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This event was synchronous with volcanism of the Central Atlantic Magmatic Province (CAMP), the ultimate cause of the extinction and related environmental perturbations. However, the continental weathering response to CAMP‐induced warming remains poorly constrained. Strontium isotope stratigraphy is a powerful correlation tool that can also provide insights into the changes in weathering regime, but the scarcity of 87 Sr/ 86 Sr data across the Triassic‐Jurassic boundary (TJB) hindered the use of this method. Here we present new high‐resolution 87 Sr/ 86 Sr data from bulk carbonates at Csővár, a continuous marine section that spans 2.5 Myrs across the TJB. We document a continuing decrease in 87 Sr/ 86 Sr ratio from the late Rhaetian to the ETE, terminated by a 300 kyr interval of a flat trend and followed by a transient increase in the early Hettangian that levels off. We suggest that the first in the series of perturbations is linked to the influx of non‐radiogenic Sr from the weathering of freshly erupted CAMP basalts, leading to a delay in the radiogenic continental weathering response. The subsequent rise in 87 Sr/ 86 Sr after the TJB is explained by intensified continental crustal weathering from elevated CO 2 levels and reduced mantle‐derived Sr flux. Using Sr flux modeling, we also find support for such multiphase, prolonged continental weathering scenarios. Aggregating the new data set with published records employing an astrochronological age model results in a highly resolved Sr isotope reference curve for an 8.5 Myr interval around the TJB.", "digital" : true, "printed" : true, "sourceYear" : 2024, "foreignEdition" : true, "foreignLanguage" : true, "fullPublication" : true, "conferencePublication" : false, "nationalOrigin" : null, "missingAuthor" : false, "oaType" : "GOLD", "oaCheckDate" : "2024-03-28", "oaFree" : true, "oaLink" : "https://doi.org/10.1029/2024GC011464", "citationCount" : 0, "citationCountUnpublished" : 0, "citationCountWoOther" : 0, "independentCitCountWoOther" : 0, "nationalOriginCitationCount" : 0, "foreignEditionCitationCount" : 0, "doiCitationCount" : 0, "wosCitationCount" : 0, "scopusCitationCount" : 0, "wosScopusCitationCount" : 0, "wosScopusCitationCountWoOther" : 0, "wosScopusIndependentCitationCount" : 0, "wosScopusIndependentCitationCountWoOther" : 0, "independentCitationCount" : 0, "selfCitationCount" : 0, "unhandledCitationCount" : 0, "citingPubCount" : 0, "independentCitingPubCount" : 0, "citingPubCountWoOther" : 0, "independentCitingPubCountWoOther" : 0, "unhandledCitingPubCount" : 0, "citedPubCount" : 4, "citedCount" : 4, "ratings" : [ { "otype" : "SjrRating", "mtid" : 11466389, "link" : "/api/sjrrating/11466389", "label" : "sjr:D1 (2024) Scopus - Geochemistry and Petrology GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 1525-2027", "listPos" : 13, "rankValue" : 0.1, "type" : "journal", "ratingType" : { "otype" : "RatingType", "mtid" : 10002, "link" : "/api/ratingtype/10002", "label" : "sjr", "code" : "sjr", "published" : true, "snippet" : true }, "subject" : { "otype" : "ClassificationExternal", "mtid" : 1906, "link" : "/api/classificationexternal/1906", "label" : "Scopus - Geochemistry and Petrology", "published" : true, "oldId" : 1906, "snippet" : true }, "ranking" : "D1", "calculation" : "FROM_PREVIOUS_TO_LAST_YEAR", "published" : true, "snippet" : true } ], "ratingsForSort" : "D1", "hasCitationDuplums" : false, "inSelectedPubs" : "10000402", "userChangeableUntil" : "2024-03-25T07:08:03.477+0000", "directInstitutesForSort" : "Földtudományi Doktori Iskola (ELTE / TTK); HUN-REN Atommagkutató Intézet; HUN-REN-MTM-ELTE Paleontológiai Kutatócsoport (ELTE / TTK / Ft_K); Általános és Alkalmazott Földtani Tanszék (ELTE / TTK / Ft_K)", "ownerAuthorCount" : 5, "ownerInstituteCount" : 24, "directInstituteCount" : 4, "authorCount" : 8, "contributorCount" : 0, "hasQualityFactor" : true, "link" : "/api/publication/34746792", "label" : "Heszler Bernát et al. 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