松辽盆地海侵事件——松科1井钙质超微化石新证据

曹文心; 席党鹏; 黄清华; 程祎; 屈海英; 高莲凤; 万晓樵

松辽盆地海侵事件——松科1井钙质超微化石新证据

1. 中国地质大学(北京)生物地质与环境地质国家重点实验室, 北京 100083;
2. 中国科学院南京地质古生物研究所现代古生物学与地层学国家重点实验室, 江苏南京 210008;
3. 大庆油田勘探开发研究院, 黑龙江大庆 163712;
4. 华北理工大学矿业工程学院, 河北唐山 063009

收稿日期: 2015-05-01

修回日期: 2015-11-23

刊出日期: 2016-06-15

Seawater incursion event in Songliao Basin: New evi-dence from calcareous nannofossils of SK-1

1. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences(Beijing), Beijing 100083, China;
2. State Key Laboratory of Palaeobiology and Stratigraphy, Chinese Academy of Sciences, Nanjing 210008, Jiangsu, China;
3. Exploration and Development Research Institute of Daqing Oil Field Company, Daqing 163712, Heilongjiang, China;
4. College of Mining Engineering, North China University of Science and Technology, Tangshan 063009, Hebei, China

Received Date: 01 May 2015

Revised Date: 23 November 2015

Publish Date: 15 June 2016

摘要

摘要: 松辽盆地作为中国最大的陆相含油气盆地,是否发生过海水侵入一直存在争议,化石能为该科学问题提供直接解释。在松科1井嫩江组一、二段发现了少量的钙质超微化石,初步鉴定出Calculites obscurus,Calculites ovalis,Quadrum sp.,Micula sp.等属种。上述钙质超微化石广泛分布于晚白垩世海相地层中,通过与国际标准海相化石的对比,将嫩江组一段中、下部的时代限定为Turonian晚期-Maastrichtian期。松辽盆地嫩江组一、二段下部的钙质超微化石保存总体一般,有一定的多样性,具有海相钙质超微化石的特征。松科1井钙质超微化石的分布、古生态及其与有孔虫化石的对应关系表明,松辽盆地嫩江组一段中-下部、二段下部沉积期湖泊水域广阔,全球海平面较高,间歇性的海水侵入事件导致西北太平洋中的钙质超微浮游生物和有孔虫等海洋生物被带入松辽盆地。
Abstract: The Songliao Basin is the largest non-marine oil-bearing basin in China. Due to the absence of sufficient evidence, the hypothesis of seawater incursion(s) into the Songliao Basin remains controversial. Marine fossil materials can provide direct explana-tions. More recently, a few calcareous nannofossils were discovered from units 1 and 2 of the Nenjiang Formation in drill hole SK-1. In these fossils, some taxa have been positively identified, namely Calculites obscurus, Calculites ovalis, Quadrum sp., and Micula sp. They were distributed in marine environment of the Cretaceous. Based on comparisons of the calcareous nannofossil assemblages from global records, the age of units 1 of the Nenjiang Formation seems to have spanned from the latest Turonian to Maastrichtian. The nannofossils from the Songliao Basin have the marine origin, characterized by common diversity and abundance. The distribu-tion and paleoecology of the calcareous nannofossils as well as the co-existing foraminifera in the SK-1 provide further evidence for seawater incursion events in the Songliao Basin. The authors hold that periodical seawater incursion(s) brought calcareous nannofossils and foraminifera into the Songliao Basin during sedimentation of units 1 and 2 of the Nenjiang Formation, when both lake and sea were at high level.
- calcareous nannofossils /
- seawater incursion /
- Songliao Basin /
- SK-1 /
- Nenjiang Formation /
- Cretaceous

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参考文献(35)

[1]	Yang W L, Li Y K, Gao R Q. Daqing oil field, People's Republic of China, a giant field with non-marine origin[J]. AAPG Bull., 1985, 69(7):1101-1111.
[2]	黄清华,陈春瑞,王平在,等.松辽盆地晚白垩世生物演化与古湖泊缺氧事件[J].微体古生物学报, 1998, 15(4):417-425.
[3]	顾知微,于菁珊.松辽地区白垩纪双壳类化石[J].中国古生物志, 188册新乙种第32号, 1999:1-155.
[4]	高瑞祺,何承全,乔秀云,等.松辽盆地白垩纪两次海侵的沟鞭藻类新属种[J]. 古生物学报, 1992, 31(1):17-29.
[5]	Zhao J, Wan X Q, Xi D P, et al. Late Cretaceous palynology and pa-leoclimate change:Evidence from the SK1(South) core, Songliao Basin, NE China[J]. Science China Earth Sciences, 2014, 57(12):2985-2997.
[6]	张弥曼,周家健,刘智成.东北白垩纪含鱼化石地层的时代和沉积环境[J].古脊椎动物与古人类, 1977, 15(3):194-198.
[7]	王璞珺,杜小弟,王东坡.松辽盆地白垩纪海侵沉积层序与海陆沟通事件的地球化学记录[J]. 岩相古地理, 1995, 15(4):14-20.
[8]	叶淑芬,魏魁生.松辽盆地白垩系的密集段及海水进侵的新证[J].地球科学-中国地质大学学报, 1996, 21(3):267-271.
[9]	黄福堂,迟元林,黄清华.松辽盆地中白垩世海侵事件的质疑[J].石油勘探与开发, 1999, 26(3):104-107.
[10]	李杰,茅绍智,徐钰林,等.松辽盆地北部晚白垩世陆相沟鞭藻及疑源类特征与沉积环境研究[J]. 现代地质, 2000, 14(3):267-272.
[11]	Feng Z H, Fang W, Wang X. Microfossils and molecular records in oil shales of the Songliao Basin and implications for paleo-deposi-tional environment[J]. Science in China (Series D), 2009, 52(10):1559-1571.
[12]	Hou D J, Li M W, Huang Q H. Marine transgressional events in the gigantic freshwater lake Songliao:Paleontological and geochem-ical evidence[J]. Org. Geochem., 2000, 31:763-768.
[13]	Sha J G. Cretaceous stratigraphy of northeast China:non-marine and marine correlation[J]. Cretaceous Research, 2007, 28(2):146-170.
[14]	席党鹏,万晓樵,冯志强,等.松辽盆地晚白垩世有孔虫的发现:来自松科1井湖海沟通的证据[J]. 科学通报, 2010, 55(35):3433-3436.
[15]	Huang Y J, Yang G S, Gu J, et al. Marine incursion events in the Late Cretaceous Songliao Basin:Constraints from sulfur geochemis-try records[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 385:152-161.
[16]	Hu J F, Peng P A, Liu M Y, et al. Seawater Incursion Events in a Cretaceous Paleo-lake Revealed by Specific Marine Biological Markers[J]. Science Report, 2015, 5:1-5.DOI:10.1038/srep09508.
[17]	孙镇城,杨革联,乔子真,等.我国咸化湖泊沉积中钙质超微化石特征及其地质意义[J].古地理学报, 2002, 4(2):56-63.
[18]	高有峰,王璞珺,王成善,等.松科1井南孔选址、岩心剖面特征与特殊岩性层的分布[J]. 地质学报, 2008, 82(5):669-676.
[19]	Wang C S. Environmental/climate change in the Cretaceous green-house world:Records from Terrestrial scientific drilling of Songliao Basin and adjacent areas of China Preface[J]. Palaeogeography Pal-aeoclimatology Palaeoecology, 2013, 385:1-5.
[20]	He H Y, Deng C L, Wang P J, et al. Toward age determination of the termination of the Cretaceous Normal Superchron[J]. Geo-chemistry, Geophysics, Geosystems, 2012, 13(2):259-262.
[21]	Deng C L, He H Y, Pan Y X, et al. Chronology of the terrestrial Upper Cretaceous in the Songliao Basin, northeast Asia[J]. Palaeo-geography Palaeoclimatology Palaeoecology, 2013, 385(5):44-54.
[22]	Li J G, Batten D J, Zhang Y Y. Palynological record from a com-posite core through Late Cretaceous-early Paleocene deposites in the Songliao Basin, Northeast China and its biostratigraphic implica-tions[J]. Cretaceous Research, 2010, 32:1-12.
[23]	Bown P R, Rutledge D C, Crux J A, et al. Early Cretaceous[C]//Bown P R. Calcareous nannofossil biostratigraphy. British Micropa-laeontological Society Publication Series, Chapman & Hall, 1998:86-131.
[24]	Qu H, Xi D, Li S, et al. Late Cretaceous-early Paleocene ostracodbiostratigraphy of Scientific Drilling Sk1(N) in the Songliao Basin, northeast China[J]. Journal of Paleontology, 2014, 88(4):786-19
[25]	Xi D P, Li S, Wan X Q, et al. Biostratigraphy and paleoenviron-mental reconstruction of Late Cretaceous section based on nonmarine Ostracodes from well CCSD-SKI(s), Songliao Basin, north-east China[J]. Hydrobiologia, 2012, 688:113-123.
[26]	Bolli H M, Saunders J M, Perch-Nielsen K, et al. Plankton Stratig-raphy (Volume 1)[M]. Cambridge:Cambridge University Press, 1989:17-571.
[27]	Smith C C. Calcareous nannoplankton and stratigraphy of late Turonian, Coniacian, and early Santonian Age of the Eagle Ford and Austin Groups of Texas[J]. Center for Integrated Data Analyt-ics Wisconsin Science Center, 1981:1-17.
[28]	唐祥华.东濮凹陷早第三纪钙质超微化石古生态及成盐环境[J]. 科学通报, 1986, 4:298-300.
[29]	郝诒纯,茅绍智.微体古生物学教程(第二版)[M]. 武汉:中国地质大学出版社, 1993:85-114.
[30]	刘传联,成鑫荣.渤海湾盆地早第三纪非海相钙质超微化石的锶同位素证据[J].科学通报, 1996, 41(10):908-910.
[31]	Sissingh W. Biostratigraphy of Cretaceous calcareous nannoplank-ton[J]. Geolgoie en Mijnbow, 1977, 56(1):37-65.
[32]	Kaiho K, Fujiwara O, Motoyama. Mid-Cretaceous faunal turnover of intermediate-water benthic foraminifera in the northwestern Pa-cific Ocean margin[J]. Marine Micropaleontol, 1993, 23(1):13-49.
[33]	Nishia H, Takashimaa R, Hatsugai T. Planktonic foraminiferal zo-nation in the Cretaceous Yezo Group, Central Hokkaido, Japan[J]. J. Asian Earth Sci., 2003, 21(8):867-886.
[34]	高瑞祺,张莹,崔同翠.松辽盆地白垩纪石油地层[M].北京:石油工业出版社, 1994:1-333.
[35]	Miller K G, Kominz M A, Browning J V, et al. The Phanerozoic record of global sea-level change[J]. Science, 2005, 310(5752):1293-1298.

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松辽盆地海侵事件——松科1井钙质超微化石新证据

Seawater incursion event in Songliao Basin: New evi-dence from calcareous nannofossils of SK-1

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