To reconstruct ancient ocean pH, scientists measure boron isotopes in fossil shells of marine organisms. However, these organisms alter their internal chemistry during shell growth—a phenomenon known as the 'vital effect'���which skews isotope ratios away from seawater equilibrium. Scientists correct for this skew by using calibration curves based on modern specimens of the same species grown in controlled environments. A recent study of the benthic foraminifer *Marginopora vertebralis* revealed that its vital effect is heavily influenced by the photosynthetic activity of its symbiotic algae, which varies with light exposure. Therefore, applying a calibration curve to fossil *M. vertebralis* specimens without accounting for the light levels they experienced is likely to ______
Which choice most logically completes the text?
- Alead to the incorrect conclusion that ancient *M. vertebralis* specimens lived in much deeper waters than modern specimens do.
- Bdemonstrate that the chemical composition of seawater has remained completely stable over geological time.
- yield inaccurate reconstructions of ancient ocean acidity levels.Answer
- Dprevent researchers from cultivating modern foraminifera specimens under controlled laboratory conditions.