Investigating boron isotopes in a middle Jurassic micritic sequence: Primary vs. diagenetic signal | INSTITUT DE PHYSIQUE DU GLOBE DE PARIS


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  Investigating boron isotopes in a middle Jurassic micritic sequence: Primary vs. diagenetic signal

Publication Type:

Journal Article


Chemical Geology, Volume 275, Issue 3-4, p.117-126 (2010)



Accession Number:




UMR 7154 ; Géochimie et Cosmochimie ; N° Contribution : 2641 ; Boron isotopes; MC-ICP-MS; Bulk rock; Carbonate; Jurassic; Diagenesis


Boron isotope abundance in carbonates provides a powerful proxy for seawater pH reconstructions. Nevertheless, application of this proxy on bulk rocks has never been clearly investigated. Herein, boron isotopes were measured in early Bajocian samples from the Terminilletto section (Italy) to explore the meaning of bulk rock delta B-11 values in paleo-environmental investigations. In the southwestern Tethys, the early Bajocian is marked by a change in sedimentation from calcareous to radiolaritic lithologies, concomitant with a delta C-13 positive excursion and a sedimentary hiatus in several calcareous sections. The isotopic compositions of boron extracted from Terminilletto samples range from 10%. to 12% and boron content from 0.75 to 1.45 ppm, both lower than modern ranges. This implies either diagenesis or a lower boron concentration in Jurassic seawater. Boron isotopic compositions are compared to major and trace element analyses to investigate potential alteration of the carbonate primary signal. Fe and Al contents provide useful information on both clay contamination and sedimentation style. The delta B-11 values measured in carbonates constrain the boron isotopic composition of the precipitating fluid, either seawater or derived from seawater, regarding that both delta B-11 and delta O-18 are consistent with marine signatures. Jurassic seawater delta B-11 might have been lower than the modem one. The delta B-11 variations, consistent with micropaleontological observations, suggest a seawater alkalinization reflecting the atmospheric CO2 decrease after a probable phase of volcanism intensification prior to the Aalenian-Bajocian boundary. The carbonate crisis itself might also have promoted pH rise through progressive [CO32-] accumulation in seawater. (C) 2010 Elsevier B.V. All rights reserved.


Paris, Guillaume Bartolini, Annachiara Donnadieu, Yannick Beaumont, Valérie Gaillardet, Jérôme