David Lubinski (he/him)

David Lubinski (he/him)

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  • PhD: University of Colorado at Boulder, 1998
  • B.S.: University of Cincinnati, 1987

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(Office) 303 735-6619




Andreev, A. A., David Lubinski (he/him), Bobrov, A. A., Ingolfsson, O., Forman, S. L., Tarasov, P. E., Moller, P. 2008: Early Holocene environments on October Revolution Island, Severnaya Zemlya, Arctic Russia. Palaeogeography Palaeoclimatology Palaeoecology, 267(1-2): 21-30. DOI: 10.1016/j.palaeo.2008.05.002

Mller, P., David Lubinski (he/him), Inglfsson, ., Forman, S. L., Seidenkrantz, M.-S., Bolshiyanov, D. Y., Lokrantz, H., Antonov, O., Pavlov, M., Ljung, K., Zeeberg, J., Andreev, A. A. 2006: Severnaya Zemlya, Arctic Russia: A nucleation area for Kara Sea ice sheets during the Middle to Late Quaternary. Quaternary Science Reviews, 25 (21-22): 2894 2936.

Forman, S. L., David Lubinski (he/him), Ingólfsson, Ó., Zeeberg, J. J., Snyder, J. A., Siegert, M. J., Matishov, G. G. 2004: A review of postglacial emergence on Svalbard, Franz Josef Land and Novaya Zemlya, northern Eurasia. Quaternary Science Reviews, 23(11-13): 1391-1434. DOI: 10.1016/j.quascirev.2003.12.007

Andreev, A. A., Tarasov, P. E., Siegert, C., Ebel, T., Klimanov, V. A., Melles, M., Bobrov, A. A., Dereviagin, A. Y., David Lubinski (he/him), Hubberten, H. W. 2003: Late Pleistocene and Holocene vegetation and climate on the northern Taymyr Peninsula, Arctic Russia. Boreas, 32(3): 484-505.

Polyak, L., Stanovoy, V., David Lubinski (he/him) 2003: Stable isotopes in benthic foraminiferal calcite from a river-influenced Arctic marine environment, Kara and Pechora Seas. Paleoceanography, 18(1): article 1003.

Polyak, L., Korsun, S., Febo, L. A., Stanovoy, V., Khusid, T., Hald, M., Paulsen, B. E., David Lubinski (he/him) 2002: Benthic foraminiferal assemblages from the southern Kara Sea, a river-influenced Arctic marine environment. Journal of Foraminiferal Research, 32(3): 252-273. DOI: 10.2113/32.3.252

David Lubinski (he/him), Polyak, L., Forman, S.L. 2001: Freshwater and Atlantic water inflows to the deep northern Barents and Kara seas since ca 13 14C ka: foraminifera and stable isotopes. Quaternary Science Reviews 20:1851-1879

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