Wang Xin, Duan Shuying, Geng Baoyin, Cui Jinzhong, Yang Yong
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, China.
BMC Evol Biol. 2007 Feb 7;7:14. doi: 10.1186/1471-2148-7-14.
The origin of angiosperms has been under debate since the time of Darwin. While there has been much speculation in past decades about pre-Cretaceous angiosperms, including Archaefructus, these reports are controversial. The earliest reliable fossil record of angiosperms remains restricted to the Cretaceous, even though recent molecular phylogenetic studies suggest an origin for angiosperms much earlier than the current fossil record.
In this paper, after careful SEM and light microscopic work, we report fossils with angiospermous traits of the Jurassic age. The fossils were collected from the Haifanggou Formation (middle Jurassic) in western Liaoning, northeast China. They include two female structures and an associated leaf on the same slab. One of the female structures is physically connected to the apex of a short shoot. The female organs are borne in pairs on short peduncles that are arranged along the axis of the female structure. Each of the female organs has a central unit that is surrounded by an envelope with characteristic longitudinal ribs. Each central unit has two locules completely separated by a vertical septum. The apex of the central unit is completely closed. The general morphology places these fossils into the scope of Schmeissneria, an early Jurassic genus that was previously attributed to Ginkgoales.
Because the closed carpel is a character only found in angiosperms, the closed apex of the central unit suggests the presence of angiospermy in Schmeissneria. This angiospermous trait implies either a Jurassic angiosperm or a new seed plant group parallel to angiosperms and other known seed plants. As an angiosperm, the Liassic age (earliest Jurassic) of Schmeissneria microstachys would suggest an origin of angiosperms during the Triassic. Although still uncertain, this could have a great impact on our perspective of the history, diversity and systematics of seed plants and angiosperms.
自达尔文时代以来,被子植物的起源一直备受争议。尽管在过去几十年里,人们对包括古果属在内的白垩纪之前的被子植物进行了诸多推测,但这些报道存在争议。被子植物最早的可靠化石记录仍局限于白垩纪,尽管最近的分子系统发育研究表明被子植物的起源比目前的化石记录要早得多。
在本文中,经过仔细的扫描电子显微镜和光学显微镜研究,我们报道了具有侏罗纪时代被子植物特征的化石。这些化石采自中国东北辽宁西部的海房沟组(中侏罗世)。它们包括同一石板上的两个雌性结构和一片相关的叶子。其中一个雌性结构与一个短枝的顶端相连。雌性器官成对生于短梗上,短梗沿雌性结构的轴排列。每个雌性器官都有一个中央单元,被一个有特征性纵向肋条的包被所包围。每个中央单元有两个完全由垂直隔膜隔开的子房室。中央单元的顶端完全封闭。总体形态将这些化石归入施氏果属的范畴,施氏果属是一个早侏罗世的属,以前被归入银杏目。
由于封闭的心皮是仅在被子植物中发现的特征,中央单元的封闭顶端表明施氏果属存在被子植物特征。这种被子植物特征意味着要么是侏罗纪被子植物,要么是与被子植物及其他已知种子植物平行的一个新的种子植物类群。作为一种被子植物,微小穗施氏果的里阿斯期(最早的侏罗世)表明被子植物起源于三叠纪。尽管仍不确定,但这可能会对我们对种子植物和被子植物的历史、多样性及系统学的认识产生重大影响。