Models of historical biogeography and continental biochronology

Authors

  • María Ángles Álvarez-Sierra Departamento de Paleontología, Universidad Complutense de Madrid Departamento de Geología Sedimentaria y Cambio Medioambiental, Instituto de Geociencias IGEO (CSIS, UCM)
  • Israel García-Paredes Departamento de Paleontología, Universidad Complutense de Madrid Departamento de Geología Sedimentaria y Cambio Medioambiental, Instituto de Geociencias IGEO (CSIS, UCM)
  • Verónica Hernández-Ballarín Departamento de Paleontología, Museo Nacional de Ciencias Naturales MNCN, CSIC
  • Lars W Van Den Hoek Ostende Naturalis Biodiversity Center, The Netherlands
  • Kees Hordijk Institute of Earth Sciences, Utrecht University
  • Paloma López-Guerrero Departamento de Paleontología, Universidad Complutense de Madrid Departamento de Geología Sedimentaria y Cambio Medioambiental, Instituto de Geociencias IGEO (CSIS, UCM)
  • Albert J Van Der Meulen Institute of Earth Sciences, Utrecht University
  • Adriana Oliver Departamento de Paleontología, Museo Nacional de Ciencias Naturales MNCN, CSIC
  • Pablo Paláez-Campomanes Departamento de Paleontología, Museo Nacional de Ciencias Naturales MNCN, CSIC

DOI:

https://doi.org/10.7203/sjp.28.2.17847

Keywords:

Micromammals, Historical Biogeography Symmetric/Asymmetric Time Model, dispersals, middle Miocene correlations, diachrony

Abstract

One of the most important contributions of Nieves López Martínez in Palaeobiogeography is the study of the ‘centre of origin of species’ concept and the proposal of the ‘Asymmetric Time Model’ as an alternative to the ‘Symmetric Time Model’, a key concept in dispersalist Historical Biogeography. As a consequence of these ideas, she discussed the methodology to establish biostratigraphic scales, pointing out that the higher number of ‘First Appearance Datum’ (FADs) over that of ‘Last Appearance Datum’ (LADs) in the fossil record supports the Asymmetrical Time Model. In this study we analyse the middle Miocene micromammal appearance and extinction events (FADs and LADs) based on well-calibrated local biostratigraphic scales from different European basins, in order to determine which of the proposed biogeographical models better fits the Miocene European micromammal record. The results support that the Asymmetric Time Model of palaeobiogeography is only applicable in rare cases. The analysed fossil record only shows one event of occurrence and one of extinction that can be considered synchronous at continental level. Finally, the implications of the biogeographic models in the proposition of biochronologic continental scales are also discussed, pointing out that palaeobiogeographic frameworks need robust biochronologies based on extensive local biostratigraphic data with independent temporal correlation

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Published

2020-07-20

How to Cite

Álvarez-Sierra, M. Ángles, García-Paredes, I., Hernández-Ballarín, V., Van Den Hoek Ostende, L. W., Hordijk, K., López-Guerrero, P., … Paláez-Campomanes, P. (2020). Models of historical biogeography and continental biochronology. Spanish Journal of Palaeontology, 28(2), 129–138. https://doi.org/10.7203/sjp.28.2.17847
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