南沙群岛新近纪碳酸盐台地中的微体化石及其意义*

doi:10.11978/2025246

热带海洋学报 ›› 2026, Vol. 45 ›› Issue (5): 80-93.doi: 10.11978/2025246CSTR: 32234.14.2025246

南沙群岛新近纪碳酸盐台地中的微体化石及其意义^*

苏翔¹^,²(), 向荣¹^,²(), 易亮³, 张强¹^,², 张亚南⁴, 秦国权⁵, 万随¹^,², 颜文¹^,²^,⁶()

¹ 中国科学院南海海洋研究所, 热带海洋环境与岛礁生态全国重点实验室, 广东广州 511458
² 中国科学院南海海洋研究所, 边缘海与大洋地质实验室, 广东广州 511458
³ 同济大学海洋地质全国重点实验室, 上海 200092
⁴ 中国科学院广州地球化学研究所, 深地过程与战略矿产资源全国重点实验室, 广东广州 510640
⁵ 中国海洋石油总公司南海东部石油公司, 广东广州 510240
⁶ 中国科学院大学, 北京 100049

收稿日期:2025-12-20 修回日期:2026-02-07 出版日期:2026-09-10 发布日期:2026-10-13
通讯作者: 向荣, 颜文
作者简介:
苏翔(1984—), 男, 副研究员, 主要从事微体化石与古海洋学研究。email: suxiang@scsio.ac.cn
* 感谢贵州省地质矿产局115地质调查大队、中国科学院南海海洋研究所岛礁中心及其同事、中国科学院南京地质古生物研究所祝幼华研究员和李保华研究员对本研究样品采集、实验方法和数据处理的贡献和支持。
基金资助:
国家重点研发计划项目(2021-06); 国家重点研发计划项目(2022-24); 国家自然科学基金面上项目(42476066)

Microfossils in the Neogene carbonate platform of Nansha Islands and their significance^*

SU Xiang¹^,²(), XIANG Rong¹^,²(), YI Liang³, ZHANG Qiang¹^,², ZHANG Yanan⁴, QIN Guoquan⁵, WAN Sui¹^,², YAN Wen¹^,²^,⁶()

¹ South China Sea Institute of Oceanology, Chinese Academy of Sciences, State Key Laboratory of Tropical Oceanography, Guangzhou 511458, China
² South China Sea Institute of Oceanology, Chinese Academy of Sciences, Laboratory of Ocean and Marginal Sea Geology, Guangzhou 511458, China
³ State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
⁴ Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, State Key Laboratory of Deep Earth Processes and Resources, Guangzhou 510640, China
⁵ CNOOC South China Sea Eastern Petroleum Corporation, Guangzhou 510240, China
⁶ University of Chinese Academy of Sciences, Beijing 100049, China

Received:2025-12-20 Revised:2026-02-07 Online:2026-09-10 Published:2026-10-13
Contact: XIANG Rong, YAN Wen
Supported by:
National Key Research and Development Program of China(2021-06); National Key Research and Development Program of China(2022-24); National Natural Science Foundation of China(42476066)

摘要/Abstract

摘要：

生物礁是生产力水平最高、生物多样性最丰富的生态系统之一, 对全球碳循环至关重要。南海发育了西太平洋最大的碳酸盐台地, 在南沙群岛美济环礁上钻取的全取心井——南科1 (NK-1)井, 为评估南海生物礁的长期演化提供了良好机会。为了揭示南沙群岛的演化历史及其控制因素, 需要对NK-1井建立更可靠的年龄约束。文章提供了NK-1井生物礁碳酸岩中微体化石(钙质超微化石、有孔虫和放射虫)丰度和多样性的新记录, 基于微体化石组合, 在NK-1井序列中识别出7个生物地层事件, 揭示了从早中新世到更新世的连续沉积序列。通过结合古地磁年代数据, 重建了南沙群岛碳酸盐台地的发育和演化。NK-1井生物礁序列的底界年龄估计为(23.03±1.06)Ma, 接近渐新世/中新世边界。新的年代地层格架揭示了3个短暂的沉积间断(3.6—2.4Ma、11.1—10.0Ma和 13.5—11.9Ma), 它们分别与210.3m、464.6m和561.6m处的显著暴露面良好对应。通过与南沙和西沙群岛生物礁深钻岩心的地层和堆积速率记录对比, 揭示了南海自新近纪以来极其相似的碳酸盐台地演化历史。结果表明, 南海碳酸盐台地的发育经历了晚渐新世/早中新世初始阶段、早—中中新世快速生长阶段、中—晚中新世侵蚀阶段、中新世—上新世稳定发育阶段和第四纪快速生长阶段, 主要受全球海平面变化、环境因素和区域构造运动(如南海海盆扩张、沙巴造山运动和东沙运动)的影响。

关键词: 碳酸盐台地, 微体化石, 构造运动, 海平面变化, 南海

Abstract:

Biogenic reefs are among the most productive and biodiverse ecosystems, and are critical to global carbon cycling. The South China Sea (SCS) has developed the largest carbonate platforms in the Western Pacific. The fully-cored Well NK-1, drilled through the reef complex on the Meiji Atoll, Nansha Islands, offers a good opportunity for assessing the long-term evolution of biogenic reefs in the SCS. To reveal the evolution history of Nansha Islands and their controlling factors, more credible age constraints on core NK-1 are needed. This research presents new records of microfossils (calcareous nannofossils, foraminifera and radiolarians) abundances and diversities in the biogenic reef carbonates of core NK-1. Based on the assemblages of the microfossils, seven biostratigraphic events are recognized from the sequence of core NK-1, revealing a general continuous succession of the Early Miocene to Pleistocene age. Combined with the magnetostratigraphic data, the development and evolution of carbonate platform in the Nansha Islands are reconstructed. The bottom age of the biogenic reef sequence of NK-1 is estimated at (23.03 ± 1.06) Ma, close to the Oligocene/Miocene boundary. The new chronostratigraphic framework highlights three short hiatuses of 3.6—2.4 Ma, 11.1—10.0 Ma, and 13.5—11.9 Ma, which are well correlated with the prominent exposed surfaces at 210.3 m, 464.6 m and 561.6 m, respectively. These records reveal a remarkably similar evolutionary history of carbonate platforms in the SCS since Neogene, by comparison with stratigraphic records and growth rates from deep drilling cores on isolated coral reefs in Nansha and Xisha Islands. The results show that carbonate platform development in the SCS experienced five phases: Late Oligocene / Early Miocene initiation phase, Early-Middle Miocene rapid growth phase, Middle-Late Miocene erosion phase, Miocene-Pliocene stable development phase, and Quaternary rapid growth phase, which were mainly influenced by global sea-level changes, environmental factors and regional tectonism such as the SCS basin spreading, the Sabah Orogeny and the Dongsha Movement.

Key words: carbonate platform, microfossils, tectonic movement, sea-level change, South China Sea

中图分类号:

P736.221

苏翔, 向荣, 易亮, 张强, 张亚南, 秦国权, 万随, 颜文. 南沙群岛新近纪碳酸盐台地中的微体化石及其意义^*[J]. 热带海洋学报, 2026, 45(5): 80-93.

SU Xiang, XIANG Rong, YI Liang, ZHANG Qiang, ZHANG Yanan, QIN Guoquan, WAN Sui, YAN Wen. Microfossils in the Neogene carbonate platform of Nansha Islands and their significance^*[J]. Journal of Tropical Oceanography, 2026, 45(5): 80-93.

图/表 9

图1

图2

图3

图4

图5

表1

图6

图7

图8

参考文献 57

[1]	罗云, 黎刚, 徐维海, 等, 2022. 南科1井第四系暴露面特征及其与海平面变化的关系[J]. 热带海洋学报, 41(1): 143-157.
	Luo Yun, Li Gang, Xu Weihai, et al, 2022. Characteristics of Quaternary exposure surfaces in Well Nanke-1 and their relationship with sea-level changes[J]. Journal of Tropical Oceanography, 41(1): 143-157 (in Chinese with English abstract).
[2]	秦国权, 1996. 微体古生物在珠江口盆地新生代晚期层序地层学研究中的应用[J]. 海洋地质与第四纪地质, 16(4): 1-18.
	Qin Guoquan, 1996. Application of micropaleontology to the sequence stratigraphic studies of Late Cenozoic in the Zhujiang River Mouth Basin[J]. Marine Geology & Quaternary Geology, 16(4): 1-18 (in Chinese with English abstract).
[3]	秦国权, 2002. 珠江口盆地新生代晚期层序地层划分和海平面变化[J]. 中国海上油气(地质), 16(1): 1-10, 18.
	Qin Guoquan, 2002. Late Cenozoic sequence stratigraphy and sea-level changes in Pearl River mouth basin, South China Sea[J]. China Offshore Oil and Gas (Geology), 16(1): 1-10, 18 (in Chinese with English abstract).
[4]	徐国强, 吕炳全, 王红罡, 2002. 新生代南海北部碳酸盐岩台地的淹没事件研究[J]. 同济大学学报(自然科学版), 30(1): 35-40.
	Xu Guoqiang, Lyu Bingquan, Wang Honggang, 2002. Drowning event research: insights from Cenozoic carbonate platforms in northern South China Sea[J]. Journal of Tongji University (Natural Science), 30(1): 35-40 (in Chinese with English abstract).
[5]	祝幼华, 刘新宇, 马瑞芳, 等, 2016. 南海西沙群岛西科1井早中新世-第四纪生物礁地层中钙质超微化石的发现及其意义[J]. 古生物学报, 55(3): 385-392.
	Zhu Youhua, Liu Xinyu, Ma Ruifang, et al, 2016. Early Miocene to quaternary calcareous nannofossils from the biogenetic reef complexes and their significance of Well XK1, Xisha Islands, South China Sea[J]. Acta Palaeontologica Sinica, 55(3): 385-392 (in Chinese with English abstract).
[6]	Barckhausen U, Engels M, Franke D, et al, 2014. Evolution of the South China Sea: Revised ages for breakup and seafloor spreading[J]. Marine and Petroleum Geology, 58: 599-611.
[7]	Berggren W A, Kent D V, Swisher C C, et al, 1995. A revised Cenozoic geochronology and chronostratigraphy[M]// Berggren W A, Kent D V, Aubry M P, et al. Geochronology, time scales and global stratigraphic correlation. Houston: SEPM Society for Sedimentary Geology: 129-212.
[8]	Betzler C, Eberli G P, Kroon D, et al, 2016. The abrupt onset of the modern South Asian Monsoon winds[J]. Scientific Reports, 6: 29838.
[9]	Bi Dongjie, Zhang Daojun, Zhai Shikui, et al, 2018. Seawater ⁸⁷Sr/⁸⁶Sr values recorded by reef carbonates from the Xisha Islands (South China Sea) since the Neogene and its response to the uplift of Qinghai-Tibetan Plateau[J]. Geological Journal, 54(6): 3878-3890.
[10]	Briais A, Patriat P, Tapponnier P, 1993. Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea: implications for the Tertiary tectonics of Southeast Asia[J]. Journal of Geophysical Research: Solid Earth, 98 (B4): 6299-6328.
[11]	Chen Wenhuang, Yan Yi, Carter A, et al, 2024. Evolution of arc-continent collision in the southeastern margin of the South China Sea: insight from the isugod basin in central-southern Palawan[J]. Tectonics, 43(6): e2023TC008078.
[12]	Cheng Jun, Wang Shuhong, Li Gang, et al, 2022. Origin of large-scale variegated reef limestones in the southern South China Sea: Implications for Miocene regional and global geological evolution[J]. Journal of Asian Earth Sciences, 230: 105202.
[13]	Clift P D, Wan Shiming, Blusztajn J, 2014. Reconstructing chemical weathering, physical erosion and monsoon intensity since 25 Ma in the northern South China Sea: a review of competing proxies[J]. Earth-Science Reviews, 130: 86-102.
[14]	Eberli G P, Anselmetti F S, Kroon D, et al, 2002. The chronostratigraphic significance of seismic reflections along the Bahamas Transect[J]. Marine Geology, 185(1/2): 1-17.
[15]	Fan Tianlai, Yu Kefu, Zhao Jianxin, et al, 2020. Strontium isotope stratigraphy and paleomagnetic age constraints on the evolution history of coral reef islands, northern South China Sea[J]. GSA Bulletin, 132(3/4): 803-816.
[16]	Fielding C R, Browne G H, Field B, et al, 2011. Sequence stratigraphy of the ANDRILL AND-2A drillcore, Antarctica: a long-term, ice-proximal record of Early to Mid-Miocene climate, sea-level and glacial dynamism[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 305(1/2/3/4): 337-351.
[17]	Fyhn M B W, Boldreel L O, Nielsen L H, et al, 2013. Carbonate platform growth and demise offshore Central Vietnam: Effects of Early Miocene transgression and subsequent onshore uplift[J]. Journal of Asian Earth Sciences, 76: 152-168.
[18]	Gradstein F M, Ogg J G, Hilgen F J, 2012. The geologic time scale[M]. Oxford: Cambridge University Press.
[19]	Holbourn A, Kuhnt W, Kochhann K G D, et al, 2015. Global perturbation of the carbon cycle at the onset of the Miocene Climatic Optimum[J]. Geology, 43(2): 123-126.
[20]	Hutchison C S, 2004. Marginal basin evolution: the southern South China Sea[J]. Marine and Petroleum Geology, 21(9): 1129-1148.
[21]	Hutchison C S, 2010. The North-West Borneo Trough[J]. Marine Geology, 271(1/2): 32-43.
[22]	Johnson K, Jackson J, Budd A, 2008. Caribbean reef development was independent of coral diversity over 28 million years[J]. Science, 319: 1521-1523.
[23]	Li Chunfeng, Xu Xing, Lin Jian, et al, 2014. Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349[J]. Geochemistry, Geophysics, Geosystems, 15(12): 4958-4983.
[24]	Li Gang, Xu Weihai, Luo Yun, et al, 2022. Strontium isotope stratigraphy and LA-ICP-MS U-Pb carbonate age constraints on the Cenozoic tectonic evolution of the southern South China Sea[J]. GSA Bulletin, 135(1/2): 271-285.
[25]	Lisiecki L E, Raymo M E, 2005. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ¹⁸O records[J]. Paleoceanography, 20(1): 2004PA001071.
[26]	Liu Jianguo, Cao Li, Xu Weihai, et al, 2022. Formation and development of coral reefs in the South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 594: 110957.
[27]	Luan Xiwu, Lunt P, 2022. Controls on Early Miocene carbonate and siliciclastic deposition in eastern Java and south Makassar Straits, Indonesia[J]. Journal of Asian Earth Sciences, 227: 105091.
[28]	Ma Xiaolin, Tian Jun, Ma Wentao, et al, 2018. Changes of deep Pacific overturning circulation and carbonate chemistry during middle Miocene East Antarctic ice sheet expansion[J]. Earth and Planetary Science Letters, 484: 253-263.
[29]	Ma Yubo, Wu Shiguo, Lyu Fuliang, et al, 2011. Seismic characteristics and development of the Xisha carbonate platforms, northern margin of the South China Sea[J]. Journal of Asian Earth Sciences, 40(3): 770-783.
[30]	Makhankova A, Sautter B, Mathew M, et al, 2021. Seismic stratigraphy and sedimentology of a Miocene carbonate platform in Luconia, South China Sea[J]. Geological Journal, 56(1): 1-17.
[31]	Martini E, 1971. Standard Tertiary and Quaternary calcareous nannoplankton zonation[M]. Farinacci A. Proceedings of the Second Planktonic Conference. Roma: Rome Edizioni Tecnoscienza: 739-785.
[32]	Mathew M, Makhankova A, Menier D, et al, 2020. The emergence of Miocene reefs in South China Sea and its resilient adaptability under varying eustatic, climatic and oceanographic conditions[J]. Scientific Reports, 10: 7141.
[33]	Meng Min, Yu Kefu, Hallock P, et al, 2022. Foraminifera indicate Neogene evolution of Yongle Atoll from Xisha Islands in the South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 602: 111163.
[34]	Miao Xiuquan, Huang Xiaolong, Yan Wen, et al, 2021. Late Triassic dacites from Well NK-1 in the Nansha Block: Constraints on the Mesozoic tectonic evolution of the southern South China Sea margin[J]. Lithos, 398: 106337.
[35]	Miller K G, Browning J V, Schmelz W J, et al, 2020. Cenozoic sea-level and cryospheric evolution from deep-sea geochemical and continental margin records[J]. Science Advances, 6(20): eaaz1346.
[36]	Milliman J D, 1993. Production and accumulation of calcium carbonate in the ocean: Budget of a nonsteady state[J]. Global Biogeochemical Cycles, 7(4): 927-957.
[37]	Morley C K, 2016. Major unconformities/termination of extension events and associated surfaces in the South China Seas: Review and implications for tectonic development[J]. Journal of Asian Earth Sciences, 120: 62-86.
[38]	Renema W, Pandolfi J M, Kiessling W, et al, 2016. Are coral reefs victims of their own past success?[J]. Science Advances, 2(4): e1500850.
[39]	Sandin S A, McNamara D E, 2012. Spatial dynamics of benthic competition on coral reefs[J]. Oecologia, 168(4): 1079-1090.
[40]	Shao Lei, Cui Yuchi, Qiao Peijun, et al, 2017a. Sea-level changes and carbonate platform evolution of the Xisha Islands (South China Sea) since the Early Miocene[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 485: 504-516.
[41]	Shao Lei, Li Qianyu, Zhu Weilin, et al, 2017b. Neogene carbonate platform development in the NW South China Sea: Litho-, bio- and chemo-stratigraphic evidence[J]. Marine Geology, 385: 233-243.
[42]	Wan Shiming, Kürschner W M, Clift P D, et al, 2009. Extreme weathering/erosion during the Miocene Climatic Optimum: Evidence from sediment record in the South China Sea[J]. Geophysical Research Letters, 36(19): 2009GL040279.
[43]	Wang Pinxian, Li Qianyu, 2009. The South China Sea: Paleoceanography and Sedimentology[M]. Dordrecht: Springer.
[44]	Wang Yasu, Jiang Shijun, 2020. Variation in middle-late Miocene sedimentation rates in the northern South China Sea and its regional geological implications[J]. Marine Micropaleontology, 160: 101911.
[45]	Warny S, Askin R A, Hannah M J, et al, 2009. Palynomorphs from a sediment core reveal a sudden remarkably warm Antarctica during the middle Miocene[J]. Geology, 37(10): 955-958.
[46]	Wu Feng, Xie Xinong, Zhu Youhua, et al, 2021. Early development of carbonate platform (Xisha Islands) in the northern South China Sea[J]. Marine Geology, 441: 106629.
[47]	Wu Shiguo, Zhang Xinyuan, Yang Zhen, et al, 2016. Spatial and temporal evolution of Cenozoic carbonate platforms on the continental margins of the South China Sea: Response to opening of the ocean basin[J]. Interpretation, 4(3): SP1-SP19.
[48]	Xie Zhiyuan, Sun Longtao, Pang Xiong, et al, 2017. Origin of the Dongsha event in the South China Sea[J]. Marine Geophysical Research, 38(4): 357-371.
[49]	Yamamoto K, Iryu Y, Sato T, et al, 2006. Responses of coral reefs to increased amplitude of sea-level changes at the Mid-Pleistocene Climate Transition[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 241(1): 160-175.
[50]	Yao Yongjian, Liu Hailing, Yang Chupeng, et al, 2012. Characteristics and evolution of Cenozoic sediments in the Liyue Basin, SE South China Sea[J]. Journal of Asian Earth Sciences, 60: 114-129.
[51]	Yi Liang, Deng Chenglong, Yan Wen, et al, 2021. Neogene-quaternary magnetostratigraphy of the biogenic reef sequence of core NK-1 in Nansha Qundao, South China Sea[J]. Science Bulletin, 66(3): 200-203.
[52]	Yi Liang, Jian Zhimin, Liu Xinyu, et al, 2018. Astronomical tuning and magnetostratigraphy of Neogene biogenic reefs in Xisha Islands, South China Sea[J]. Science Bulletin, 63(9): 564-573.
[53]	Young J R, 1998. Neogene[M]// Bown P R. Calcareous nannofossil biostratigraphy. Dordrecht: Springer: 225-265.
[54]	Yu Kefu, Zhao Jianxin, 2009. Coral reefs[M]// Wang Pinxian, Li Qianyu. The South China Sea: Paleoceanography and Sedimentology. Dordrecht: Springer: 229-255.
[55]	Zachos J, Pagani M, Sloan L, et al, 2001. Trends, rhythms, and aberrations in global climate 65 Ma to present[J]. Science, 292(5517): 686-693.
[56]	Zeng Lili, Wang Dongxiao, Chen Ju, et al, 2016. SCSPOD14, a South China Sea physical oceanographic dataset derived from in situ measurements during 1919-2014[J]. Scientific Data, 3: 160029.
[57]	Zhao Meixia, Zhong Yu, Zhang Shuqi, et al, 2022. Coral community of Holocene coral reef in the southern South China Sea and its significance for reef growth[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 602: 111152.

时代	化石类型	化石带	生物地层事件	深度/m	年龄/Ma	阶段	参考文献
更新世	钙质超微化石	NN21	Emiliania huxleyi初现面	19.2	0.29	4	Gradstein等(2012)
更新世	浮游有孔虫	PL6	Globigerinoides extremus末现面	200.8	2.40	3	秦国权(2002)
上新世	浮游有孔虫	PL5	Globoquadrina altispira末现面	210.5	2.80
中新世	浮游有孔虫	M12	Globoquadrina dehiscens末现面	469.4	10.00
	钙质超微化石	NN7	Cyclicargolithus floridanus末现面	562.9	11.85	2	Gradstein等(2012)
	钙质超微化石	NN6/5	Sphenolithus heteromorphus末现面	562.9	13.53
	钙质超微化石	NN4	Sphenolithus heteromorphus初现面	845.6	17.71

南沙群岛新近纪碳酸盐台地中的微体化石及其意义^*

Microfossils in the Neogene carbonate platform of Nansha Islands and their significance^*

RichHTML

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

图/表 9

参考文献 57

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	罗云, 黎刚, 张喜洋, 徐维海, 朱小畏, 周婉秋, 黄慧文, 钟福昌, 颜文. 基于美济礁深钻的南海岛礁差异白云石化过程研究[J]. 热带海洋学报, 2026, 45(5): 108-127.
[2]	朱小畏, 莫梓谊, 茅晟懿, 田雨杭, 罗云, 苗莉, 徐维海, 黎刚, 颜文. 南沙美济礁南科1井生物标志物组成分布特征及其环境指示^*[J]. 热带海洋学报, 2026, 45(5): 162-177.
[3]	黎刚, 徐维海, 罗云, 刘建国, 赵建新, 俸月星, 程俊, 孙珍, 向荣, 徐敏, 颜文. 基于南沙美济礁深钻的南海南部新生代构造演化研究[J]. 热带海洋学报, 2026, 45(5): 16-34.
[4]	刘建国, 黄云, 徐维海, 黎刚, 向荣, 苏翔, 罗云, 赵中贤, 颜文. 南海美济珊瑚礁的形成与演化^*[J]. 热带海洋学报, 2026, 45(5): 94-107.
[5]	苗秀全, 张运迎, 颜文. 海扩张机制的制约^*[J]. 热带海洋学报, 2026, 45(5): 35-52.
[6]	邸鹏飞, 李牛, 宫尚桂, Jörn Peckmann, 王淑红, 陈多福, 颜文. 碳酸盐结合硫酸盐记录海水硫酸盐的δ³⁴S和δ¹⁸O: 来自南海南部礁相碳酸盐岩的启示^*[J]. 热带海洋学报, 2026, 45(5): 178-198.
[7]	李东平, 石豪磊, 罗中原, 曹建涛, 贾国东. 南海表层水悬浮颗粒物脂肪酸组成特征及其生态指示意义^*[J]. 热带海洋学报, 2026, 45(3): 61-73.
[8]	张云帆, 唐丹玲, 孙珍, 邱宁. 南海U形海疆线的地质构造特征研究[J]. 热带海洋学报, 2026, 45(3): 10-24.
[9]	李开枝, 黄良民, 尹健强, 连喜平, 柳原, 谭烨辉. 我国南海浮游动物生态学研究回顾与展望[J]. 热带海洋学报, 2026, 45(2): 1-15.
[10]	梁顺, 黄桂槟, 何国梅, 张永垂, 周毅, 汪洋, 洪梅. 南海土台风时空变化特征分析[J]. 热带海洋学报, 2026, 45(2): 59-70.
[11]	陈钰宸, 付东洋, 陶邦一, 李姬喆, 祝依娴, 刘贝, 林烨, 柴霞. 南海典型岛礁浅海地形遥感监测及时序变化研究^*[J]. 热带海洋学报, 2025, 44(5): 140-153.
[12]	朱小宇, 杨华, 毛蓓蓓, 郑雨轩. 南海东北部深层次的细结构观测与湍流混合研究^*[J]. 热带海洋学报, 2025, 44(5): 22-30.
[13]	李若安, 李旭清, 陈天然. 南海南部珊瑚骨骼δ¹⁸O和Sr/Ca对ENSO的分级响应[J]. 热带海洋学报, 2025, 44(4): 45-55.
[14]	周志乾, 连喜平, 谭烨辉. 南海磷虾科长螯磷虾属Stylocheiron——新纪录种的形态特征^*[J]. 热带海洋学报, 2025, 44(3): 66-71.
[15]	熊鑫, 冯英辞, 杨仁辉, 孙杰, 李健, 詹文欢, 吕开云. 基于声学背散射数据的南海北部东沙海域内孤立波特征研究^*[J]. 热带海洋学报, 2025, 44(3): 14-23.

南沙群岛新近纪碳酸盐台地中的微体化石及其意义*

Microfossils in the Neogene carbonate platform of Nansha Islands and their significance*

RichHTML

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

图/表 9

参考文献 57

相关文章 15

Metrics

本文评价

推荐阅读 0

南沙群岛新近纪碳酸盐台地中的微体化石及其意义^*

Microfossils in the Neogene carbonate platform of Nansha Islands and their significance^*