English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/133460
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:
DC FieldValueLanguage
dc.contributor.authorGómez Fernández, J. J.es_ES
dc.contributor.authorComas-Rengifo, M. J.es_ES
dc.contributor.authorGoy Goy, A.es_ES
dc.date.accessioned2016-06-15T07:01:15Z-
dc.date.available2016-06-15T07:01:15Z-
dc.date.issued2016-05-20-
dc.identifier.citationClimate of the Past, 12 (5): 1199-1214 (2016)es_ES
dc.identifier.issn1814-9324-
dc.identifier.urihttp://hdl.handle.net/10261/133460-
dc.description.abstractOne of the main controversial themes in palaeoclimatology involves elucidating whether climate during the Jurassic was warmer than the present day and if it was the same over Pangaea, with no major latitudinal gradients. There has been an abundance of evidence of oscillations in seawater temperature throughout the Jurassic. The Pliensbachian (Early Jurassic) constitutes a distinctive time interval for which several seawater temperature oscillations, including an exceptional cooling event, have been documented. To constrain the timing and magnitude of these climate changes, the Rodiles section of the Asturian Basin (Northern Spain), a well exposed succession of the uppermost Sinemurian, Pliensbachian and Lower Toarcian deposits, has been studied. A total of 562 beds were measured and sampled for ammonites, for biochronostratigraphical purposes, and for belemnites, to determine the palaeoclimatic evolution through stable isotope studies. Comparison of the recorded latest Sinemurian, Pliensbachian and Early Toarcian changes in seawater palaeotemperature with other European sections allows characterization of several climatic changes that are likely of a global extent. A warming interval partly coinciding with a δ13Cbel negative excursion was recorded at the Late Sinemurian. After a “normal” temperature interval, with temperatures close to average values of the Late Sinemurian–Early Toarcian period, a new warming interval containing a short-lived positive δ13Cbel peak, developed during the Early–Late Pliensbachian transition. The Late Pliensbachian represents an outstanding cooling interval containing a δ13Cbel positive excursion interrupted by a small negative δ13Cbel peak. Finally, the Early Toarcian represented an exceptional warming period, which has been pointed out as being responsible for the prominent Early Toarcian mass extinction.es_ES
dc.description.sponsorshipThis research work was financed by project CGL2015- 66604-R of the Spanish Ministerio de Economía y Competitividad, and by projects GR3/14/910431, and GI 910429 of the Universidad Complutense de Madrides_ES
dc.language.isoenges_ES
dc.publisherCopernicus Publicationses_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccesses_ES
dc.titlePalaeoclimatic oscillations in the Pliensbachian (Early Jurassic) of the Asturian Basin (Northern Spain)es_ES
dc.typeartículoes_ES
dc.identifier.doi10.5194/cp-12-1199-2016-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.5194/cp-12-1199-2016es_ES
dc.identifier.e-issn1814-9332-
dc.contributor.funderMinisterio de Economía y Competitividad (España)es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003329es_ES
Appears in Collections:(IGEO) Artículos
Files in This Item:
File Description SizeFormat 
CP_2016_12_1199.pdf6,4 MBAdobe PDFThumbnail
View/Open
Show simple item record
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.