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«
Cylindrical calcareous bodies often tapered or restricted at the
base and top. A few are broadly rounded at the top. They appear to
have grown one above the other like a string of sausages. A few show
budding or branching.
The plant probably developed extended fronds, each composed of many
segments somewhat similar to the modern Cymopolia barbata
HARVEY. The fossils represent the individual segments.
The central stem is relatively narrow (about 1/4 to 1/5 width or the
entire fossils). Primary branches perpendicular to the axis of the
stem, except at ends where they are inclined. Primary branches in
alternating annular rows. Secondary branches, small, and steeply
inclined to the primary branches bending so tips are approximately
parallel to outer surface. Sporangia large, nearly spherical,
attached to main stem. They occur in vertical rows separated by
primary branches. These vertical rows alternate in position, so that
in both vertical and annular rows, there is an alternation of
primary branches and sporangia. The tapering ends of the thallus
appear to contain only branches, no sporangia. » (JOHNSON, 1954). |
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JOHNSON, J.H. (1954) -
Cretaceous Dasycladaceae from Gillespie
County, Texas. Journal of Paleontology, Tulsa, vol. 28, N° 6, p.
787-790, 1 pl. h.-t. (93).
МАСЛОВ,
В.П. (1960) -
Новые
водоросли
мела Копет-Дага
(Туркмения).
Докладу
Академии
Наук СССР,
Москва, Том
134, N° 4, p. 939-941. |