Molteno sphenophytes: Late Triassic biodiversity in southern Africa
Date
2018-06-28
Authors
Anderson, Heidi M.
Anderson, John M.
Journal Title
Journal ISSN
Volume Title
Publisher
Evolutionary Studies Institute
Abstract
This comprehensive systematic study of the sphenophytes (Equisetophyta, horsetails) is the fifth
monograph in a series describing the flora of the Molteno Fm., Karoo Basin (Late Triassic,
Carnian) of South Africa. The introductory part of the study gives an overview of the Molteno
flora and fauna and its significance in global context. In the collection of ca 27 200 catalogued
slabs, the sphenophytes fall third, after Dicroidium and the conifer Heidiphyllum, as the most
abundant vegetative elements.
The study is based on 43 super-localities encompassing 100 assemblages or taphocoenoses
(TCs). Sphenophytes occur in 59 of the TCs. In 16 of these TCs, they are the mono-dominant
plant group and represent the ‘Equisetophyte marsh’ habitat; in a further 18 TCs, they are common
to co-dominants; and in the remaining 25 TCs they occur sparsely to rarely. Habit-habitat reconstructions
have been made for nine of the Molteno sphenophyte species. These occur in ‘Equisetophyte
marsh’ and ‘Dicroidium riparian forest’ habitats. Present evidence suggests that these
plants were not only dominant in much of the Molteno floodplain but also grew to sizes similar
to modern giant bamboos, and may be referred to as giant horsetails.
The described material includes a total of fi ve genera and 14 species of dispersed strobili;
and eight genera and 23 vegetative species. The latter are mostly based on leaves attached to
stems but include one species of isolated leaves and one of sculptured stems. Other isolated
stems and nodal diaphragms are recorded but not named at generic or specific level. These fertile
and vegetative genera fall in two distinctive orders – the Echinostachyales and Equisetales.
None of the strobili have been found attached to vegetative material (grade 5 affiliation). In one
case, Kraaiostachys plaatkoppensis (from Kra 211), a numerous collection of strobili is found
in monospecific association with vegetative material (grade 4 affiliation). In all other cases, the
affiliations are based essentially on co-occurrence of lesser levels of certainty (grades 2–3,5). In
terms of whole-plant taxa, two orders, three families, seven genera and 26 species of Molteno
sphenophytes are recognised.
This study describes 14 new fertile and 23 new vegetative species. These fall in two previously
described strobilus genera (Echinostachys, 1 sp; Equisetostachys, 9 spp) and six previously
described vegetative genera (Schizoneura, 2 spp; Paraschizoneura, 4 spp; Asinisetum, 1 sp;
Townroviamites, 3 spp; Zonulamites, 4 spp; Equisetites, 6 spp). A total of three strobilus genera
(Cetistachys, 1 sp; Kraaiostachys, 1 sp; Viridistachys, 2 spp) and two vegetative genera (Moltenomites,
2 spp; Balenosetum,1 sp) are described as new. All genera and species are described
following the format established in the previous Molteno monographs, and are extensively
illustrated (pen sketches, black/white and colour photographs).
In Gondwana Triassic context, the Molteno sphenophytes are now by far the most comprehensively
known and the most diverse. Included is a review of all known Gondwana Triassic
plant-yielding formations which reveals a total of 10 whole-plant genera and 42 whole-plant
species of sphenophytes. A global review of sphenophytes including Laurasia and other geological
periods has not been attempted, but the most relevant plants beyond the Gondwana Triassic
have been compared.
Description
Keywords
Molteno sphenophytes
Triassic ecosystems
palaeobotany