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Terrestrial Palaeoecology and Global Change

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Chapter 4. Palaeoecogeography<br />

89<br />

Mongolia (Krassilov, 1982). These allochthonous remains form a morphologic link between<br />

the Jurassic Schizolepis–Pityospermum complex <strong>and</strong> an extant laricoid genus<br />

Pseudolarix, <strong>and</strong> are sometimes assigned to the latter (Fig. 40). Pseudolarix kempferi,<br />

a temperate montane species, is the only survivor of the Cretaceous complex of heteroblastic<br />

shoot-dropping conifers that, with the mid-Eocene montane glaciation, conceivably<br />

gave rise both to the deciduous laricoids with persistent spur-shoots <strong>and</strong>, by a pedomorphic<br />

transformation of heteroblastic shoot system, to the homoblastic piceoids.<br />

c<br />

a<br />

b<br />

e<br />

d<br />

Fig. 40. A precursor of mountain taiga, the Early Cretaceous Pseudolarix forest abundantly represented by<br />

leafy short-shoots <strong>and</strong> detached cone-scales in the rift valley deposits of Transbaikalia <strong>and</strong> Mongolia: (a-c)<br />

P. erensis, a modern-type pinaceous conifer growing side by side with (d-f) Swedenborgia, an archaic<br />

voltziaceous conifer probably ancestral to the Pinaceae (Krassilov, 1982).<br />

f

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