Triskelia scotlandica, an enigmatic Rhynie chert microfossil revisited

PalZ ◽  
2020 ◽  
Author(s):  
Michael Krings
Keyword(s):  
2018 ◽  
Author(s):  
Christine Strullu-Derrien ◽  
Paul Kenrick ◽  
Tomasz Goral ◽  
Andrew H. Knoll
Keyword(s):  

2006 ◽  
Vol 5 (3) ◽  
pp. 178-184 ◽  
Author(s):  
Nora Dotzler ◽  
Michael Krings ◽  
Thomas N. Taylor ◽  
Reinhard Agerer
Keyword(s):  

The Chert Bed of Middle, or possibly Lower, Old Red Sandstone age discovered by Dr. W. Mackie (1914) at Rhynie, in Aberdeenshire, has become famous among palæo-botanists on account of the beautifully preserved remains of the earliest known land plants, described by the late Dr. Kidston and Prof. Lang (1917-1921). In addition to the plants, however, the Rhynie Chert also contains animal remains, for the most part very small and in a very fragmentary condition, although the fragments themselves are in many cases exceedingly well preserved. The vast majority of these animal remains are evidently Crustacean in character, and it was at first thought (see British Association Report, 1919, p. 110) that they belonged to several, or at least to two, different species. Subsequent work has, however, convinced me that all the Crustacean remains so far seen in the Rhynie Chert belong to the one species described in this paper.


Author(s):  
Nigel H Trewin
Keyword(s):  

Author(s):  
Winfried Remy ◽  
Paul A. Selden ◽  
Nigel H. Trewin
Keyword(s):  

1922 ◽  
Vol 41 ◽  
pp. 117-118
Author(s):  
R. Kidston ◽  
W. H. Lang

AbstractPART IV.—This paper concludes the authors’ account of the Vascular Cryptogams found in the Rhynie deposit. Restorations of the four plants, Rhynia Gwynne-Vaughani, R. major, Hornea Lignieri, and Asteroxylon Mackiei, are given. A few additional features, supplementary to the descriptions of these plants in the preceding papers of the series, are described and illustrated. The hemispherical projections of Rhynia Gwynne-Vaughani are shown to have originated underneath stomata. A comparison is made between them and certain intumescences in existing plants. Areas of necrosis and marked wound-reactions of the tissues around them are described for both species of Rhynia. The apex of a stem of R. major is figured. For Asteroxylon additional figures are given of a large rhizome, of the leaf-arrangement and immature structure of the stem in the region of a shoot-apex, and of the longitudinal markings on the epidermal cells resembling those found in Rhynia Gwynne-Vaughani. The discussion summarises the authors’ views on the main bearings of the facts described in Parts 1–4 on various problems in plant morphology.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.


1992 ◽  
Vol 79 (11) ◽  
pp. 1233-1241 ◽  
Author(s):  
Thomas N. Taylor ◽  
Winfried Remy ◽  
Hagen Hass
Keyword(s):  

1991 ◽  
Vol 82 (4) ◽  
pp. 324-332 ◽  
Author(s):  
A. G. Lyon ◽  
Dianne Edwards

ABSTRACTFragmentary remains of a vascular sporophyte from the Rhynie Chert are described as a new genus and species, Trichopherophyton teuchansii. The plant, which is characterised by the possession of unicellular spinous hairs, exarch xylem and laterally attached, marginally dehiscent sporangia, is assigned to the Zosterophyllophytina, but lack of information on the arrangement of sporangia prevents its more precise positioning within the subdivision. Unusual features include the combination of circinate tips to axes with almost terete xylem strands, and the lack of a thick-walled outer cortical zone. Associated axes, lacking spinous hairs, but having papillate or rhizoid-like epidermal emergences, are interpreted as likely rhizomes of Trichopherophyton. Features, such as unicellular spinous hairs, rhizoid-like emergences, circinate tipsand parenchymatous cortex are considered in relation to the functioning and growth of aplant inhabiting an early Devonian wetland.


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