Distribution characteristics and paleo-climatic significance of continental climate-sensitive sediments in the Late Cretaceous in China

Authors

Bin XU, Hebei State Key Laboratory of Mine Disaster Prevention, North China Institute of Science and Technology, Beijing 101601, China
Fang XIANG, State Key Laboratory of Oil &Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaFollow
Shuxia LI, School of Geoscience and Surveying Engineering, China University of Mining and Technology(Beijing), Beijing 100083, China

Abstract

The Cretaceous is a typical period for studying the greenhouse climate and the earth system interactions, and the world's most extensive terrestrial strata are mainly in East Asia, especially in China. Continental sediments can effectively reflect the paleo-climate change, but the previous studies of the Late Cretaceous paleo-climate, based on the combined characteristics of continental climate-sensitive sediments, were barely found in China. To obtain the Late Cretaceous paleo-climate characteristics of China, the distribution characteristics of different continental climate-sensitive sediment types in the early, middle and Late Cretaceous in China were studied in detail. According to the distribution and combination characteristics and types of continental climate-sensitive sediments, seven climate types can be divided: 1) warm-humid and warm-dry climate; 2) hot and dry climate; 3) hot-dry and arid climate; 4) hot-dry and semiarid climate; 5) hot-dry and hot-wet climate; 6) hot-dry and warm-humid climate; 7) hot-dry and warm-dry climate. The results show that in the early Late Cretaceous, the hot and dry climate was the most widespread, followed by warm-humid and warm-dry climate, but the climate was drier than the paleo-climate of the previous study of Early Cretaceous. Hot and dry climate zone became wider in the Coniacian and Maastrichtian; furthermore, it covered Xinjiang to the east of China from east to west after the Santonian Period. The hot-dry and semiarid climate zone was nearly latitudinally distributed from the northwest to the southeast and it shows a further increase in aridification. Global geological events, paleogeographic features and regional tectonic evolution had significant impacts on the paleoclimate of China in the Late Cretaceous, such as global eruptive events of volcanoes led to the temperature increase in China in the early Late Cretaceous; coastal mountain ranges in southeastern China led to the drying of the Late Cretaceous climate in southern China; Xuefeng Mountains, Wuling Mountains, Nanling Mountains and Tai-hang Mountains were the dividing line between the hot and dry climate zone and hot-dry and arid climate zone in the early Late Cretaceous, and Altun Mountains were the dividing line between the southeastern section of the hot and dry climate zone in western China in the middle Late Cretaceous.

Keywords

Late Cretaceous, continental, climate-sensitive sediments, China, climate type, influence factor

DOI

10.3969/j.issn.1001-1986.2021.05.021

Recommended Citation

Bin XU, Fang XIANG, Shuxia LI, et al. (2021) "Distribution characteristics and paleo-climatic significance of continental climate-sensitive sediments in the Late Cretaceous in China," Coal Geology & Exploration: Vol. 49: Iss. 5, Article 22.
DOI: 10.3969/j.issn.1001-1986.2021.05.021
Available at: https://cge.researchcommons.org/journal/vol49/iss5/22

Reference

[1] WANG Chengshan, CAO Ke, HUANG Yongjian. Sedimentary record and Cretaceous earth surface system changes[J]. Earth Science Frontiers, 2009, 16(5): 1-14.

[2] SKELTON P, SPICER R, KELLEY S, et al. The Cretaceous world[M]. Cambridge: Cambridge University Press, 2003.

[3] YANG Weidong, CHEN Nansheng, NI Shijun, et al. Cretaceous red beds carbonate rocks and the composition of dinosaur eggshell by carbon and oxygen isotope and its environmental significance[J]. Chinese Science Bulletin, 1993, 38(23): 2161-6163.

[4] CAO Ke, LI Xianghui, WANG Chengshan. Paleoclimate indicator and quantitative determination of paleotemperature in the Cretaceous red beds[J]. Acta Geologica Sichuan, 2006, 26(4): 198-209.

[5] FRIEDMAN M, TARDUNO J A, BRINKMAN D B. Fossil fishes from the high Canadian Arctic: Further palaeobiological evidence for extreme climatic warmth during the Late Cretaceous(Turonian-Coniacian)[J]. Cretaceous Research, 2003, 24(6): 615-632.

[6] HASEGAWA T. A global carbon-isotope event in the Middle Turonian(Cretaceous) sequences in Japan and Russian Far East[J]. Proceedings of the Japan Academy, 2003, 79(6). Doi: 10.2183/pjab.79B.141

[7] TSIKOS H, JENKYNS H C, WALSWORTH-Bell B, et al. Carbon-isotope stratigraphy recorded by the Cenomanian-Turonian Oceanic Anoxic Event: Correlation and implications based on three key localities[J]. Journal of the Geological Society of London, 2004, 161(4): 711-719.

[8] GRCKE D R, HESSELBO S P, JENKYNS H C. Carbon-isotope composition of Lower Cretaceous fossil wood: Ocean-atmosphere chemistry and relation to sea-level change[J]. Geology, 1999, 27(2): 155-158.

[9] WAN Xiaoqiao, LI Gang, HUANG Qinghua, et al. Division and correlation of Terrestrial Cretaceous stages in China[J]. Journal of Stratigraphy, 2013, 37(4): 457-470.

[10] CAO Ke. Cretaceous Terrestrial stratigraphic correlation in China[J]. Geological Review, 2013, 59(1): 24-40.

[11] CHEN Peiji. Coastal Mountains of SE China, desertization and saliniferous lakes of Central China during the Upper Cretaceous[J]. Journal of Stratigraphy, 1997, 21(3): 203-213.

[12] YIN Hongfu. Paleobiogeography of China[M]. Beijing: China University of Geosciences Press, 1988.

[13] LIU Zhaojun, WANG Dongpo, LIU Li, et al. Sedimentary characteristics of the Cretaceous Songliao Basin[J]. Acta Geologica Sinica, 1992, 66(4): 327-338.

[14] WANG Hongzhen, LI Sennan, LIU Benpei. Tectonopalaeogeography and Palaeobiogeography of China and adjacent Regions[M]. Beijing: China University of Geosciences Press, 1990.

[15] WU Genyao. Cretaceous: A key transition period of the plate tectonic evolution in China and its adjacent areas[J]. Geology in China, 2006, 33(1): 64-77.

[16] CAI Youxian. Cretaceous paleoclimate, sedimentary environment and oil-gas prospect in the Hetao Basin, Inner Mongolia[J]. Geological Review, 1990, 36(2): 105-115.

[17] ZHAO Xiwen. Paleo-climate Science Foundation[M]. Beijing: Geological Publishing House, 1992.

[18] PEI Junling, YANG Zhenyu, ZHAO Yue, et al. Cretaceous paleomagnetism of the northeast China and adjacent regions and the geodynamic setting of block rotations[J]. Acta Geologica Sinica, 2009, 83(5): 617-627.

[19] TIAN Xin, XIANG Fang, LUO Lai, et al. Climate significance of continental special deposits[J]. Earth Science Frontiers, 2009, 16(5): 71-78.

[20] XIANG Fang, SONG Jianchun, LUO Lai, et al. Distribution characteristics and climate significance of continental special deposits in the Early Cretaceous[J]. Earth Science Frontiers, 2009, 16(5): 48-62.

[21] BOUCOT A, XU Chen, SCOTESE C R. Phanerozoic Paleoclimate: An atlas of lithologic indicators of climate[M]. Society for Sedimentary Geology, 2013.

[22] CHUMAKOV N M. Climatic zones in the middle of the Cretaceous Period[J]. Stratigr. Geol. Korrelyatsiya, 1995, 3: 3-14.

[23] HAY W W, FLOEGEL S. New thoughts about the Cretaceous climate and oceans[J]. Earth-Science Reviews, 2012, 115(4): 262-272.

[24] LIU Yongqing, KUANG Hongwei, PENG Nan, et al. Sedimentary facies of dinosaur trackways and bonebeds in the Cretaceous Jiaolai Basin, eastern Shandong, China, and their paleogeographical implications[J]. Earth Science Frontiers, 2011, 18(4): 9-24.

[25] WANG Licheng, WEI Yushuai. Apatite fission track thermochronology evidence for the Mid-Cretaceous tectonic event in the Qiangtang Basin Tibet[J]. Acta Petrologica Sinica, 2013, 29 (3): 1039-1047.

[26] CAO Ke. Cretaceous continental sedimentology and Paleogeography in China[D]. Beijing: China University of Geosciences(Beijing), 2010.

[27] CAO Shulu, ZHU Zhijun, LIU Teng, et al. Δ13C and δ18O Values of the Cretaceous Zhoutian Formation in the Xinjiang Basin[J]. Acta Geologica Sichuan, 2016, 36(3): 506-520.

[28] CHENG Shoutian, LI Zhide, HUANG Yanqiu. Discovery and Its Genetic Evidences of Early Cretaceous Glacial Debris Flow in The Northeast Margin of Ordos[J]. Geological Science and Technology Information, 2002, 21(2): 36-40.

[29] WANG Dongpo, RAKES L A. The discovery and significance of cretaceous ice-rafting deposits in Songliao Basin[J]. Journal of Changchun University of Earth Sciences, 1996, 26(4): 382-387.

[30] CHAMLEY H. Clay sedimentology[M]. Berlin: Spring Verlag, 1989.

[31] 《Chinese stratigraphic code》Editorial board. Chinese stratigraphic code Jurassic[M]. Beijing: Geological Publishing House, 2000.

[32] WANG Xiaofeng, CHEN Xiaohong. Stratigraphic division and correlation of various geological ages in China[M]. Beijing: Geological Publishing House, 2005.

[33] ZIEGLER A, ESHEL G, REES P M, et al. Tracing the tropics across land and sea: Permian to present[J]. Lethaia, 2003, 36(3): 227-254.

[34] BAOYIN Y, ZHENGKAI X, BAOSHENG L, et al. Chronostratigraphy and stratigraphic division of red soil in Southern China[J]. Quaternary Sciences, 2008, 28(1): 1-13.

[35] BOUCOT A J, CHEN Xu, SCOTESE C R, et al. Reconstruction of Phanerozoic global Paleoclimate[M]. Beijing: Science Press, 2009.

[36] YAO Tong, IBARRA D E, CAVES J K, et al. Constraining basin thermal history and petroleum generation using palaeoclimate data in the Piceance Basin, Colorado[J]. Basin Research, 2017, 29(4): 542-553.

[37] CHEN Genwen, XIA Bin, WU Yanzhi, et al. Controls of sedimentary rock on sandstone hosted copper deposits in Chuxiong Basin[J]. Journal Petrol, 2002, 22(3): 24-28.

[38] CHEN Zhong, MA Haizhou, Cao Guangchao, et al. The discussion about the relationship between carbonate in loess and climate environment[J]. Yunnan Geographic Environment Research, 2007, 19(3): 7-10.

[39] CARROLL A R, BOHACS K.M. Lake-type controls on petroleum source rock potential in nonmarine basin[J]. AAPG Bulletin, 2001, 85(6): 1039-1053.

[40] HUANG Qinghua, ZHENG Yulong, YANG Mingjie, et al. On Cretaceous paleoclimate in the Songliao Basin[J]. Acta Micropalaeontologica Sinica, 1999, 16(1): 95-103.

[41] XIANG Fang, ZHANG Deyan, CHEN Kang, et al. Early Cretaceous paleoclimate characteristics of China: Clues from continental climate-indicative sediments[J]. Acta Geologica Sinica, 2015, 89(4): 1307-1318.

[42] JIANG Xinsheng, PAN Zhongxi, XU Jinsha, et al. Late Cretaceous aeolian dunes and reconstruction of palaeo-wind belts of the Xinjiang Basin, Jiangxi Province, China[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2008, 257(1/2): 58-66.

[43] LI Baosheng WEN Xiaohao, ZHANG D D, et al. Millennial-scale climate fluctuations during the last interstadial recorded in the AQS3 segment of the Aqiang loess section in the north piedmont of the Kunlun Mountains[J]. Quaternary Sciences, 2008, 28(1): 140-149.

[44] LIU Zhaojun, WANG Dongpo, LIU Li et al. Sedimentary Characteristics of the Cretaceous in the Songliao Basin[J]. Acta Geologica Sinica(English Edition), 1993, 6(2): 167-180.

[45] LUO Jinglan ZHANG Yunxiang. Petrologic study on the Late Neogene Hipparion red clay in the Middle Reaches of the Yellow River and implications for climatic evolution[J]. Acta Sedimentologica Sinica, 1999, 17(2): 214-220.

[46] XU Lei, CAO Yingchang, WANG Yanzhong, et al. Genetic model of salt-gypsum rock of Paleogene in Dongying depression and its relationship with hydrocarbon reservoir[J]. Journal of China University of Petroleum(Edition of Natural Science), 2008, 32(3): 30-35.

[47] ZHU Guangyou, JIN Qiang, ZHANG Shuichang, et al. Characteristics and origin of deep lake oil shale of the Shahejie Formation of Paleogene in Dongying Sag, Jiyang Depression[J]. Journal of Palaeogeography, 2005, 7(1): 59-69.

[48] HE Shun, QIN Qirong, FAN Cunhui, et al. Shale Reservoir characteristics and influencing factors of Wufeng-Longmaxi formation in Dingshan area, Southeast Sichuan[J]. Reservoir Evaluation and Development, 2019, 9(4): 61-67.

[49] YAN Huanrong, ZHU Jianwei, LI Dianchao. Formation condition and exploitation prospect of oil shale in Renziping exploration area, Qinxian Basin, Guangxi Province[J]. Journal of Jilin University(Earth Science Edition), 2006, 36(6): 986-990.

[50] ZHENG Jinping, ZHAO Yuanyi, LIU Junying. Quaternary saline lake deposition and paleoclimate[J]. Quaternary Sciences, 1998, 18(4): 297-307.

[51] SONG Zhichen, LI Wenben, HE Chengquan. Distribution of flora and organic rock in Cretaceous and Early Eogene in China[J]. Science in China(Series B), 1983, B(2): 169-176.

[52] WANG Daning, SUN Xiuyu, ZHAO Yingniang, et al. Late Cretaceous to Early Eogene Sporopollen assemblage sequence in some parts of China[J]. Geological Review, 1984, 30(1): 8-18.

[53] HUBER B T, HODELL D A, HAMILTON C P. Middle-Late Cretaceous climate of the southern high latitudes: Stable isotopic evidence for minimal equator-to-pole thermal gradients[J]. Geological Society of America Bulletin, 1995, 107(10): 1164-1191.

[54] WILSON K M P A, NORRIS R D, COOPER M J. Testing the Cretaceous greenhouse hypothesis using glassy foraminiferal calcite from the core of the Turonian tropics on Demerara Rise[J]. Geology, 2002, 30(7): 607-610.

[55] JENKYNS H C, GALE A S, CORFIELD R M. Carbon-and oxygen-isotope stratigraphy of the English Chalk and Italian Scaglia and its palaeoclimatic significance[J]. Geological Magazine, 1994, 131(01): 1-34.

[56] CLARKE L J, JENKYNS H C. New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere[J]. Geology, 1999, 27(8): 699.

[57] WIGNALL P B. Large igneous provinces and mass extinctions[J]. Earth Science Reviews, 2001, 53(1): 1-33.

[58] GUO Zhengfu, LIU Jiaqi. Research advance in effect of volcanism on climate changes[J]. Advance in Earth Sciences, 2002, 17(4): 595-604.

[59] JONES C E, JENKYNS H C. Seawater strontium isotopes, oceanic anoxic events, and seafloor hydrothermal activity in the Jurassic and Cretaceous[J]. American Journal of Science, 2001, 301(2): 112-149.

[60] LARSON R. Latest pulse of Earth: Evidence for a Mid-Cretaceous superplume[J]. Geology, 1991, 19: 547-550.

[61] LARSON R, ERBA E. Onset of the Mid-Cretaceous greenhouse in the Barremian-Aptian: Igneous events and the biological, sedimentary, and geochemical responses[J]. Paleoceanography, 1999, 14: 663-678.

[62] HU Xiumian. Greenhouse climate and ocean during Cretaceous[J]. Geology in China, 2004, 31(4): 442-448.

[63] HILDE T W C, UYEDA S, KROENKE L. Evolution of the western pacific and its margin[J]. Tectonophysics, 1977, 38(1/2): 145-165.

[64] YU Jingxian. Late Cretaceous sopro-pollen Assemblages of Shache Distict, Xinjiang[J]. Acta Geologica Sinica, 1981, 55(2): 93-102(in Chinese).

[65] TANG Shuangli. Late-Cretaceous and Cenozoic uplifting process of Xuefeng Mountain and its adjacent area: Evidence from apatite fission[D]. Beijing: China University of Geosciences(Beijing), 2011.

[66] BAI Daoyuan, HUANG Jianzhong, MENG Debao, et al. Meso-Cenozoic thermochronological analysis of the uplift process of mountains in southeast Hunan[J]. Acta Geoscientica Sinica, 2006, 27(6): 525-536.

[67] JOLIVET M, BRUNEL M, SEWARD D, et al. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan plateau: Fission-track constraints[J]. Tectonophysics, 2001, 343(1/2): 113-114.

[68] GE Xiaohong, LIU Yongjiang, REN Shoumai. Uplift dynamics of the Qinghai-Tibet Plateau and Altun fault[J]. Geology in China, 2002, 29(4): 346-350.

[69] LI Haibing, YANG Jingsui. Evidence for Cretaceous uplift of the northern Qinghai-Tibetan plateau[J]. Earth Science Frontiers, 2004, 11(4): 345-359.

[70] CHEN Yunhua. Late Cretaceous sedimentary responses to the "Coast Range" and Paleoclimate[D]. Chengdu: Chendu University of Technology, 2008.

[71] Compilation Group of regional stratigraphic tables in Fujian Province. Regional stratigraphic table of East China: Volume of Fujian Province[M]. Beijing: Geological Publishing House, 1979.

[72] Stratigraphic Paleontological Group of Fujian Petroleum Geological Team. Division of Cretaceous red beds in Western Fujian: Mesozoic Cenozoic red beds in South China[M]. Beijing: Science Press, 1979.