Li, Q;
              
      
            
                Parrish, RR;
              
      
            
                Horstwood, MSA;
              
      
            
                McArthur, JM;
              
      
        
        
  
(2014)
  U–Pb dating of cements in Mesozoic ammonites.
Chemical Geology
, 376
      
    
     76 - 83.
    
         10.1016/j.chemgeo.2014.03.020.
  
  
       
    
  
| ![[thumbnail of 2014 Chem Geol Li U-Pb ammonites.pdf]](https://discovery.ucl.ac.uk/style/images/fileicons/application_pdf.png) | PDF 2014 Chem Geol Li U-Pb ammonites.pdf Available under License : See the attached licence file. Download (2MB) | 
Abstract
Dating sedimentary carbonates using the U-Pb method can help improve the Phanerozoic timescale. Using a novel combination of laser-ablation, multi-collector, inductively-coupled-plasma, mass-spectrometry (LA–MC–ICP–MS) and thermal ionization multi-collector mass spectrometry (TIMS), U-Pb numerical ages were obtained on early-diagenetic calcite cements in Jurassic ammonites in which concentrations of U range from 0.47 to 5.3 ppm. The calcite cements of two ammonites, IS1 and IS2, from the uppermost Bifrons Zone of the Toarcian (179–180Ma) of the UK, gave TIMS-normalized LA U–Pb dates of 164.9±5.3 Ma and 166.7±4.8Ma respectively. Normalizing LA–ICP–MC–MS data to an in-house calcite standard gave a more precise date of 165.5±3.3 Ma for IS1 cement. An unzoned ammonite, SS2, of Bajocian age (168–170 Ma) yield a TIMS-normalized LA U–Pb age of 158.8 ± 4.3 Ma for its early-diagenetic cement. Both the combined LA–MC–ICP–MS and TIMS approach, and the use of a calcite laser ablation standard can result in accurate ages of cements with uncertainties of 2–3% (2σ). The later, however, is more efficient and precise. These U-Pb dates of cements are 10 to 20 Myr younger than the numerical ages of the biostratigraphic intervals from which the ammonites derive. The U-Pb dates are taken to represent the time at which the aragonite shell of the ammonite inverted to calcite and released its U to precipitate in a late-diagenetic alteration of early-diagenetic fringing cements. Concentrations of U and Pb in a range of other pristine biogenic carbonateswere found too low(U b 0.01 ppm) for meaningful dating using laser ablation method.
| Type: | Article | 
|---|---|
| Title: | U–Pb dating of cements in Mesozoic ammonites | 
| Location: | UK | 
| Open access status: | An open access version is available from UCL Discovery | 
| DOI: | 10.1016/j.chemgeo.2014.03.020 | 
| Publisher version: | http://dx.doi.org/10.1016/j.chemgeo.2014.03.020 | 
| Language: | English | 
| Additional information: | This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. | 
| UCL classification: | UCL UCL > Provost and Vice Provost Offices > UCL BEAMS UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences | 
| URI: | https://discovery.ucl.ac.uk/id/eprint/1452726 | 
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