{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,24]],"date-time":"2026-03-24T11:39:25Z","timestamp":1774352365340,"version":"3.50.1"},"reference-count":145,"publisher":"Geological Society of London","issue":"5","license":[{"start":{"date-parts":[[2020,7,22]],"date-time":"2020-07-22T00:00:00Z","timestamp":1595376000000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"funder":[{"DOI":"10.13039\/501100007185","name":"Total","doi-asserted-by":"crossref","id":[{"id":"10.13039\/501100007185","id-type":"DOI","asserted-by":"crossref"}]}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["JGS"],"published-print":{"date-parts":[[2020,9]]},"abstract":"<jats:p>\n            Continental carbonate bodies are widespread in the Tabernas basin, eastern Betic Cordillera. Their relationships with the topographic evolution, climate changes and extensional regional tectonic processes recognized in the region are, however, still unclear. Travertine deposits exhibit facies of cascade and pool environments often reported as related to water\u2013air surface processes. Calcretes show a large panel of facies, indicating control by groundwater and pedogenic processes. New U\/Th dates on both travertine and calcrete reveal that they precipitated from 354\u2005ka\u2009\u00b1\u200976 to 8\u2005ka\u2009\u00b1\u20090.2. The U\/Th dates obtained on calcretes are in good agreement with global climate changes and support that precipitation of recent CaCO\n            <jats:sub>3<\/jats:sub>\n            is episodic and occurs mainly during warm and wet conditions. C and O stable isotope geochemistry reveals travertines are thermogenic and characterized by hydrothermal fluids enriched in CO\n            <jats:sub>2<\/jats:sub>\n            that interacted with aquifers. This thermogenic origin suggests a deep source of CO\n            <jats:sub>2<\/jats:sub>\n            (higher positive \u03b4\n            <jats:sup>13<\/jats:sup>\n            C values) likely triggered by the presence of an anomalously hot mantle that reflects thinning of the regional lithosphere and volcanism. Further analyses of the distribution of calcrete show they are carbonate-rich fluvial terraces, whose formation is controlled by the response of the river network to regional uplift and climate.\n          <\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary Materials<\/jats:bold>\n            : reproducibility for \u03b4\n            <jats:sup>13<\/jats:sup>\n            C and \u03b4\n            <jats:sup>18<\/jats:sup>\n            O of the NSB-18 internal standard available in\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.4996514\">Supplementary Table 1<\/jats:ext-link>\n            (SP1) and reproducibility for U and Th of the HU-1 standard available in\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.4996514\">Supplementary Table 2<\/jats:ext-link>\n            (SP2) at\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.4996514\">https:\/\/doi.org\/10.6084\/m9.figshare.c.4996514<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2020-025","type":"journal-article","created":{"date-parts":[[2020,6,2]],"date-time":"2020-06-02T20:05:20Z","timestamp":1591128320000},"page":"939-954","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":3,"title":["Quaternary tectonic and climate changes at the origin of travertine and calcrete in the eastern Betics (Almer\u00eda region, SE Spain)"],"prefix":"10.1144","volume":"177","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-3432-6987","authenticated-orcid":false,"given":"Marine","family":"Larrey","sequence":"first","affiliation":[{"name":"G\u00e9osciences Environnement Toulouse, UMR 5563, Universit\u00e9 Paul Sabatier, 14 avenue Edouard Belin, 31400 Toulouse, France"},{"name":"TOTAL SA, CSTJF, avenue Larribau, 64000 Pau, France"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7073-4905","authenticated-orcid":false,"given":"Fr\u00e9d\u00e9ric","family":"Mouthereau","sequence":"additional","affiliation":[{"name":"G\u00e9osciences Environnement Toulouse, UMR 5563, Universit\u00e9 Paul Sabatier, 14 avenue Edouard Belin, 31400 Toulouse, France"}]},{"given":"Emmanuel","family":"Masini","sequence":"additional","affiliation":[{"name":"CEO, Researcher &amp; Consultant at M&amp;U sas, 3 rue des Abattoirs, 38120 Saint-Egr\u00e8ve, France"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0244-4345","authenticated-orcid":false,"given":"Damien","family":"Huyghe","sequence":"additional","affiliation":[{"name":"Centre de G\u00e9osciences, MINES ParisTech, PSL University, 35 rue St Honor\u00e9, 77305 Fontainebleau, France"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-7976-8455","authenticated-orcid":false,"given":"Eric C","family":"Gaucher","sequence":"additional","affiliation":[{"name":"TOTAL SA, CSTJF, avenue Larribau, 64000 Pau, France"}]},{"given":"Aur\u00e9lien","family":"Virgone","sequence":"additional","affiliation":[{"name":"TOTAL SA, CSTJF, avenue Larribau, 64000 Pau, France"}]},{"given":"V\u00e9ronique","family":"Miegebielle","sequence":"additional","affiliation":[{"name":"TOTAL SA, CSTJF, avenue Larribau, 64000 Pau, France"}]}],"member":"1881","published-online":{"date-parts":[[2020,7,22]]},"reference":[{"key":"e_1_3_5_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.yqres.2015.05.002"},{"key":"e_1_3_5_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.geomorph.2007.10.025"},{"key":"e_1_3_5_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0070-4571(09)06105-6"},{"key":"e_1_3_5_5_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1525-1314.2005.00581.x"},{"key":"e_1_3_5_6_1","doi-asserted-by":"publisher","DOI":"10.1029\/2004TC001687"},{"key":"e_1_3_5_7_1","first-page":"223-239","article-title":"Calcrete features and age estimates from U\/Th dating: Implications for the analysis of Quaternary erosion rates in the northern limb of the Sierra Nevada range (Betic Cordillera, southeast Spain)","volume":"416","author":"Aza\u00f1\u00f3n J.","year":"2006","unstructured":"Aza\u00f1\u00f3n, J., Tuccimei, P., Azor, A., S\u00e1nchez-Almazo, I., Alonso-Zarza, A., Soligo, M. and P\u00e9rez-Pe\u00f1a, J. 2006. 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