“…Hydrologically, the karstic nature of the YP and its lack of topographic relief constraint the surface water fluxes to ET and precipitation, which quickly infiltrates deep into the substrate due to the high permeability of the soil and rocks of the YP, leading to the formation of groundwater flows. Ecosystems in the YP strongly depend on groundwater resources especially on those areas where the water table is found at less than 30‐m depth (Bauer‐Gottwein et al, ; Gondwe, Lerer, et al, ; Gondwe, Merediz‐Alonso, & Bauer‐Gottwein, ). Previous studies carried out in the aquifer of the Sian Ka'an Biosphere show how the water balance partitioning and the distribution of groundwater recharge are dominated by the vegetation behaviour, geology, topography and by the proximity of the water table to the ground surface (Gondwe, Hong, Wdowinski, & Bauer‐Gottwein, ; Gondwe, Lerer, et al, ).…”