A Late Devonian tree lycopsid with large strobili and isotomous roots.

Commun Biol

Science Press, China Science Publishing & Media Ltd., Beijing, 100717, China.

Published: September 2022

AI Article Synopsis

  • Tree lycopsids were crucial to the Late Devonian forest ecosystem and influenced Earth's climate, but their reproductive structures show limited morphological variation, making it hard to understand their ecology.
  • Researchers have discovered a new species, Omprelostrobus gigas, from Upper Devonian deposits in China, featuring the largest strobili known for its time, which adaptively differed in form to enhance photosynthesis.
  • The diverse sizes of the strobili were not directly linked to the plants' body structure, indicating that larger strobili might have evolved as a strategy for reproductive success in unstable, flood-prone environments.

Article Abstract

Tree lycopsids prospered in the Late Devonian and constituted a major part of the Late Paleozoic forest ecosystem that deeply impacted the Earth's climate. However, the fertile organs of these early tree lycopsids display low morphological disparity, which has hampered further knowledge about their ecological habit. Here, we report Omprelostrobus gigas gen. et sp. nov. from the Upper Devonian (Famennian) Wutong Formation at Changxing, Zhejiang, China. The collection includes aerial axes, strobili and associated roots. The strobili are the largest among coeval lycopsids to our knowledge, and are divided into proximal and distal portions by dimorphic sporophylls with differentiated laminae and probable strong photosynthetic capacity. The associated but not attached roots displaying multiple isotomous branches lack rootlets and typical rootlet scars. The varied strobili sizes of early tree lycopsids were relatively independent of their body plan, but the large strobili could suggest increased reproductive investment to overcome the disadvantages of the disturbed flooded habitat.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9478126PMC
http://dx.doi.org/10.1038/s42003-022-03934-4DOI Listing

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