@article{
 title = {Long-term dynamics of water and carbon in semi-arid ecosystems: a gradient analysis in the Patagonian steppe},
 type = {article},
 year = {2000},
 identifiers = {[object Object]},
 keywords = {crn1},
 pages = {133-143-143},
 volume = {150},
 websites = {http://dx.doi.org/10.1023/a:1026578403956,citeulike-article-id:7752942},
 month = {10},
 publisher = {Springer Netherlands},
 day = {1},
 id = {a795f0e9-0a7b-3469-8a53-97fa7e769b43},
 created = {2019-04-01T18:01:50.764Z},
 file_attached = {false},
 profile_id = {1f5347e3-dec5-3349-a941-3b484c2dfce9},
 group_id = {184ee5d4-bd93-3566-938b-14cc43849390},
 last_modified = {2019-04-01T18:01:50.764Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {false},
 hidden = {false},
 source_type = {JOUR},
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 abstract = {We used a soil water simulation model and remotely sensed data to study the long-term dynamics of transpiration, evaporation, drainage and net primary production across a precipitation gradient in Northwestern Patagonia (Argentina). The proportion of precipitation transpired, the precipitation use efficiency and the transpiration use efficiency were constant across the gradient that covered a range of 150 to 600 mm. The proportion of water evaporated was higher than the proportion drained at the driest extreme of the gradient. The opposite relationship was observed at the wet extreme.},
 bibtype = {article},
 author = {Paruelo, J M and Sala, O E and Beltrán, Adriana},
 journal = {Plant Ecology},
 number = {1}
}

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