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Cambrian ichnofossils from the Zhoujieshan Formation (Quanji Group) overlying tillites in the northern margin of the Qaidam Basin, NW China
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  • 作者:Yue Wang (1)
    Xunlian Wang (2)
    Ye Wang (2)

    1. School of Resources and Environments
    ; Guizhou University ; Guiyang ; 550025 ; China
    2. School of Earth Sciences and Resources
    ; China University of Geosciences ; Beijing ; 100083 ; China
  • 关键词:Cambrian ; ichnofossil ; Zhoujieshan Formation ; Quanji Group ; Daqaidam ; NW China
  • 刊名:Journal of Earth Science
  • 出版年:2015
  • 出版时间:April 2015
  • 年:2015
  • 卷:26
  • 期:2
  • 页码:203-210
  • 全文大小:944 KB
  • 参考文献:1. A, Y S (2003) On the Quanji Movement. Northwestern Geology 36: pp. 30-34
    2. Brasier, M D, Cowie, J W, Taylor, M (1994) Decision on the Precambrian-Cambrian Boundary Stratotype. Episodes 17: pp. 3-8
    3. Bromley, R G, Asgaard, U (1991) Ichnofacies: A Mixture of Taphofacies and Biofacies. Lethaia 24: pp. 153-163 CrossRef
    4. Crimes, T P (1992) Changes in the Trace Fossil Biota across the Proterozoic-Phanerozoic Boundary. Journal of the Geological Society 149: pp. 637-646 CrossRef
    5. Crimes, T P, Anderson, M M (1985) Trace Fossils from Late Precambrian Early Cambrian Strata of Southeastern Newfoundland (Canada): Temporal and Environmental Implications. Journal of Paleontology 59: pp. 310-343
    6. Crimes, T P, Legg, I, Marcos, A Late Precambrian-Lower Cambrian Trace Fossils From Spain. In: Crimes, T P, Harper, J C eds. (1976) Trace Fossils 2. Seel House Press, Liverpool, pp. 91-138
    7. Gehling, J G, Jensen, S, Droser, M L (2001) Burrowing below the Basal Cambrian GSSP, Fortune Head, Newfoundland. Geological Magazine 138: pp. 213-218 CrossRef
    8. Hoffman, P F, Schrag, D P (2002) The Snowball Earth Hypothesis: Testing the Limits of Global Change. Terra Nova 14: pp. 129-155 CrossRef
    9. Jensen, G, Grant, S W F (1993) Implications from Trace Fossils for the Vendian-Cambrian Boundary in the Tornetr盲sk Formation, Northern Sweden. Lundadagarna I Historisk Geologi och Paleontologi. Lund Publications in Geology 109: pp. 15-16
    10. Jensen, S (1997) Trace Fossils from the Lower Cambrian Mickwitzia Sandstone, South-Central Sweden. Fossils and Strata 42: pp. 111
    11. Jiang, G, Kennedy, M J, Christie-Blick, N (2006) Stratigraphy, Sedimentary Structures, and Texture of the Late Neoproterozoic Doushantuo Cap Carbonate in South China. Journal of Sedimentary Research 76: pp. 978-995 CrossRef
    12. Jiang, G, Shi, X, Zhang, S (2011) Stratigraphy and Paleogeography of the Ediacaran Doushantuo Formation (ca. 635-551 Ma) in South China. Gondwana Research 19: pp. 831-849 CrossRef
    13. Landing, E (1994) Precambrian-Cambrian Boundary Global Stratotype Ratified and a New Perspective of Cambrian Time. Geology 22: pp. 179-182 CrossRef
    14. Li, H K, Lu, S N, Wang, H C (2003) The Geological Records of the Supcontinental Breakup in the Neoprotozoic, the Quanji Group in the Northern Margin of Qaidam Basin, Qinghai. Geologial Survey and Research 26: pp. 27-37
    15. Li, R H (1991) Trace Fossils and the Sinian-Cambrian Boundary in the Meishucun Section, Eastern Yunnan, China, and Their Relations to Small Shelly Fossils. Geological Review 37: pp. 214-220
    16. Li, R H, Yang, S P, Li, W Q (1997) Trace Fossils from Sinian-Cambrian Boundary Strata in China. Geological Publishing House, Beijing
    17. Li, Y P, McWilliams, M, Tan, C Z (1986) The Paleomagnetic Study of the Quanji Group (Sinian) of the Chaidam Terrane. Xinjiang Geology 6: pp. 35-40
    18. Lu, S N, Yu, H F, Jin, W (2002) Microcontinents on the Eastern Margin of Tarim Paleocontinent. Acta Petorlogica et Mineralogica 21: pp. 317-326
    19. Lu, S N, Li, H, Zhang, C (2008) Geological and Geochronological Evidence for the Precambrian Evolution of the Tarim Craton and Surrounding Continental Fragments. Precambrian Research 160: pp. 94-107 CrossRef
    20. Luo, H L, Jiang, Z W, Wu, X C (1991) The Global Biostratigraphical Correlation of Meishucunian Stage and the Precambrian-Cambrian Boundary. Science China Series B 34: pp. 377-384
    21. Pemberton, S G, Frey, R W (1982) Trace Fossils Nomenclature and the Planolites-Palaeophycus Dilemma. Journal of Paleontology 56: pp. 843-881
    22. Peng, S C (2005) Towards a New Global Subdivision of the Cambrian System. Journal of Stratigraphy 29: pp. 171-177
    23. Qian, Y, Zhu, M Y, He, T Q (1996) New Investigation of Precambrian-Cambrian Boundary Sections in Eastern Yunnan. Acta Micopalaeontologica Sinica 13: pp. 225-240
    24. Qian, Y, Zhu, M Y, Li, G X (2002) A Supplemental Precambrian-Cambrian Boundary Global Stratotype Section in SW China. Acta Palaeontologica Sinica 41: pp. 19-26
    Regional Strata of Northwest China, Qinghai Volume. Geological Publishing House, Beijing
    25. Seilacher, A (1955) Spuren und Fazies im Unterkambrium. Beitr盲ge Zur Kenntnis des Kambrium in der Salt Range (Pakistan). Abhandlungen der Akademie der Wissenschadten und der Literatur, Mainz, Mathematisch-Naturwissenschadtliche Klass 10: pp. 373-399
    26. Seilacher, A Biogenic Sedimentary Structures. In: Imbrie, J, Newell, N D eds. (1964) Approaches to Paleoceology. Wiley, New York, pp. 296-316
    27. Seilacher, A (1967) Bathymetry of Trace Fossils. Maine Geology 5: pp. 413-428 CrossRef
    28. Seilacher, A Cruziana Stratigraphy of 鈥淣on-Fossiliferous鈥?Paleozoic Sandstone. In: Crimes, T P, Harper, J C eds. (1970) Trace Fossils. Seel House Press, Liverpool, pp. 447-477
    29. Seilacher, A (1985) Trilobite Palaeobiology and Substrate Relationships. Transactions of the Royal Society of Edinburgh 76: pp. 231-237 CrossRef
    30. Shen, B, Xiao, S, Dong, L (2007) Problematic Macro-Fossils from Ediacaran Successions in the North China and Chaidam Blocks: Implications for Their Evolutionary Roots and Biostratigraphic Significance. Journal of Paleontology 81: pp. 1396-1411 CrossRef
    31. Shen, B, Xiao, S, Zhou, C (2010) Carbon and Sulfur Isotope Chemostratigraphy of the Neoproterozoic Quanji Group of the Chaidam Basin, NW China: Basin Stratification in the Aftermath of an Ediacaran Glaciations Postdating the Shuram Event?. Precambrian Research 177: pp. 241-252 CrossRef
    32. Steiner, M, Li, G X, Qian, Y (2007) Neoproterozoic to Early Cambrian Small Shelly Fossil Assemblages and a Revised Biostratigraphic Correlation of the Yangtze Platform (China). Palaeogeography, Palaeoclimatology, Palaeoecology 254: pp. 67-99 CrossRef
    33. Sun, C R, La, J D, Wang, W Sinian-Middle Silurian. In: Sun, C R, Chen, G L, Li, Z R eds. (1997) Multiple Classification and Correlation of the Stratigraphy of China (63): Stratigraphy (Lithostratigraphic) of Qinghai Province. China University of Geosciences Press, Wuhan, pp. 59-69
    34. Sun, W G, Feng, W M (1999) Re-Selecting the Global Stratotype for the Precambrian-Cambrian Boundary. Geoscience 13: pp. 139-140
    35. Tangri, S K, Bhargava, O N, Pande, A C (2003) Late Precambrian-Early Cambrian Trace Fossils from Tethyan Himalaya, Bhutan and Their Bearing on the Precambrian-Cambrian Boundary. Journal Geological Society of India 62: pp. 708-716
    36. Walter, M R, Elphistone, R, Heys, G R (1989) Proterozoic and Early Cambrian Trace Fossils from the Amadeus and Georgina Basins, Central Australia. Alcheringa 13: pp. 209-256 CrossRef
    37. Wang, Y (2004) Some Trace Fossils after the Frasnian-Famennian Extinct in Dushan Area, Southern Guizhou Province, China. Acta Palaeontologica Sinica 43: pp. 132-141
    38. Wang, Y (2007) Arthropods Tracks in Kaili Ichnocoenosis from Lower-Middle Cambrian Kaili Formation in Jianhe County, Guizhou Province, China. Geologial Review 53: pp. 539-555
    39. Wang, Y, Wang, P L (2006) Ichnofossil Treptichnus from the Kaili Formation at Taijiang County, Guizhou Province. Geological Review 52: pp. 1-9
    40. Wang, Y, Zhou, Z C, Zhao, Y L (2006) Relationship between Ichnocoenosis and Sedimentary Environment in the Lower-Middle Cambrian Kaili Formation of Taijiang, Guizhou, China. Acta Palaeontologica Sinica 45: pp. 243-251
    41. Wang, Y S (1977) Confirmatoin of the Hongtiegou Glacial Tillite Layer in Quanji Mountain, Qinghai. Geology of Northwest China. pp. 36-39
    42. Wang, Y S, Zhuang, Q X, Shi, C Y (1980) Quanji Group along the Northern Margin of Qaidam Basin. Research on Precambrian Geology, Sinian Suberathem in China. Tianjin Science and Technology Press, Tianjin, pp. 214-229
    43. Wetzel, A, Bromley, F (1996) Re-Evalution of the Ichnogenus Helminthopsis: A New Look at the Type Material. Palaeontology 39: pp. 1-19
    44. Xin, H T, Hao, G J, Wang, H C (2002) New Idea on Presinian Strata in the Northern Margin of Qaidam Massif. Progress in Precambrian Research 25: pp. 113-119
    45. Yang, S P, Wang, X C (1991) Middle Cambrian Hsuchuangian Trace Fossils from Southern North China Platform and Their Sedimentological Significance. Acta Palaeontologica Sinica 30: pp. 74-89
    46. Yang, S P, Zhang, J P, Yang, M F (2004) Trace Fossils of China. Science Press, Beijing
    47. Ying, T F, Zhuang, Q X, He, G T Stratigraphy. In: Li, D F, Lun, Z Q, Guo, J Y eds. (1991) Regional Geology of Qinghai Province. Geological Publishing House, Beijing, pp. 8-40
    48. Young, F G (1972) Early Cambrian and Older Trace Fossils from the Southern Cordillera of Canada. Canadian Journal of Earth Science 9: pp. 1-17 CrossRef
    49. Zhang, L, Ba, J, Chen, N S (2012) U-Ph Age Spectra and Trace Elements of Detrital Zircon from Quanji Group Implications for Thermal Events and Early Evolution in the Basement. Earth Science鈥擩ournal of China University of Geosciences 37: pp. 28-37
    50. Zhang, L Y, Qiu, S Y, Hua, H (1993) Symbiotic Characteristics between Tube-Shaped Fossils and Stromatolites in the Precambrian, and Their Significances. Journal of Hebei College of Geology 16: pp. 315-320
    51. Zhu, M (1997) Precambrian-Cambrian Trace Fossils from Eastern Yunnan, China: Implications for Cambrian Explosion. Bulletin of National Museum of Natural Science 10: pp. 275-321
    52. Zhu, M, Zhang, J, Yang, A (2007) Integrated Ediacaran (Sinian) Chronostratigraphy of South China. Palaeogeography, Palaeoclimatology, Palaeoecology 254: pp. 7-61 CrossRef
  • 刊物主题:Earth Sciences, general; Geotechnical Engineering & Applied Earth Sciences; Biogeosciences; Geochemistry; Geology;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1867-111X
文摘
The Quanji Group is composed of siliciclastics and carbonates and was deposited on a relatively stable block, in the northern margin of the Qaidam Basin, NW China. It is one of the research hotspots in the Qilian-Qinling-Kunlun tectonic zones. However, it has long been argued whether the upper Quanji Group should be assigned to the Precambrian or the Cambrian for lack of convincing fossil evidence. The discovery of ichnofossils, including Rusophycus, Cruziana, Dimorphichnus, Treptichnus, Skolithos, Arenicolites, Palaeophycus, and Helminthopsis, indicates that the upper member of the Zhoujieshan Formation (top Quanji Group) is Cambrian in age, and at least above the Treptichnus (Phycodes) pedum Biozone, the lowermost biozone in the Cambrian. The lower member of the Zhoujieshan Formation should belong to the Cambrian. During the time when the upper member of the Zhoujieshan Formation was deposited, the northern margin of the Qaidam Basin was dominated by the Cruziana Ichnofacies, characterizing a lower-energy shelf (shallow) sea environment with moderate-rich oxygen contents. In addition, the conglomerates in the Hongtiegou Formation of the Quanji Group underlying the Zhoujieshan Formation were generally regarded as tillites. However, the dolostones of the lower member of the Zhoujieshan Formation are, in lithology and geochemistry, different from the typical cap-dolostones of the Doushantuo Formation in South China, so it is necessary to further study the origins of the lower member of the Zhoujieshan Formation and the conglomerates of the Hongtiegou Formation.

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