Eocene palynoflora and paleoclimate reconstruction in Weixi’nan sag,Beibuwan Basin

doi:10.7623/syxb202502005

Acta Petrolei Sinica ›› 2025, Vol. 46 ›› Issue (2): 355-371.DOI: 10.7623/syxb202502005

• PETROLEUM EXPIORATION • Previous Articles Next Articles

Eocene palynoflora and paleoclimate reconstruction in Weixi’nan sag,Beibuwan Basin

Liu Zixuan^1,2,3, Yan Detian^2,3, Yu Jianxin⁴, Deng Yong⁵, Ding Yan^2,3

1. Key Laboratory of Coalbed Methane Resource and Reservoir Formation Process, Ministry of Education(China University of Mining and Technology), Jiangsu Xuzhou 221116, China;
2. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Hubei Wuhan 430074, China;
3. Hubei Provincial Key Laboratory of Oil and Gas Exploration and Development Theory and Technology, Hubei Wuhan 430074, China;
4. School of Earth Sciences, China University of Geosciences, Hubei Wuhan 430074, China;
5. Zhanjiang Branch, CNOOC China Limited, Guangdong Zhanjiang 524057, China

Received:2024-08-07 Revised:2024-10-24 Online:2025-03-13 Published:2025-03-13

北部湾盆地涠西南凹陷始新世孢粉植物群与古气候重建

刘紫璇^1,2,3, 严德天^2,3, 喻建新⁴, 邓勇⁵, 丁延^2,3

1. 中国矿业大学煤层气资源与成藏过程教育部重点实验室江苏徐州 221116;
2. 中国地质大学(武汉)构造与油气资源教育部重点实验室湖北武汉 430074;
3. 油气勘探开发理论与技术湖北省重点实验室湖北武汉 430074 ;
4. 中国地质大学(武汉)地球科学学院湖北武汉 430074;
5. 中海石油(中国)有限公司湛江分公司广东湛江 524057

通讯作者: 严德天,男,1977年12月生,2008年获中国科学院地质与地球物理研究所博士学位,现为中国地质大学(武汉)资源学院教授、博士生导师,主要从事沉积学、沉积地球化学和盆地分析工作。Email:yandetian@cug.edu.cn
作者简介:刘紫璇,女,1996年7月生,2024年获中国地质大学(武汉)博士学位,现为中国矿业大学博士后,主要从事富有机质页岩形成机理方面的研究。Email:tbh493@cumt.edu.cn
基金资助:
中海石油(中国)有限公司湛江分公司项目"涠西南凹陷流沙港组古湖泊、古环境及沉积体系研究"(CCL2023ZJFN0420)资助。

Abstract

Abstract: Sporopollen fossils play an important role in stratigraphy division and correlation, vegetation succession, and paleoclimate reconstruction. This study focuses on Liushagang Formation in the Weixi’nan sag of Beibuwan Basin, where palynological analysis was conducted to quantitively reconstruct the paleoclimate during its depositional period. The research results are as follows. (1) The sporopollen assemblage is mainly dominated by angiosperm pollen, with notable abundances of Quercoidites and Cupuliferoipollenites. Besides, the gymnosperm pollen is primarily represented by Abietineaepollenites and Piceaepollenites, while the fern spores are dominated by Polypodiaceaesporites. (2) Based on variations in sporopollen content and species composition, three sporopollen assemblages have been identified in Liushagang Formation, including Assemblage Ⅰ (Polypodiaceaesporites-Cupuliferoipollenites-Osmundacidites) in the middle-lower part of the third Member of Liushagang Formation, Assemblage Ⅱ (Quercoidites-Ulmipollenites-Pentapollenites) in the upper part of the third Member of Liushagang Formation to the upper part of the second Member of Liushagang Formation, and Assemblage Ⅲ (Leiosphaeridia-Granodiscus) in the top of the second Member of Liushagang Formation to the lower part of the first Member of Liushagang Formation. (3) Through analyzing the vegetation, humidity, and climate types of the nearest living relatives of sporopollen fossils, the vegetation and paleoclimate for each assemblage were quantitatively reconstructed. During the development of Assemblage Ⅰ, vegetation was dominated by deciduous and evergreen broad-leaved trees, with well-developed herbaceous plants. The content of mesophytic sporopollen was the lowest among the three assemblages, while that of helophytic and hygrophytic sporopollen is the highest, indicating a semi-humid subtropical climate. During the development of Assemblage Ⅱ, herbaceous plants declined, conifers and evergreen broad-leaved trees increased, mesophytic sporopollen rose, and helophytic types decreased, reflecting a semi-humid to semi-arid central subtropical climate. During the development of Assemblage Ⅲ, the evergreen broad-leaved trees continued to develop, and the content of mesophytic sporopollen further increased, indicating a sustained semi-humid to semi-arid subtropical climate. (4) Quantitative paleoclimate reconstruction using the coexistence approach reveals that during the deposition of Liushagang Formation, the mean annual temperature (MAT) ranged from 13.3 ℃ to 19.8 ℃, the warmest month mean temperature from 25.8 ℃ to 27.5 ℃, and the coldest month mean temperature from 1.9 ℃ to 11.9 ℃. Moreover, the mean annual precipitation (MAP) ranged between 797.5 mm and 1 113.2 mm, and the average maximum and minimum monthly precipitation ranged from 179 4 mm to 239.1 mm and from 10.2 mm to 11.3 mm, respectively. Climatic fluctuations occurred within the depositional period, with an overall trend of decreasing MAT and MAP from the third Member to the first Member of Liushagang Formation.

Key words: Beibuwan Basin, Weixi’nan sag, Liushagang Formation, sporopollen analysis, paleoclimate, coexistence approach

摘要： 孢粉在地层划分对比、植被演替和古气候恢复等方面具有重要意义。以北部湾盆地涠西南凹陷始新统流沙港组为研究对象,通过孢粉分析对流沙港组沉积期的古气候进行了定量恢复。研究结果表明:①流沙港组的孢粉类型以被子植物花粉为主,栎粉属和栗粉属含量较突出。裸子植物花粉以单束松粉属和云杉粉属为主,蕨类孢子以水龙骨单缝孢属为主。②根据孢粉含量及种属变化,将流沙港组划分为3个孢粉组合,其中,流沙港组三段中—下部为孢粉组合Ⅰ(Polypodiaceaesporites-Cupuliferoipollenites-Osmundacidites组合),流沙港组三段上部—流沙港组二段上部为孢粉组合Ⅱ(Quercoidites-Ulmipollenites-Pentapollenites组合),流沙港组二段顶部—流沙港组一段下部为孢粉组合Ⅲ(Leiosphaeridia-Granodiscus组合)。③根据孢粉对应的最近亲缘关系类群的生态、干湿度及气候条件,对不同孢粉组合的植被面貌和古气候进行了恢复。孢粉组合Ⅰ发育期,植被面貌以落叶阔叶树和常绿阔叶树为主,草本植物较发育,中生类孢粉含量在3个孢粉组合中最低,而沼生类和湿生类孢粉含量在3个孢粉组合中最高,指示该时期整体为半湿润的南亚热带气候;孢粉组合Ⅱ发育期,草本植物减少,针叶树和常绿阔叶树增多,中生类孢粉含量升高而沼生类孢粉含量降低,指示该时期整体为半湿润—半干旱的中亚热带气候;孢粉组合Ⅲ发育期,常绿阔叶树进一步扩张,中生类孢粉含量进一步升高,指示该时期整体为半湿润—半干旱的中亚热带气候。④共存因子分析法对流沙港组沉积期古气候进行定量恢复的结果认为,流沙港组沉积期的年平均温度为13.3~19.8 ℃,最热月平均温度为25.8~27.5 ℃,最冷月平均温度为1.9~11.9 ℃,年平均降水量为797.5~1113.2 mm,平均最大月降水量为179.4~239.1 mm,平均最小月降水量为10.2~11.3 mm,且流沙港组沉积期内部存在气候波动,从流沙港组三段沉积期到流沙港组一段沉积期整体表现为年平均温度和年平均降水量降低的趋势。

关键词: 北部湾盆地, 涠西南凹陷, 流沙港组, 孢粉分析, 古气候, 共存因子分析法

CLC Number:

TE121.3

Liu Zixuan, Yan Detian, Yu Jianxin, Deng Yong, Ding Yan. Eocene palynoflora and paleoclimate reconstruction in Weixi’nan sag,Beibuwan Basin[J]. Acta Petrolei Sinica, 2025, 46(2): 355-371.

刘紫璇, 严德天, 喻建新, 邓勇, 丁延. 北部湾盆地涠西南凹陷始新世孢粉植物群与古气候重建[J]. 石油学报, 2025, 46(2): 355-371.

References

[1] WESTERHOLD T,MARWAN N,DRURY A J,et al.An astronomically dated record of Earth’s climate and its predictability over the last 66 million years[J].Science,2020,369(6509):1383-1387.
[2] ZACHOS J C,DICKENS G R,ZEEBE R E.An Early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics[J].Nature,2008,451(7176):279-283.
[3] HYLAND E G.,SHELDON N D.Coupled CO₂-climate response during the Early Eocene Climatic Optimum[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2013,369:125-135.
[4] LI Yuanji,SUN Pingchang,FALCON-LANG H J,et al.Eocene hyperthermal events drove episodes of vegetation turnover in the Fushun Basin,northeast China:evidence from a palaeoclimate analysis of palynological assemblages[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2023,610:111317.
[5] 刘萍,谭先锋,陈青,等.早始新世极热气候时期湖盆水体性质及生烃环境——以东营凹陷古近系孔店组为例[J].石油与天然气地质,2017,38(1):39-48.
LIU Ping,TAN Xianfeng,CHEN Qing,et al.Water redox conditions and environment for source rock deposition in lacustrine during the Initial Eocene Thermal Maximum (IETM):a case study on the Paleogene Kongdian Formation in the Dongying sag[J].Oil & Gas Geology,2017,38(1):39-48.
[6] 柳蓉,张坤,刘招君,等.中国油页岩富集与地质事件研究[J].沉积学报,2021,39(1):10-28.
LIU Rong,ZHANG Kun,LIU Zhaojun,et al.Oil shale mineralization and geological events in China[J].Acta Sedimentologica Sinica,2021,39(1):10-28.
[7] 刘招君,孙平昌.中国陆相盆地油页岩形成环境与成矿机制[J].古地理学报,2021,23(1):1-17.
LIU Zhaojun,SUN Pingchang.Formation environment and mineralization mechanism of oil shale in continental basins of China[J].Journal of Palaeogeography,2021,23(1):1-17.
[8] 白悦悦,王灼,孙平昌,等.温室背景下陆相抚顺盆地始新世西露天组古气候演化[J].地球学报,2022,43(6):917-924.
BAI Yueyue,WANG Zhuo,SUN Pingchang,et al.Paleoclimate evolution of the Eocene Xiloutian Formation in the continental Fushun Basin in the warm house background[J].Acta Geoscientica Sinica,2022,43(6):917-924.
[9] WU Yuqi,JIANG Fujie,XU Yunlong,et al.Doubthouse climate influences on the carbon cycle and organic matter enrichment in lacustrine basins:astrochronological and paleontological perspectives[J].Journal of Asian Earth Sciences,2024,267:106155.
[10] BOHATY S M,ZACHOS J C.Significant Southern Ocean warming event in the Late Middle Eocene[J].Geology,2003,31(11):1017-1020.
[11] ABELS H A,CLYDE W C,GINGERICH P D,et al.Terrestrial carbon isotope excursions and biotic change during Palaeogene hyperthermals[J].Nature Geoscience,2012,5(5):326-329.
[12] 黄侠超,钟瀚霆,曹海洋,等.北部湾盆地始新世古环境演化及沉积学意义[J].成都理工大学学报(自然科学版),2024,51(2):193-209.
HUANG Xiachao,ZHONG Hanting,CAO Haiyang,et al.Paleoenvironmental evolution and sedimentological significance of the Beibuwan Basin in the Eocene[J].Journal of Chengdu University of Technology (Science & Technology Edition),2024,51(2):193-209.
[13] HERZSCHUH U,TARASOV P,WVNNEMANN B,et al.Holocene vegetation and climate of the Alashan Plateau,NW China,reconstructed from pollen data[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2004,211(1/2):1-17.
[14] SUN Xiangjun,WANG Pinxian.How old is the Asian monsoon system?—Palaeobotanical records from China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2005,222(3/4):181-222.
[15] 孙湘君,孔昭宸,李明兴,等.南海北部早第三纪流沙港组孢粉组合[J].植物分类学报,1982,20(1):63-72.
SUN Xiangjun,KONG Zhaochen,LI Mingxing,et al.Palynoflora of the Liushagang Formation (Eocene-Early Oligocene)in the northern part of South China Sea[J].Acta Phytotaxonomica Sinica,1982,20(1):63-72.
[16] 谢金有,李君,麦文,等.北部湾盆地涠洲组和流沙港组孢粉组合及时代[J].古生物学报,2012,51(3):385-394.
XIE Jinyou,LI Jun,MAI Wen,et al.Palynofloras and age of the Liushagang and Weizhou formations in the Beibuwan Basin,South China Sea[J].Acta Palaeontologica Sinica,2012,51(3):385-394.
[17] WEI Xiaosong,DENG Yong,YAN Detian,et al.Organic matter enrichment in Asia’s palaeolake controlled by the early and Middle Eocene global warming and astronomically driven precessional climate[J].Marine and Petroleum Geology,2023,154:106342.
[18] 罗威,谢金有,刘新宇,等.北部湾盆地海中凹陷古近纪古气候研究[J].微体古生物学报,2013,30(3):288-296.
LUO Wei,XIE Jinyou,LIU Xinyu,et al.The study of Paleogene climate in the Haizhong depression,Beibuwan Basin,northern South China Sea[J].Acta Micropalaeontologica Sinica,2013,30(3):288-296.
[19] 李君,王任,覃军干,等.北部湾盆地涠西南凹陷古、新近系古生物记录及古环境意义[J].海洋地质与第四纪地质,2020,40(2):29-36.
LI Jun,WANG Ren,QIN Jungan,et al.Paleogene-Neogene micropaleontological records of the Weixinan depression,Beibuwan Basin and their paleoenvironmental significance[J].Marine Geology & Quaternary Geology,2020,40(2):29-36.
[20] 徐长贵,邓勇,范彩伟,等.北部湾盆地涠西南凹陷页岩油地质特征与资源潜力[J].中国海上油气,2022,34(5):1-12.
XU Changgui,DENG Yong,FAN Caiwei,et al.Geological characteristics and resource potential of shale oil in Weixinan sag of Beibu Gulf Basin [J].China Offshore Oil and Gas,2022,34(5):1-12.
[21] 邓勇,胡德胜,朱继田,等.北部湾盆地油气成藏规律与勘探新领域、新类型、资源潜力[J].石油学报,2024,45(1):202-225.
DENG Yong,HU Desheng,ZHU Jitian,et al.Hydrocarbon accumulation regularities,new fields and new types of exploration,and resource potentials in Beibuwan Basin[J].Acta Petrolei Sinica,2024,45(1):202-225.
[22] HUANG Baojia,ZHU Weilin,TIAN Hui,et al.Characterization of Eocene lacustrine source rocks and their oils in the Beibuwan Basin,offshore South China Sea[J].AAPG Bulletin,2017,101(9):1395-1423.
[23] 朱伟林,江文荣.北部湾盆地涠西南凹陷断裂与油气藏[J].石油学报,1998,19(3):6-10.
ZHU Weilin,JIANG Wenrong.Relations between fractures and hydrocarbon reservoirs in Weixinan sag[J].Acta Petrolei Sinica,1998,19(3):6-10.
[24] 张智武,刘志峰,张功成,等.北部湾盆地裂陷期构造及演化特征[J].石油天然气学报,2013,35(1):6-10.
ZHANG Zhiwu,LIU Zhifeng,ZHANG Gongcheng,et al.The chasmic stage and structural evolution features of Beibuwan Basin[J].Journal of Oil and Gas Technology,2013,35(1):6-10.
[25] 秦春雨.北部湾盆地涠西南凹陷古近系双层构造演化及沉积响应[D].武汉:中国地质大学,2020.
QIN Chunyu.The Paleogene evolution of double-layer structure and the response of sedimentation of Weixi’nan sag,Beibuwan Basin[D].Wuhan:China University of Geosciences,2020.
[26] 罗碧华,何杰,姜平,等.北部湾盆地涠西南凹陷古近系流二段滩坝沉积特征及控制因素[J].地质科技情报,2019,38(1):186-196.
LUO Bihua,HE Jie,JIANG Ping,et al.Sedimentary characteristics of lacustrine beach-bars and their formation of the second Member of Liushagang Formation in the Paleogene Weixinan depression of Beibuwan Basin[J].Geological Science and Technology Information,2019,38(1):186-196.
[27] 国家能源局.化石孢粉分析鉴定:SY/T 5915—2018[S].北京:中国标准出版社,2018.
National Energy Administration.Analysis and identification for fossil spore and pollen.SY/T 5915-2018[S].Beijing:Standard Press of China,2018.
[28] 杨久成,刘佳,李雨,等.滇东南普阳盆地含煤地层孢粉组合特征及其年代[J].生物多样性,2022,30(11):81-90.
YANG Jiucheng,LIU Jia,LI Yu,et al.Palynological assemblage and age of the Cenozoic coal-accumulation strata in the Puyang Basin,southeastern Yunnan Province[J].Biodiversity Science,2022,30(11):81-90.
[29] 杨荣玉.广西合浦盆地下第三系孢粉组合及时代[J].广西地质,1996,9(3):32-41.
YANG Rongyu.Association and time of Eocene sporo-pollen in Hepu Basin,Guangxi[J].Guangxi Geology,1996,9(3):32-41.
[30] 朱宗浩,郑国光,赵传本.中国含油气盆地孢粉学论文集[M].北京:石油工业出版社,2000.
ZHU Zonghao,ZHENG Guoguang,ZHAO Chuanben.Symposium on palynology of petroliferous basins in China [M].Beijing:Petroleum Industry Press,2000.
[31] 石油化学工业部石油勘探开发规划研究院,中国科学院南京地质古生物研究所.渤海沿岸地区早第三纪沟鞭藻类和疑源类[M].北京:科学出版社,1978.
Research Institute of Petroleum Exploration & Development,Nanjing Institute of Geology and Palaeontology,Chinese Academy of sciences.Early Tertiary dinoflagellates and acritarchs in the coastal area of the Bohai Sea[M].Beijing:Science Press,1978.
[32] 钱泽书,郑亚惠,宋之琛.苏北盆地阜宁群孢粉[J].古生物学报,1993,32(1):49-63.
QIAN Zeshu,ZHENG Yahui,SONG Zhichen.Spores and pollen grains from Funing group of north Jiangsu[J].Acta Palaeontologica Sinica,1993,32(1):49-63.
[33] 何月明,孙湘君.江西清江盆地下第三系孢子花粉的初步研究Ⅰ[J].植物学报,1977,19(1):72-82.
HE Yueming,SUN Xiangjun.Palynological investigation of Paleogene in the Qingjiang Basin in Kiangsi Province Ⅰ[J].Acta Botanica Sinica,1977,19(1):72-82.
[34] 张一勇.雷州半岛第三纪孢粉[J].古生物学报,1981,20(5):449-458.
ZHANG Yiyong.Tertiary spores and pollen grains from the Leizhou Peninsula[J].Acta Palaeontologica Sinica,1981,20(5):449-458.
[35] 李元吉.抚顺盆地古近纪古环境演化与有机质富集机制研究[D].长春:吉林大学,2022.
LI Yuanji.Paleogene paleoenvironmental evolution and organic matter accumulation mechanisms,Fushun Basin[D].Changchun:Jilin University,2022.
[36] 叶得泉.中国油气区第三系(Ⅰ)总论[M].北京:石油工业出版社,1993.
YE Dequan.Tertiary in petroliferous regions of China[M].Beijing:Petroleum Industry Press,1993.
[37] 韩箫屿.抚顺盆地古城子组孢粉组合特征及其古植被和古气候[D].长春:吉林大学,2020.
HAN Xiaoyu.Palynoflora from the Guchengzi Formation of the Fushun Basin and its paleoenvironment implications[D].Changchun:Jilin University,2020.
[38] 柳蓉,闫旭,刘招君,等.银额盆地下白垩统巴音戈壁组含油页岩岩系孢粉化石特征及地质意义[J].吉林大学学报(地球科学版),2020,50(2):341-355.
LIU Rong,YAN Xu,LIU Zhaojun,et al.Characteristics and geological significance of palynological fossils from Bayingebi Formation of Lower Cretaceous in Yin’e Basin[J].Journal of Jilin University (Earth Science Edition),2020,50(2):341-355.
[39] 赵秀兰,赵传本,关学婷,等.利用孢粉资料定量解释我国第三纪古气候[J].石油学报,1992,13(2):215-225.
ZHAO Xiulan,ZHAO Chuanben,GUAN Xueting,et al.The application of spore-pollen data in a quantitative explanation of Tertiary palaeoclimate in our country[J].Acta Petrolei Sinica,1992,13(2):215-225.
[40] 王丽岩,孙跃武,乔秀云,等.海拉尔盆地早白垩世孢粉古气候特征[J].大庆石油地质与开发,2008,27(5):38-42.
WANG Liyan,SUN Yuewu,QIAO Xiuyun,et al.The Early Cretaceous palynologic palaeoclimate of Hailaer Basin[J].Petroleum Geology & Oilfield Development in Daqing,2008,27(5):38-42.
[41] 严德天,陆江,魏小松,等.断陷湖盆富有机质页岩形成环境及主控机制浅析——以涠西南凹陷流沙港组二段为例[J].中国海上油气,2019,31(5):21-29.
YAN Detian,LU Jiang,WEI Xiaosong,et al.Sediment environment and major controlling factors of organic-rich shales in the rift lake basin:a case study of the 2nd Member of Liushagang Formation of the Weixinan sag[J].China Offshore Oil and Gas,2019,31(5):21-29.
[42] MOSBRUGGER V,UTESCHER T.The coexistence approach—a method for quantitative reconstructions of Tertiary terrestrial palaeoclimate data using plant fossils[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1997,134(1/4):61-86.
[43] WANG Qing,FERGUSON D K,FENG Guangping,et al.Climatic change during the Palaeocene to Eocene based on fossil plants from Fushun,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,295(1/2):323-331.
[44] UTESCHER T,BRUCH A A,ERDEI B,et al.The coexistence approach—theoretical background and practical considerations of using plant fossils for climate quantification[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2014,410:58-73.
[45] ZHANG Qianqian,SMITH T,YANG Jian,et al.Evidence of a cooler continental climate in East China during the warm Early Cenozoic[J].PLoS One,2016,11(5):e0155507.
[46] POSTIGO-MIJARRA J M,ALTOLAGUIRRE Y,MORENO-DOMíNGUEZ R, et al.Climatic reconstruction at the Early Miocene La Rinconada mine (Ribesalbes-Alcora Basin,eastern Spain)based on coexistence approach,CLAMP and LMA analysis[J].Review of Palaeobotany and Palynology,2022,304:104714.
[47] 魏金辉,郑卓,彭环环,等.基于孢粉植物类群气候区间的古气候定量重建方法[J].第四纪研究,2013,33(6):1080-1090.
WEI Jinhui,ZHENG Zhuo,PENG Huanhuan,et al.Methods of quantitative paleoclimate reconstruction based on pollen flora and their climatic intervals[J].Quaternary Sciences,2013,33(6):1080-1090.
[48] GRIMM G W,DENK T.Reliability and resolution of the coexistence approach—a revalidation using modern-day data[J].Review of Palaeobotany and Palynology,2012,172:33-47.
[49] 秦锋,赵艳.基于孢粉组合定量重建古气候的方法在中国的运用及思考[J].第四纪研究,2013,33(6):1054-1068.
QIN Feng,ZHAO Yan.Methods of quantitative climate reconstruction based on palynological data and their applications in China[J].Quaternary Sciences,2013,33(6):1054-1068.
[50] YAO Yifeng,BERA S,FERGUSON D K,et al.Reconstruction of paleovegetation and paleoclimate in the Early and Middle Eocene,Hainan Island,China[J].Climatic Change,2009,92(1/2):169-189.
[51] 韦一,杨兵,邓会娟.百色盆地渐新世古植被与古气候[J].地质科技通报,2022,41(4):197-206.
WEI Yi,YANG Bing,DENG Huijuan.Paleovegetation and paleoclimate in the Baise Basin during Oligocene[J].Bulletin of Geological Science and Technology,2022,41(4):197-206.
[52] 徐景先.云南中西部地区晚第三纪孢粉植物群及其古植被和古气候研究[D].北京:中国科学院植物研究所,2002.
XU Jingxian.Palynology,paleovegetation and paleoclimate of Neogene central-western Yunnan,China[D].Beijing:Institute of Botany,Chinese Academy of Sciences,2002.
[53] 金建华,廖文波,王伯荪,等.海南岛第三纪沉积环境与古植物群落的多样性及其变迁[J].生态学报,2002,22(3):425-432.
JIN Jianhua,LIAO Wenbo,WANG Bosun,et al.Paleodiversification of the environment and plant community of Tertiary in Hainan Island[J].Acta Ecologica Sinica,2002,22(3):425-432.
[54] ZHANG Zhongshi,FLATOY F,WANG Huijun,et al.Early Eocene Asian climate dominated by desert and steppe with limited monsoons[J].Journal of Asian Earth Sciences,2012,44:24-35.
[55] ZHANG Ran,JIANG Dabang,LI Xiangyu,et al.East Asian climate evolution during the Cenozoic:a review from the modeling perspective[J].Fundamental Research,2023.
[56] SCOTESE C R.Global climate change (modern times to 540 million years ago)[C]//Proceedings of the Departmental Seminar.Evanston:Earth & Environmental Sciences,Northwestern University,2016.

Eocene palynoflora and paleoclimate reconstruction in Weixi’nan sag,Beibuwan Basin

北部湾盆地涠西南凹陷始新世孢粉植物群与古气候重建

PDF

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 11

Recommended Articles

Metrics

Comments

[1]	Fan Caiwei, Zhou Gang, Tang Xu, Chen Kui. Accumulation conditions and key technologies for exploration and development of Wushi oilfield in Beibuwan Basin [J]. Acta Petrolei Sinica, 2025, 46(2): 466-482.
[2]	Li Jianfeng, Li Xiangbo, Ma Bo, Huang Junping, Kong Qingfen, Zhang Yan, Ji Liming. Palynofacies and sedimentary paleoenvironment reconstruction of Triassic Yanchang Formation in southern Ordos Basin [J]. Acta Petrolei Sinica, 2024, 45(7): 1092-1103.
[3]	Deng Yong, Hu Desheng, Zhu Jitian, Liu Guochang, Chen Kui, Tong Chuanxin, Zhang Daojun, Xu Xinde, Man Yong, You Junjun, Man Xiao, Wu Yunpeng, Zhou Gang, Zhang Jianxin. Hydrocarbon accumulation regularities, new fields and new types of exploration, and resource potentials in Beibuwan Basin [J]. Acta Petrolei Sinica, 2024, 45(1): 202-225.
[4]	Wang Liliang, Niu Chengmin, Yang Haifeng, Gao Yanfei, Zhao Dijiang. Evolution of channel patterns and its geological significance for oil and gas exploration in the Lower Member of Minghuazhen Formation in Laibei low uplift,Bohai Bay Basin [J]. Acta Petrolei Sinica, 2022, 43(3): 364-375.
[5]	Jiang Ping, Zhang Hui, Wang Lei, Wang Xinguang, Xiang Yaoquan. An evaluation method of reservoir “sweet spots” in low permeability oilfields of Beibuwan Basin [J]. Acta Petrolei Sinica, 2021, 42(6): 751-764.
[6]	Jiang Xue, Liu Lifang, Sun Hefeng, Huang Shengbing, Geng Mingyang, Chen Shaoping, Li Nan, Shen Pu. Differential distribution of high-quality lacustrine source rocks controlled by climate and tectonics:a case study from Bozhong sag [J]. Acta Petrolei Sinica, 2019, 40(2): 165-175.
[7]	Li Youchuan, Lan Lei, Wang Ke, Yang Yongcai. Differences in lacustrine source rocks of Liushagang Formation in the Beibuwan Basin [J]. Acta Petrolei Sinica, 2019, 40(12): 1451-1459.
[8]	XU Xinde, ZHANG Yingzhao, HUANG Yiwen, XIONG Xiaofeng, LI Xuhong. Major controlling factors for development of oil shale in Liushagang Formation of Wushi sag, Beibuwan Basin [J]. ACTA PETROLEI SINICA, 2013, 34(增刊二): 66-73.
[9]	LI Chunrong　ZHANG Gongcheng　LIANG Jianshe　ZHAO Zhigang　XU Jianyong. Characteristics of fault structure and its control on hydrocarbons in the Beibuwan Basin [J]. Editorial office of ACTA PETROLEI SINICA, 2012, 33(2): 195-203.
[10]	HUANG Baojia　HUANG Heting　WU Guoxuan　YOU Junjun. Geochemical characteristics and formation mechanism of Eocene lacustrine organic-rich shales in the Beibuwan Basin [J]. Editorial office of ACTA PETROLEI SINICA, 2012, 33(1): 25-31.
[11]	Zhao Xiafei, Ding Guiming, Wang Hengjian, Gao Ruiqi. AN ANALYSIS OF PALEOCHANNEL OF QUANTOU FORMATION IN SONGLIAO BASIN [J]. Editorial office of ACTA PETROLEI SINICA, 1995, 16(4): 32-39.