Isotopic composition of plant water sources/Evaristo et al. reply
In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates...
Ausführliche Beschreibung
Autor*in: |
Mathieu Javaux [verfasserIn] |
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Artikel |
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Sprache: |
Englisch |
Erschienen: |
2016 |
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Übergeordnetes Werk: |
Enthalten in: Nature - London : Macmillan Publishers Limited, part of Springer Nature, 1869, 536(2016), 7617, Seite E1 |
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Übergeordnetes Werk: |
volume:536 ; year:2016 ; number:7617 ; pages:E1 |
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DOI / URN: |
10.1038/nature18946 |
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10.1038/nature18946 doi PQ20161201 (DE-627)OLC1982123885 (DE-599)GBVOLC1982123885 (PRQ)p573-c3d5ac267a2886cba666447d7ad2788076803e0cf09eab899390da5b601578cd0 (KEY)0072945020160000536761700001isotopiccompositionofplantwatersourcesevaristoetal DE-627 ger DE-627 rakwb eng 070 500 DE-101 500 AVZ BIODIV fid Mathieu Javaux verfasserin aut Isotopic composition of plant water sources/Evaristo et al. reply 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. Flowers & plants Groundwater recharge Isotopes Precipitation Groundwater Botany Stream flow Youri Rothfuss oth Jan Vanderborght oth Harry Vereecken oth Nicolas Brüggemann oth J Evaristo oth S Jasechko oth J J McDonnell oth Enthalten in Nature London : Macmillan Publishers Limited, part of Springer Nature, 1869 536(2016), 7617, Seite E1 (DE-627)129292834 (DE-600)120714-3 (DE-576)014473941 0028-0836 nnns volume:536 year:2016 number:7617 pages:E1 http://dx.doi.org/10.1038/nature18946 Volltext http://search.proquest.com/docview/1815374783 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_154 GBV_ILN_168 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_290 GBV_ILN_294 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2016 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2095 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4700 AR 536 2016 7617 E1 |
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10.1038/nature18946 doi PQ20161201 (DE-627)OLC1982123885 (DE-599)GBVOLC1982123885 (PRQ)p573-c3d5ac267a2886cba666447d7ad2788076803e0cf09eab899390da5b601578cd0 (KEY)0072945020160000536761700001isotopiccompositionofplantwatersourcesevaristoetal DE-627 ger DE-627 rakwb eng 070 500 DE-101 500 AVZ BIODIV fid Mathieu Javaux verfasserin aut Isotopic composition of plant water sources/Evaristo et al. reply 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. Flowers & plants Groundwater recharge Isotopes Precipitation Groundwater Botany Stream flow Youri Rothfuss oth Jan Vanderborght oth Harry Vereecken oth Nicolas Brüggemann oth J Evaristo oth S Jasechko oth J J McDonnell oth Enthalten in Nature London : Macmillan Publishers Limited, part of Springer Nature, 1869 536(2016), 7617, Seite E1 (DE-627)129292834 (DE-600)120714-3 (DE-576)014473941 0028-0836 nnns volume:536 year:2016 number:7617 pages:E1 http://dx.doi.org/10.1038/nature18946 Volltext http://search.proquest.com/docview/1815374783 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_154 GBV_ILN_168 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_290 GBV_ILN_294 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2016 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2095 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4700 AR 536 2016 7617 E1 |
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10.1038/nature18946 doi PQ20161201 (DE-627)OLC1982123885 (DE-599)GBVOLC1982123885 (PRQ)p573-c3d5ac267a2886cba666447d7ad2788076803e0cf09eab899390da5b601578cd0 (KEY)0072945020160000536761700001isotopiccompositionofplantwatersourcesevaristoetal DE-627 ger DE-627 rakwb eng 070 500 DE-101 500 AVZ BIODIV fid Mathieu Javaux verfasserin aut Isotopic composition of plant water sources/Evaristo et al. reply 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. Flowers & plants Groundwater recharge Isotopes Precipitation Groundwater Botany Stream flow Youri Rothfuss oth Jan Vanderborght oth Harry Vereecken oth Nicolas Brüggemann oth J Evaristo oth S Jasechko oth J J McDonnell oth Enthalten in Nature London : Macmillan Publishers Limited, part of Springer Nature, 1869 536(2016), 7617, Seite E1 (DE-627)129292834 (DE-600)120714-3 (DE-576)014473941 0028-0836 nnns volume:536 year:2016 number:7617 pages:E1 http://dx.doi.org/10.1038/nature18946 Volltext http://search.proquest.com/docview/1815374783 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_154 GBV_ILN_168 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_290 GBV_ILN_294 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2016 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2095 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4700 AR 536 2016 7617 E1 |
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10.1038/nature18946 doi PQ20161201 (DE-627)OLC1982123885 (DE-599)GBVOLC1982123885 (PRQ)p573-c3d5ac267a2886cba666447d7ad2788076803e0cf09eab899390da5b601578cd0 (KEY)0072945020160000536761700001isotopiccompositionofplantwatersourcesevaristoetal DE-627 ger DE-627 rakwb eng 070 500 DE-101 500 AVZ BIODIV fid Mathieu Javaux verfasserin aut Isotopic composition of plant water sources/Evaristo et al. reply 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. Flowers & plants Groundwater recharge Isotopes Precipitation Groundwater Botany Stream flow Youri Rothfuss oth Jan Vanderborght oth Harry Vereecken oth Nicolas Brüggemann oth J Evaristo oth S Jasechko oth J J McDonnell oth Enthalten in Nature London : Macmillan Publishers Limited, part of Springer Nature, 1869 536(2016), 7617, Seite E1 (DE-627)129292834 (DE-600)120714-3 (DE-576)014473941 0028-0836 nnns volume:536 year:2016 number:7617 pages:E1 http://dx.doi.org/10.1038/nature18946 Volltext http://search.proquest.com/docview/1815374783 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_154 GBV_ILN_168 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_290 GBV_ILN_294 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2016 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2095 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4700 AR 536 2016 7617 E1 |
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10.1038/nature18946 doi PQ20161201 (DE-627)OLC1982123885 (DE-599)GBVOLC1982123885 (PRQ)p573-c3d5ac267a2886cba666447d7ad2788076803e0cf09eab899390da5b601578cd0 (KEY)0072945020160000536761700001isotopiccompositionofplantwatersourcesevaristoetal DE-627 ger DE-627 rakwb eng 070 500 DE-101 500 AVZ BIODIV fid Mathieu Javaux verfasserin aut Isotopic composition of plant water sources/Evaristo et al. reply 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. Flowers & plants Groundwater recharge Isotopes Precipitation Groundwater Botany Stream flow Youri Rothfuss oth Jan Vanderborght oth Harry Vereecken oth Nicolas Brüggemann oth J Evaristo oth S Jasechko oth J J McDonnell oth Enthalten in Nature London : Macmillan Publishers Limited, part of Springer Nature, 1869 536(2016), 7617, Seite E1 (DE-627)129292834 (DE-600)120714-3 (DE-576)014473941 0028-0836 nnns volume:536 year:2016 number:7617 pages:E1 http://dx.doi.org/10.1038/nature18946 Volltext http://search.proquest.com/docview/1815374783 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_154 GBV_ILN_168 GBV_ILN_170 GBV_ILN_171 GBV_ILN_211 GBV_ILN_290 GBV_ILN_294 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2016 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2095 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4700 AR 536 2016 7617 E1 |
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isotopic composition of plant water sources/evaristo et al. reply |
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abstract |
In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. |
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In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. |
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In their study, Evaristo et al.1 collected an extensive data set on the basis of which they statistically determined the isotopic compositions of the plant water source (δ 18Ointersect and δ 2Hintersect, called respectively δ 18Ointercept and δ 2Hintercept in their paper) as the x and y coordinates in (δ 18O, δ 2H) space of the intersection between the local meteoric water line (LMWL) and the plant xylem water 'evaporation line' (EL) for a range of climates and vegetation types. |
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