@article{fdi:010077399, title = {{T}he role of deep vadose zone water in tree transpiration during drought periods in karst settings - {I}nsights from isotopic tracing and leaf water potential}, author = {{C}arri{\`e}re, {S}. {D}. and {M}artin-{S}t{P}aul, {N}. {K}. and {C}akpo, {C}. {B}. and {P}atris, {N}icolas and {G}illon, {M}. and {C}halikakis, {K}. and {D}oussan, {C}. and {O}lioso, {A}. and {B}abic, {M}. and {J}ouineau, {A}. and {S}imioni, {G}. and {D}avi, {H}.}, editor = {}, language = {{ENG}}, abstract = {{K}arst environments are unusual because their dry, stony and shallow soils seem to be unfavorable to vegetation, and yet they are often covered with forests. {H}ow can trees survive in these environments? {W}here do they find the water that allows them to survive? {T}his study uses midday and predawn water potentials and xylem water isotopes of branches to assess tree water status and the origin of transpired water. {M}onitoring was conducted during the summers of 2014 and 2015 in two dissimilar plots of {M}editerranean forest located in karst environments. {T}he results show that the three monitored tree species ({A}bies alba {M}ill, {F}agus sylvatica {L}, and {Q}uercus ilex {L}.) use deep water resources present in the karst vadose zone (unsaturated zone) more intensively during drier years. {Q}uercus ilex, a species well- adapted to water stress, which grows at the drier site, uses the deep water resource very early in the summer season. {C}onversely, the two other species exploit the deep water resource only during severe drought. {T}hese results open up new perspectives to a better understanding of ecohydrological equilibrium and to improved water balance modeling in karst forest settings.}, keywords = {{ZONE} {MEDITERRANEENNE}}, booktitle = {}, journal = {{S}cience of the {T}otal {E}nvironment}, volume = {699}, numero = {}, pages = {art. 134332 [10 p.]}, ISSN = {0048-9697}, year = {2020}, DOI = {10.1016/j.scitotenv.2019.134332}, URL = {https://www.documentation.ird.fr/hor/fdi:010077399}, }