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dc.contributor.authorGébelin, Aen
dc.contributor.authorWitt, Cen
dc.contributor.authorRadkiewicz, Men
dc.contributor.authorMulch, Aen
dc.date.accessioned2021-06-12T13:54:27Z
dc.date.available2021-06-12T13:54:27Z
dc.date.issued2021-05-28en
dc.identifier.issn2296-6463en
dc.identifier.urihttp://hdl.handle.net/10026.1/17248
dc.description.abstract

<jats:p>Determining how the elevation of the Northern Andes has evolved over time is of paramount importance for understanding the response of the Northern Andes to deformational and geodynamic processes and its role as an orographic barrier for atmospheric vapor transport over geologic time. However, a fundamental requirement when using stable isotope data for paleoaltimetry reconstructions is knowledge about the present-day changes of δ<jats:sup>18</jats:sup>O and δD with elevation (isotopic lapse rate). This study defines the present-day river isotopic lapse rate near the Equator (∼3°S) based on analysis of δ<jats:sup>18</jats:sup>O and δD of surface waters collected from streams across the Western Cordillera and the Inter-Andean depression in Southern Ecuador. The results for the two domains show a decrease of δ<jats:sup>18</jats:sup>O with elevation which fits a linear regression with a slope of −0.18‰/100 m (R<jats:sup>2</jats:sup> = 0.73, <jats:italic>n</jats:italic> = 83). However, we establish a present-day lapse rate of −0.15‰/100 m for δ<jats:sup>18</jats:sup>O (R<jats:sup>2</jats:sup> = 0.88, <jats:italic>n</jats:italic> = 19) and -1.4‰/100 m for δD (R<jats:sup>2</jats:sup> = 0.93, <jats:italic>n</jats:italic> = 19) from water samples collected along the west facing slopes of the Western Ecuadorian Cordillera which is mainly subject to moisture transport from the Pacific. We argue that this empirical relationship, consistent with those obtained in different tropical areas of the world, can inform stable isotope paleoaltimetry reconstructions in tropical latitudes.</jats:p>

en
dc.language.isoenen
dc.publisherFrontiers Mediaen
dc.titleImpact of the Southern Ecuadorian Andes on Oxygen and Hydrogen Isotopes in Precipitationen
dc.typeJournal Article
plymouth.volume9en
plymouth.journalFrontiers in Earth Scienceen
dc.identifier.doi10.3389/feart.2021.664590en
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
dcterms.dateAccepted2021-05-05en
dc.rights.embargodate2021-06-15en
dc.identifier.eissn2296-6463en
dc.rights.embargoperiodNot knownen
rioxxterms.versionofrecord10.3389/feart.2021.664590en
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserveden
rioxxterms.licenseref.startdate2021-05-28en
rioxxterms.typeJournal Article/Reviewen


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