Palaeoenvironment and ecology of the middle Cretaceous Grebenka flora of northeastern Asia

By R. Spicer, A. Ahlberg, A. Herman, S. Kelley, M. Raikevich, P. Rees. 2002

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Araucariaceae (Pinopsida): Aspects in palaeobiogeography and palaeobiodiversity in the Mesozoic (2007, background): “The occurrence of Araucaria in a truly polar vegetation (4721N palaeolatitude) is recorded by Spicer et al. (2002) from the uppermost Albian to lowermost Cenomanian Grebenka flora, Krivorechevskaya Formation in NE Russia.”
Digital Future for Paleoclimate Estimation from Fossil Leaves? Preliminary Results (2003, background): “…is the use of correlations observed in living forests betweenclimatic and leaf size and shape variables (Bailey and Sinnott, 1915; Wolfe, 1979, 1993; Greenwood and Wing, 1995; Herman and Spicer, 1996; Wing et al., 2000; Gregory-Wodzicki, 2000; Jacobs, 2002; Spicer et al., 2002; Wilf et al., 2003).”
Ecological conservatism in the “living fossil” Ginkgo (2003, background): “…from at least the Jurassic, members of Ginkgoales at high latitudes are often associated with sandy channel deposits (Hughes 1976; Spicer and Parrish 1986; Falcon-Lang et al. 2001; Spicer and Herman 2001; Spicer et al. 2002; L.J.H. unpublished field data from the Jurassic in Yorkshire, England).”