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Absorption maxima were recorded with an accuracy of 0.5 nm.
Absorption maxima were recorded at 342 nm (B-band), 612 nm (vibrational band) and 668 nm (Q-band).
For studies of seasonal biomass changes, the annual maxima were recorded.
Two distinct production maxima were recorded instead of the one seen in isoflavone concentration curves characteristic for shake flask-grown cells (Figs. 3b d and 4b d).
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Sometimes the T-value for individual peak maxima is recorded, sometimes not.
The average and maximum HRs achieved, together with the time spent with HR greater than 65% of age-predicted HR maximum, were recorded.
At each temperature, [H+] and absorbance at λ = 529 nm (the H2I absorbance maximum) were recorded, along with isosbestic point absorbances, which were used to account for dilution due to the acid additions.
Exceptionally, a basin-wide regression maximum is recorded some time before the Cretaceous Tertiary boundary (K/T).
The minimum surface water temperature was recorded during monsoon season (November 2012) and maximum was recorded during the summer season (May 2013) Fig. 3.
The temperature of the study sites ranges from 19 to 30 °C, the maximum is recorded in the months of May and June (Fig. 1).
Their proliferation maximum is recorded in the first postnatal week followed by elongation and migration into the internal granular layer.
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