A new Oligocene Calocedrus from South China and its implications for transpacific floristic exchanges
• Premise of the Study: Calocedrus is among the genera with a typical eastern Asian–western North American disjunct distribution today. The origin of its modern distribution pattern can be better understood by examining its fossil record. • Methods: The present article reports for the first time a n...
| Published in: | American Journal of Botany |
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| Main Authors: | , , |
| Other Authors: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
2012
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.3732/ajb.1100331 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.3732%2Fajb.1100331 http://onlinelibrary.wiley.com/wol1/doi/10.3732/ajb.1100331/fullpdf |
| Summary: | • Premise of the Study: Calocedrus is among the genera with a typical eastern Asian–western North American disjunct distribution today. The origin of its modern distribution pattern can be better understood by examining its fossil record. • Methods: The present article reports for the first time a new fossil species of this genus based on compressed material from the Oligocene Ningming Formation of Guangxi, South China, in its present major distribution area in eastern Asia. • Key Results: Calocedrus huashanensis sp. nov. is most similar to the two extant eastern Asian species, C. macrolepis and C . formosana , in gross morphology of foliage shoots and bears a close resemblance to the latter in cuticle structure. It shows a general similarity to the North American fossil representatives of the genus in alternately branched foliage shoots but is clearly different from the European Paleogene species characterized by oppositely branched leafy shoots. • Conclusions: This discovery provides new evidence for the floristic exchange of this genus between eastern Asia and North America before the Oligocene (most likely in the Eocene), presumably via the Bering land bridge. The flattened leafy shoots and dimorphic leaves with thin cuticle, open stomatal pits, and shallowly sunken guard cells of the present fossils suggest a rather humid climate during the Oligocene in the Ningming area, South China. |
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