热带海洋学报 ›› 2022, Vol. 41 ›› Issue (1): 143-157.doi: 10.11978/2021013CSTR: 32234.14.2021013
罗云1,2,3(), 黎刚1,2(
), 徐维海1,2, 程俊1,2,3, 刘建国1,2, 颜文1,2,3(
)
收稿日期:
2021-02-02
修回日期:
2021-05-13
出版日期:
2022-01-10
发布日期:
2021-05-21
通讯作者:
黎刚,颜文
作者简介:
罗云(1992—), 河南信阳市人, 博士研究生, 主要从事珊瑚礁碳酸盐岩研究。email: 基金资助:
LUO Yun1,2,3(), LI Gang1,2(
), XU Weihai1,2, CHENG Jun1,2,3, LIU Jianguo1,2, YAN Wen1,2,3(
)
Received:
2021-02-02
Revised:
2021-05-13
Online:
2022-01-10
Published:
2021-05-21
Contact:
LI Gang,YAN Wen
Supported by:
摘要:
珊瑚礁地层中的暴露面是海平面变化的忠实记录, 对地层层序的划分和研究珊瑚礁体的生长发育过程具有重要意义。本文基于手标本观察与薄片鉴定、碳氧同位素和矿物组成分析, 识别了南沙美济岛南科1井第四纪生物礁碳酸盐岩地层中的典型暴露面, 剖析了主要暴露面与海平面变化及珊瑚礁发育演化的关系。在南科1井(NK-1)第四纪地层中典型暴露面附近以出现大量溶蚀孔穴和红褐色或锈黄色钙质结核为特征, 其碳氧同位素偏负, 并富集Al、Th、Fe和稀土元素, 具有典型碳酸盐岩风化壳的特征。南科1井全新世礁体发育在晚更新世暴露面之上, AMS14C和U-Th年龄数据证实美济岛全新世珊瑚礁生长时段与南海其他珊瑚岛礁一致, 主要发育在8.2~4.7ka时期, 该时段海平面的缓慢上升为珊瑚礁连续垂向生长提供了有利环境。Sr同位素和古地磁年龄标定的南科1井更新世地层中的主要暴露面时代与南沙永暑礁和西沙群岛珊瑚礁地层中的暴露面时代基本一致, 主要暴露面对应于全球第四纪低海平面时期。
中图分类号:
罗云, 黎刚, 徐维海, 程俊, 刘建国, 颜文. 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, 2022, 41(1): 143-157.
LUO Yun, LI Gang, XU Weihai, CHENG Jun, LIU Jianguo, YAN Wen. Characteristics of Quaternary exposure surfaces in Well Nanke-1 and their relationship with sea-level changes[J]. Journal of Tropical Oceanography, 2022, 41(1): 143-157.
图3
岩心手标本和镜下薄片显示的南科1井第四系暴露面特征 a. 暴露面/不整合面(20.2m; 上部为松散生物碎屑, 下部为固结珊瑚礁灰岩); b. 暴露面(28.5m; 受铁质侵染, 发育有红褐色钙质结壳, 溶蚀孔洞发育); c. 暴露面(85.6m; 钙质结核和溶蚀孔洞发育, 孔洞内部发育瘤状结核构造, 结核排列不规则, 表面光滑); d. 暴露面/不整合面(120m; 上部为珊瑚礁灰岩, 下部为珊瑚礁白云岩, 二者结合处为缝合线构造); e. 暴露面(128m; 钙质结核和溶蚀孔洞发育); f. 暴露面(185m; 上部为珊瑚骨架灰岩, 岩心表面多见珊瑚骨架和生物壳体铸模, 溶蚀孔洞发育); g. 暴露面(210m; 岩心破碎, 碎屑分选差, 表面呈黄褐色); h. 生屑灰岩(87m; 生物碎屑被溶蚀形成亮晶, 部分溶孔受铁质侵染呈黄褐色); i. 粒泥灰岩 (85.8m; 生物骨架被溶蚀, 溶孔发育, 孔内形成悬垂状方解石); j. 珊瑚骨架灰质白云岩(165m; 珊瑚格架被亮晶或泥晶充填); k. 泥晶白云岩(214m)。C: 钙质结壳; NC: 瘤状结核构造, 亦称葡萄状构造; SL: 缝合线构造; CS: 珊瑚骨架; BM: 生物壳体铸模"
表2
南科1井珊瑚样品的U-Th测年结果"
样品编号 | 深度/m | U/ppm | 232Th/ppb | (230Th/232Th) | (230Th/238U) | (234U/238U) | 230Th年龄/a | 日历年龄/ a BP | δ234U | |
---|---|---|---|---|---|---|---|---|---|---|
未校正 | 校正 | |||||||||
U-Th-01 | 5.1 | 2.5862±0.0013 | 0.251±0.001 | 1547.46±6.62 | 0.0495±0.0002 | 1.1472±0.0013 | 4807±17 | 4804±17 | 4735 | 147.2±1.3 |
U-Th-02 | 7.2 | 3.1834±0.0015 | 1.666±0.011 | 315.15±2.90 | 0.0544±0.0004 | 1.1447±0.0013 | 5299±36 | 5286±36 | 5217 | 144.7±1.3 |
U-Th-03 | 7.5 | 2.8472±0.0008 | 1.620±0.003 | 290.52±2.12 | 0.0545±0.0004 | 1.1450±0.0010 | 5311±38 | 5296±39 | 5227 | 145.0±1.0 |
U-Th-04 | 10.8 | 2.8481±0.0011 | 7.352±0.013 | 66.37±0.40 | 0.0565±0.0003 | 1.1449±0.0009 | 5509±33 | 5442±46 | 5373 | 144.9±0.9 |
U-Th-05 | 19.0 | 2.5728±0.0011 | 0.424±0.001 | 1530.45±8.47 | 0.0831±0.0004 | 1.1446±0.0015 | 8203±43 | 8198±43 | 8129 | 144.6±1.5 |
表3
南科1井上部220m岩心的Sr同位素测年结果"
样品编号 | 深度/m | 87Sr/86Sr | 2σ | 平均年龄/Ma |
---|---|---|---|---|
NK1-Sr-01 | 30.9 | 0.709183 | 0.000008 | 0.07 |
NK1-Sr-02 | 40.5 | 0.709171 | 0.000009 | 0.13 |
NK1-Sr-03 | 48.0 | 0.709163 | 0.000010 | 0.40 |
NK1-Sr-04 | 56.5 | 0.709160 | 0.000009 | 0.49 |
NK1-Sr-05 | 61.2 | 0.709153 | 0.000009 | 0.65 |
NK1-Sr-06 | 65.3 | 0.709140 | 0.000009 | 1.00 |
NK1-Sr-07 | 70.2 | 0.709126 | 0.000009 | 1.20 |
NK1-Sr-08 | 85.6 | 0.709118 | 0.000008 | 1.29 |
NK1-Sr-09 | 89.8 | 0.709117 | 0.000011 | 1.30 |
NK1-Sr-10 | 109.9 | 0.709105 | 0.000009 | 1.45 |
NK1-Sr-11 | 118.1 | 0.709100 | 0.000009 | 1.55 |
NK1-Sr-12 | 123.1 | 0.709130 | 0.000009 | 1.63 |
NK1-Sr-13 | 125.3 | 0.709123 | 0.000008 | 1.65 |
NK1-Sr-14 | 125.8 | 0.709140 | 0.000009 | 1.67 |
NK1-Sr-15 | 130.2 | 0.709141 | 0.000010 | 1.70 |
NK1-Sr-16 | 138.1 | 0.709130 | 0.000009 | 1.71 |
NK1-Sr-17 | 143.6 | 0.709111 | 0.000011 | 1.80 |
NK1-Sr-18 | 163.6 | 0.709086 | 0.000008 | 1.87 |
NK1-Sr-19 | 178.2 | 0.709070 | 0.000009 | 2.15 |
NK1-Sr-20 | 187.9 | 0.709072 | 0.000009 | 2.35 |
NK1-Sr-21 | 200.5 | 0.709068 | 0.000010 | 2.40 |
NK1-Sr-22 | 204.2 | 0.709064 | 0.000009 | 2.45 |
NK1-Sr-23 | 210.2 | 0.709057 | 0.000010 | 2.50 |
NK1-Sr-24 | 222.0 | 0.709063 | 0.000011 | 2.55 |
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