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Both localities are characterized by dense dendritic drainage systems (Fig. 1b).
Cm-scale displacement faults at both localities display ramp-flat geometries.
In both localities, timber is harvested via reduced-impact logging (RIL) practices.
Both localities show floristic impoverishment within the 20th Century, with relatively recent single-taxon supremacy.
In both localities, d-excess values varied widely from 10.07 to 17.34 ‰ with a mean value of 13.70 ‰.
The isotopic enrichments characterised low convective activity before and after the onset of the monsoon in both localities.
The habitat in both localities is open secondary scrub that has been affected by recurring forest fires (Fig. 1).
The generated local meteoric water lines are useful in assessing the origin and mechanism of groundwater recharge in both localities.
Both localities present cold, dry and humid, warm fluctuations at the transition between the Early and the Middle Pleistocene.
A combined geophysical survey on the flysch rocks was performed on both localities to enhance our present findings.
The study provides additional stable isotope data for groundwater recharge studies in both localities (especially the first meteoric line in Yaounde) and climatological investigations in tropical Africa.
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