Articles | Volume 17, issue 3
https://doi.org/10.5194/cp-17-1199-2021
https://doi.org/10.5194/cp-17-1199-2021
Research article
 | 
16 Jun 2021
Research article |  | 16 Jun 2021

Climate reconstructions based on GDGT and pollen surface datasets from Mongolia and Baikal area: calibrations and applicability to extremely cold–dry environments over the Late Holocene

Lucas Dugerdil, Sébastien Joannin, Odile Peyron, Isabelle Jouffroy-Bapicot, Boris Vannière, Bazartseren Boldgiv, Julia Unkelbach, Hermann Behling, and Guillemette Ménot

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Cited articles

Aichner, B., Feakins, S. J., Lee, J. E., Herzschuh, U., and Liu, X.: High-resolution leaf wax carbon and hydrogen isotopic record of the late Holocene paleoclimate in arid Central Asia, Clim. Past, 11, 619–633, https://doi.org/10.5194/cp-11-619-2015, 2015. a, b
An, C.-B., Chen, F.-H., and Barton, L.: Holocene environmental changes in Mongolia: a review, Global Planet. Change, 63, 283–289, 2008. a, b, c, d
Arnold, T. W.: Uninformative parameters and model selection using Akaike's Information Criterion, J. Wildlife Manage., 74, 1175–1178, 2010. a, b, c
Atahan, P., Heijnis, H., Dodson, J., Grice, K., Le Metayer, P., Taffs, K., Hembrow, S., Woltering, M., and Zawadzki, A.: Pollen, biomarker and stable isotope evidence of late Quaternary environmental change at Lake McKenzie, southeast Queensland, J. Paleolimnol., 53, 139–156, 2015. a
Bartlein, P. J., Prentice, I. C., and Webb III, T.: Climatic response surfaces from pollen data for some eastern North American taxa, J. Biogeogr., 13, 35–57, 1986. a
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Short summary
Since the understanding of Holocene climate change appears to be a relevant issue for future climate change, the paleoclimate calibrations have to be improved. Here, surface samples from Mongolia and Siberia were analyzed to provide new calibrations for pollen and biomarker climate models. These calibrations appear to be more powerful than global calibrations, especially in an arid central Asian context. These calibrations will improve the understanding of monsoon Holocene oscillations.
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