000129939 001__ 129939
000129939 005__ 20240116090136.0
000129939 0247_ $$2doi$$a10.1111/sed.12440
000129939 0248_ $$2sideral$$a107614
000129939 037__ $$aART-2018-107614
000129939 041__ $$aeng
000129939 100__ $$0(orcid)0000-0002-4212-0524$$aArenas, C.$$uUniversidad de Zaragoza
000129939 245__ $$aSeasonal temperatures from d18O in recent Spanish tufa stromatolites: Equilibrium redux!
000129939 260__ $$c2018
000129939 5060_ $$aAccess copy available to the general public$$fUnrestricted
000129939 5203_ $$aThis study focuses on recent debate over the value of stable isotope-based environmental proxies recorded in riverine tufa stromatolites. A twelve-year record (1999 to 2012) of river-bed tufa stromatolites in the River Piedra (north-east Spain) was recovered in this study, along with a partly overlapping fifteen-year record (1994 to 2009) of accumulations in a drainage pipe: both deposits formed in water with near identical physico/chemical parameters. Measured water temperature data and near-constant d18Owater composition allowed selection of an ‘equilibrium’ palaeotemperature equation that best replicated actual temperatures. This study, as in some previous studies, found that just two published formulas for water temperature calculation from equilibrium calcite d18O compositions were appropriate for the River Piedra, where tufa deposition rates are high, with means between 5·6 mm and 10·8 mm in six months. The d18Ocalcite in both the river and the pipe deposits essentially records the full actual seasonal water temperature range. Only the coldest times (water temperature <10°C), when calcite precipitation mass decreased to minimum, are likely to be unrepresented, an effect most noticeable in the pipe where depositional masses are smaller and below sample resolution. While kinetic effects on d18Ocalcite-based calculated water temperature cannot be ruled out, the good fit between measured water temperature and d18Ocalcite-calculated water temperature indicates that temperature is the principal control. Textural and deposition rate variability between the river and pipe settings are caused by differences in flow velocity and illumination. In the river, calcification of growing cyanobacterial mat occurred throughout the year, producing composite dense and porous laminae, whereas in the pipe, discontinuous cyanobacterial growth in winter promoted more abiogenic calcification. High-resolution d18Ocalcite data from synchronous pipe and river laminae show that reversals in water temperature occur within laminae, not at lamina boundaries, a pattern consistent with progressive increase in calcite precipitation rate as cyanobacterial growth re-established in spring.
000129939 536__ $$9info:eu-repo/grantAgreement/ES/MICINN/CGL2013-42867$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2009-09216-CLI
000129939 540__ $$9info:eu-repo/semantics/openAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/
000129939 590__ $$a3.244$$b2018
000129939 591__ $$aGEOLOGY$$b4 / 46 = 0.087$$c2018$$dQ1$$eT1
000129939 592__ $$a1.571$$b2018
000129939 593__ $$aStratigraphy$$c2018$$dQ1
000129939 593__ $$aGeology$$c2018$$dQ1
000129939 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000129939 700__ $$0(orcid)0000-0002-5246-366X$$aOsácar, M.C.$$uUniversidad de Zaragoza
000129939 700__ $$0(orcid)0000-0003-1463-1682$$aAuqué, L.F.$$uUniversidad de Zaragoza
000129939 700__ $$aAndrews, J.E.
000129939 700__ $$0(orcid)0000-0001-6082-5301$$aPardo, G.
000129939 700__ $$aMarca, A.
000129939 700__ $$0(orcid)0000-0002-2141-2624$$aMartín-Bello, L.$$uUniversidad de Zaragoza
000129939 700__ $$0(orcid)0000-0002-1802-2115$$aPérez-Rivarés, F.J.
000129939 7102_ $$12000$$2685$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Petrología y Geoquímica
000129939 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000129939 7102_ $$12000$$2120$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Cristalografía Mineralog.
000129939 773__ $$g65, 5 (2018), 1611-1630$$pSedimentology$$tSEDIMENTOLOGY$$x0037-0746
000129939 8564_ $$s4697991$$uhttps://zaguan.unizar.es/record/129939/files/texto_completo.pdf$$yPostprint
000129939 8564_ $$s1289895$$uhttps://zaguan.unizar.es/record/129939/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000129939 909CO $$ooai:zaguan.unizar.es:129939$$particulos$$pdriver
000129939 951__ $$a2024-01-16-08:24:10
000129939 980__ $$aARTICLE