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176 resultados para 3 [3 tert butylthio 1 (4 chlorobenzyl) 5 isopropyl 2 indolyl] 2,2 dimethylpropionic acid

em Publishing Network for Geoscientific

Integrated net oxygen production as measured from on-deck incubators

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(Table 3) Different core locations in the North Atlantic, Nordic Seas, and the northern Barents Sea and their AMS 14C dated IRD events corresponding to andror are similar in timing with the Heinrich Events 1-4 in the North Atlantic

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A 1.4.3.3. Data of the saturated column experiments with the sandy fraction of harbour sediments - flow-path sampling after 282 days - trace elements

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A 1.4.3.2. Data of the saturated column experiments with the sandy fraction of harbour sediments - flow-path sampling after 282 days - main elements

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(Table 3) Spherules analyses from DSDP Hole 5-32

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A 1.4.3.1. Data of the saturated column experiments with the sandy fraction of harbour sediments - flow-path sampling after 90 days - liquid/solid ratio, electric conductivity, pH and Eh value, inorganic carbon, dissolved organic carbon and anions

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A 1.4.3.1. Data of the saturated column experiments with the sandy fraction of harbour sediments - flow-path sampling after 282 days - liquid/solid ratio, electric conductivity, pH and Eh value, inorganic carbon, dissolved organic carbon and anions

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A 1.4.3.3. Data of the saturated column experiments with the sandy fraction of harbour sediments - flow-path sampling after 90 days - trace elements

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(Table 2.2.1.4) Individual width of sympagic meiofauna in sections of sea-ice core IO-3

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A 1.4.2.3. Data of the saturated column experiments with the sandy fraction of harbour sediments - outlet - trace elements

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(Table 1) Average fluorescence in the surface layer during POLARSTERN expedition ANT-XXIV/3

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(Table 2.2.1.4) Individual width of sympagic meiofauna in sections of sea-ice core IO-5

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A 1.4.3.2. Data of the saturated column experiments with the sandy fraction of harbour sediments - flow-path sampling after 90 days - main elements

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(Table 3) Basement analyses from DSDP Hole 5-32

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Diversity, standing stock and distribution of living benthic foraminifera suborder groups (Table 3+5)

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