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m = measured isotopic composition corrected for blank contribution and mass discrimination.
The change of absorbance at 340 nm was measured and corrected for blank values not including d-galactose.
The comparison of (40Ar/36Ar m and (38Ar/36Ar m ratios for eleven plagioclase-rich lithic fragments, corrected for blank and mass discrimination, is shown in Fig. 2.
Argon data for the plagioclase-rich lithic fragments, corrected for blank contribution, and reactor-produced interferences are given in Table 2.
For the sake of clarity, all values shown below have been corrected for blank value before calculation of the aluminum concentration.
The measured 36Ar abundance (36Arm) in eleven plagioclase-rich lithic fragments, corrected for blank contribution and mass discrimination, varies from 0.41 × 10−6 cm3 STP/g (i.e., Plag#23) to 4.1 × 10−6 cm3 STP/g (i.e., Plag#10) (Table 2).
Similar(48)
IC50 values and error margins were determined after logit-log-transformation of the respective values corrected for blanks.
A450nm values were obtained via plate reader and were corrected for blank-well absorbance.
Absorbance readings of samples were made at 420 nm and corrected for blank-well absorbance.
Absorbance (450 nm) values were obtained via plate reader, corrected for blank-well absorbance, and the values for replicate samples were averaged.
All ratios were normalized to 86Sr/88Sr to account for mass fractionation and all results were corrected for blanks.
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