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Published on: February 28, 2017
TIMING DEEP DIVERGENCE EVENTS IN CALCAREOUS DINOFLAGELLATES(1)
Marc Gottschling1, Susanne S Renner1, K J Sebastian Meier1
1Institut für Geologische Wissenschaften, Fachrichtung Paläontologie, Freie Universität Berlin, Malteserstr. 74-100, D-122 49 Berlin, GermanySystematische Botanik, Ludwig-Maximilians-Universität München, Menzingerstr. 67, D-80 638 Munich, GermanyInstitut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Str. 16, D-24118, Kiel, GermanyFachbereich Geowissenschaften - Historische Geologie and Paläontologie, Universität Bremen, Klagenfurter Str., D-28 359 Bremen, GermanyInstitut für Geologische Wissenschaften, Fachrichtung Paläontologie, Freie Universität Berlin, Malteserstr. 74-100, D-122 49 Berlin, Germany.
Calcareous dinoflagellates diversified in the Late Jurassic, with three major clades established by the Cretaceous. Molecular clock estimates suggest the K/T boundary had minimal impact on their diversity.
Area of Science:
- Paleontology
- Molecular Biology
- Marine Biology
Background:
- Calcareous dinoflagellates (Thoracosphaeraceae, Peridiniales) form a monophyletic group with three main clades.
- Understanding their evolutionary history requires integrating morphological and molecular data.
Purpose of the Study:
- To determine the divergence times of calcareous dinoflagellate clades using molecular clock analysis.
- To investigate the impact of the K/T boundary on dinoflagellate diversity.
Main Methods:
- Relaxed Bayesian molecular clocks were applied to nuclear rRNA sequences of 18 dinoflagellate representatives.
- Stratigraphically documented first occurrences of archeopyle types were used as calibration points.
- Divergence estimates were compared with first stratigraphic occurrences of taxa not used as constraints.
Main Results:
- The initial diversification of extant calcareous dinoflagellates likely occurred in the Late Jurassic.
- All three major clades were established by the Cretaceous period.
- The K/T boundary showed a limited effect on the diversity of this group, with lineages predating 65 million years ago.
Conclusions:
- Molecular clock estimates align with stratigraphic occurrences of key taxa like Thoracosphaera and Calciodinellum.
- Independent evolution of mesoepicystal operculum types from apical archeopyles is suggested.
- Discrepancies in some taxa may stem from fossil misassignment due to homoplasy or incomplete knowledge of extant diversity.
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