Water relations of riparian plants from warm desert regions
Riparian plants have been classified as “drought avoiders” due to their access to an abundant subsurface water supply. Recent water-relations research that tracks water sources of riparian plants using the stable isotopes of water suggests that many plants of the riparian zone use ground water rathe...
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Veröffentlicht in: | Wetlands (Wilmington, N.C.) N.C.), 1998-12, Vol.18 (4), p.687-696 |
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description | Riparian plants have been classified as “drought avoiders” due to their access to an abundant subsurface water supply. Recent water-relations research that tracks water sources of riparian plants using the stable isotopes of water suggests that many plants of the riparian zone use ground water rather than stream water, and not all riparian plants are obligate phreatophytes (dependent on ground water as a moisture source) but may occasionally be dependent on unsaturated soil moisture sources. A more thorough understanding of riparian plant-water relations must include water-source dynamics and how those dynamics vary over both space and time. Many rivers in the desert, Southwest have been invaded by the exotic shrubTamarix ramosissima (saltcedar). Our studies ofTamarix invasion into habitats formerly dominated by native riparian forests of primarilyPopulus andSalix have shown thatTamarix successfully invades these habitats because of its (1) greater tolerance to water stress and salinity, (2) status, as a facultative, rather than obligate, phreatophyte and, therefore, its ability to recover from droughts and periods of ground-water drawdown, and (3) superior regrowth after fire. Analysis of water-loss rates indicate thatTamarix-dominated stands can have extremely high evapotranspiration rates when water tables are high but not necessarily when water tables are lower.Tamarix has leaf-level transpiration rates that are comparable to native species, whereas sap-flow rates per unit sapwood area are higher than in natives, suggesting thatTamarix maintains higher leaf area than can natives, probably due to its greater water stress tolerance.Tamarix desiccates and salinizes floodplains, due to its salt exudation and high transpiration rates, and may also accelerate fire cycles, thus predisposing these ecosystems to further loss of native taxa. Riparian species on regulated rivers can be exposed to seasonal water stress due to depression of floodplain water tables and elimination of annual floods. This can potentially result in a community shift toward more stress-tolerant taxa, such asTamarix, due to the inability of other riparian species to germinate and establish in the desiccated floodplain environment Management efforts aimed at maintaining native forests on regulated rivers and slowing the spread ofTamarix invasion must include at least partial reintroduction of historical flow, regimes, which favor the recruitment of native riparian species and reverse long |
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Recent water-relations research that tracks water sources of riparian plants using the stable isotopes of water suggests that many plants of the riparian zone use ground water rather than stream water, and not all riparian plants are obligate phreatophytes (dependent on ground water as a moisture source) but may occasionally be dependent on unsaturated soil moisture sources. A more thorough understanding of riparian plant-water relations must include water-source dynamics and how those dynamics vary over both space and time. Many rivers in the desert, Southwest have been invaded by the exotic shrubTamarix ramosissima (saltcedar). Our studies ofTamarix invasion into habitats formerly dominated by native riparian forests of primarilyPopulus andSalix have shown thatTamarix successfully invades these habitats because of its (1) greater tolerance to water stress and salinity, (2) status, as a facultative, rather than obligate, phreatophyte and, therefore, its ability to recover from droughts and periods of ground-water drawdown, and (3) superior regrowth after fire. Analysis of water-loss rates indicate thatTamarix-dominated stands can have extremely high evapotranspiration rates when water tables are high but not necessarily when water tables are lower.Tamarix has leaf-level transpiration rates that are comparable to native species, whereas sap-flow rates per unit sapwood area are higher than in natives, suggesting thatTamarix maintains higher leaf area than can natives, probably due to its greater water stress tolerance.Tamarix desiccates and salinizes floodplains, due to its salt exudation and high transpiration rates, and may also accelerate fire cycles, thus predisposing these ecosystems to further loss of native taxa. Riparian species on regulated rivers can be exposed to seasonal water stress due to depression of floodplain water tables and elimination of annual floods. This can potentially result in a community shift toward more stress-tolerant taxa, such asTamarix, due to the inability of other riparian species to germinate and establish in the desiccated floodplain environment Management efforts aimed at maintaining native forests on regulated rivers and slowing the spread ofTamarix invasion must include at least partial reintroduction of historical flow, regimes, which favor the recruitment of native riparian species and reverse long-term desiccation of desert floodplain environments.</description><identifier>ISSN: 0277-5212</identifier><identifier>EISSN: 1943-6246</identifier><identifier>DOI: 10.1007/BF03161683</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Annual floods ; Desert environments ; Desert plants ; Deserts ; Desiccation ; Drawdown ; Drought ; Environmental management ; Evapotranspiration ; Exudation ; Floodplains ; Flow rates ; Groundwater ; Indigenous species ; Isotopes ; Leaf area ; Leaves ; Phreatophytes ; Plants (botany) ; Populus ; Regrowth ; Regulated rivers ; Reintroduction ; Riparian forests ; Riparian land ; River regulations ; Rivers ; Salix ; Soil moisture ; Stable isotopes ; Subsurface water ; Tamarix ; Tamarix ramosissima ; Taxa ; Transpiration ; Unsaturated soils ; Water analysis ; Water relations ; Water shortages ; Water stress ; Water supply ; Water table</subject><ispartof>Wetlands (Wilmington, N.C.), 1998-12, Vol.18 (4), p.687-696</ispartof><rights>Society of Wetland Scientists 1998.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c354t-741d266cedb64e9e605c1ddba7fb3785d4ef84121a0f422baa1dedabeb4185763</citedby><cites>FETCH-LOGICAL-c354t-741d266cedb64e9e605c1ddba7fb3785d4ef84121a0f422baa1dedabeb4185763</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.proquest.com/docview/2919515664?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>315,782,786,21397,27933,27934,33753,33754,43814,64394,64396,64398,72478</link.rule.ids></links><search><creatorcontrib>Smith, Stanley D.</creatorcontrib><creatorcontrib>Devitt, Dale A.</creatorcontrib><creatorcontrib>Sala, Anna</creatorcontrib><creatorcontrib>Cleverly, James R.</creatorcontrib><creatorcontrib>Busch, David E.</creatorcontrib><title>Water relations of riparian plants from warm desert regions</title><title>Wetlands (Wilmington, N.C.)</title><description>Riparian plants have been classified as “drought avoiders” due to their access to an abundant subsurface water supply. Recent water-relations research that tracks water sources of riparian plants using the stable isotopes of water suggests that many plants of the riparian zone use ground water rather than stream water, and not all riparian plants are obligate phreatophytes (dependent on ground water as a moisture source) but may occasionally be dependent on unsaturated soil moisture sources. A more thorough understanding of riparian plant-water relations must include water-source dynamics and how those dynamics vary over both space and time. Many rivers in the desert, Southwest have been invaded by the exotic shrubTamarix ramosissima (saltcedar). Our studies ofTamarix invasion into habitats formerly dominated by native riparian forests of primarilyPopulus andSalix have shown thatTamarix successfully invades these habitats because of its (1) greater tolerance to water stress and salinity, (2) status, as a facultative, rather than obligate, phreatophyte and, therefore, its ability to recover from droughts and periods of ground-water drawdown, and (3) superior regrowth after fire. Analysis of water-loss rates indicate thatTamarix-dominated stands can have extremely high evapotranspiration rates when water tables are high but not necessarily when water tables are lower.Tamarix has leaf-level transpiration rates that are comparable to native species, whereas sap-flow rates per unit sapwood area are higher than in natives, suggesting thatTamarix maintains higher leaf area than can natives, probably due to its greater water stress tolerance.Tamarix desiccates and salinizes floodplains, due to its salt exudation and high transpiration rates, and may also accelerate fire cycles, thus predisposing these ecosystems to further loss of native taxa. Riparian species on regulated rivers can be exposed to seasonal water stress due to depression of floodplain water tables and elimination of annual floods. This can potentially result in a community shift toward more stress-tolerant taxa, such asTamarix, due to the inability of other riparian species to germinate and establish in the desiccated floodplain environment Management efforts aimed at maintaining native forests on regulated rivers and slowing the spread ofTamarix invasion must include at least partial reintroduction of historical flow, regimes, which favor the recruitment of native riparian species and reverse long-term desiccation of desert floodplain environments.</description><subject>Annual floods</subject><subject>Desert environments</subject><subject>Desert plants</subject><subject>Deserts</subject><subject>Desiccation</subject><subject>Drawdown</subject><subject>Drought</subject><subject>Environmental management</subject><subject>Evapotranspiration</subject><subject>Exudation</subject><subject>Floodplains</subject><subject>Flow rates</subject><subject>Groundwater</subject><subject>Indigenous species</subject><subject>Isotopes</subject><subject>Leaf area</subject><subject>Leaves</subject><subject>Phreatophytes</subject><subject>Plants (botany)</subject><subject>Populus</subject><subject>Regrowth</subject><subject>Regulated rivers</subject><subject>Reintroduction</subject><subject>Riparian forests</subject><subject>Riparian land</subject><subject>River regulations</subject><subject>Rivers</subject><subject>Salix</subject><subject>Soil moisture</subject><subject>Stable isotopes</subject><subject>Subsurface water</subject><subject>Tamarix</subject><subject>Tamarix ramosissima</subject><subject>Taxa</subject><subject>Transpiration</subject><subject>Unsaturated soils</subject><subject>Water analysis</subject><subject>Water relations</subject><subject>Water shortages</subject><subject>Water stress</subject><subject>Water supply</subject><subject>Water table</subject><issn>0277-5212</issn><issn>1943-6246</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNpd0M1KxDAUBeAgCo6jG5-gILgQqrn5bXGlg6PCgBvFZUibG-nQNjVpEd_eDiMIrs7m43A4hJwDvQZK9c39mnJQoAp-QBZQCp4rJtQhWVCmdS4ZsGNyktKWUlCMwYLcvtsRYxaxtWMT-pQFn8VmsLGxfTa0th9T5mPosi8bu8xhwjjO-mNnT8mRt23Cs99ckrf1w-vqKd-8PD6v7jZ5zaUYcy3AMaVqdJUSWKKisgbnKqt9xXUhnUBfCGBgqReMVdaCQ2crrAQUUiu-JJf73iGGzwnTaLom1djO6zBMyYAGAUrpGV78g9swxX7eZlgJpQSplJjV1V7VMaQU0ZshNp2N3wao2b1o_l7kP641Y7Q</recordid><startdate>19981201</startdate><enddate>19981201</enddate><creator>Smith, Stanley D.</creator><creator>Devitt, Dale A.</creator><creator>Sala, Anna</creator><creator>Cleverly, James R.</creator><creator>Busch, David E.</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H97</scope><scope>L.G</scope></search><sort><creationdate>19981201</creationdate><title>Water relations of riparian plants from warm desert regions</title><author>Smith, Stanley D. ; Devitt, Dale A. ; Sala, Anna ; Cleverly, James R. ; Busch, David E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c354t-741d266cedb64e9e605c1ddba7fb3785d4ef84121a0f422baa1dedabeb4185763</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>Annual floods</topic><topic>Desert environments</topic><topic>Desert plants</topic><topic>Deserts</topic><topic>Desiccation</topic><topic>Drawdown</topic><topic>Drought</topic><topic>Environmental management</topic><topic>Evapotranspiration</topic><topic>Exudation</topic><topic>Floodplains</topic><topic>Flow rates</topic><topic>Groundwater</topic><topic>Indigenous species</topic><topic>Isotopes</topic><topic>Leaf area</topic><topic>Leaves</topic><topic>Phreatophytes</topic><topic>Plants (botany)</topic><topic>Populus</topic><topic>Regrowth</topic><topic>Regulated rivers</topic><topic>Reintroduction</topic><topic>Riparian forests</topic><topic>Riparian land</topic><topic>River regulations</topic><topic>Rivers</topic><topic>Salix</topic><topic>Soil moisture</topic><topic>Stable isotopes</topic><topic>Subsurface water</topic><topic>Tamarix</topic><topic>Tamarix ramosissima</topic><topic>Taxa</topic><topic>Transpiration</topic><topic>Unsaturated soils</topic><topic>Water analysis</topic><topic>Water relations</topic><topic>Water shortages</topic><topic>Water stress</topic><topic>Water supply</topic><topic>Water table</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Smith, Stanley D.</creatorcontrib><creatorcontrib>Devitt, Dale A.</creatorcontrib><creatorcontrib>Sala, Anna</creatorcontrib><creatorcontrib>Cleverly, James R.</creatorcontrib><creatorcontrib>Busch, David E.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Environmental Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Wetlands (Wilmington, N.C.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Smith, Stanley D.</au><au>Devitt, Dale A.</au><au>Sala, Anna</au><au>Cleverly, James R.</au><au>Busch, David E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Water relations of riparian plants from warm desert regions</atitle><jtitle>Wetlands (Wilmington, N.C.)</jtitle><date>1998-12-01</date><risdate>1998</risdate><volume>18</volume><issue>4</issue><spage>687</spage><epage>696</epage><pages>687-696</pages><issn>0277-5212</issn><eissn>1943-6246</eissn><abstract>Riparian plants have been classified as “drought avoiders” due to their access to an abundant subsurface water supply. Recent water-relations research that tracks water sources of riparian plants using the stable isotopes of water suggests that many plants of the riparian zone use ground water rather than stream water, and not all riparian plants are obligate phreatophytes (dependent on ground water as a moisture source) but may occasionally be dependent on unsaturated soil moisture sources. A more thorough understanding of riparian plant-water relations must include water-source dynamics and how those dynamics vary over both space and time. Many rivers in the desert, Southwest have been invaded by the exotic shrubTamarix ramosissima (saltcedar). Our studies ofTamarix invasion into habitats formerly dominated by native riparian forests of primarilyPopulus andSalix have shown thatTamarix successfully invades these habitats because of its (1) greater tolerance to water stress and salinity, (2) status, as a facultative, rather than obligate, phreatophyte and, therefore, its ability to recover from droughts and periods of ground-water drawdown, and (3) superior regrowth after fire. Analysis of water-loss rates indicate thatTamarix-dominated stands can have extremely high evapotranspiration rates when water tables are high but not necessarily when water tables are lower.Tamarix has leaf-level transpiration rates that are comparable to native species, whereas sap-flow rates per unit sapwood area are higher than in natives, suggesting thatTamarix maintains higher leaf area than can natives, probably due to its greater water stress tolerance.Tamarix desiccates and salinizes floodplains, due to its salt exudation and high transpiration rates, and may also accelerate fire cycles, thus predisposing these ecosystems to further loss of native taxa. Riparian species on regulated rivers can be exposed to seasonal water stress due to depression of floodplain water tables and elimination of annual floods. This can potentially result in a community shift toward more stress-tolerant taxa, such asTamarix, due to the inability of other riparian species to germinate and establish in the desiccated floodplain environment Management efforts aimed at maintaining native forests on regulated rivers and slowing the spread ofTamarix invasion must include at least partial reintroduction of historical flow, regimes, which favor the recruitment of native riparian species and reverse long-term desiccation of desert floodplain environments.</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1007/BF03161683</doi><tpages>10</tpages></addata></record> |
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subjects | Annual floods Desert environments Desert plants Deserts Desiccation Drawdown Drought Environmental management Evapotranspiration Exudation Floodplains Flow rates Groundwater Indigenous species Isotopes Leaf area Leaves Phreatophytes Plants (botany) Populus Regrowth Regulated rivers Reintroduction Riparian forests Riparian land River regulations Rivers Salix Soil moisture Stable isotopes Subsurface water Tamarix Tamarix ramosissima Taxa Transpiration Unsaturated soils Water analysis Water relations Water shortages Water stress Water supply Water table |
title | Water relations of riparian plants from warm desert regions |
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