{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,11,4]],"date-time":"2025-11-04T16:12:20Z","timestamp":1762272740733,"version":"3.40.5"},"reference-count":172,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2021,1,1]],"date-time":"2021-01-01T00:00:00Z","timestamp":1609459200000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["SP"],"published-print":{"date-parts":[[2021,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n          <jats:p>The Toarcian Oceanic Anoxic Event (T-OAE) is marked by major palaeoenvironmental and palaeoceanographical changes on a global scale, associated with a severe disturbance of the global carbon cycle and organic-rich facies deposition. Here, a multiproxy approach (petrographic and geochemical techniques) was applied to the study of the organic content of the T-OAE of the Paris Basin, whose phytoplanktonic origin has been previously inferred by its geochemical signature.<\/jats:p>\n          <jats:p>\n            The top of the\n            <jats:italic>tenuicostatum<\/jats:italic>\n            Zone is characterized by palynomorphs and marine phytoplankton-derived amorphous organic matter (AOM), representing a proximal marine environment with emplacement of euxinic conditions at the top (total organic carbon\/sulfur content and increase in AOM). At the base of the\n            <jats:italic>serpentinum<\/jats:italic>\n            Zone the proliferation of bacterial biomass begins, with phytoplankton playing a secondary role. This indicates the development of stagnant and restrictive conditions in a proximal environment, with water column stratification (neohop-13(18)-ene). The majority of the\n            <jats:italic>serpentinum<\/jats:italic>\n            Zone is dominated by bacterial biomass, suggesting a marine environment with bottom-water stagnation, possibly related to basin palaeogeomorphology and circulation patterns, with episodic euxinia.\n          <\/jats:p>\n          <jats:p>This therefore suggests that the T-OAE organic fraction is dominated by bacterial biomass, not phytoplankton, showing the importance of an integrated approach to the determination of the organic facies.<\/jats:p>","DOI":"10.1144\/sp514-2020-167","type":"journal-article","created":{"date-parts":[[2021,3,1]],"date-time":"2021-03-01T15:25:32Z","timestamp":1614612332000},"page":"309-334","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":10,"title":["Boosted microbial productivity during the Toarcian Oceanic Anoxic Event in the Paris Basin, France: new evidence from organic geochemistry and petrographic analysis"],"prefix":"10.1144","volume":"514","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-4794-3271","authenticated-orcid":false,"given":"Carolina","family":"Fonseca","sequence":"first","affiliation":[{"name":"G\u00e9osciences Environnement Toulouse, Universit\u00e9 de Toulouse, CNES, CNRS, IRD, UPS, 14 avenue \u00c9douard Belin, F-31400 Toulouse, France"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-8997-0270","authenticated-orcid":false,"given":"Jo\u00e3o Graciano","family":"Mendon\u00e7a Filho","sequence":"additional","affiliation":[{"name":"Laborat\u00f3rio de Palinof\u00e1cies e F\u00e1cies Org\u00e2nica (LAFO), Departamento de Geologia, Instituto de Geoci\u00eancias, Universidade Federal do Rio de Janeiro, Av. Athos da Silveira, 274, pr\u00e9dio do CCMN, sala J1020, Campus Ilha do Fund\u00e3o, Cidade Universit\u00e1ria, CEP 21.949-900, Rio de Janeiro, RJ, Brazil"}]},{"given":"Carine","family":"L\u00e9zin","sequence":"additional","affiliation":[{"name":"G\u00e9osciences Environnement Toulouse, Universit\u00e9 de Toulouse, CNES, CNRS, IRD, UPS, 14 avenue \u00c9douard Belin, F-31400 Toulouse, France"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-3180-459X","authenticated-orcid":false,"given":"Fran\u00e7ois","family":"Baudin","sequence":"additional","affiliation":[{"name":"Sorbonne Universit\u00e9, CNRS, ISTeP UMR 7193, 4 Place Jussieu, 75005 Paris, France"}]},{"given":"Ant\u00f3nio Donizeti","family":"de Oliveira","sequence":"additional","affiliation":[{"name":"Laborat\u00f3rio de Palinof\u00e1cies e F\u00e1cies Org\u00e2nica (LAFO), Departamento de Geologia, Instituto de Geoci\u00eancias, Universidade Federal do Rio de Janeiro, Av. Athos da Silveira, 274, pr\u00e9dio do CCMN, sala J1020, Campus Ilha do Fund\u00e3o, Cidade Universit\u00e1ria, CEP 21.949-900, Rio de Janeiro, RJ, Brazil"}]},{"given":"Jaqueline Torres","family":"Souza","sequence":"additional","affiliation":[{"name":"Laborat\u00f3rio de Palinof\u00e1cies e F\u00e1cies Org\u00e2nica (LAFO), Departamento de Geologia, Instituto de Geoci\u00eancias, Universidade Federal do Rio de Janeiro, Av. Athos da Silveira, 274, pr\u00e9dio do CCMN, sala J1020, Campus Ilha do Fund\u00e3o, Cidade Universit\u00e1ria, CEP 21.949-900, Rio de Janeiro, RJ, Brazil"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9025-5896","authenticated-orcid":false,"given":"Lu\u00eds V.","family":"Duarte","sequence":"additional","affiliation":[{"name":"University of Coimbra, MARE - Marine and Environmental Sciences Centre, Faculty of Sciences and Technology, Department of Earth Sciences, Rua S\u00edlvio Lima, 3030-790 Coimbra, Portugal"}]}],"member":"1881","published-online":{"date-parts":[[2021,5,19]]},"reference":[{"key":"e_1_3_5_2_1","doi-asserted-by":"publisher","DOI":"10.2516\/ogst:1978025"},{"key":"e_1_3_5_3_1","doi-asserted-by":"publisher","DOI":"10.1144\/0016-76492010-025"},{"key":"e_1_3_5_4_1","volume-title":"Standard Test Methods for Sulfur in the Analysis Sample of Coal and Coke Using High-Temperature Tube Furnace Combustion Methods","author":"ASTM D4239-08","year":"2008","unstructured":"ASTM D4239-08 2008. 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