Evidence of non-vascular land plants from the early Silurian (Llandoverian) of Virginia, U.S.A. – ScienceOpen
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      Evidence of non-vascular land plants from the early Silurian (Llandoverian) of Virginia, U.S.A.

      , ,
      Review of Palaeobotany and Palynology
      Elsevier BV

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          XXXIII.—On Old Red Sandstone Plants showing Structure, from the Rhynie Chert Bed, Aberdeenshire. Part V. The Thallophyta occurring in the Peat-Bed; the Succession of the Plants throughout a Vertical Section of the Bed, and the Conditions of Accumulation and Preservation of the Deposit

          In this concluding part of the series of papers on the plants preserved in the Rhynie chert-band, various remains of lower plants that occur in the peat will be described, and some general questions concerning the accumulation and preservation of the deposit considered. The paper is divided naturally into the parts enumerated below.
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            The origin of land plants: a matter of mycotrophism.

            It is hypothesized that terrestrial plants are the product of an ancient and continuing symbiosis of a semi-aquatic ancestral green alga and an aquatic fungus-an oomycete. The Siluro-Devonian "explosive" colonization of land, and indeed the very evolution of plants, was possible only through such mutualistic partnerships-partnerships that were equipped to cope with the problems of desiccation and starvation associated with terrestrial existence.
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              On the Plant-Remains from the Downtonian of England and Wales

              W Lang (1937)
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                Author and article information

                Journal
                Review of Palaeobotany and Palynology
                Review of Palaeobotany and Palynology
                Elsevier BV
                00346667
                March 1978
                March 1978
                : 25
                : 2
                : 121-149
                Article
                10.1016/0034-6667(78)90034-9
                0265a544-220f-41dd-8c21-fdd03eb750b7
                © 1978

                http://www.elsevier.com/tdm/userlicense/1.0/

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