Articles | Volume 13, issue 9
Biogeosciences, 13, 2757–2768, 2016
https://doi.org/10.5194/bg-13-2757-2016

Special issue: Integrated perspectives on biological and geological dynamics...

Biogeosciences, 13, 2757–2768, 2016
https://doi.org/10.5194/bg-13-2757-2016

Research article 11 May 2016

Research article | 11 May 2016

Aligning and synchronization of MIS5 proxy records from Lake Ohrid (FYROM) with independently dated Mediterranean archives: implications for DEEP core chronology

Giovanni Zanchetta et al.

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Cited articles

Albert, P. G., Hardiman, M., Keller, J., Tomlinson, E. L., Smith, V. C., Bourne, A. J., Wulf, S., Zanchetta, G., Sulpizio, R., Müller, U. C., Pross, J., Ottolini, L., Matthews, I. P., Blockley S. P. E., and Menzies, M. A.: Revisiting the Y-3 tephrostratigraphic marker: a new diagnostic glass geochemistry, age estimate, and details on its climatostratigraphical context, Quaternary Sci. Rev., 118, 105–121, https://doi.org/10.1016/j.quascirev.2014.04.002, 2015.
Albrecht, C. and Wilke, T.: Lake Ohrid: Biodiversity and evolution, Hydrobiologia, 615, 103–140, 2008.
Almogi-Labin, A., Bar-Matthews, M., Shriki, D., Kolosovsky, E., Paterne, M., Schilman, B., Ayalon, A., Aizenshtat, Z., and Matthews, A.: Climatic variability during the last 90 ka of the southern and northern Levantine Basin as evident from marine records and speleothems, Quaternary Sci. Rev., 28, 2882–2896, 2009.
Anovski, T., Andonovski, B., and Minceva, B.: Study of the hydrological relationship between Lake Ohrid and Prespa, Proc Symp Isotope Techn Water Res Dev. IAEA, Vienna, Austria, March 1991, 737–740, 1992.
Bard, E., Delaygue, G., Rostek, F., Antonioli, F., Silenzi, S., and Schrag, D.: Hydrological conditions in the western Mediterranean basin during the deposition of Sapropel 6 (ca. 175 kyr), Earth Planet. Sc. Lett., 202, 481–494, 2002.
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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.
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