Sedimentary sequence and paleoclimate evolution of the Marinoan Glacier in the Daba Mountains: Evidence from petrology and geochemistry

PENG Zhoujun; LI Xiaogang; XIONG Guoqing; XIE Zhongping; FENG Xiangyou; CHEN Chunzhu; PENG Huixue; LIN Mao

doi:10.19826/j.cnki.1009-3850.2024.06003

Sedimentary Geology and Tethyan Geology > 2025 > 45(1): 69-89. > DOI: 10.19826/j.cnki.1009-3850.2024.06003

PENG Z J，LI X G，XIONG G Q，et al.，2025. Sedimentary sequence and paleoclimate evolution of the Marinoan Glacier in the Daba Mountains: Evidence from petrology and geochemistry[J]. Sedimentary Geology and Tethyan Geology，45(1)：69−89. DOI: 10.19826/j.cnki.1009-3850.2024.06003

Citation:

PDF (14155 KB)

Sedimentary sequence and paleoclimate evolution of the Marinoan Glacier in the Daba Mountains: Evidence from petrology and geochemistry

1.
College of Petroleum and Natural Gas Engineering, Chongqing University of Science and Technology, Chongqing 401331, China
2.
Chongqing Key Laboratory of Complex Oil and Gas Exploration and Development, Chongqing University of Science and Technology, Chongqing 401331, China
3.
Chengdu Center, China Geological Survey (Geosciences Innovation Center of Southwest China), Chengdu 610218, China
4.
Chongqing Gas Mine, Southwest Oil & Gas Field Company of PetroChina, Chongqing 400707, China

More Information

Received Date: March 02, 2024
Revised Date: April 09, 2024
Accepted Date: April 17, 2024

Graphical Abstract

Abstract

Abstract

There has been a long-standing debate that whether the earth was a "hard snowball" or a "slush snowball" during the Neoproterozoic Marinoan Ice Age. The glacial sediments of the Nantuo Formation from the Liangqiao section of Chengkou, in the Dabashan area, are complete with extensive development, providing an ideal target for studying the Marinoan glacial sedimentary sequence. Geochemical evidence is of great significance for reconstructing the late Neoproterozoic paleoclimate. The petrological characteristics of the Nantuo Formation show that it is predominantly composed of gray-green and gray-purple pebbly siltstone in the Daba Mountain area. The geochemical characteristics of the moraine deposits reveal that the Nantuo Formation in this area underwent low chemical weathering and was in a cold and dry climate. Paleoclimatic indicators, such as the chemical index of alteration (CIA), chemical index of weathering (CIW), and plagioclase index of alteration (PIA), exhibit clear cyclic variations. The gray-purple pebbly siltstone gradually decreases upwards from a high value in the bottom, while the gray-green pebbly siltstone gradually increases from bottom to top starting from a low value, implying multiple cold and warm paleoclimatic fluctuations in the early Nantuo period. Regional correlations and sedimentary patterns of the Nantuo Formation in the Yangtze area indicate that the Nantuo glacial period can be further divided into an early gradual freezing period, a middle frozen period, and a late thawing period. The climatic changes mainly occurred during the early and late Nantuo periods, especially in the shallow-water sedimentary areas. Therefore, evidence from the glacial sedimentary sequence and paleoclimatic variation of the Nantuo Formation supports the hypothesis that the earth was a "slush snowball" at the end of the Neoproterozoic era.
- Dabashan area,
- Marinoan Ice Age,
- sedimentary geochemistry,
- glacial sedimentary sequence,
- paleoclimatic evolution

FullText(HTML)

References (107)

References

[1]	Allen P A,Leather J,Brasier M D,2004. The Neoproterozoic Fiq glaciation and its aftermath,Huqf supergroup of Oman[J]. Basin Research,16(4):507 − 534. DOI: 10.1111/j.1365-2117.2004.00249.x
[2]	Allen P A,Etienne J L,2008. Sedimentary challenge to snowball Earth[J]. Nature Geoscience,1(12):817 − 825. DOI: 10.1038/ngeo355
[3]	Abbot D S,Voigt A,Koll D,2011. The Jormungand global climate state and implications for Neoproterozoic glaciations[J]. Journal of Geophysical Research:Atmospheres,116(D18):4121 − 4132.
[4]	安志辉,童金南,叶琴,等,2014. 峡东青林口地区新元古代地层序列及沉积演变[J]. 地球科学,39(7):795 − 806. An Z H,Tong J Y,Ye Q,et al.,2014. Neoproterozoic stratigraphic sequence and sedimentary evolution at Qinglinkou section,East Yangtze Gorges area[J]. Earth Science,39(7):795 − 806 (in Chinese with English abstract).
[5]	Ali D O,Spencer A M,Fairchild I J,et al.,2018. Indicators of relative completeness of the glacial record of the Port Askaig Formation,Garvellach Islands,Scotland[J]. Precambrian Research,319:65 − 78. DOI: 10.1016/j.precamres.2017.12.005
[6]	安志辉,叶琴,胡军,等,2023. 神农架成冰纪宋洛生物群的赋存层位厘定[J]. 地质科学,48(10):3799 − 3811. An Z H,Ye Q,Hu J,et al.,2023. Stratigraphic position of Cryogenian Songluo biota in Shennongjia area[J]. Chinese Journal of Geology,48(10):3799 − 3811 (in Chinese with English abstract).
[7]	Bodiselitsch B,Koeberl C,Master S,et al.,2005. Estimating duration and intensity of Neoproterozoic snowball glaciations from Ir anomalies[J]. Science,308(5719):239 − 242. DOI: 10.1126/science.1104657
[8]	Busfield M E,Le Heron D P,2014. Sequencing the Sturtian icehouse:dynamic ice behaviour in South Australia[J]. Journal of the Geological Society,171(3):443 − 456.
[9]	毕晨时,2015. 贵州南沱冰期海洋磷的地球化学[D]. 贵阳:贵州大学. Bi C S,2015. Marine Phosphours Geochemistry in Nantuo Ice Age in Southern China[D]. Guiyang:Guizhou University (in Chinese with English abstract).
[10]	Busfield M E,Le Heron D P,2016. A Neoproterozoic ice advance sequence,Sperry Wash,California[J]. Sedimentology,63(2):307 − 330.
[11]	Bai H Q,Kuang H W,Liu Y Q,et al.,2020. Marinoan-aged red beds at Shennongjia,South China:Evidence against global-scale glaciation during the Cryogenian[J]. Palaeogeography,Palaeoclimatology,palaeoecology,559:109967.
[12]	Cullers R L,Podkovyrov V N,2000. Geochemistry of the Mesoproterozoic Lakhanda shales in southeastern Yakutia,Russia:implications for mineralogical and provenance control,and recycling[J]. Precambrian Research,104(1):77 − 93.
[13]	Cullers R L,Podkovyrov V N,2002. The source and origin of terrigenous sedimentary rocks in the Mesoproterozoic Ui group,southeastern Russia[J]. Precambrian Research,117(3 − 4):157 − 183. DOI: 10.1016/S0301-9268(02)00079-7
[14]	Condon D,Zhu M,Bowring S,et al.,2005. U-Pb ages from the neoproterozoic Doushantuo Formation,China[J]. Science,308(5718):95 − 98. DOI: 10.1126/science.1107765
[15]	崔翔,2017. 扬子地块新元古代冰期地层和基性岩浆事件[D]. 南京:南京大学. Cui X,2017. Neoproterozoic glacial deposits and mafic magmatism in the the Yangtze Block[D]. Nanjing:Nanjing University (in Chinese with English abstract).
[16]	蔡雄飞,罗中杰,叶琴,2017. 湖南四都坪南沱组沉积特征与古气候变化耦合关系[J]. 华东地质,38(2):91 − 98. Cai X F,Luo Z J,Ye Q,2017. Sedimentary characteristics of the Nantuo Formation in Siduping,Hunan and its coupling relationship with paleoclimate[J]. East China Geology,38(2):91 − 98 (in Chinese with English abstract).
[17]	Chen X S,Kuang H W,Liu Y Q,et al.,2021. Revisiting the Nantuo Formation in Shennongjia,South China:A new depositional model and multiple glacial cycles in the Cryogenian[J]. Precambrian Research,356:106132.
[18]	董树文,张岳桥,龙长兴,等,2007. 中国侏罗纪构造变革与燕山运动新诠释[J]. 地质学报,81(11):1449 − 1461. DOI: 10.3321/j.issn:0001-5717.2007.11.001 Dong S W,Zhang Y Q,Long C X,et al.,2007. Jurassic tectonic revolution in China and new interpretation of the Yanshan movement[J]. Acta Geologica Sinica,81(11):1449 − 1461 (in Chinese with English abstract). DOI: 10.3321/j.issn:0001-5717.2007.11.001
[19]	邓乾忠,杨青雄,毛新武,等,2016. 湖北武当−随枣地区中−晚南华世岩石地层序列与年代学研究[J]. 资源环境与工程,30(2):132 − 142. Deng Q Z,Yang Q X,Mao X W,et al.,2016. Study of lithostratigraphic sequences and chronology of middle-late Nanhua in Wudang-Suizhou area[J]. Resources Environment and Engineering,30(2):132 − 142 (in Chinese with English abstract).
[20]	邓奇,崔晓庄,汪正江,等,2023. 扬子陆块北缘构造演化新认识:来自原花山群年代学和地球化学的制约[J]. 沉积与特提斯地质,43(1):212 − 225. DOI: 10.3969/j.issn.1009-3850.2023.01.016 Deng Q,Cui X Z,Wang Z J,et al.,2023. New understanding of the tectonic evolution of the northern margin of Yangtze Block:Constraints from the geochronology and geochemistry of the Huashan Group[J]. Sedimentary Geology and Tethyan Geology,43(1):212 − 225 (in Chinese with English abstract). DOI: 10.3969/j.issn.1009-3850.2023.01.016
[21]	Fedo C M,Wayne Nesbitt H,Young G M,1995. Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols,with implications for paleoweathering conditions and provenance[J]. Geology,23(10):921 − 924. DOI: 10.1130/0091-7613(1995)023<0921:UTEOPM>2.3.CO;2
[22]	Fedo C M,Young G M,Nesbitt H W,et al.,1997. Potassic and sodic metasomatism in the southern province of the Canadian Shield:Evidence from the Paleoproterozoic Serpent Formation,Huronian Supergroup,Canada[J]. Precambrian Research,84(1 − 2):17 − 36. DOI: 10.1016/S0301-9268(96)00058-7
[23]	冯连君,储雪蕾,张启锐,等,2003. 化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J]. 地学前缘,10(4):539 − 544. DOI: 10.3321/j.issn:1005-2321.2003.04.019 Feng L J,Chu X L,Zhang Q R,et al.,2003. CIA (chemical index of alteration) and its application in the Neoproterozoic clastic rocks[J]. Geoscience Frontiers,10(4):539 − 544 (in Chinese with English abstract). DOI: 10.3321/j.issn:1005-2321.2003.04.019
[24]	顾尚义,2013. 新元古代南沱冰期气候波动的沉积地球化学记录−来自贵州剑河五河剖面的证据[J]. 高校地质学报,19:72 − 73. Gu S Y,2013. Sedimentary geochemical records of climate fluctuations during the Neoproterozoic Nantuo glaciation: Evidence from the Wuhe Section of Jianhe,Guizhou Province[J]. Geological Journal of China Universities,19:72 − 73 (in Chinese with English abstract).
[25]	顾尚义,毕晨时,2015. 贵州地区南沱冰期的冰下化学风化作用及其对海洋磷富集的意义[J]. 贵州大学学报:自然科学版,32(6):22 − 28. Gu S Y,2015. Subglacial chemical weathering and its significance in Marine phosphorus enrichment during Nantuo Ice Age in Guizhou Province[J]. Journal of Guizhou University (Natural Science Edition),32(6):22 − 28 (in Chinese with English abstract).
[26]	官开萍,田力,安志辉,等,2016. 湖北神农架西部南华纪地层序列及其区域对比[J]. 地学前缘,23(6):236 − 244. Guan K P,Tian L,An Z H,et al.,2016. Stratigraphic succession of the Nanhuan Period in the Shennongjia area in western Hubei and its regional correlation[J]. Earth Science Frontiers,23(6):236 − 244 (in Chinese with English abstract).
[27]	Gu S Y,Fu Y,Long J,et al.,2019. Predominantly ferruginous conditions in south china during the marinoan glaciation:Insight from REE geochemistry of the SYN-glacial dolostone from the Nantuo Formation in Guizhou province,China[J]. Minerals,9(6):348. DOI: 10.3390/min9060348
[28]	Griffiths H J,Whittle R J,Mitchell E G,2023. Animal survival strategies in Neoproterozoic ice worlds[J]. Global Change Biology,29(1):10 − 20. DOI: 10.1111/gcb.16393
[29]	Harnois L,1988. The CIW index:A new chemical index of weathering[J]. Sedimentary Geology,55(3-4):319 − 322. DOI: 10.1016/0037-0738(88)90137-6
[30]	Hoffman P F,Kaufman A J,Halverson G P,et al.,1998. A Neoproterozoic Snowball Earth[J]. Science,281(5381):1342 − 1346. DOI: 10.1126/science.281.5381.1342
[31]	Hyde W T,Crowley T J,Baum S K,et al.,2000. Neoproterozoic 'snowball Earth' simulations with a coupled climate/ice-sheet model[J]. Nature,405(6785):425 − 429. DOI: 10.1038/35013005
[32]	Hoffman P F,Schrag D P,2002. The snowball Earth hypothesis:testing the limits of global change[J]. Terra nova,14(3):129 − 155. DOI: 10.1046/j.1365-3121.2002.00408.x
[33]	Halverson G P,Dudás F Ö,Maloof A C,et al.,2007. Evolution of the ⁸⁷Sr/⁸⁶Sr composition of Neoproterozoic seawater[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,256(3 − 4):103 − 129. DOI: 10.1016/j.palaeo.2007.02.028
[34]	Hoffman P F,Li Z X,2009. A palaeogeographic context for Neoproterozoic glaciation[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,277(3 − 4):158 − 172.
[35]	Hossain H M Z ,Roser B P ,Kimura J I,2010. Petrography and whole-rock geochemistry pf the Tertiary Sylhet succession,northeastern Bengal basin,Bangladesh:provenance and source area weathering[J]. Sedimentary Geology,228(3 − 4):171 − 183. DOI: 10.1016/j.sedgeo.2010.04.009
[36]	Hood A V S,Wallace M W,Drysdale R,2011. Neoproterozoic aragonite-dolomite seas? Widespread marine dolomite precipitation in Cryogenian reef complexes[J]. Geology,39(9):871 − 874. DOI: 10.1130/G32119.1
[37]	Hu J,Wang J S,Chen H R,et al.,2011. Multiple cycles of glacier advance and retreat during the Nantuo (Marinoan) glacial termination in the Three Gorges area[J]. Frontiers of Earth Science,6(1):101 − 108.
[38]	Hoffman P F,2016. Cryoconite pans on Snowball Earth:supraglacial oases for Cryogenian eukaryotes?[J]. Geobiology,14(6):531 − 542. DOI: 10.1111/gbi.12191
[39]	Huang K J,Teng F Z,Shen B,et al.,2016. Episode of intense chemical weathering during the termination of the 635 Ma Marinoan glaciation[J]. Proceedings of the National Academy of Sciences,113(52):14904 − 14909. DOI: 10.1073/pnas.1607712113
[40]	胡蓉,李双庆,王伟,等,2016. 扬子北部三峡地区南沱组冰碛岩的物源特征:锆石年龄和地球化学证据[J]. 地球科学,41(10):1630 − 1654. Hu R,Li S Q,Wang W,et al.,2016. Source characteristics of tillite the Nantuo formation in Three Gorges,northern Yangtze Block: Evidences from zircon ages and geochemical composition [J]. Earth Science,41(10):1630 − 1654 (in Chinese with English abstract).
[41]	Hawes I,Jungblut A D,Matys E D,et al.,2018. The “Dirty Ice” of the McMurdo Ice Shelf:Analogues for biological oases during the Cryogenian[J]. Geobiology,16(4):369 − 377. DOI: 10.1111/gbi.12280
[42]	Hu J,Li C,Tong J,et al.,2020. Glacial origin of the Cryogenian Nantuo Forma tion in eastern Shennongjia area (South China):Implications for macroalgal survival[J]. Precambrian Research,351:105969. DOI: 10.1016/j.precamres.2020.105969
[43]	胡军,2021. 华南神农架地区新元古代南沱组沉积古地理和古海洋环境研究[D]. 北京:中国地质大学. Hu J,2021. Sedimentary characteristics,paleogeography and paleomarine environment of the Neoproterozoic Nantuo Formation in Shennongjia area(South China)[D]. Beijing:China University of Geosciences (in Chinese with English abstract).
[44]	Johnson B W,Poulton S W,Goldblatt C,2017. Marine oxygen production and open water supported an active nitrogen cycle during the Marinoan Snowball Earth[J]. Nature Communications,8(1):1316.
[45]	江新胜,崔晓庄,卓皆文,等,2020. 华南扬子陆块西缘新元古代康滇裂谷盆地开启时间新证据[J]. 沉积与特提斯地质,40(3):31 − 37. Jiang X S,Cui X Z,Zhuo J W,et al.,2020. New evidence for the opening time of the Neoproterozoic Kangdian rift basin,western Yangtze Block,South China[J]. Sedimentary Geology and Tethyan Geology,40(3):31 − 37 (in Chinese with English abstract).
[46]	季泽龙,刘晓峰,2023. 峡东地区成冰系南沱组新认识[J]. 地质学报,97(6):1753 − 1765. Ji Z L,Liu X F,2023. New insights about the Cryogenian Nantuo Formation in the East Yangtze Gorges area[J]. Acta Geologica Sinica,97(6):1753 − 1765 (in Chinese with English abstract).
[47]	Kirschvink J L,1992. Late Proterozoic low-latitude global glaciation:The snowball Earth. The Proterozoic Biosphere:A multidisciplinary study[J].New York: Cambridge University Press: 51 − 52.
[48]	旷红伟,2017. 神农架成冰系“南沱组”宏观藻应属于大塘坡组的新证据[J]. 中国地质,44(6):1257 − 1258. DOI: 10.12029/gc20170617 Kuang H W,2017. Benthic macroscopic phototrophs of the Cryogenian in Shennongjia that survived in interglacial period between Sturtian and Marinoan glaciations[J]. Geology in China,44(6):1257 − 1258 (in Chinese with English abstract). DOI: 10.12029/gc20170617
[49]	刘英俊, 曹励明, 李兆麟, 等, 1984. 元素地球化学[M]. 北京: 科学出版社. Le Heron D P,Craig J,2012. Neoproterozoic deglacial sediments and their hydrocarbon source rock potential[J]. Geological Society,368:381 − 393.
[50]	Le Heron D P,2015. The significance of ice-rafted debris in Sturtian glacial successions[J]. Sedimentary Geology,322:19 − 33.
[51]	Le Heron D P,Busfield M E,2016. Pulsed iceberg delivery driven by Sturtian ice sheet dynamics:An example from Death Valley,California[J]. Sedimentology,63(2):331 − 349. DOI: 10.1016/j.sedgeo.2015.04.001
[52]	Lang X G,Chen J,Cui H,et al.,2018. Cyclic cold climate during the Nantuo Glaciation:Evidence from the Cryogenian Nantuo Formation in the Yangtze Block,South China[J]. Precambrian Research,310:243 − 255. DOI: 10.1111/sed.12225
[53]	李明龙,2019. 鄂西走马地区南华纪古城期−南沱早期古气候和古氧相演化:来自细碎屑岩元素地球化学的证据[J]. 地质学报,93(9):2158 − 2170. DOI: 10.1016/j.precamres.2018.03.004 Li M L,2019. Paleoclimate and paleo-oxygen evolution during the Gucheng Period-early Nantuo Period of Nanhua System in the Zouma area,West Hubei:evidence from element geochemistry of fine clastic rocks[J]. Acta Geologica Sinica,93(9):2158 − 2170 (in Chinese with English abstract). DOI: 10.1016/j.precamres.2018.03.004
[54]	李路顺,汪泽成,肖安成,等,2021. 扬子北缘南华纪裂谷系统:基于重力异常及沉积学证据[J]. 地球科学,46(10):3496 − 3508. Li L S,Wang Z C,Xiao A C,et al.,2021. Rift system in the northern Yangtze Block during Nanhua period:Implications from gravity anomaly and sedimentology[J]. Journal of Earth Science,46(10):3496 − 3508 (in Chinese with English abstract).
[55]	李明龙,杨波涌,郑顺德,等,2021. 鄂西走马地区南华纪大塘坡间冰期古气候研究[J]. 地质论评,67(1):39 − 55. Li M L,Yang B Y,Zheng S D,et al.,2021. Study on the paleoclimate during the Datangpo interglacial stage of the Nanhua Period in the Zouma area,western Hubei Province[J]. Geological Review,67(1):39 − 55 (in Chinese with English abstract).
[56]	刘春来,熊国庆,董国明,2021. 扬子北缘奥陶纪−志留纪之交泥岩地球化学特征及其源区、构造背景[J]. 地质论评,67(5):1263 − 1279. Liu C L,Xiong G Q,Dong G M,2021. Geochemical characteristics of mudstones and its provenance and tectonic setting during the Ordovician-Silurian period in northern margin of Yangtze Block[J]. Geological Review,67(5):1263 − 1279 (in Chinese with English abstract).
[57]	刘春来, 熊国庆, 董国明, 2021. 扬子北缘奥陶纪−志留纪之交泥岩地球化学特征及其源区、构造背景[J]. 地质论评, 67（5）: 1263 − 1279. Liu Y J,Cao L M,Li Z L,et al.,1984. Element geochemistry[M]. Beijing:Science Press.
[58]	Liu P J,Li X H,Chen N M,et al.,2015. New SIMS U-Pb zircon age and its constraint on the beginning of the Nantuo glaciation[J]. Science Bulletin,60(10):958 − 963.
[59]	Lan Z W,Huyskens M H,Le Hir G,et al.,2022. Massive volcanism may have foreshortened the Marinoan snowball Earth[J]. Geophysical Research Letters,49(6):0094 − 8276. DOI: 10.1007/s11434-015-0790-3
[60]	Lan Z W,Huyskens M H,Le Hir G,et al.,2022. Massive volcanism may have foreshortened the Marinoan snowball Earth[J]. Geophysical Research Letters,49(6):e2021GL097156.
[61]	Lu L,Mok B W Y,Chen L L,et al.,2022. Neutralization of severe acute respiratory syndrome coronavirus 2 omicron variant by sera from BNT162b2 or CoronaVac vaccine recipients[J]. Clinical Infectious Diseases,75(1):822 − 826. DOI: 10.1029/2021GL097156
[62]	Li J,Li X G,Wu C,et al.,2023. Geochronology and geochemistry of the Cryogenian sedimentary rocks and Early Paleozoic mafic dykes of the South Qinling belt:Implications for the tectonic evolution of the northwestern South China craton[J]. Lithos,444(445):107129. DOI: 10.1093/cid/ciab1041
[63]	郎咸国,陈家乐,2023. 沉积与特提斯地质,43(3):651−660. Lang X G,Chen J L,2023. Research progress on environmental effects of the Cryogenian global glaciation[J]. Sedimentary Geology and Tethyan Geology,43(3):651−660 (in Chinese with English abstract).
[64]	兰中伍,2023. 华南南华系年代地层学研究进展[J]. 沉积与特提斯地质,43(1):180 − 187. Lan Z W,2023. Research progress on the chronostratigraphic study of Nanhua System in South China[J]. Sedimentary Geology and Tethyan Geology,43(1):180 − 187 (in Chinese with English abstract).
[65]	兰中伍, 2023. 华南南华系年代地层学研究进展[J]. 沉积与特提斯地质, 43（1）: 180 − 187. DOI: 10.3969/j.issn.1009-3850.2023.01.014 McLennan S M,1989. Rare Earth Elements in sedimentaw rocks:Influence of provenance and sedimenta y processes[J]. Review in Mineralogy,21(1):169 − 200. DOI: 10.3969/j.issn.1009-3850.2023.01.014
[66]	MacDonald F A,Schmitz M D,Crowley J L,et al.,2010. Calibrating the cryogenian[J]. Science,327(5970):1241 − 1243.
[67]	毛黎光,肖安成,魏国齐,等,2011. 扬子地块北缘晚古生代−早中生代裂谷系统的分布及成因分析[J]. 岩石学报,27(3):721 − 731. DOI: 10.1126/science.1183325 Mao L G,Xiao A C,Wei G Q,et al.,2011. Distribution and origin of the Late Paleozoic-Mesozoic rift systems in the northern margin of the Yangtze block[J]. Acta Petrologica Sinica,27(3):721 − 731 (in Chinese with English abstract). DOI: 10.1126/science.1183325
[68]	牟传龙,葛祥英,余谦,等,2019. 川西南地区五峰−龙马溪组黑色页岩古气候及物源特征:来自新地2井地球化学记录[J]. 古地理学报,21(5):835 − 854. Mou C L,Ge X Y,Yu Q,et al.,2019. Palaeoclimatology and provenance of black shales from Wufeng-Longmaxi Formations in southwestern Sichuan Province:From geochemical records of Well Xindi-2[J]. Journal of Palaeogeography,21(5):835 − 854 (in Chinese with English abstract).
[69]	毛帆,裴先治,李瑞保,等,2021. 扬子板块西北缘碧口微地块南华系碎屑锆石U-Pb年龄及其物源示踪[J]. 沉积与特提斯地质,41(1):41 − 57. DOI: 10.7605/gdlxb.2019.05.057 Mao F,Pei X Z,Li R B,et al.,2021. The LA-ICP-MS U-Pb dating of detrital zircons from the Nanhua System in Bikou Terrane,northwestern margin of Yangtze Block[J]. Sedimentary Geology and Tethyan Geology,41(1):41 − 57 (in Chinese with English abstract). DOI: 10.7605/gdlxb.2019.05.057
[70]	毛帆, 裴先治, 李瑞保, 等, 2021. 扬子板块西北缘碧口微地块南华系碎屑锆石U-Pb年龄及其物源示踪[J]. 沉积与特提斯地质, 41（1）: 41 − 57. Ma H R,Shen B,Lang X G,et al.,2022. Active biogeochemical cycles during the Marinoan global glaciation[J]. Geochimica et Cosmochimica Acta,321:155 − 169.
[71]	Ma X C,Wang J S,Wang Z,et al.,2023. Geochronological constraints on Cryogenian ice ages:Zircon U–Pb ages from a shelf section in South China[J]. Global and Planetary Change,222:104071.
[72]	Nesbitt H W,Young G M,1982. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature,299(5885):715 − 717. DOI: 10.1016/j.gloplacha.2023.104071
[73]	Nesbitt H W,Young G M,1984. Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J]. Geochimica Cosmochimic Acta,48(7):1523 − 1534. DOI: 10.1038/299715a0
[74]	Nelson L L,Smith E F,Hodgin E B,et al.,2020. Geochronological constraints on Neoproterozoic rifting and onset of the Marinoan glaciation from the Kingston Peak Formation in Death Valley,California (USA)[J]. Geology,48(110):1083 − 1087. DOI: 10.1016/0016-7037(84)90408-3
[75]	Peltier W R,Liu Y,Crowley J W,2007. Snowball Earth prevention by dissolved organic carbon remineralization[J]. Nature,450(7171):813 − 818.
[76]	Pierrehumbert R T,Abbot D S,Voigt A,et al.,2011. Climate of the Neoproterozoic[J]. Annual Review of Earth and Planetary Sciences,39:417 − 460. DOI: 10.1038/nature06354
[77]	谯文浪,汪建国,陈武,等,2013. 贵州丹寨地区南华系地层地球化学特征及其对古气候,古环境的意义[J]. 地质科学,48(3):847 − 859. DOI: 10.1146/annurev-earth-040809-152447 Jiao W L,Wang J G,Chen W,et al.,2013. Geochemistry of Nanhuan sedimentary rocks in Danzhai,southeast Guizhou and implications for changes of paleoenvironment and palaeoclimate[J]. Chinese Journal of Geology,48(3):847 − 859 (in Chinese with English abstract). DOI: 10.1146/annurev-earth-040809-152447
[78]	齐靓,徐亚军,杜远生,等,2023. 华夏地块新元古代沉积记录与超大陆重建[J]. 沉积与特提斯地质,43(1):188 − 211. DOI: 10.3969/j.issn.0563-5020.2013.03.020 Qi L,Xu Y J,Du Y S,et al.,2023. Neoproterozoic sedimentary records in the Cathaysia Block and their implications for the supercontinent reconstruction[J]. Sedimentary Geology and Tethyan Geology,43(1):188 − 211 (in Chinese with English abstract). DOI: 10.3969/j.issn.0563-5020.2013.03.020
[79]	齐靓, 徐亚军, 杜远生, 等, 2023. 华夏地块新元古代沉积记录与超大陆重建[J]. 沉积与特提斯地质, 43（1）: 188 − 211. DOI: 10.3969/j.issn.1009-3850.2023.01.015 Rieu R,Allen P A,Plotze M,et al.,2007a. Compositional and mineralogical variations in a Neoproterozoic glacially influenced succession,Mirbat area,south Oman:Implications for paleoweathering conditions[J]. Precambrian Research,154(3-4):248 − 265. DOI: 10.3969/j.issn.1009-3850.2023.01.015
[80]	Rose B E J,2015. Stable "Waterbelt" climates controlled by tropical ocean heat transport:A nonlinear coupled climate mechanism of relevance to Snowball Earth[J]. Journal of Geophysical Research:Atmospheres,120(4):1404 − 1423. DOI: 10.1016/j.precamres.2007.01.003
[81]	Sun S S,McDonough W F,1989. Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J]. Geological Society London Special Publications,42(1):313 − 345.
[82]	孙娇鹏,陈世悦,彭渊,等,2016. 欧龙布鲁克地块新元古代早期冰川事件:来自CIA指数的证据[J]. 地质论评,62(1):29 − 36. DOI: 10.1144/GSL.SP.1989.042.01.19 Sun J P,Chen S Y,Peng Y,et al.,2016. Early Neoproterozoic Glacier Event in Oulongbuluke Block:Evidence from CIA Index[J]. Geological Review,62(1):29 − 36 (in Chinese with English abstract). DOI: 10.1144/GSL.SP.1989.042.01.19
[83]	沈洪娟,2020. 贵州东部南沱冰期碳循环研究[D]. 贵州:贵州大学. Shen H J,2020. A study on carbon cycle of Nantuo ice age in eastern Guizhou Province,China[D]. Guizhou:Guizhou University (in Chinese with English abstract).
[84]	隋佩珊,2021. 冰碛岩对中国新元古代古沉积环境与大陆上地壳平均成分的制约−以华北罗圈组及华南南沱组为例[D]. 中国科学院大学. Sui P S,2021. Constraints of diamictite on Neoproterozoic paleoenvironment and the upper crust composition of China-a case study of Luoquan Formation in North China and Nantuo Formation in South China[D]. University of Chinese Academy of Sciences (in Chinese with English abstract).
[85]	隋佩珊, 2021. 冰碛岩对中国新元古代古沉积环境与大陆上地壳平均成分的制约−以华北罗圈组及华南南沱组为例[D]. 中国科学院大学. Song H Y,An Z H,Ye Q,et al.,2023. Mid-latitudinal habitable environment for marine eukaryotes during the waning stage of the Marinoan snowball glaciation[J]. Nature Communications,14:1564.
[86]	唐将,林源,2002. 南秦岭大巴山地区的下震旦统及前震旦系[J]. 中国地质,29(2):143 − 146. DOI: 10.1038/s41467-023-37172-x Tang J,Lin Y,2002. The lower Sinian and pre-Sinian of the Daba Mountain area of the South Qinling region[J]. Geology in China,29(2):143 − 146 (in Chinese with English abstract). DOI: 10.1038/s41467-023-37172-x
[87]	唐婷婷,牟军,王安华,等,2019. 贵州铜仁地区南华系铁丝坳组−南沱组沉积环境及古气候演变[J]. 贵州学报,37(6):67 − 73. DOI: 10.3969/j.issn.1000-3657.2002.02.007 Tang T T,Mou J,Wang A H,et al.,2019. Sedimentary environment and paleoclimate research of Tiesi’ao Formation-Nantuo Formation in Tongren,Guizhou[J]. Guizhou Science,37(6):67 − 73 (in Chinese with English abstract). DOI: 10.3969/j.issn.1000-3657.2002.02.007
[88]	王剑,刘宝珺,潘桂棠,2001. 华南新元古代裂谷盆地演化:Rodinia 超大陆解体的前奏[J]. 矿物岩石,21(3):135 − 145. Wang J,Liu B J,Pan G T,2001. Neoproterozoic rifting history of South China:Significance to Rodinia breakup[J]. Mineralogy Petrology,21(3):135 − 145 (in Chinese with English abstract).
[89]	王自强,尹崇玉,高林志,等,2006. 宜昌三斗坪地区南华系化学蚀变指数特征及南华系划分、对比的讨论[J]. 地质论评,52(5):577 − 585. DOI: 10.3969/j.issn.1001-6872.2001.03.021 Wang Z Q,Ying C Y,Gao L Z,et al.,2006. The character of the chemical index of alteration and discussion of subdivision and correlation of the Nanhua System in Yichang area[J]. Geological Review,52(5):577 − 585 (in Chinese with English abstract). DOI: 10.3969/j.issn.1001-6872.2001.03.021
[90]	王自强,2009. 黔南−桂北地区南华系化学地层特征[J]. 地球学报,30,(4):465 − 474. DOI: 10.3321/j.issn:0371-5736.2006.05.008 Wang Z Q,2009. Chemostratigraphic characteristics of Nanhua System in Southern Guizhou-Northern Guangxi Area[J]. Acta Geoscientica Sinica,30,(4):465 − 474 (in Chinese with English abstract). DOI: 10.3321/j.issn:0371-5736.2006.05.008
[91]	吴忠银,顾尚义,2019. 华南新元古代南沱杂砾岩中富钾现象的研究−以贵州松桃南沱组为例[J]. 贵州大学学报:自然科学版,36(5):43 − 49. DOI: 10.3321/j.issn:1006-3021.2009.04.007 Wu Z Y,2019. Potassium enrichment of diamictite in Neoproterozoic Nantuo glaciation in South China:An example from the Cryogenian Nantuo Formation in Songtao,Guizhou Province[J]. Journal of Guizhou University (Natural Sciences),36(5):43 − 49 (in Chinese with English abstract). DOI: 10.3321/j.issn:1006-3021.2009.04.007
[92]	吴黎军,李明龙,陈林,等,2019. 鄂西走马地区ZK701南华系大塘坡组主量元素地球化学对古气候的指示[J]. 河南理工大学学报:自然科学版,38(6):47 − 54. Wu L J,Li M L,Chen L,et al.,2019. Geochemistry characteristics of major elements and their indication to paleoclimate in the Datangpo formation of Nanhua system of ZK701 drillcore in Zouma area of western Hubei province[J]. Journal of Henan Polytechnic University (Natural Science),38(6):47 − 54 (in Chinese with English abstract).
[93]	肖安成,魏国齐,沈中延,等,2011. 扬子地块与南秦岭造山带的盆山系统与构造耦合[J]. 岩石学报,27(3):601 − 611. Xiao A C,Wei G Q,Shen Z Y,et al.,2011. Basin-mountain system and tectonic coupling between Yangtze block and South Qinling orogen[J]. Acita Peirologica Sinica,27(3):601 − 611 (in Chinese with English abstract).
[94]	肖安成, 魏国齐, 沈中延, 等, 2011. 扬子地块与南秦岭造山带的盆山系统与构造耦合[J]. 岩石学报, 27（3）: 601 − 611. Xiang Z J,Yan Q R,White J D L,et al.,2015. Geochemical constraints on the provenance and depositional setting of Neoproterozoic volcaniclastic rocks on the northern margin of the Yangtze Block,China:Implications for the tectonic evolution of the northern margin of the Yangtze Block[J]. Precambrian Research,264:140 − 155.
[95]	熊国庆,王剑,李园园,等,2017. 大巴山西段上奥陶统−下志留统五峰组−龙马溪组斑脱岩锆石U-Pb年龄及其地质意义[J]. 沉积与特提斯地质,37(2):46 − 58. DOI: 10.1016/j.precamres.2015.04.012 Xiong G Q,Wang J,Li Y Y,et al.,2017. Zircon U-Pb dating and geological significance of the bentonites from the Upper Ordovician Wufeng Formation and Lower Silurian Longmaxi Formation in western Daba Mountains[J]. Sedimentary Geology and Tethyan Geology,37(2):46 − 58 (in Chinese with English abstract). DOI: 10.1016/j.precamres.2015.04.012
[96]	徐小涛,邵龙义,2018. 利用泥质岩化学蚀变指数分析物源区风化程度时的限制因素[J]. 古地理学报,20(3):515 − 522. DOI: 10.3969/j.issn.1009-3850.2017.02.006 Xu X T,Shao L Y,2018. Limiting factors in utilization of chemical index of alteration of mudstones to quantify the degree of weathering in provenance[J]. Journal of Palaeogeography,20(3):515 − 522 (in Chinese with English abstract). DOI: 10.3969/j.issn.1009-3850.2017.02.006
[97]	熊国庆,王剑,李园园,等,2019. 南大巴山东段上奥陶统五峰组−下志留统龙马溪组钾质斑脱岩锆石U-P b年龄及其构造意义[J]. 地质学报,93(4):843 − 864. DOI: 10.7605/gdlxb.2018.03.038 Xiong G Q,Wang J,Li Y Y,et al.,2019. Zircon U-Pb dating of K-bentonite from Late Ordovician Wufeng Formation and Earlier Silurian Longmaxi Formation in the eastern section of south Dabashan and its tectonic signification[J]. Acta Geologica Sinica,93(4):843 − 864 (in Chinese with English abstract). DOI: 10.7605/gdlxb.2018.03.038
[98]	熊国庆, 王剑, 李园园, 等, 2019. 南大巴山东段上奥陶统五峰组−下志留统龙马溪组钾质斑脱岩锆石U-P b年龄及其构造意义[J]. 地质学报, 93（4）: 843 − 864. Young G M,Wayne Nesbitt H,1999. Paleoclimatology and provenance of the glaciogenic Gowganda Formation (Paleoproterozoic),Ontario,Canada:A chemostratigraphic approach[J]. Geological Society of America Bulletin,111(2):264 − 274.
[99]	Ye Q,Tong J N,Xiao S H,et al.,2015. The survival of benthic macroscopic phototrophs on a Neoproterozoic snowball Earth[J]. Geology,43(6):507 − 510. DOI: 10.1130/0016-7606(1999)111<0264:PAPOTG>2.3.CO;2
[100]	Ye Y T,Wang H J,Zhai L N,2018. Contrasting Mo-U enrichments of the basal Datangpo Formation in South China:Implications for the Cryogenian interglacial ocean redox[J]. Precambrian Research,315:66 − 74. DOI: 10.1130/G36640.1
[101]	Yan B,Shen W B,Zhao N N,et al.,2020. Constraint on the nature of Marinoan glaciation:Cyclic sedimentary records of the Nantuo Formation,South China[J]. Journal of Asian Earth Sciences,189:104137. DOI: 10.1016/j.precamres.2018.07.013
[102]	Ye Y T,Wang X M,Wang H J,et al.,2024. Exploring climate variability during the Marinoan glaciation:A study of black shale geochemistry[J]. Gondwana Research,128:315 − 324.
[103]	周传明,袁训来,肖书海,2002. 扬子地台新元古代陡山沱期磷酸盐化生物群[J]. 科学通报,47:1734 − 1739. Zhou C M,Yuan X L,Xiao S H,2002. The Neoproterozoic Doushantuo phosphorylation biota in the Yangtze Platform[J]. Chinese Scientia Bulletin,47:1734 − 1739 (in Chinese with English abstract).
[104]	周传明, 袁训来, 肖书海, 2002. 扬子地台新元古代陡山沱期磷酸盐化生物群[J]. 科学通报, 47: 1734 − 1739. DOI: 10.3321/j.issn:0023-074X.2002.22.013 Zhang S H,Jiang G G,Han Y G,et al.,2008. The age of the Nantuo Formation and Nantuo glaciation in South China[J]. Terra Nova,20(4):289 − 294. DOI: 10.3321/j.issn:0023-074X.2002.22.013
[105]	赵妮娜,2016. 华南新元古代冰期沉积的岩石地层及年代学研究[D]. 北京:中国地质大学. DOI: 10.1111/j.1365-3121.2008.00819.x Zhao N N,2016. The lithostratigraphy and geochronology of Neoproterozoic glaciogenic sediments in South China[D]. Beijing:China University of Geosciences (in Chinese with English abstract). DOI: 10.1111/j.1365-3121.2008.00819.x
[106]	赵思凡,顾尚义,沈洪娟,等,2020. 华南地区南沱冰期海洋氧化还原环境研究−来自贵州松桃南沱组白云岩稀土元素地球化学的指示[J]. 沉积学报,38(6):1140 − 1151. Zhao S F,Gu S Y,Shen H J,et al.,2020. Ocean redox environment in the Nantuo Ice Age of South China:An indication of the rare earth element geochemistry in the dolomites from the Nantuo Formation in Guizhou province[J]. Acta Sedimentologica Sinica,38(6):1140 − 1151 (in Chinese with English abstract).
[107]	刘英俊,曹励明,李兆麟,等,1984. 元素地球化学[M]. 北京:科学出版社. Zhao S F, Gu S Y, Shen H J, et al., 2020. Ocean redox environment in the Nantuo Ice Age of South China: An indication of the rare earth element geochemistry in the dolomites from the Nantuo Formation in Guizhou province[J]. Acta Sedimentologica Sinica, 38（6）: 1140 − 1151.

[1]	ZHAO Wenpu, LI Yifan, ZHAO Shuang, FAN Tailiang, YUAN Yuxuan, ZHANG Tan. High-resolution sequence stratigraphic characteristics and organic matter enrichment mechanism of fine-grained sedimentary rocks in the Tiesiao-Datangpo Formations in northeastern Guizhou[J]. Sedimentary Geology and Tethyan Geology, 2023, 43(4): 871-891. DOI: 10.19826/j.cnki.1009-3850.2023.11005
[2]	TAO Lanchu, ZHU Xingqiang, MA Yiqi, ZHANG Qidao, PANG Long, TU Chunlin, HE Chengzhong. Genesis of geothermal water in the Laochang area, eastern Yunnan Province: Constraints from hydrochemistry and C-H-O-S isotopes[J]. Sedimentary Geology and Tethyan Geology, 2023, 43(2): 295-310. DOI: 10.19826/j.cnki.1009-3850.2023.02007
[3]	ZHENG Jie, YANG Zhengxi, LIU Shilei, AN Xianyin, SANG Yongheng, MA Jianfei. The chemical alteration indexes and their significance for the Nanhuan Liangjiehe Formation in northeastern Guizhou[J]. Sedimentary Geology and Tethyan Geology, 2019, 39(1): 50-59.
[4]	LUO Liang, WANG Dong-bing, YIN Fu-guang, REN Fei, NING Kuo-bu. Carbon isotope chemostratigraphy of the Lower Permian Dingjiazhai Formation in the Baoshan Block,Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2017, 37(4): 58-68.
[5]	QIN Jian-hua, LIAO Zhen-wen, ZHU Si-bao, LAI Yang. Mineralization of the carbonate-hosted Pb-Zn deposits in the SichuanYunnan-Guizhou area, southwestern China[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(1): 1-13.
[6]	XIONG Guo-qing. Doushantuo Formation in northwestern Fanjing Mountains, Guizhou[J]. Sedimentary Geology and Tethyan Geology, 2006, 26(2): 106-109.
[7]	HE Ming-hua, YU Mei-yi, WANG Yue, YUAN Liang-jun, ZHAO Yuanlong, HUANG Long-hui. Sedimentary facies and palaeogeography of NE Guizhou and its adjacent areas during the Doushantuoan(Neoproterozoic)[J]. Sedimentary Geology and Tethyan Geology, 2006, 26(1): 41-46.
[8]	HE Ming-hua. Sedimentary facies and palaeogeography during the Early Sinian and potential of the rhodochrosite deposits in northeastern Guizhou and its adjacent areas[J]. Sedimentary Geology and Tethyan Geology, 2001, 21(3): 39-47.
[9]	Yang Ruidong. PALAEOECOLOGY AND FOSSIL COMMUNITIES IN SOUTHERN AND CENTRAL GUIZHOU DURING TRIASSIC TIME[J]. Sedimentary Geology and Tethyan Geology, 1996, 16(6): 42-47.
[10]	Yang Zhenqiang, Jiang Dehe, Zhao Shijiu. A NEW SEDIMENTOLOGICAL EXPLANTION OF STABLE ISOTOPIC COMPOSITIONS IN ORDOVICIAN AND SINIAN MANGANESE-BEARING BEDS IN CENTRAL HUNAN[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(2): 25-36.

Supplements (1)

Supplements
Other Related Supplements
- DOCX format
  大巴山地区Marinoan冰川沉积序列及其古气候演化-附表 Download(109KB)

Cited By

Get Citation

PDF

XML

Article views (14) PDF downloads (10)

Turn off MathJax

Article Contents

Abstract

References

Supplements

Sedimentary sequence and paleoclimate evolution of the Marinoan Glacier in the Daba Mountains: Evidence from petrology and geochemistry

Abstract

References

Related Articles

Supplements

Other Related Supplements

DOCX format

Catalog

Sedimentary sequence and paleoclimate evolution of the Marinoan Glacier in the Daba Mountains: Evidence from petrology and geochemistry

Abstract

References

Related Articles

Supplements

Other Related Supplements

DOCX format

Catalog

Export File

Citation

Format

Content