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The position and map of Gough Island with stars indicating places where
the species was found. It is apparently a moss-inhabiting species, present on
exposed areas, most abundant on localities close to the sea, from where it was
originally described by Carter.
An intriguing Eunotia species (Bacillariophyta) from
Gough Island (Tristan da Cunha Archipelago)
Petra Vinšová1, Kateřina Kopalová1 and Bart Van de Vijver2,3
1Charles University in Prague, Faculty of Science, Department of Ecology, Viničná 7, CZ-12844 Prague 2, Czech Republic
2Botanic Garden Meise, Department ofBryophyta & Thallophyta, Nieuwelaan 38, B-1860 Meise, Belgium (bart.vandevijver@jardinbotaniquemeise.be)
3University of Antwerp, Department ofBiology, ECOBE, Universiteitsplein 1, B-2610 Wilrijk, Belgium
INTRODUCTION
Gough Island (40 ° 21'S, 9 ° 53 'W), is a small remote and uninhabited island of volcanic origin, positioned in
the cool-temperate zone in the southern Altantic Ocean. Despite its very interesting geographical position,
oceanic origin, extreme isolation and the number of interesting habitats, our knowledge of the non-
marine diatom flora of Gough Island is very poor. Carter (1966) described many new species in the Tristan
da Cunha Island Group, and reported the presence of a very diverse diatom flora including a large number
of new taxa, now rarely seen elsewhere. Recently, a new analysis of the moss-inhabiting flora of Gough
Island has started. The dominant genera include Eunotia, Frustulia and Pinnularia. Several taxa of these
genera can not be identified using the currently available taxonomic literature.
One species, originally described by Carter (1966) in the genus Pseudoeunotia as P. linearis, but most likely
belonging to the genus Eunotia, is of our particular interest.
Pseudo-eunotia
Grunow in Van Heurck
(Koizumi & Yanagisawa 1990)
‘Differs from Eunotia by the absence of terminal
nodules and from Synedra and Ceratoneis by the
absolute lack of a median line’
Differences from Eunotia
Raphe structure
Presence of raised costae/ridges on valve face
Biseriate striae
ACKNOWLEDGEMENTS: The authors wish to thank Dr. Niek Gremmen who performed the sampling on Gough Island.
REFERENCES: Carter, J. (1966): ‚Some freshwater diatoms of Tristan da Cunha and Gough Island‘. Nowa Hedwigia 9: 443-492. Koizumi, I., &
Yanagisawa, Y. (1990): ‚Evolutionary change in diatom morphology—an example from Nitzschia fossilis to Pseudoeunotia doliolus‘. Transactions
and Proceedings of the Palaeontological Society of Japan 157:347-359.
TAXONOMICAL CONCLUSION
Clearly, based on its morphology, the position of this taxon in the genus Pseudo-
eunotia is doubtful. A transfer in the genus Eunotia is likely but still remains to be
analyzed due to several unique features such as the spines, the structure of the
areolae and the absence of rimportulae.
Described by Carter (1966): Valves linear with rounded ends about 10–35 µm long and 4 µm
wide. Striae irregular about 11 in 10 µm minutely punctated.‘
OUR EXAMINATION • Valves length 10 to 39 µm, width 2,2 to 3,7 µm, striae from 8 to 15 in
10 µm (middle) and up to 17 when close to apex. • Frustule length 11,5–33 µm, width 4,1–10 µm,
and striae 7–20 in 10 µm (mostly one side is denser). Aerolae mostly 4 in 1 µm.
Pseudoeunotia linearis
Carter (1966)
Unusual morphology for the genus Eunotia
Presence of spines on the junction between valve face
and mantle
Colony formation
Presence of granules on the mantle
Girdle composed of several copulae
•
Visually, number of striae in 10 µm rather low
Striae composed of large round areolae bordered by a
small raised edge
Raphe quite short, sometimes bordered by ridges
Rimportulae and apical pore fields absent
Helictoglossae poorly developed
•