Micaela Chaumeil Rodríguez , Juan Pablo Pérez Panera , Jorge E. Spangenberg , Alejandro R. Gómez Dacal , Guillaume Suan , Alberto C. Garrido , Emanuela Mattioli
{"title":"冈瓦纳西南部早侏罗世和中侏罗世环境扰动:以阿根廷neuquacimen盆地为例","authors":"Micaela Chaumeil Rodríguez , Juan Pablo Pérez Panera , Jorge E. Spangenberg , Alejandro R. Gómez Dacal , Guillaume Suan , Alberto C. Garrido , Emanuela Mattioli","doi":"10.1016/j.gr.2025.03.019","DOIUrl":null,"url":null,"abstract":"<div><div>The Sierra Chacai Co and Los Molles formations in the Neuquén Basin, Argentina, are expressions of the first widespread marine transgression from the Pacific Ocean occurring in the Early to Middle Jurassic Period and provide a unique sedimentary record. Because of the presence of continuous and well-exposed outcrops, the basin has the potential to shed light on the global extent of the carbon isotope events (CIEs), as well as to test the large-scale occurrence of other environmental events so far only documented in western Tethys. The Neuquén Basin in Argentina is one of the rare places in south-western Gondwana where strata deposited during the Toarcian Oceanic Anoxic Event (T-OAE) have been documented. Here, we present the results of a multidisciplinary study integrating geochemical (δ<sup>13</sup>C<sub>org</sub>, TOC, major and trace elements) and calcareous nannofossil data from a novel section in the southern part of Neuquén Basin. The new data set allowed the identification of the T-OAE time-equivalent besides two additional significant negative carbon isotope excursions distributed across the middle Toarcian and Toarcian-Aalenian intervals. Six calcareous nannofossil zones and several subzones were recognised, covering the Pliensbachian-Aalenian interval, allowing to place the δ<sup>13</sup>C excursions within a precise stratigraphic framework and correlate them to other records worldwide. The new geochemical and calcareous nannofossils data provide the most continuous and time-extended record for the Neuquén Basin and the SW Gondwana. Additionally, these results support the global extent of CIE of the T-OAE and the presence of other Early to Middle Jurassic isotopic excursions. These findings illustrate the utility of combining organic carbon stable isotopes and calcareous nannofossils for global age correlations and palaeoenvironmental reconstructions in the evolution of the marine community during major, long-term environmental changes.</div></div>","PeriodicalId":12761,"journal":{"name":"Gondwana Research","volume":"144 ","pages":"Pages 1-19"},"PeriodicalIF":7.2000,"publicationDate":"2025-05-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Early and Middle Jurassic environmental perturbations in south-western Gondwana: An example from the Neuquén Basin, Argentina\",\"authors\":\"Micaela Chaumeil Rodríguez , Juan Pablo Pérez Panera , Jorge E. Spangenberg , Alejandro R. Gómez Dacal , Guillaume Suan , Alberto C. Garrido , Emanuela Mattioli\",\"doi\":\"10.1016/j.gr.2025.03.019\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The Sierra Chacai Co and Los Molles formations in the Neuquén Basin, Argentina, are expressions of the first widespread marine transgression from the Pacific Ocean occurring in the Early to Middle Jurassic Period and provide a unique sedimentary record. Because of the presence of continuous and well-exposed outcrops, the basin has the potential to shed light on the global extent of the carbon isotope events (CIEs), as well as to test the large-scale occurrence of other environmental events so far only documented in western Tethys. The Neuquén Basin in Argentina is one of the rare places in south-western Gondwana where strata deposited during the Toarcian Oceanic Anoxic Event (T-OAE) have been documented. Here, we present the results of a multidisciplinary study integrating geochemical (δ<sup>13</sup>C<sub>org</sub>, TOC, major and trace elements) and calcareous nannofossil data from a novel section in the southern part of Neuquén Basin. The new data set allowed the identification of the T-OAE time-equivalent besides two additional significant negative carbon isotope excursions distributed across the middle Toarcian and Toarcian-Aalenian intervals. Six calcareous nannofossil zones and several subzones were recognised, covering the Pliensbachian-Aalenian interval, allowing to place the δ<sup>13</sup>C excursions within a precise stratigraphic framework and correlate them to other records worldwide. The new geochemical and calcareous nannofossils data provide the most continuous and time-extended record for the Neuquén Basin and the SW Gondwana. Additionally, these results support the global extent of CIE of the T-OAE and the presence of other Early to Middle Jurassic isotopic excursions. These findings illustrate the utility of combining organic carbon stable isotopes and calcareous nannofossils for global age correlations and palaeoenvironmental reconstructions in the evolution of the marine community during major, long-term environmental changes.</div></div>\",\"PeriodicalId\":12761,\"journal\":{\"name\":\"Gondwana Research\",\"volume\":\"144 \",\"pages\":\"Pages 1-19\"},\"PeriodicalIF\":7.2000,\"publicationDate\":\"2025-05-02\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Gondwana Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1342937X25001121\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Gondwana Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1342937X25001121","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Early and Middle Jurassic environmental perturbations in south-western Gondwana: An example from the Neuquén Basin, Argentina
The Sierra Chacai Co and Los Molles formations in the Neuquén Basin, Argentina, are expressions of the first widespread marine transgression from the Pacific Ocean occurring in the Early to Middle Jurassic Period and provide a unique sedimentary record. Because of the presence of continuous and well-exposed outcrops, the basin has the potential to shed light on the global extent of the carbon isotope events (CIEs), as well as to test the large-scale occurrence of other environmental events so far only documented in western Tethys. The Neuquén Basin in Argentina is one of the rare places in south-western Gondwana where strata deposited during the Toarcian Oceanic Anoxic Event (T-OAE) have been documented. Here, we present the results of a multidisciplinary study integrating geochemical (δ13Corg, TOC, major and trace elements) and calcareous nannofossil data from a novel section in the southern part of Neuquén Basin. The new data set allowed the identification of the T-OAE time-equivalent besides two additional significant negative carbon isotope excursions distributed across the middle Toarcian and Toarcian-Aalenian intervals. Six calcareous nannofossil zones and several subzones were recognised, covering the Pliensbachian-Aalenian interval, allowing to place the δ13C excursions within a precise stratigraphic framework and correlate them to other records worldwide. The new geochemical and calcareous nannofossils data provide the most continuous and time-extended record for the Neuquén Basin and the SW Gondwana. Additionally, these results support the global extent of CIE of the T-OAE and the presence of other Early to Middle Jurassic isotopic excursions. These findings illustrate the utility of combining organic carbon stable isotopes and calcareous nannofossils for global age correlations and palaeoenvironmental reconstructions in the evolution of the marine community during major, long-term environmental changes.
期刊介绍:
Gondwana Research (GR) is an International Journal aimed to promote high quality research publications on all topics related to solid Earth, particularly with reference to the origin and evolution of continents, continental assemblies and their resources. GR is an "all earth science" journal with no restrictions on geological time, terrane or theme and covers a wide spectrum of topics in geosciences such as geology, geomorphology, palaeontology, structure, petrology, geochemistry, stable isotopes, geochronology, economic geology, exploration geology, engineering geology, geophysics, and environmental geology among other themes, and provides an appropriate forum to integrate studies from different disciplines and different terrains. In addition to regular articles and thematic issues, the journal invites high profile state-of-the-art reviews on thrust area topics for its column, ''GR FOCUS''. Focus articles include short biographies and photographs of the authors. Short articles (within ten printed pages) for rapid publication reporting important discoveries or innovative models of global interest will be considered under the category ''GR LETTERS''.