Biblioteca Digital

57 resultados para Coenzyme Q

(Table B1) Principal Component Loadings of dinocyst Q-mode assemblages, dinocyst diversity and equity, and sporomorph/dinocyst index for the Fischschiefer unit of core Bodenheim

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(Table 3) Chemical composition of hot fluids (end members) from the Q hydrothermal field, East Pacific Rise

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(Table 15) Communalities and factor loadings used in the Q-mode model for sediments from DSDP Hole 93-603B

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(Table B1) Principal Component Loadings of dinocyst Q-mode assemblages, dinocyst diversity and equity, and sporomorph/dinocyst index for the Fischschiefer unit of core Frei-Laubersheim

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Rare earth elements determined in ice core EDC by inductively coupled plasma quadrupole mass spectrometry (ICP-Q-MS)

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Numbers and statistics of benthic foraminiferal Q-mode assemblages for the Lower Oligocene of section Poetschbichl in the Lower Inn Valley area

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(Table 1) NRM intensity, MDF, susceptibility and Q-ratio of serpentinized peridotites recovered from ODP Hole 109-670A

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(Table B1) Principal Component Loadings of dinocyst Q-mode assemblages, dinocyst diversity and equity, and sporomorph/dinocyst index for the Fischschiefer unit of core Bosenheim

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(Table 3) Scaled Varimax species factor scores derived from Q-mode factor analysis of 30 species of benthic foraminifera from 43 samples of Pliocene age from DSDP Hole 72-518

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(Appendix 5) Principal Component Scores of benthic foraminifera Q-mode assemblages from sediment core M5/2_KL15

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(Table 2) Foraminiferal assemblages shown by the five varimax-rotated Q-mode principal component scores

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Rare earth elements determined in ice core EDML by inductively coupled plasma quadrupole mass spectrometry (ICP-Q-MS)

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Q-mode varimax factor scores matrix of benthic foraminifera assemblage of sediment profile GeoB9526

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Rare earth elements determined in ice core EDML by laser-ablation inductively coupled plasma quadrupole mass spectrometry (La-ICP-Q-MS) in 269-270 m depth

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Q-Mode varimax factor scores matrix of diatom assemblages of sediment surface samples

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