A new rhyniopsid with novel sporangium organization from the Lower Devonian of South Wales
A new rhyniopsid with novel sporangium organization from the Lower Devonian of South Wales
复制标题
南威尔士下泥盆统具有新颖孢子囊组织的新菱藻类
DOI:
10.1111/j.1095-8339.1989.tb01713.x
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发表时间:
1989
影响因子:
2.4
通讯作者:
D. Edwards
中科院分区:
文献类型:
--
作者:
C. H. Shute;D. Edwards
Re-investigation of permineralized plants originally called Cooksonia sp. from the Lower Old Red Sandstone (Siegenian) of Gwent, S. Wales shows them to be rhyniopsids with simple isotomous branching in smooth axes and ellipsoidal terminal sporangia that are longer than wide and that possess a complex wall organization. They are thus placed in a new genus. The sporangial wall is several cells thick, the outermost comprising a layer with pronounced thickening of the anticlinal and outer periclinal walls, which is interrupted by a zone of thinner-walled cells parallel to the longest dimension of the ellipsoidal organ and considered to be involved in its dehiscence into two equal halves. The alete isospores have a bilayered wall, the outer interpreted as an ornamented perispore. Similar granular ornament seen on sheets and globules in the vicinity of the spores and on the innermost surface of the sporangium wall possibly demonstrates the activity of a periplasmodial tapetum. The permineralized sporangia are considered conspecific with those in compression fossils with elliptical outlines and pronounced borders. Comparison of presumed dehiscence mechanisms in a number of Silurian and early Devonian fossils suggests that splitting into two equal valves along the longest dimension, so that a maximum area of spores was exposed to the atmosphere, arose independently in a number of unrelated plants.
DOI:
10.1111/j.1095-8339.1986.tb01020.x
发表时间:
1986-09-01
影响因子:
2.4
作者:
EDWARDS, DS
通讯作者:
EDWARDS, DS