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华南泥盆纪遗迹化石及遗迹相*

DOI: 10.7605/gdlxb.2011.04.004, PP. 397-418

Keywords: 遗迹化石,遗迹相,泥盆纪,古环境,华南

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Abstract:

通过对华南泥盆系6条剖面(四川北川甘溪、广西横县六景、广西桂林杨堤、贵州独山大河口—白虎坡、贵州贵阳乌当、四川广元后高坪)的遗迹沉积学系统研究,鉴定和描述遗迹化石15属24种,包括Arenicolitescarbonaria,Arenicolitesisp.,Chondritescf.intricatus,Chondritesfenxiangensis,Chondritesfilifalx,Chondritesisp.,Chondritesmaqianensis,Circulichnisisp.,Dushanichnusdahekouensis,Diplocraterionparallelum,Rusophycuslungmenshanensis,?Helminthopsisisp.,Palaeophycustubularis,Palaeophycuscurvatus,Phycodespalmatus,Planolitesbeverleyensis,Planolitesisp.,Planoliteskwangsiensis,Rosseliasocialis,Rhizocoralliumjenense,Rhizocoralliumisp.,Skolithoslinearis,Thalassinoidesisp.,Zoophycosisp.。根据遗迹化石之间的共生组合关系、实体化石特征和其他相标志,识别出4种遗迹相:Skolithos,Rhizocorallium,Cruziana和Zoophycos遗迹相。Skolithos遗迹相主要发育于浪控型海岸体系、潮控型海岸体系和障壁岛—潟湖沉积体系的高能沉积区;Rhizocorallium遗迹相主要发育于潮控型海岸体系和障壁岛—潟湖沉积体系的低能沉积区;Cruziana遗迹相发育在浅海陆棚、具有丰富的生物及食物的砂泥岩和灰岩为主的低能沉积区;Zoophycos遗迹相沿泥岩和泥灰岩发育的滨外沉积区分布。华南泥盆纪遗迹相从早泥盆世到晚泥盆世的演替规律是从Skolithos遗迹相→Rhizocorallium遗迹相→Cruziana遗迹相→Zoophycos遗迹相→Rhizocorallium遗迹相。早泥盆世晚期以后华南泥盆纪同时期的遗迹相自西南向东北的空间变化规律则表现为Zoophycos遗迹相→Cruziana遗迹相→Rhizocorallium遗迹相→Skolithos遗迹相。

References

[1]  杨式溥.1986.遗迹相及其古环境的意义[J].地球科学——中国地质大学学报,11(5):455-463.
[2]  杨式溥.1989.广州花县晚泥盆世和早石炭世遗迹化石[J].地球科学——中国地质大学学报,14(6):573-580.
[3]  杨式溥,胡昌铭,孙永传.1987.汉阳锅顶山地区晚泥盆世遗迹化石的发现及其意义[J].地球科学——中国地质大学学报,12(1):1-8.
[4]  杨式溥,张建平,杨美芳.2004.中国遗迹化石[M].北京: 科学出版社,56-107.
[5]  张立军,龚一鸣.2009.四川后高坪地区晚泥盆世植物和遗迹化石的新发现[J].地层学杂志,33(2):138-146.
[6]  张欣平,卿上康.1988.湖南新化上泥盆统的遗迹化石及其沉积环境[J].石油与天然气地质,9(3):252-260.
[7]  张欣平,张纯臣,王大任.1986.湘西北地区志留系泥盆系的痕迹化石[J].湖南地质,5(2):49-59.
[8]  赵锡文.1985.晚泥盆世中国古地理图[M].见: 王鸿祯.中国古地理图集.北京: 地图出版社,65-66.
[9]  周志澄.1996.广西横县六景民塘组Treptichnus的发现及其环境意义[J].古生物学报,35(1):123-128.
[10]  Bischoff B.1968.Zoophycos a polychaete annelid,Eocene of Greece[J].Journal of Paleontology,42: 1439-1443.
[11]  Bottjer D J,Droser M L,Jablonski D.1987.Bathymetric trends in the history of trace fossils[C].In: Bottjer D J(ed).New Concepts in the Use of Biogenic Sedimentary Structures for Palaeoenvironmental Interpretation.Pacific Section,Society of Economic Paleontologists and Mineralogists,57-65.
[12]  Bromley R G.1990.Trace Fossils: Biology and Taphonomy[M].London: Unwin Hyman,280.
[13]  Bromley R G,Asgaard U.1993.Two bioerosion ichnofacies produced by early and later burial associated with sea-level change[J].Geologische Rundschan,82: 872-874.
[14]  Bromley R G,Pemberton S G,Rahmani R A.1984.A Cretaceous woodground: The Teredolites ichnofaices[J].Journal of Paleontology,58: 488-498.
[15]  Buatois L A,Mangano M G.1995.The paleoenvironmental and paleoecological significance of the lacustrine Mermia ichnofacies: An archetypical subaqueous nonmarine trace fossil assemblage[J].Ichnos,4: 151-161.
[16]  Crimes T P.1987.Trace fossils and correlation of Late Precambrian and Early Cambrian strata[J].Geological Magazine,124: 97-119.
[17]  Droser M L,Bottjer D J,Sheehan P M, et al.2000.Decoupling of taxonomic and ecologic severity of Phanerozoic marine mass extinctions[J].Geology,28(8):675-678.
[18]  Ekdale A A,Bromley R G.1984.Comparative ichnology of shelf-sea and deep-sea chalk[J]. Journal of Paleontology,58: 322-332.
[19]  Ekdale A A,Lewis D W.1991.The New Zealand Zoophycos revisitied:Morphology,ethology,and paleoecology[J].Ichnos,1(3):183-194.
[20]  Fillion D,Pickerill R K.1984.On Arthraria antiquate Billings,1872 and its relationship to Diplocraterion Torell,1870,and Bifungites Desio,1940[J].Journal of Paleontology,58(3):683-696.
[21]  Frey R W,Pemberton S G.1987.The Psilonichnus ichnocenose,and its relaionship to adjacent marine and nonmarine ichnocoenoses along the Georgia coast[J].Bulletin of Canadian Petroleum Geology,35: 333-357.
[22]  Frey R W,Seilacher A.1980.Uniformity in marine invertebrate ichnology[J].Lethaia,13: 183-207.
[23]  Fürsich F T.1974.On Diplocraterion Torell 1870 and the significance of morphological features in vertical,spreiten-bearing,U-shaped trace fossils[J].Journal of Paleontology,48: 952-962.
[24]  Fu S.1991.Funktion,Verhalten and Einteilung fucoider and lophocteniider Lebensspuren[J].Courier Forschungsinstitut Senckenberg,135: 1-79.
[25]  Kotake N.1991.Non-selective surface deposit feeding by the Zoophycos producers[J].Lethaia,24: 379-385.
[26]  MacEachern J A,Pemberton S G,Gingras M K, et al. 2007.The ichnofacies paradigm: A fifty-year retrospective[C].In: Miller Ⅲ(ed).Trace Fossils Concepts,Problems,Prospects.Amesterdam: Elsevier Press,110-134.
[27]  Osgood R G.1970.Trace fossils of the Cincinnati area[J].Paleontogr America,6(41):81-144.
[28]  Pemberton S G,Frey R W.1982.Trace fossil nomenclature and the Planolithoes-Plaeophycus dilemma[J].Journal of Paleontology,56(4):843-881.
[29]  Seilacher A.1953a.Sutdien zur palichnologie.Ⅰ.Uber die methoden der palichnologie[J].Neues Jahrbuch fur Geologie und Paleontologies,Abhandlugnen,98: 87-124.
[30]  Seilacher A.1953b.Uber die methoden der palichnologie,Ⅱ,Studien von Palichnologie[J].Neues Jahrbuch fur Geologie und Paleontologies,Abhandlugnen,96: 421-452.
[31]  Seilacher A.1967.Bathymetry of trace fossils[J].Marine Geology,5: 413-428.
[32]  Seilacher A.1970.Cruziana stratigraphy of ‘non-fossiliferous Palaeozoic sandstones[J].Geological Journal,3: 447-476.
[33]  Seilacher A.1990.Aberrations in bivalve evolution related to photo-and chemosymbiosis[J].Historical Biology,3(4):289-311.
[34]  Smith R M H,Mason T R,Ward J D.1993.Flash-flood sediments and ichnofacies of the Later Pleistocene Homeb Silts,Kuiseb River,Namibia[J].Sedimentary Geology,85: 579-599.
[35]  Wetzel A,Werner F.1981.Morphology and ecological significance of Zoophycos in deep-sea sediments of NW Africa[J].Palaeogeography,Palaeoclimatology,Palaeoecology,32:185-212.
[36]  白顺良.1998.泥盆纪弗拉阶—法门阶事件的化学—生物地层学研究[J].北京大学学报(自然科学版),34(2-3): 363-369.
[37]  陈代钊,陈其英.1994.华南泥盆纪沉积演化及海水进退规程[J].地质科学,29(3):246-255.
[38]  陈云明,王建,白培荣,等.2005.贵阳乌当泥盆系马鬃岭组上部地层中的遗迹化石[J].贵州地质,22(4):273-280.
[39]  龚一鸣.1985.湘西南早—中泥盆世碎屑岩地层岩相及古地理[J].湖南地质,4(4):26-38.
[40]  龚一鸣.1987.湘西南早—中泥盆世碎屑岩地层遗迹化石与沉积环境的关系[J].岩相古地理文集,4: 98-116.
[41]  龚一鸣.2004.遗迹化石Chondrites的指相意义和阶层分布[J].古生物学报,43(1):94-102.
[42]  龚一鸣,李保华,吴诒.2002.广西泥盆系弗拉阶一法门阶之交分子地层研究[J].自然科学进展,12(3):292-297.
[43]  龚一鸣,刘本培,肖诗宇,等.1997.中国海相泥盆纪遗迹组构及其与沉积层序的关系[J].地球科学——中国地质大学学报,22(2):123-128.
[44]  龚一鸣,徐冉,汤中道,等.2005.晚泥盆世F-F之交菌藻微生物繁荣与集群灭绝的关系: 来自碳同位素和分子化石的启示[J].中国科学(D辑),35(2):140-148.
[45]  顾德兴.2000.普通生物学[M].北京: 高等教育出版社,1-348.
[46]  何远碧,高卫东,张廷山.1985.黔南桑朗地区上二叠统和泥盆系中的遗迹化石及其沉积环境[J].沉积学报,3(2):75-83.
[47]  李博,杨栋,林鹏.2000.生态学[M].北京: 高等教育出版社,1-416.
[48]  林文球,林宗文,王洪峰.1986.四川龙门山平驿铺组沉积环境及U形蹼状构造潜穴探讨[J].矿物岩石,6(3):121-129.
[49]  廖卫华.2001.中国晚泥盆世F/F 生物集群灭绝事件及其后的生物复苏的研究[J].中国科学(D辑),31(18):663-667.
[50]  齐永安,胡斌,Mistiaen B,等.2005.粤北晚泥盆世天子岭组遗迹组构及其环境解释[J].煤田地质与勘探,33(2):11-14.
[51]  王大任,林祖蔚,张欣平.1988.湘西中泥盆世云台观组三叶虫遗迹群落的古生态[J].古生物学报,27(1):48-62.
[52]  王约.1992.独山中泥盆统独山组宋家桥段的遗迹化石及其环境意义[J].贵州地质,9(2):178-183.
[53]  王约.2003.贵州独山泥盆系大河口组遗迹化石Teichichnus 及其地质意义[J].贵州地质,20(3):145-150.
[54]  王约.2004.贵州独山泥盆纪弗拉期—法门期生物灭绝后的生物遗迹[J].古生物学报,43(1):132-141.
[55]  王约,龚一鸣.1997.黔南泥盆系的风暴遗迹相[J].岩相古地理,17(1):39-44.
[56]  王约,陈洪德,田景春,等.1998.黔南独山下、中泥盆统层序地层及界线讨论[J].矿物岩石,18(2):40-46.
[57]  王约,沈建伟,周志澄.1997.黔南独山下、中泥盆统遗迹相与层序地层学研究[J].微体古生物学报,14(2):203-213.
[58]  王约,王训练,史晓颖.2006.贵州独山地区晚泥盆世F-F生物灭绝后的先驱生物及其在生态系统重建过程中的意义[J].中国科学(D辑),36(4):305-315.
[59]  吴诒,龚一鸣,杜远生.1997.华南泥盆纪层序地层及海平面变化[M].湖北武汉: 中国地质大学出版社,6-57.
[60]  徐冉,龚一鸣,汤中道.2006.菌藻类繁盛:晚泥盆世大灭绝的疑凶?[J].地球科学——中国地质大学学报,31(6):787-797.
[61]  杨式溥.1983.广西横县六景早泥盆世遗迹化石及其古生态学意义[J].中国区域地质,5: 11-20.

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