Show simple item record

dc.contributor.authorMüller, Ten
dc.contributor.authorPrice, GDen
dc.contributor.authorMattioli, Een
dc.contributor.authorLeskó, MZen
dc.contributor.authorKristály, Fen
dc.contributor.authorPálfy, Jen
dc.date.accessioned2021-11-19T10:59:25Z
dc.date.available2021-11-19T10:59:25Z
dc.date.issued2021-05-21en
dc.identifier.issn0305-8719en
dc.identifier.urihttp://hdl.handle.net/10026.1/18392
dc.description.abstract

<jats:title>Abstract</jats:title><jats:p>The Jenkyns Event or Toarcian Oceanic Anoxic Event was an episode of severe environmental perturbations reflected in carbon isotope and other geochemical anomalies. Although well studied in the epicontinental basins in NW Europe, its effects are less understood in open marine environments. Here we present new geochemical (carbon isotope, CaCO<jats:sub>3</jats:sub>, [Mn]) and nannofossil biostratigraphic data from the Tölgyhát and Kisgerecse sections in the Gerecse Hills (Hungary). These sections record pelagic carbonate sedimentation near the margin of the Tethys Ocean. A negative carbon isotope excursion of <jats:italic>c.</jats:italic> 6‰ is observed in the Tölgyhát section, in a condensed clay and black shale layer where the CaCO<jats:sub>3</jats:sub> content drops in association with the Jenkyns Event. At Kisgerecse, bio- and chemostratigraphic data suggest a gap in the lower Toarcian. The presence of an uppermost Pliensbachian hardground, the absence of the lowermost Toarcian Tenuicostatum ammonite zone and the condensed record of the Jenkyns Event at Tölgyhát, together with a condensed Tenuicostatum Zone and the missing negative carbon isotope anomaly at Kisgerecse, imply arrested carbonate sedimentation. A calcification crisis and sea-level rise together led to a decrease in carbonate production and terrigenous input, suggesting that volcanogenic CO<jats:sub>2</jats:sub>-driven global warming may have been their common cause.</jats:p>

en
dc.format.extent269 - 289en
dc.languageenen
dc.language.isoenen
dc.publisherGeological Society of Londonen
dc.titleHardground, gap and thin black shale: spatial heterogeneity of arrested carbonate sedimentation during the Jenkyns Event (T-OAE) in a Tethyan pelagic Basin (Gerecse Mts, Hungary)en
dc.typeJournal Article
plymouth.issue1en
plymouth.volume514en
plymouth.journalGeological Society, London, Special Publicationsen
dc.identifier.doi10.1144/sp514-2020-266en
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group/Plymouth/Research Groups
plymouth.organisational-group/Plymouth/Research Groups/Marine Institute
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
plymouth.organisational-group/Plymouth/Users by role/Researchers in ResearchFish submission
dcterms.dateAccepted2021-03-25en
dc.rights.embargodate2022-05-21en
dc.identifier.eissn2041-4927en
dc.rights.embargoperiodNot knownen
rioxxterms.versionofrecord10.1144/sp514-2020-266en
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserveden
rioxxterms.licenseref.startdate2021-05-21en
rioxxterms.typeJournal Article/Reviewen


Files in this item

Thumbnail
Thumbnail

This item appears in the following Collection(s)

Show simple item record


All items in PEARL are protected by copyright law.
Author manuscripts deposited to comply with open access mandates are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author.
Theme by 
@mire NV