03.01.2015 Views

Terrestrial Palaeoecology and Global Change

Terrestrial Palaeoecology and Global Change

Terrestrial Palaeoecology and Global Change

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Chapter 3. <strong>Palaeoecology</strong><br />

49<br />

Certain morphological phenomena in extinct plant groups seem also related to leaf<br />

mimicry. Thus, cycadophytes constitute a heterogeneous group of Mesozoic gymnosperms<br />

including cycads, nilssonias, bennettites <strong>and</strong> pentoxyleans. These orders, though<br />

not closely related, are indistinguishable on the basis of their gross leaf (cataphyll) morphologies<br />

(Fig. 26). Formal genera for fossil leaf morphotypes include representatives of<br />

a<br />

c<br />

d<br />

b<br />

Fig. 26. Leaf convergence in the Mesozoic nilssonias (a, b) <strong>and</strong> bennettites (c-e) from the Late Jurassic to<br />

Early Cretaceous of Bureya Basin, Russian Far East.<br />

e

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!