Articles | Volume 19, issue 10
https://doi.org/10.5194/cp-19-2027-2023
https://doi.org/10.5194/cp-19-2027-2023
Research article
 | 
26 Oct 2023
Research article |  | 26 Oct 2023

Disentangling environmental drivers of subarctic dinocyst assemblage compositional change during the Holocene

Sabrina Hohmann, Michal Kucera, and Anne de Vernal

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Cited articles

Allan, E., de Vernal, A., Knudsen, M. F., and Hillaire-Marcel, C.: Late Holocene sea-surface instabilities in the Disko Bugt area, west Greenland, in phase with δ18O-oscillations at Camp Century, Paleogeography and Paleoclimatology, 33, 227–224, https://doi.org/10.1002/2017PA003289, 2018. 
Andresen, C. S., Mccarthy, D. J., Dylmer, C. V., Seidenkrantz, M., Kuijpers, A., and Lloyd, J. M.: Interaction between subsurface ocean waters and calving of the Jakobshavn Isbræ during the late Holocene, The Holocene, 21, 211–224, https://doi.org/10.1177/0959683610378877, 2010. 
Belt, S. T. and Müller, J.: The Arctic sea ice biomarker IP25: a review of current understanding, recommendations for future research and applications in palaeo sea ice reconstructions, Quat. Sci. Rev., 79, 9–25, https://doi.org/10.1016/ j.quascirev.2012.12.001, 2013. 
Berger, A. and Loutre, M. F.: Insolation values for the climate of the last 10 million years, Quat. Sci. Rev., 10, 297–317, 1991. 
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Short summary
Drivers for dinocyst assemblage compositions differ regionally and through time. Shifts in the assemblages can sometimes only be interpreted robustly by locally and sometimes globally calibrated transfer functions, questioning the reliability of environmental reconstructions. We suggest the necessity of a thorough evaluation of transfer function performance and significance for downcore applications to disclose the drivers for present and fossil dinocyst assemblages in a studied core location.
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