Describe the trend. As temperature increases, the mean absorbance of the solution increases, showing that more betalain pigment leaks out and the membrane becomes more permeable. The rise is small and gradual from 20 °C to 40 °C (absorbance only rises from 0.12 to 0.22, a change of 0.10), but then increases sharply between 40 °C and 60 °C (from 0.22 to 0.95, a change of 0.73). Above 60 °C the increase levels off / plateaus (60 °C to 70 °C rises only from 0.95 to 1.04).
Explain the gradual region (20–40 °C). At these temperatures the phospholipids and proteins have relatively low kinetic energy; the bilayer stays largely intact and stable, so the membrane remains partially permeable and little pigment escapes.
Explain the sharp rise (40–60 °C). As temperature rises further the molecules gain more kinetic energy and move more, opening gaps; crucially, above about 45 °C the membrane proteins denature — the hydrogen bonds and other interactions holding their tertiary structure break, so the proteins change shape — and the phospholipid bilayer becomes increasingly disrupted. The membrane is therefore far more permeable, so a much larger amount of betalain leaks from the vacuole into the water, giving the steep rise in absorbance.
Explain the plateau (above 60 °C). Above 60 °C the membrane is already maximally disrupted and most of the available pigment has already leaked out, so absorbance cannot rise much further.
Evaluation. The data do support the conclusion that membrane disruption is greatest between 40 °C and 60 °C, because that is where absorbance rises most steeply (the largest gradient), consistent with protein denaturation occurring over this range. However, the support is limited: the temperature intervals are wide (10 °C), so the exact threshold between 40 °C and 50 °C is not resolved — readings at, say, 42, 44, 46 and 48 °C would pinpoint it. There is also no indication of repeats or error bars, so the reliability and spread of the means cannot be judged, and a single anomalous tube could distort a point. To strengthen the conclusion the student should repeat each temperature and calculate means with a measure of spread, and take smaller temperature intervals around 40–60 °C.