In situ forest with lycopsid trees bearing lobed rhizomorphs from the Upper Devonian of Lincheng, China

Author:

Qin Min12ORCID,Wang Deming3ORCID,Liu Le4ORCID,Liu Lu5,Zhou Yi6

Affiliation:

1. College of Life Sciences, Linyi University , Linyi 276000 , PR China

2. Key Laboratory of Stratigraphy and Palaeontology, Ministry of Natural Resources , Beijing 100037 , PR China

3. Key Laboratory of Orogenic Belts and Crustal Evolution, Department of Geology, Peking University , Beijing 100871 , PR China

4. School of Geoscience and surveying engineering, China University of Mining and Technology (Beijing) , Beijing 100083 , PR China

5. Department of Earth Sciences, National Natural History Museum of China , Beijing 100050 , PR China

6. School of Life Sciences, Sun Yat-sen University , Guangzhou 510275 , PR China

Abstract

Abstract The earliest forests in the Devonian were reported from only four localities worldwide. The tree lycopsids, sometimes as the primary elements of Devonian forests, had evolved several types of rooting systems. In recent years, we found and excavated a Late Devonian (Famennian, 374–359 Ma) lycopsid forest from Zhejiang Province, China. The fossil forest occurs at seven locations of Lincheng Town of Changxing County and mainly consists of in situ small tree lycopsid (Heliodendron longshanense gen. et sp. nov.) stems usually connected to lobed cormose rhizomorphs. The four short lobes of each rhizomorph often branch once and bear roots arranged radially. Allometry is observed between the trunk diameter of Heliodendron and the length of its rhizomorphic lobes, indicating that the trunk develops later than the rhizomorph in tree lycopsid plants. The Devonian witnessed the transformation from clastic nonlycopsid dominated forests to Carboniferous swampy forests dominated by giant lycopsid trees. These trees form a multigenerational community, as shown by the in situ preserved stems at various levels within the same area due to frequent sedimentation events.

Funder

National Natural Science Foundation of China

Natural Science Foundation of Shandong Province

Key Laboratory of Stratigragy and Paleontology, Ministry of Natural Resources

Publisher

Oxford University Press (OUP)

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