Articles | Volume 13, issue 9
https://doi.org/10.5194/bg-13-2757-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-2757-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Aligning and synchronization of MIS5 proxy records from Lake Ohrid (FYROM) with independently dated Mediterranean archives: implications for DEEP core chronology
Giovanni Zanchetta
CORRESPONDING AUTHOR
Dipartimento di Scienze della Terra, University of Pisa,
Pisa, Italy
Eleonora Regattieri
Institute of Environmental Geology and Geoengineering,
IGAG-CNR, Montelibretti, Rome, Italy
Biagio Giaccio
Institute of Environmental Geology and Geoengineering,
IGAG-CNR, Montelibretti, Rome, Italy
Bernd Wagner
Institute of Geology and Mineralogy, University of
Cologne, Cologne, Germany
Roberto Sulpizio
Dipartimento di Scienze della Terra e Geoambientali,
University of Bari, Bari, Italy
Alex Francke
Institute of Geology and Mineralogy, University of
Cologne, Cologne, Germany
Hendrik Vogel
Institute of Geological Sciences & Oeschger Centre for
Climate Change Research, University of Bern, Bern,
Switzerland
Laura Sadori
Dipartimento di Biologia Ambientale, University of Roma
“La Sapienza” Roma, Italy
Alessia Masi
Dipartimento di Biologia Ambientale, University of Roma
“La Sapienza” Roma, Italy
Gaia Sinopoli
Dipartimento di Biologia Ambientale, University of Roma
“La Sapienza” Roma, Italy
Jack H. Lacey
Centre for Environmental Geochemistry, School of
Geography, University of Nottingham, Nottingham, UK
NERC Isotope Geosciences Facilities, British Geological
Survey, Keyworth, Nottingham, UK
Melanie J. Leng
Centre for Environmental Geochemistry, School of
Geography, University of Nottingham, Nottingham, UK
NERC Isotope Geosciences Facilities, British Geological
Survey, Keyworth, Nottingham, UK
Niklas Leicher
Institute of Geology and Mineralogy, University of
Cologne, Cologne, Germany
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Short summary
Chronology is fundamental in paleoclimatology for understanding timing of events and their origin. In this paper we try to obtain a more detailed chronology for the interval comprised between ca. 140 and 70 ka for the DEEP core in Lake Ohrid using regional independently-dated archives (i.e. speleothems and/or lacustrine succession with well-dated volcanic layers). This allows to insert the DEEP chronology within a common chronological frame between different continental and marine proxy records.
Chronology is fundamental in paleoclimatology for understanding timing of events and their...
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