Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

WANG Yin; LI XiangHui; ZHOU Yong; LIU Ling

doi:10.14027/j.cnki.cjxb.2015.01.012

Volume 33 Issue 1

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WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012

Citation:

WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012

Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

doi: 10.14027/j.cnki.cjxb.2015.01.012

1.
TEAM 814 East China Mineral Exploration and Development Bureau, Nanjing 210007;
2.
State Key Laboratory of Mineral Deposit Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093;
3.
402th Geological Survey, Sichuan Bureau of Geology and Mineral Resources, Chengdu 611730

Received Date: 2013-12-09
Rev Recd Date: 2014-05-26
Publish Date: 2015-02-10

Abstract

According to relative content of terrigenous clastic rock's components (clay minerals of claystone and clastic composition of sandstone), analyzing paleoclimate of Late Cretaceous - Paleocene Nanxiong Basin in northern Guangdong and southern Jiangxi. The climate index of sandstone clastic components (feldspar/quartz, F/Q) is between 0.02 to 0.14; Clay mineral assemblage is mainly illite, with an average of 79%; Illite crystallinity index and chemical index is 0.25~0.39 and 0.31~0.7. During this period, the climate of the study area is mainly arid climate, with some warm and humid climate intermittent, paleoclimate can be divided into three stages: arid-semiarid Maastrichtian, warm and moist semiarid early Danian, and the semiarid late Danian. Climate evolution is consistent with the same period of global climate change.
- F/Q ratio,
- clay mineral,
- paleoclimate,
- Late Cretaceous,
- Paleocene,
- Nanxiong Basin

References

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[48]	Vanderaveroet P. Miocene to Pleistocene clay mineral sedimentation on the New Jersey shelf [J]. Oceanologica Acta, 2000, 23(1): 25-36.
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[50]	Winkler A, Wolf-Welling T, Stattegger K, et al. Clay mineral sedimentation in high northern latitude deep-sea basins since the Middle Miocene(ODP Leg 151, NAAG) [J]. International Journal of Earth Sciences, 2002, 91(1): 133-148.
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[53]	Chamley H. Clay Sedimentology [M]. Berlin: Springer-Verlag, 1989.
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[55]	Boero V, Premoli A, Melis P, et al. Influence of climate on the iron oxidemineralogy of Terra Rossa [J]. Clays and Clay Minerals, 1992, 40(1): 8-13.
[56]	蓝先洪. 海洋沉积物中粘土矿物组合特征的古环境意义[J]. 海洋地质动态,2001,17(1): 4-7.[Lan Xianhong. Marine sediments of clay mineral assemblages paleoenvironmental significance [J]. Marine Geology Development, 2001, 17(1): 4-7.]
[57]	陈涛,王欢,张祖青,等. 粘土矿物对古气候指示作用浅析[J]. 岩石矿物学杂志,2003,22(4): 416-420.[Chen Tao, Wang Huan, Zhang Zuqing, et al. Clay minerals as indicators of paleoclimate [J]. Acta Petrologica et Mineralogica, 2003, 22(4): 416-420.]
[58]	Thiry M. Palaeoclimatic interpretation of clay minerals in marine deposits: an outlook from the continental origin [J]. Earth-Science Reviews, 2000, 49(1/2/3/4): 201-221.
[59]	Keller G. The end-Cretaceous mass extinction in the marine realm: year 2000 assessment [J]. Planetary and Space Science, 2001, 49(8): 817-830.
[60]	张显球,李罡. 广东南雄盆地罗佛寨群的介形类动物群[J]. 微体古生物学报,2008,25(1): 44-77.[Zhang Xianqiu, Li Gang. Ostracod faunas from the Luofozhai Group in the Nanxiong Basin of Guangdong province, China[J]. Acta Micropalaeontologica Sinica, 2008, 25(1): 44-77.]
[61]	Erben H K, Ashraf A R, Boehm H, et al. Die Kreide/Tertiär-Grenze im Nanxiong-Becken: Kontinentalfazies, SüdostChina = The Cretaceous/Tertiary boundary in the Nanxiong-Basin: continental facies, SE-China [M]. Stuttgart: F. Steiner,1995: 32.
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[63]	赵资奎,严正. 广东南雄盆地白垩系—第三系界线剖面恐龙蛋壳稳定同位素记录: 地层及古环境意义[J]. 中国科学(D 辑),2000,30(2): 135-141.[Zhao Zikui, Yan Zheng. Nanxiong Cretaceous-Tertiary boundary section of dinosaur eggs stable isotope record: stratigraphic and paleoenvironmental significance[J].Science in China (Series D), 2000, 30(2): 135-141.]
[64]	Gradstein F M, Ogg J G, Kranendonk M. On the geologic time scale 2008 [J]. Newsletters on Stratigraphy, 2008, 43(1): 5-13.
[65]	Clyde W C, Ting S, Snell K E, et al. New paleomagnetic and stable-isotope results from the Nanxiong Basin, China: Implications for the K/T boundary and the timing of paleocene mammalian turnover [J]. The Journal of Geology, 2010, 118(2): 131-143.
[66]	Boucot A J,陈旭,Scotese C R,等. 显生宙全球古气候重建[M]. 北京: 科学出版社,2009.[Boucot A J, Chen Xu, Scotese C R, et al. Phanerozoic Global Paleoclimate Reconstruction [M]. Beijing: Science Press, 2009.]

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沈阳化工大学材料科学与工程学院沈阳 110142

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Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

1. TEAM 814 East China Mineral Exploration and Development Bureau, Nanjing 210007;

2. State Key Laboratory of Mineral Deposit Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093;

3. 402th Geological Survey, Sichuan Bureau of Geology and Mineral Resources, Chengdu 611730

Received Date: 2013-12-09

Rev Recd Date: 2014-05-26

Publish Date: 2015-02-10

Key words:

Abstract: According to relative content of terrigenous clastic rock's components (clay minerals of claystone and clastic composition of sandstone), analyzing paleoclimate of Late Cretaceous - Paleocene Nanxiong Basin in northern Guangdong and southern Jiangxi. The climate index of sandstone clastic components (feldspar/quartz, F/Q) is between 0.02 to 0.14; Clay mineral assemblage is mainly illite, with an average of 79%; Illite crystallinity index and chemical index is 0.25~0.39 and 0.31~0.7. During this period, the climate of the study area is mainly arid climate, with some warm and humid climate intermittent, paleoclimate can be divided into three stages: arid-semiarid Maastrichtian, warm and moist semiarid early Danian, and the semiarid late Danian. Climate evolution is consistent with the same period of global climate change.

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Reference (66)

[1]	Bocherens H, Friis E M, Mariotti A, et al. Carbon isotopic abundances in Mesozoic and Cenozoic fossil plants: Palaeoecological implications [J]. Lethaia, 1994, 26(4): 347-358.
[2]	洪汉烈,于娜,薛惠娟,等. 临夏盆地晚更新世沉积物黏土矿物的特征及其古气候指示[J]. 现代地质,2007,21(2):406-414.[Hong Hanlie, Yu Na, Xue Huijuan, et al. Clay mineralogy and its palaeoclimatic indicator of the Late Pleistocene in Linxia Basin [J]. Geoscience, 2007, 21(2): 406-414.]
[3]	李祥辉,徐宝亮,陈云华,等. 华北—东北南部地区中生代中晚期粘土矿物与古气候[J]. 地质学报,2008,82(5):683-691.[Li Xianghui, Xu Baoliang, Chen Yunhua, et al. Clay minerals of the Middle-Late Mesozoic mudrocks from North and Northeast China: Implications to paleoclimate and paleohighland [J]. Acta Geologica Sinica, 2008, 82(5): 683-691.]
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Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

doi: 10.14027/j.cnki.cjxb.2015.01.012

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