of Terrasovoje, Radok and Beaver lakes, Amery Oasis...
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Table A.1 Trace element concentrations of sulfides from Pemba
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