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Biostratigraphy as a Tool to Validate High-Resolution OSL, CRN, and Sequence-Stratigraphic Data

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STRATI 2013

Part of the book series: Springer Geology ((SPRINGERGEOL))

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Abstract

We present a biostratigraphic study of the Enza section that provides robust constraints on the timing of deposition in a case where the lack of magnetic polarity reversals in the marine part of the section does not allow palaeomagnetic age constraints to be obtained.

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References

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Author information

Authors and Affiliations

  1. Dipartimento di Scienze della Vita e dell’Ambiente, Università Politecnica delle Marche, Ancona, Italy

    Alessandra Negri & Anna Sabbatini

  2. Department Dipartimento di Scienze Biologiche. Geologiche e Ambientali, University of Bologna, Bologna, Italy

    Rossella Capozzi, Vincenzo Picotti & Alesio Ponza

  3. Lehigh University Department of Earth and Environmental Sciences, Bethlehem, PA, USA

    Kellen Gunderson & Frank J. Pazzaglia

Authors
  1. Alessandra Negri
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  2. Anna Sabbatini
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  3. Rossella Capozzi
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  4. Kellen Gunderson
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  5. Vincenzo Picotti
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  6. Alesio Ponza
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  7. Frank J. Pazzaglia
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Corresponding author

Correspondence to Alessandra Negri .

Editor information

Editors and Affiliations

  1. Faculdade de Ciências e Tecnologia Ciências da Terra, Universidade Nova de Lisboa, Caparica, Grande Lisboa, Portugal

    Rogério Rocha

  2. Faculdade Ciências e Tecnologia Ciencias da Terra, Universidade Nova de Lisboa, Caparica, Grande Lisboa, Portugal

    João Pais

  3. Ciências da Terra, Faculdade de Ciências e Tecnologia, Caparica, Grande Lisboa, Portugal

    José Carlos Kullberg

  4. Geological Sciences, California State University Long Beach, Long Beach, California, USA

    Stanley Finney

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© 2014 Springer-Verlag Berlin Heidelberg

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Negri, A. et al. (2014). Biostratigraphy as a Tool to Validate High-Resolution OSL, CRN, and Sequence-Stratigraphic Data. In: Rocha, R., Pais, J., Kullberg, J., Finney, S. (eds) STRATI 2013. Springer Geology. Springer, Cham. https://doi.org/10.1007/978-3-319-04364-7_218

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