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Precambrian phosphatized embryos and larvae from the Doushantuo Formation and their affinities, Guizhou (SW China) 被引量:5

Precambrian phosphatized embryos and larvae from the Doushantuo Formation and their affinities, Guizhou (SW China)
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摘要 Weng,an phosphates of the Precambrian Dou-shantuo Formation, Guizhou (southwestern China) preserve a large number of exquisite biological structures, which are mostly micro-spherical and represent seaweeds, acritarchs and developing eggs related to various groups of metazoans. Here is a report of a variety of developing eggs and larvae, which are most probably of Cnidarian affinity. The eggs ex-amined in the study are composed of early cleavage embryos and two-layered gastrulae. The early cleavage embryos are radial and total cleavage with equal-size blastomeres. The gastrulae mostly bear a large archenteron, which is filled with yolk-degrading organic matter. Ovoid to fusiform planula-like larvae identified in thin sections under light microscope are mostly mouthless and their gastrovascularcavity is filled with possible yolk-degrading organic matter. They are likely representatives of non-feeding larva. The uncommon planula-like structures are hollow, with each having a mouth-like structure on its narrow end. We inter-pret them as feeding larva. Study of these embryos with pos-sible Cnidarian affinities shed new insight on the origin ofmetazoans. Weng'an phosphates of the Precambrian Doushantuo Formation, Guizhou (southwestern China) preserve a large number of exquisite biological structures, which are mostly micro-spherical and represent seaweeds, acritarchs and developing eggs related to various groups of metazoans. Here is a report of a variety of developing eggs and larvae, which are most probably of Cnidarian affinity. The eggs examined in the study are composed of early cleavage embryos and two-layered gastrulae. The early cleavage embryos are radial and total cleavage with equal-size blastomeres. The gastrulae mostly bear a large archenteron, which is filled with yolk-degrading organic matter. Ovoid to fusiform planula-like larvae identified in thin sections under light microscope are mostly mouthless and their gastrovascular cavity is filled with possible yolk-degrading organic matter. They are likely representatives of non-feeding larva. The uncommon planula-like structures are hollow, with each having a mouth-like structure on its narrow end. We interpret them as feeding larva. Study of these embryos with possible Cnidarian affinities shed new insight on the origin of metazoans.
出处 《Chinese Science Bulletin》 SCIE EI CAS 2005年第19期2193-2200,共8页
基金 This work was supported jointly by the National Natural Science Foundation of China (Grant No. 40132010, 40302004);Chinese Acad-emy of Sciences (Grant No. KZCX3 SW-14l) ; Ministry of Science and Technology of China (Grant No. G2000077700).
关键词 中国 贵州 寒武纪 磷酸盐晶胚 化石 生物学结构 Weng'an fauna, fossil embryos, fossil planulae, Cnidarians.
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