Seasonal variations in moisture use in a piñon–juniper woodland
Seasonal variations in moisture use in a piñon–juniper woodland
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DOI:
10.1007/s00442-007-0777-0
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发表时间:
2007-06
期刊:
影响因子:
2.7
通讯作者:
A. West;K. Hultine;K. Burtch;J. Ehleringer
中科院分区:
文献类型:
--
作者:
A. West;K. Hultine;K. Burtch;J. Ehleringer
In water-limited environments of the intermountain region of North America, summer precipitation may play a role in the structure and function of aridland communities and ecosystems. This study examined the potential reliance on summer precipitation of two widespread, coexisting woody species in the southwestern United States,Pinus edulisEnglmn. (Colorado piñon) andJuniperus osteosperma(Torr) Little (Utah juniper). The current distributions ofP.edulisandJ.osteospermaare highly suggestive of different dependencies on summer rainfall. We hypothesized thatP. eduliswas dependent on summer precipitation, utilizing summer precipitation even during extremely dry summers, whereasJ. osteospermawas not dependent, using summer precipitation only when amounts were above some minimum threshold. Using sap flux and stable isotopic methods to assess seasonal water sources and water use efficiency, we examined the response of these two species to seasonal variations in moisture at a site located near the northern limits of the North American monsoon. Both sap flux and isotopic results indicated thatP. eduliswas responsive to summer rain, whileJ. osteospermawas not. Following summer rain events, sap flux density increased inP. edulisfor several days, but not inJ. osteosperma. Isotopic evidence indicated thatP. edulistook up summer-derived moisture to a greater extent thanJ. osteosperma. Values of the natural abundance stable isotope ratio of carbon of leaf soluble carbohydrates increased over the summer forP. edulis, indicative of assimilation at higher water use efficiency, but were invariant forJ. osteosperma. Our results supported the hypothesis thatP. edulisandJ. osteospermaare differentially sensitive to summer precipitation and are discussed in the light of potential changes in the seasonality of precipitation associated with climate change.