华南伊迪卡拉纪类水母化石新发现

唐烽; 钟玲; 金幸生; 郭东辉; 尹崇玉

华南伊迪卡拉纪类水母化石新发现

1. 国土资源部地层与古生物重点实验室, 北京 100037;
2. 中国地质科学院地质研究所, 北京 100037;
3. 四川省博物院, 四川成都 610071;
4. 浙江省自然历史博物馆, 浙江杭州 310014;
5. 厦门大学海洋环境科学学院, 福建厦门 361005

收稿日期: 2014-12-09

修回日期: 2015-07-01

刊出日期: 2016-01-15

Hydrozoan-like Ediacaran fossils from South China

1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
2. Key Laboratory of Stratigraphy and Paleontology, Ministry of Land and Resources, Beijing 100037, China;
3. Sichuan Museum, Chengdu 610071, Sichuan, China;
4. Zhejiang Museum of Natural History, Hangzhou 310014, Zhejiang, China;
5. College of Oceanography & Environmental Science, Xiamen University, Xiamen 361005, Fujian, China

Received Date: 09 December 2014

Revised Date: 01 July 2015

Publish Date: 15 January 2016

摘要

摘要: 华南黔东北地区伊迪卡拉系陡山沱组黑色页岩中产出丰富多样的海相底栖宏体化石组合,其中包含2个新属种Kullingiarotadiscopsis sp. nov.和Eoaequorea xingi gen. & sp. nov.。新类别具有保存清晰的碳质同心环纹和辐射状纹饰,形态上相似于国外广泛分布在碎屑岩和碳酸盐岩中的伊迪卡拉纪典型的圆盘状化石,例如Aspidella,Ediacaria,Cyclomedusa,Eoporpita,Ovatoscutum,Spriggia,Kullingia等。上述化石在国外几乎都保存为印痕,近年来多被解释为不明亲缘底栖生物的圆形固着痕迹或抓痕、圆环状扫痕等,华南陡山沱组碳质压膜保存的圆盘状宏体化石显然不支持该解释。目前,还没有充分的证据表明华南新发现的碳膜化石与国外形态类似的印痕化石如Kullingia和Aspidella具有相同的亲缘关系,但支持将华南化石归属为可能最早的浮游型水螅水母。
- 伊迪卡拉纪 /
- 圆盘状宏体化石 /
- 华南 /
- 似水母生物
Abstract: An abundant and diversified assemblage of benthic fossils from the Ediacaran Doushantuo black shales in the Wenghui section of Guizhou Province contains two discoidal carbonaceous forms, Kullingia rotadiscopsis sp. nov. and Eoaequorea xingi gen. & sp. nov. The fossils have well-preserved concentric rings and radiating lines, and resemble many circular casts and moulds in Edia-caran clastic and carbonate rocks in the world, such as Aspidella, Ediacaria, Cyclomedusa, Eoporpita, Ovatoscutum, Spriggia and Kullingia. The Doushantuo carbonaceous macrofossils help us to inquire into the current functional identifications of circular disks as the holdfasts of unknown organism or scratch circles. Although there is not sufficient correspondence in morphology to warrant reinterpreting all previously described Kullingia and Aspidella form-genus-type structures, these carbonaceous compressions are prone to be the ancestor of pelagic jellyfish-like organisms with medusoid hydrozoan affinity.
- Ediacara /
- discoidal macrofossils /
- South China /
- medusoid organisms

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参考文献(32)

[1]	Narbonne G M, Hofmann H J. Ediacaran biota of the Wernecke Mountains, Yukon, Canada[J]. Palaeontology, 1987, 30:647-676.
[2]	Xiao S, Yuan X, Steiner M, et al. Macroscopic carbonaceous com-pressions in a terminal Proterozoic shale:A systematic reassessment of the Miaohe biota, South China[J]. J. Paleontol., 2002, 76:345-374.
[3]	Gehling J G, Narbonne G M, Anderson M M. The first named Edia-caran body fossil, Aspidella terranovica[J]. Palaeontology, 2000, 43:427-456.
[4]	Narbonne G M. The Ediacara biota:Neoproterozoic origin of ani-mals and their ecosystems[J]. Annu. Rev. Earth Pl. Sc., 2005, 33:421-442.
[5]	Mapstone N B, MacIlroy D. Ediacaran fossil preservation:Taphono-my and diagenesis of a discoid biota from the Amadeus Basin, central Australia[J]. Precambrian Res., 2006, 149:126-148.
[6]	MacGabhann B A. Discoidal fossils of the Ediacaran biota:a review of current understanding[C]//Vickers-Rich P, Komarower P. The Rise and Fall of the Ediacaran Biota. Geological Society Special Pub-lications, 2007:297-313.
[7]	Xiao S, Laflamme M. On the eve of animal radiation:phylogeny, ecology and evolution of the Ediacara biota[J]. Trends in Ecology and Evolution(Cell), 2009, 24:31-40.
[8]	Sprigg R C. Jellyfish from the Basal Cambrian in South Australia[J]. Nature, 1948, 161:568-569.
[9]	Glaessner M F, Wade M. The late Precambrian fossils from Ediacara, South Australia[J]. Palaeontology, 1966, 9:599-628.
[10]	Laflamme M, Narbonne G M, Greentree C, et al. Morphology and taphonomy of an Ediacaranfrond:Charnia from the Avalon Penin-sula of Newfoundland[C]//Vickers-Rich P, Komarower P. The Rise and Fall of the Ediacaran Biota. Geological Society Special Publications, 2007:237-257.
[11]	Serezhnikova E A. Vendian Hiemalora from Arctic Siberia inter-preted as holdfasts of benthic organisms[C]//Vickers-Rich P, Ko-marower P. The Rise and Fall of the Ediacaran Biota. Geological Society Special Publications, 2007:331-337.
[12]	Serezhnikova E A. Colonization of substrates:Vendian sedentary benthos[J]. Paleontol. J., 2010, 44:1560-1569.
[13]	Fedonkin M A, Gehling J G, Grey K, et al. The Rise of Animals:Evolution and Diversification of the Kingdom Animalia[M]. Johns Hopkins Univ. Press, 2007:1-326.
[14]	Laflamme M, Narbonne G M. Ediacaran fronds[J]. Palaeogeogr. Pa-laeoclimatol. Palaeoecol., 2008, 258:162-179.
[15]	Hofmann H J, O'brien S J, King A F. Ediacaran biota on Bonavista Peninsula, Newfoundland, Canada[J]. J. Paleontol., 2008, 82:1-36.
[16]	Burzynski G, Narbonne G M. The discs of Avalon:Relating dis-coid fossils to frondose organisms in the Ediacaran of Newfound-land, Canada[J]. Palaeogeogr. Palaeoclimatol. Palaeoecol., 2015,(doi.org/10.1016/j.palaeo.2015.01.014).
[17]	Peterson K J, Waggoner B, Hagadorn J W. A fungal analog for Newfoundland Ediacaran fossils[J]. Integr. Comp. Biol., 2003, 43(1):127-136.
[18]	Grazhdankin D, Gerdes G. Ediacaran microbial colonies[J]. Lethaia, 2007, 40:201-210.
[19]	Seilacher A. Vendobionta and Psammocorallia:lost constructions of Precambrian evolution[J]. J. Geol. Soc. London, 1992, 149:607-613.
[20]	Seilacher A, Grazhdankin D V, Legouta A. Ediacaran Biota:The dawn of animal life in the shadow of giant protists[J]. Paleontol. Res., 2003, 7:43-54.
[21]	Jensen S, Gehling J G, Droser M L, Grant S W F. A scratch circle origin for the medusoid fossil Kullingia[J]. Lethaia, 2002, 35:291-299.
[22]	Sun W, Hou X. Early Cambrian medusa from Chengjiang, Yun-nan, China[J]. Acta Palaeont. Sin., 1987, 26:257-270.
[23]	Narbonne G M, Myrow P, Landing E, et al. A Chondrophorine(Medusoid Hydrozoan) from the Basal Cambrian(Placentian) of Newfoundland[J]. J. Paleontol., 1991, 65:186-191.
[24]	Fedonkin M A. Promorphology of Vendian Radialia. in Stratigra-phy and Palaeontology of the Most Ancient Phanerozoic[C]//Iva-novsky A B, Ivanov A B. Moscow:Palaeontology Nauka, 1984:30-58.
[25]	Fedonkin M A. Precambrian metazoans:The problems of preserva-tion, systematics and evolution[J]. Philos. Trans. Roy. Soc. Lon-don, 1985, B311:27-45.
[26]	Zhao Y, Zhu M. Medusiform fossils of Kaili fauna from Taijiang, Guizhou[J]. Acta Palaeont. Sin., 1994, 33:272-280.
[27]	Tang F, Gao L Z, Yin C Y,et al. Largest macroalgae carbonaceous compressions in Doushantuo shales(551-580Ma) rooted as Edia-caran impression in limestones and sandstones[J]. Geological Re-view, 2014, 60(5):1009-1018.
[28]	Tang F, Bengtson S, Wang Y, et al. Eoandromeda and the origin of Ctenophora[J]. Evol. Dev., 2011, 13:408-414.
[29]	Wikipedia. Porpita porpita[EB/OL](2015-06-08)http://en.wikipe-dia.org/wiki/Porpita_porpita. 2015.
[30]	Wikipedia. Portuguese Man[EB/OL](2015-12-28)http://en.wiki-pedia.org/wiki/Portuguese_Man_o%27_War. 2015.
[31]	Gehling J G, Droser M L, Jensen S. Ediacaran fossil myths[C]//Ab-stracts with Programs-Geological Society of America, 2003, 35(6):495.
[32]	Gehling J G, Droser M L. How well do fossil assemblages of the Ediacara Biota tell time[J]. Geology, 2013, 41:447-450.

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华南伊迪卡拉纪类水母化石新发现

1. 国土资源部地层与古生物重点实验室, 北京 100037;2. 中国地质科学院地质研究所, 北京 100037;3. 四川省博物院, 四川 成都 610071;4. 浙江省自然历史博物馆, 浙江 杭州 310014;5. 厦门大学海洋环境科学学院, 福建 厦门 361005

Hydrozoan-like Ediacaran fossils from South China

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目录

1. 国土资源部地层与古生物重点实验室, 北京 100037;
2. 中国地质科学院地质研究所, 北京 100037;
3. 四川省博物院, 四川成都 610071;
4. 浙江省自然历史博物馆, 浙江杭州 310014;
5. 厦门大学海洋环境科学学院, 福建厦门 361005