Articles | Volume 36, issue 1
https://doi.org/10.1144/jmpaleo2015-043
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.1144/jmpaleo2015-043
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Salinity-driven size variability in Cyprideis torosa (Ostracoda, Crustacea)
Ian Boomer
GEES, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK
Peter Frenzel
Institut für Geowissenschaften, Friedrich-Schiller-Universität Jena, Burgweg 11, 07749 Jena, Germany
Martin Feike
Institut für Biowissenschaften, Universität Rostock, Universitätsplatz 4, 18055 Rostock, Germany
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We present initial results from a 650 m long core of Late Triasssic to Early Jurassic (190–202 Myr) sedimentary strata from the Cheshire Basin, UK, which is shown to be an exceptional record of Earth evolution for the time of break-up of the supercontinent Pangaea. Further work will determine periodic changes in depositional environments caused by solar system dynamics and used to reconstruct orbital history.
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This paper records the spatial and temporal distribution of deep-sea benthic microfossils (Foraminifera, single-celled organisms) from the latest Oligocene to earliest Pliocene (about 28 to 4 million years ago) from Ocean Drilling Program cores in the southern Indian Ocean. Key taxa are illustrated and their stratigraphic distribution is presented as they respond to a period of marked global climatic changes, with a pronounced warm period in the mid-Miocene followed by subsequent cooling.
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Sci. Dril., 32, 1–25, https://doi.org/10.5194/sd-32-1-2023, https://doi.org/10.5194/sd-32-1-2023, 2023
Short summary
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We present initial results from a 650 m long core of Late Triasssic to Early Jurassic (190–202 Myr) sedimentary strata from the Cheshire Basin, UK, which is shown to be an exceptional record of Earth evolution for the time of break-up of the supercontinent Pangaea. Further work will determine periodic changes in depositional environments caused by solar system dynamics and used to reconstruct orbital history.
Dana Ridha, Ian Boomer, and Kirsty M. Edgar
J. Micropalaeontol., 38, 189–229, https://doi.org/10.5194/jm-38-189-2019, https://doi.org/10.5194/jm-38-189-2019, 2019
Short summary
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This paper records the spatial and temporal distribution of deep-sea benthic microfossils (Foraminifera, single-celled organisms) from the latest Oligocene to earliest Pliocene (about 28 to 4 million years ago) from Ocean Drilling Program cores in the southern Indian Ocean. Key taxa are illustrated and their stratigraphic distribution is presented as they respond to a period of marked global climatic changes, with a pronounced warm period in the mid-Miocene followed by subsequent cooling.
Ian Boomer and Ben Gearey
J. Micropalaeontol., 29, 115–118, https://doi.org/10.1144/0262-821X09-011, https://doi.org/10.1144/0262-821X09-011, 2010
Ian Boomer, Francois Guichard, and Gilles Lericolais
J. Micropalaeontol., 29, 119–133, https://doi.org/10.1144/0262-821X10-003, https://doi.org/10.1144/0262-821X10-003, 2010
I. Boomer, A. R. Lord, K. N. Page, P. R. Bown, F. M. D. Lowry, and J. B. Riding
J. Micropalaeontol., 28, 67–85, https://doi.org/10.1144/jm.28.1.67, https://doi.org/10.1144/jm.28.1.67, 2009
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