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      A Fossilized Microcenosis In Triassic Amber

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      The Journal of Eukaryotic Microbiology
      Wiley-Blackwell

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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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            Phylogenetic position of some Chlorella species within the chlorococcales based upon complete small-subunit ribosomal RNA sequences.

            Complete small-subunit rRNA (16S-like rRNA) coding region sequences were determined for eight species of the Chlorococcales (Chlorophyceae). The genera investigated include Prototheca, Ankistrodesmus, Scenedesmus, and five Chlorella species. Distance matrix methods were used to infer a phylogenetic tree that describes evolutionary relationships between several plant and green algal groups. The tree exhibits a bifurcation within the Chlorococcales consistent with the division into Oocystaceae and Scenedesmaceae, but three of the five Chlorella species are more similar to other algae than to Chlorella vulgaris. All of the sequences contain primary and secondary structural features that are characteristic of 16S-like rRNAs of chlorophytes and higher plants. Anikstrodesmus stipitatus, however, contains a 394-bp group I intervening sequence in its 16S-like rRNA coding region.
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              Terrestrial soft-bodied protists and other microorganisms in triassic amber.

              Protozoa, cyanobacteria, sheathed algae, sheathed fungi, germinating pollen or spores, and fungal spores have been found in amber 220 to 230 million years old. Many of these microorganisms can be assigned to present-day groups. This discovery of terrestrial, soft-bodied protists that can be referred to modern groups indicates that morphological evolution is very gradual in many protists and that both structural and probably functional stasis extend back at least to the Upper Triassic period.
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                Author and article information

                Journal
                The Journal of Eukaryotic Microbiology
                J Eukaryotic Microbiology
                Wiley-Blackwell
                1066-5234
                1550-7408
                November 1999
                November 1999
                : 46
                : 6
                : 571-584
                Article
                10.1111/j.1550-7408.1999.tb05133.x
                75f71045-71e4-4d1f-b896-02af3f1804f2
                © 1999

                http://doi.wiley.com/10.1002/tdm_license_1.1

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