000057490 001__ 57490
000057490 005__ 20200221144326.0
000057490 0247_ $$2doi$$a10.1016/j.sedgeo.2016.09.004
000057490 0248_ $$2sideral$$a96441
000057490 037__ $$aART-2016-96441
000057490 041__ $$aeng
000057490 100__ $$0(orcid)0000-0002-5246-366X$$aOsácar, M. Cinta$$uUniversidad de Zaragoza
000057490 245__ $$aDiscerning the interactions between environmental parameters reflected in d13C and d18O of recent fluvial tufas: Lessons from a Mediterranean climate region
000057490 260__ $$c2016
000057490 5060_ $$aAccess copy available to the general public$$fUnrestricted
000057490 5203_ $$ad13C and d18O of recent, continuous tufa records, obtained during a monitoring period spanning 3 to 13 years, are compared with the corresponding, known environmental conditions. Three rivers in NE Iberia (located along a 200-km N–S transect) are used for this comparison. The isotopic variations through space and time are discussed in terms of the environmental and geological parameters that operate on different scales, focusing on discerning the interactions between these parameters and providing examples of possible misinterpretation of climatic conditions, which is important to past climate studies based on isotopic data. The calculation of the actual isotopic fractionation coefficients, and the comparison with the literature-derived coefficients, demonstrates that the studied tufa formation was close to isotopic equilibrium to reflect the water temperature. The difference between mean measured water temperature (Tw) and mean calculated Tw (based on d18Ocalcite and measured d18Owater) is less than 2.7 °C. Tendencies of these calculated Tw are similar to the regional air temperature (Tair) tendencies through time, in particular in the case of the 13-year record, although certain deviations exist over shorter time spans. The best agreement between measured and calculated Tw and between d18Ocalcite-based Tw tendencies and Tair tendencies corresponds to the tufa stromatolite facies. Differences between the d18Ocalcite records of the three rivers cannot be attributed to temperature changes, but to the varying influences of groundwater inputs and isotopic rainfall composition in each river.Without considering these parameters, d18Ocalcite-based Tw calculations yield inaccurate results when comparing the study sites. d13Ccalcite values do not exhibit distinct patterns over time, and d13Ccalcite variations are likely caused by local processes that do not reflect general environmental changes. These findings underscore the significance of accounting for both groundwater behaviour and rainfall stable isotope composition when interpreting climate parameters in carbonate systems, particularly when differences between the isotopic signatures of deposits exist in the same region.
000057490 536__ $$9info:eu-repo/grantAgreement/ES/REN2002-03575-CLI$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2009-09216-CLI$$9info:eu-repo/grantAgreement/ES/MICINN/CGL2013-42867$$9info:eu-repo/grantAgreement/ES/MICINN/CGL2006-05063-BTE
000057490 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000057490 590__ $$a2.373$$b2016
000057490 591__ $$aGEOLOGY$$b10 / 47 = 0.213$$c2016$$dQ1$$eT1
000057490 592__ $$a1.129$$b2016
000057490 593__ $$aStratigraphy$$c2016$$dQ1
000057490 593__ $$aGeology$$c2016$$dQ1
000057490 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000057490 700__ $$0(orcid)0000-0002-4212-0524$$aArenas, Concha$$uUniversidad de Zaragoza
000057490 700__ $$0(orcid)0000-0003-1463-1682$$aAuqué, Luis$$uUniversidad de Zaragoza
000057490 700__ $$0(orcid)0000-0002-1304-2264$$aSancho, Carlos$$uUniversidad de Zaragoza
000057490 700__ $$0(orcid)0000-0001-6082-5301$$aPardo, Gonzalo$$uUniversidad de Zaragoza
000057490 700__ $$aVázquez-Urbez, Marta
000057490 7102_ $$12000$$2685$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Petrología y Geoquímica
000057490 7102_ $$12000$$2427$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Externa
000057490 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000057490 7102_ $$12000$$2120$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Cristalografía Mineralog.
000057490 773__ $$g345 (2016), 126-144$$pSediment. geol.$$tSedimentary Geology$$x0037-0738
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000057490 951__ $$a2020-02-21-13:44:09
000057490 980__ $$aARTICLE