[an error occurred while processing this directive] 世界地质 2018, 37(4) 991-1003 DOI:   10.3969/j.issn.1004-5589.2018.04.001  ISSN: 1004-5589 CN: 22-1111/P

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三江盆地
东基三井
晚白垩世
海浪组
孢粉组合
本文作者相关文章
万传彪
张艳
薛云飞
张昕
金玉东
陈润
乔秀云
孙跃武
PubMed
Article by Wan C
Article by Zhang Y
Article by Xue Y
Article by Zhang X
Article by Jin Y
Article by Chen R
Article by Qiao X
Article by Sun Y
黑龙江三江盆地晚白垩世海浪组孢粉组合
万传彪1,2, 张艳3, 薛云飞1, 张昕1, 金玉东1, 陈润1, 乔秀云1, 孙跃武2
1. 大庆油田有限责任公司勘探开发研究院, 黑龙江 大庆 163712;
2. 吉林大学东北亚生物演化与环境教育部重点实验室, 长春 130026;
3. 吉林省誉华公路工程有限公司, 长春 130062
摘要: 依据东基三井1 226.0~1 538.0 m井段的孢粉鉴定结果,结合前人资料,首次将该井段孢粉组合命名为Cyathidites-Taxodiaceaepolleni-Aquilapollenites组合。其组合特征为:裸子植物花粉占48.10%~78.58%,蕨类孢子占2.44%~34.18%,被子植物花粉占0%~28.26%;蕨类孢子中Cyathidites百分含量最高(0.79%~37.50%),其次是Cicatricosisporites(0%~12.50%)和Leiotriletes(0%~10.00%),重要分子有Appendicisporites、Schizaeoisporites、LygodiumsporitesLygodioisporites;裸子植物花粉中Inaperturopllenites的百分含量最高(11.29%~38.83%),其次是Taxodiaceaepollenites(12.66%~28.57%),重要分子有Tsugaepollenites、Parcisporites、Parvisaccites、EphedripitesClassopollis等;被子植物花粉中Tricolpites的百分含量最高(0%~16.46%),其次是Betulaepollenites(0%~15.22%),含量较高的还有MomipitesTricolporopollenites,重要分子有Aquilapollenites、FibulapollisProteacidites等。该组合可以与松辽盆地嫩江组孢粉组合对比,地质时代为晚白垩世Santonian-Campanian期。鉴于宁安市南团子山、高家等露头区海浪组所产Estherites mitsuishii、E.liuxinensis、Tylestheria cf.shanhoensis、Halysestheria yui、Calestherites sp.和Brachygrapta?sp.等叶肢介化石群,系松辽盆地嫩江组常见分子,故将东基三井1 226.0~1 538.0 m井段划归为海浪组,废弃"七星河组"一名。
关键词 三江盆地   东基三井   晚白垩世   海浪组   孢粉组合  
Palynological assemblage from Late Cretaceous Hailang Formation in Sanjiang Basin, Heilongjiang
WAN Chuan-biao1,2, ZHANG Yan3, XUE Yun-fei1, ZHANG Xin1, JIN Yu-dong1, CHEN Run1, QIAO Xiu-yun1, SUN Yue-wu2
1. Institute of Exploration and Development, Daqing Oilfield Company Ltd., Daqing 163712, Heilongjiang, China;
2. Key Laboratory for Evolution of Past Life and Environment in Northeast Asian(Jilin University), Ministry of Education, Changchun 130026, China;
3. Yuhua Highway Engineering of Jilin Province Company Ltd., Changchun 130062, China
Abstract: Based on the palynological data from 1 226.0~1 538.0 m of Dongji 3 borehole, the Cyathidites-Taxodiaceaepolleni-Aquilapollenites assemblage is established for the Upper Cretaceous in Sanjiang Basin, eastern Heilongjiang. The assemblage is characterized by abundant gymnosperm pollen (48.10%~78.58%), fern spores (2.44%~34.18%) and angiosperm pollen (0%~28.26%).Fern spores mainly consist of Cyathidites (0.79%~37.50%), Cicatricosisporites (0%~12.50%) and Leiotriletes (0%~10.00%). Important spores are Appendicisporites, Schizaeoisporites, Lygodiumsporites and Lygodioisporites.Among the gymnosperm pollen, Inaperturopllenites (11.29%~38.83%) and Taxodiaceaepollenites (12.66%~28.57%) are dominant, followed by Tsugaepollenites, Parcisporites, Parvisaccites, Ephedripites and Classopollis. The angiosperm pollen is characterized by high content of Tricolpites (0%~16.46%) and Betulaepollenites (0%~15.22%), followed by Momipites and Tricolporopollenites, with Aquilapollenites, Fibulapollis and Proteacidites as important components. The assemblage can be closely correlated to the palynological assemblage from Nenjiang Formation in Songliao Basin, with an age of Santonian-Campanian. In view of the conchostracan fauna represented by Estherites mitsuishii, E. liuxinensis, Tylestheria cf. shanhoensis, Halysestheria yui, Calestherites sp. and Brachygrapta? sp. was found in the Hailang Formation in the outcrops at Nantuanshanzi and Gaojia villages in Ning'an City, eastern Heilongjiang, and the fauna is also common in the Nenjiang Formation in Songliao Basin, the strata at depth 1 226.0~1 538.0 m in Dongji 3 borehole should be assigned to Hailang Formation. Therefore, the former Qixinghe Formation should be abandoned.
Keywords: Sanjiang Basin   Late Cretaceous   Hailang Formation   palynological assemblage  
收稿日期 2018-09-01 修回日期 2018-11-07 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2018.04.001
基金项目:

国家自然科学基金项目(30670138,31270277).

通讯作者: 孙跃武(1966-),教授,从事古生物学与地层学研究.E-mail:sunyuewu@jlu.edu.cn
作者简介:
作者Email: sunyuewu@jlu.edu.cn

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