A new species of Adoketophyton from the Lower Devonian (Pragian) Posongchong Formation of Yunnan, China

被引:11
作者
Zhu, Xiao [1 ]
Xue, Jin-Zhuang [1 ]
Hao, Shou-Gang [1 ]
Wang, De-Ming [1 ]
机构
[1] Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
基金
中国国家自然科学基金;
关键词
Adokerophyton; strobilus; sporophyll; circinate tip; Early Devonian; fossil plant; LAND PLANTS; LYCOPSIDS; LEAVES; GENUS;
D O I
10.1016/j.revpalbo.2011.01.003
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
A new species of early vascular plant, Adoketophyton parvulum sp. nov., is described from the Lower Devonian (Pragian) Posongchong Formation of Yunnan, China. The plant is composed of main axes, lateral vegetative branches and isotomous or anisotomous fertile axes. The vegetative axes branch isotomously or pseudomonopodially in three dimensions, with some laterals ending in terminal circinately coiled tips. K-shaped branching and tubercles are preserved. Terminal strobili consist of four vertical rows of fertile units, arranged in opposite and decussate pairs. Each fertile unit comprises a fan-shaped sporophyll and a sporangium attached adaxially by a short stalk at the base of the sporophyll. The strobili and fertile units (sporophylls and associated sporangia) of this new species are much smaller than those of the type species, Adoketophyton subverticillatum, and the ratio of heights of sporangia to sporophyll laminae in the two species shows a large discrepancy. The affinity and evolution of Adokerophyron are discussed. The various leaf-like appendages in plants reported from the Early Devonian of South China are considered a phenomenon of convergent evolution. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:238 / 246
页数:9
相关论文
共 28 条
[1]  
[Anonymous], [No title captured]
[2]   Evolution of leaf-form in land plants linked to atmospheric CO2 decline in the Late Palaeozoic era [J].
Beerling, DJ ;
Osborne, CP ;
Chaloner, WG .
NATURE, 2001, 410 (6826) :352-354
[3]   HETEROSPOROUS, BARINOPHYTACEAN PLANTS FROM THE UPPER DEVONIAN OF NORTH-AMERICA AND A DISCUSSION OF THE POSSIBLE AFFINITIES OF THE BARINOPHYTACEAE [J].
BRAUER, DF .
REVIEW OF PALAEOBOTANY AND PALYNOLOGY, 1981, 33 (2-4) :347-362
[4]   BARINOPHYTON-CITRULLIFORME (BARINOPHYTALES INCERTAE-SEDIS, BARINOPHYTACEAE) FROM THE UPPER DEVONIAN OF PENNSYLVANIA [J].
BRAUER, DF .
AMERICAN JOURNAL OF BOTANY, 1980, 67 (08) :1186-1206
[5]  
Cai C., 1977, ACTA PALAEONTOL, V16, P12
[6]  
EDWARDS D, 1968, Palaeontology (Oxford), V11, P683
[7]   Climate signals in Paleozoic land plants [J].
Edwards, D .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES B-BIOLOGICAL SCIENCES, 1998, 353 (1365) :141-156
[8]  
GENG B-Y, 1983, Acta Botanica Sinica, V25, P574
[9]  
Gensel P.G., 1984, PLANT LIFE DEVONIAN