Fish-Produced Markings: A Special Structure on Yellow River Point Bar

WANG Guan min; WEN Zhi feng; MA Zai ping

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Article Navigation > Acta Sedimentologica Sinica > 2003 > 21(4): 579-585

WANG Guan min, WEN Zhi feng, MA Zai ping. Fish-Produced Markings: A Special Structure on Yellow River Point Bar[J]. Acta Sedimentologica Sinica, 2003, 21(4): 579-585.

Citation:

WANG Guan min, WEN Zhi feng, MA Zai ping. Fish-Produced Markings: A Special Structure on Yellow River Point Bar[J]. Acta Sedimentologica Sinica, 2003, 21(4): 579-585.

Fish-Produced Markings: A Special Structure on Yellow River Point Bar

1.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou 510640;
2.
Postgraduate School of the Chinese Academy of Sciences, Beijing 100039;
3.
Earth Science and Information College, Petroleum University, Dongying Shandong 257061

Received Date: 2002-10-29
Rev Recd Date: 2003-03-21
Publish Date: 2003-12-10

Abstract

Many fish-produced markings are well developed on the argillaceous sediment overlying the Yellow River point bar.They are:(1)swimming trace, i.e.the simple wave line elongating in the linear or nonlinear form due to the scratch of the tail fin of fish;the simple line elongating in the linear form induced by anal fin;the parallel paired wave line on the argillaceous sediment caused by the vent ral fin;the intermittent discordant paired wave line caused by the swing of pectoral fin;and the combinations of wave lines above.(2)round or pit-like pascichnia, combined together in the grape, curved, disperse, linear, zig zag, banded form etc, produced by the fish grazinging.(3)fecal pellet.In this paper, the feature, genesis, and the environment related to the fish-produced markings are discussed in detail, and therefore inferring that the argillaceous sediment subsiding slowly is the prerequisite for the forming and preservation of fish-produced markings.
- The Yellow River,
- point bar,
- fish-produced,
- markings,
- swimming trace

References

[1]	Turek V. Fish and Amphibian trace fossils from Westphalian sediments of bohemia[J]. Paleontology, 1989,32: 623～643
[2]	胡斌,王冠忠,齐永安. 痕迹学理论与应用[M]. 江苏徐州:中国矿业大学出版社,1997. 32～63[Hu Bin, Wang Guanzhong, Qi Yong'an. The Theory of Ichnology and its Aplication[M].Xuzhou Jiangsu: China University of Mining Technology Press,1997.32～63]
[3]	Anderson A M. Fish trails from the Early Permian of South Africa[J]. Palaeontology, 1976,19:397～409
[4]	Archer A W, Maples C G. Trace-fossil distribution acros a marine-to-nonmarine gradient in the Pennsylvanian of southwestern Indiana[J]. Journal of Paleontology, 1984,58:448～466
[5]	Bainbridge R. Caudal fin and body movement in the propulsion of some fish[J]. Journal of Experimental Biology, 1962, 40:32～56
[6]	Higgs R. Fish trail in the Upper Carboniferous of Sourth-West England[J]. Paleontology, 1988, 31:255～272
[7]	Nelson C H. Grey whale and walras feeding excauation on the Bering shelf[J]. Sedimentary Petrography, 1987, 57(3):419～430
[8]	Stanley D J. Fish-produced markings on the outer continental margin east of the middle Atlantic states[J]. Journal of Sedimentary Petrology, 1971,41: 159～170
[9]	Warren A. Queensland trace fossils pose a 230 million old problem[J]. Australian Natural History, 1972. 160～162
[10]	尹赞勋. 记鱼粪化石[A]. 1945. 见:尹赞勋文集[C]. 北京:科学出版社,1984.101～105[Yin Zanxun. The note for fish coprolites[A]. In: Yin Zanxun's Corpus[C]. Beijing: Science Press, 1984.101～105]
[11]	卢宗盛,陈斌. 陕西横山晚三叠纪鱼类游泳遗迹(Undichna)的发现[J].古生物学报,1998,37(1):77～82[Lu Zhongsheng, Chen Bin. Discovery of late Triassic fish trails (Undichna) in Hengshan county, Shaanxi,China[J]. Acta Paleontologica Sinica, 1998, 37(1): 77～82 ]
[12]	钟建华,马在平. 泥砂钟乳-一种特殊的沉积构造[J]. 科学通报,1997,42(17):1 853～1 856[Zhong Jianhua, Ma Zaiping. The silt stalactite:a peculiar kind of sedimentary structures[J]. Chinese Science Bulletin, 1997, 42(23):1 974～1 977]
[13]	钟建华,马在平. 黄河三角洲胜利Ⅰ号心滩的研究[J]. 沉积学报,1998,16(3):38～43[Zhong Jianhua, Ma Zaiping. The study to Shengli I point bar on Yellow river delta[J]. Acta Sedimentologica Sinica, 1998, 16(3): 38～43]
[14]	钟建华,马在平. 黄河三角洲变形层理的研究[J]. 沉积学报,1998,16(1):45～49[Zhong Jianhua, Ma Zaiping. Study on the deformation bedding in the delta of Yellow river[J]. Acta Sedimentologica Sinica. 1998, 16(1):45～49]
[15]	钟建华,周瑶琪. 黄河三角洲平原上的泄气坑的发现[J]. 科学通报,1999,44(11):1 026～1 028[Zhong Jianhua, Zhou Yaoqi. The discovery of air-discharge holes on the Yellow river delta[J]. Chinese Science Bulletin,1999, 44(11):1 026～1 028]
[16]	钟建华,候启军,钟延秋. 黄河三角洲(泄水)包卷层理的成因研究[J]. 地质论评,1999,45(3):306～312[Zhong Jianhua, Hou Qijun, Zhong Yanqiu. Genesis of the (sluicing)convolute bedding in the Yellow River Delta[J]. Geological Review,1999, 45(3): 306～312]
[17]	钟建华,李理. 黄河断流后三角洲(水上平原)的滑塌构造研究[J]. 沉积学报,2000,18(1):7～10[Zhong Jianhua, Li Li. Study of slump structure on the Yellow river delta during its zero[J]. Acta Sedimentologica Sinica, 2000, 18(1):7～10]
[18]	钟建华,倪晋仁,吴孔友,等. 黄河三角洲上特殊侵蚀沟槽的研究[J]. 高校地质学报,2000,6(3):462～468[Zhong Jianhua, Ni Jinren, Wu Kongyou, et al. Unusual erosion channels in Yellow river delta: features and genesis[J].Geological Journal of China Universities, 2000, 6(3): 452～468]
[19]	Zhong Jianhua, Wu Kongyou, Ni Jinren. A preliminary study of rill marks in the Yellow river delta[J].Acta Sedimentologica Sinica, 2000,18(4):527～533
[20]	钟建华,倪晋仁,宋维奇,等. 黄河三角洲上的冰成隆丘的研究[J]. 沉积学报,2001,19(3):357～362[Zhong Jianhua, Ni Jinren, Song Weiqi, et al. Study on the ice-induced heaving in Yellow river delta[J]. Acta Sedimentologica Sinica, 2001, 19(3): 357～362]
[21]	钟建华,倪晋仁,沈晓华,等. 黄河下游壶穴的研究[J]. 地质学报, 2002, 76(2):36～48[Zhong Jianhua, Ni Jinren, Shen Xiaohua, et al. Study of potholes in the lower reaches of the Yellow River [J]. Acta Geologica Sinica, 2002,76(2): 36～48]
[22]	钟建华,王冠民,王夕宾,等. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报,2002,20(2):261～266[Zhong Jianhua, Wang Guanmin, Wang Xibin, et al. Study on the ice-induced slump and subsidence structures in the lower course of yellow river[J]. Acta Sedimentologica Sinica, 2002, 20(2): 261～266]
[23]	Zhong Jianhua,Shen Xiaohua, Ni Jinren. The Shengli I point bar on Yellow river delta: Three-Dimensional structures and their evolution[J]. Geologica Sinica(English edition),2002,76(4):463～477
[24]	钟建华,王洪宝. 黄河下游河道的冻裂研究[J]. 沉积学报,2002,20(2):650～655[Zhong Jianhua, Wang Hongbao. Study on the frozen cracks in the lower reaches of Yellow river[J]. Acta Sedimentologica Sinica, 2002,20(2):650～655]

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Fish-Produced Markings: A Special Structure on Yellow River Point Bar

1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou 510640;

2. Postgraduate School of the Chinese Academy of Sciences, Beijing 100039;

3. Earth Science and Information College, Petroleum University, Dongying Shandong 257061

Received Date: 2002-10-29

Rev Recd Date: 2003-03-21

Publish Date: 2003-12-10

Key words:

Abstract: Many fish-produced markings are well developed on the argillaceous sediment overlying the Yellow River point bar.They are:(1)swimming trace, i.e.the simple wave line elongating in the linear or nonlinear form due to the scratch of the tail fin of fish;the simple line elongating in the linear form induced by anal fin;the parallel paired wave line on the argillaceous sediment caused by the vent ral fin;the intermittent discordant paired wave line caused by the swing of pectoral fin;and the combinations of wave lines above.(2)round or pit-like pascichnia, combined together in the grape, curved, disperse, linear, zig zag, banded form etc, produced by the fish grazinging.(3)fecal pellet.In this paper, the feature, genesis, and the environment related to the fish-produced markings are discussed in detail, and therefore inferring that the argillaceous sediment subsiding slowly is the prerequisite for the forming and preservation of fish-produced markings.

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Reference (24)

[1]	Turek V. Fish and Amphibian trace fossils from Westphalian sediments of bohemia[J]. Paleontology, 1989,32: 623～643
[2]	胡斌,王冠忠,齐永安. 痕迹学理论与应用[M]. 江苏徐州:中国矿业大学出版社,1997. 32～63[Hu Bin, Wang Guanzhong, Qi Yong'an. The Theory of Ichnology and its Aplication[M].Xuzhou Jiangsu: China University of Mining Technology Press,1997.32～63]
[3]	Anderson A M. Fish trails from the Early Permian of South Africa[J]. Palaeontology, 1976,19:397～409
[4]	Archer A W, Maples C G. Trace-fossil distribution acros a marine-to-nonmarine gradient in the Pennsylvanian of southwestern Indiana[J]. Journal of Paleontology, 1984,58:448～466
[5]	Bainbridge R. Caudal fin and body movement in the propulsion of some fish[J]. Journal of Experimental Biology, 1962, 40:32～56
[6]	Higgs R. Fish trail in the Upper Carboniferous of Sourth-West England[J]. Paleontology, 1988, 31:255～272
[7]	Nelson C H. Grey whale and walras feeding excauation on the Bering shelf[J]. Sedimentary Petrography, 1987, 57(3):419～430
[8]	Stanley D J. Fish-produced markings on the outer continental margin east of the middle Atlantic states[J]. Journal of Sedimentary Petrology, 1971,41: 159～170
[9]	Warren A. Queensland trace fossils pose a 230 million old problem[J]. Australian Natural History, 1972. 160～162
[10]	尹赞勋. 记鱼粪化石[A]. 1945. 见:尹赞勋文集[C]. 北京:科学出版社,1984.101～105[Yin Zanxun. The note for fish coprolites[A]. In: Yin Zanxun's Corpus[C]. Beijing: Science Press, 1984.101～105]
[11]	卢宗盛,陈斌. 陕西横山晚三叠纪鱼类游泳遗迹(Undichna)的发现[J].古生物学报,1998,37(1):77～82[Lu Zhongsheng, Chen Bin. Discovery of late Triassic fish trails (Undichna) in Hengshan county, Shaanxi,China[J]. Acta Paleontologica Sinica, 1998, 37(1): 77～82 ]
[12]	钟建华,马在平. 泥砂钟乳-一种特殊的沉积构造[J]. 科学通报,1997,42(17):1 853～1 856[Zhong Jianhua, Ma Zaiping. The silt stalactite:a peculiar kind of sedimentary structures[J]. Chinese Science Bulletin, 1997, 42(23):1 974～1 977]
[13]	钟建华,马在平. 黄河三角洲胜利Ⅰ号心滩的研究[J]. 沉积学报,1998,16(3):38～43[Zhong Jianhua, Ma Zaiping. The study to Shengli I point bar on Yellow river delta[J]. Acta Sedimentologica Sinica, 1998, 16(3): 38～43]
[14]	钟建华,马在平. 黄河三角洲变形层理的研究[J]. 沉积学报,1998,16(1):45～49[Zhong Jianhua, Ma Zaiping. Study on the deformation bedding in the delta of Yellow river[J]. Acta Sedimentologica Sinica. 1998, 16(1):45～49]
[15]	钟建华,周瑶琪. 黄河三角洲平原上的泄气坑的发现[J]. 科学通报,1999,44(11):1 026～1 028[Zhong Jianhua, Zhou Yaoqi. The discovery of air-discharge holes on the Yellow river delta[J]. Chinese Science Bulletin,1999, 44(11):1 026～1 028]
[16]	钟建华,候启军,钟延秋. 黄河三角洲(泄水)包卷层理的成因研究[J]. 地质论评,1999,45(3):306～312[Zhong Jianhua, Hou Qijun, Zhong Yanqiu. Genesis of the (sluicing)convolute bedding in the Yellow River Delta[J]. Geological Review,1999, 45(3): 306～312]
[17]	钟建华,李理. 黄河断流后三角洲(水上平原)的滑塌构造研究[J]. 沉积学报,2000,18(1):7～10[Zhong Jianhua, Li Li. Study of slump structure on the Yellow river delta during its zero[J]. Acta Sedimentologica Sinica, 2000, 18(1):7～10]
[18]	钟建华,倪晋仁,吴孔友,等. 黄河三角洲上特殊侵蚀沟槽的研究[J]. 高校地质学报,2000,6(3):462～468[Zhong Jianhua, Ni Jinren, Wu Kongyou, et al. Unusual erosion channels in Yellow river delta: features and genesis[J].Geological Journal of China Universities, 2000, 6(3): 452～468]
[19]	Zhong Jianhua, Wu Kongyou, Ni Jinren. A preliminary study of rill marks in the Yellow river delta[J].Acta Sedimentologica Sinica, 2000,18(4):527～533
[20]	钟建华,倪晋仁,宋维奇,等. 黄河三角洲上的冰成隆丘的研究[J]. 沉积学报,2001,19(3):357～362[Zhong Jianhua, Ni Jinren, Song Weiqi, et al. Study on the ice-induced heaving in Yellow river delta[J]. Acta Sedimentologica Sinica, 2001, 19(3): 357～362]
[21]	钟建华,倪晋仁,沈晓华,等. 黄河下游壶穴的研究[J]. 地质学报, 2002, 76(2):36～48[Zhong Jianhua, Ni Jinren, Shen Xiaohua, et al. Study of potholes in the lower reaches of the Yellow River [J]. Acta Geologica Sinica, 2002,76(2): 36～48]
[22]	钟建华,王冠民,王夕宾,等. 黄河下游冰成滑塌与塌陷构造的研究[J]. 沉积学报,2002,20(2):261～266[Zhong Jianhua, Wang Guanmin, Wang Xibin, et al. Study on the ice-induced slump and subsidence structures in the lower course of yellow river[J]. Acta Sedimentologica Sinica, 2002, 20(2): 261～266]
[23]	Zhong Jianhua,Shen Xiaohua, Ni Jinren. The Shengli I point bar on Yellow river delta: Three-Dimensional structures and their evolution[J]. Geologica Sinica(English edition),2002,76(4):463～477
[24]	钟建华,王洪宝. 黄河下游河道的冻裂研究[J]. 沉积学报,2002,20(2):650～655[Zhong Jianhua, Wang Hongbao. Study on the frozen cracks in the lower reaches of Yellow river[J]. Acta Sedimentologica Sinica, 2002,20(2):650～655]

Fish-Produced Markings: A Special Structure on Yellow River Point Bar

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