柴达木盆地西部中更新世气候转型期的古水温:来自SG-1钻孔石盐流体包裹体的证据

doi:10.13745/j.esf.sf.2021.1.39

地学前缘 ›› 2021, Vol. 28 ›› Issue (6): 115-124.DOI: 10.13745/j.esf.sf.2021.1.39

柴达木盆地西部中更新世气候转型期的古水温:来自SG-1钻孔石盐流体包裹体的证据

倪艳华¹, 李明慧^1,2,*, 方小敏^1,2,3, 孟凡巍⁴, 颜茂都^1,2, 刘迎新⁵

1.中国科学院青藏高原研究所, 北京 100101;
2.青藏高原卓越中心, 北京 100101;
3.中国科学院大学, 北京 100049;
4.中国科学院南京地质古生物研究所, 江苏南京 210008;
5.中国地质大学(北京) 珠宝学院, 北京 100083

收稿日期:2020-12-22 修回日期:2021-01-24 出版日期:2021-11-25 发布日期:2021-11-25
通讯作者: ^*李明慧(1974—),女,博士,副研究员,主要从事环境矿物学、盐类矿床学、湖泊沉积与环境变化方面的研究。E-mail: liminghui@itpcas.ac.cn
作者简介:倪艳华(1993—),女,硕士,主要从事矿物与矿床地质、地球化学研究。E-mail: vavanee@163.com
基金资助:
国家重点研发计划项目(2017YFC0602803); 中国科学院战略性先导专项(XDA20070201,XDA20070101,XDA20020100); 第二次青藏科考项目(2019QZKK0707,2019QZKK0202)); 国家自然科学基金项目(41620104002,41831177,41561144009)

Paleotemperature during the Mid-Pleistocene Transition in western Qaidam Basin: Evidence from fluid inclusions in halite from drill hole SG-1

NI Yanhua¹, LI Minghui^1,2,*, FANG Xiaomin^1,2,3, MENG Fanwei⁴, YAN Maodu^1,2, LIU Yingxin⁵

1. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;
2. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China;
3. University of Chinese Academy of Sciences, Beijing 100049, China;
4. Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China;
5. School of Gemmology, China University of Geosciences(Beijing), Beijing 100083, China;

Received:2020-12-22 Revised:2021-01-24 Online:2021-11-25 Published:2021-11-25

摘要/Abstract

摘要： 中更新世气候转型事件(MPT)是全球性冷气候事件,在柴达木盆地也有记录,但关于该事件形成时的古温度数据较少。石盐原生流体包裹体形成于浅水环境,其均一温度可直接反映晶体形成时的卤水温度,是恢复古温度常用的指标之一。本文选择柴达木盆地西部钻孔SG-1中1.22~0.88 Ma期间的石盐晶体进行流体包裹体均一温度测试,共获得390个石盐流体包裹体数据。其均一温度最高为50 ℃,最低为6.8 ℃,90%以上温差值在10 ℃以内,且石盐流体包裹体大小与温度没有明显线性相关关系,这说明SG-1钻孔石盐流体包裹体被捕获后没有受到后期热液的改造。均一温度数据反映了石盐沉积时的古水温特征。石盐晶体主要在暖季析出,原生流体包裹体恢复的古水温可能是暖季节的温度。均一温度的最高值可能受到热液和气候的共同作用。MPT时期,石盐流体包裹体均一温度(中位值T_h,med)接近于现代盆地7月份大气温度的平均值,高于盆地的全年温度及MPT时期的全球气温,与MPT时期地中海的海水表面温度相当,均一温度的平均值(T_h,avg)高于以上温度。SG-1钻孔记录的柴达木盆地MPT事件最冷期出现在约1.165~1.0 Ma。

关键词: 石盐, 流体包裹体, 均一温度, 气候变化

Abstract: The Mid-Pleistocene Transition (MPT) is a global cold event and also recorded in the Qaidam Basin, but the paleotemperature data is rather lacking. Halite is generally formed in shallow water environment, and the homogenization temperature (T_h) of primary fluid inclusions in halite can directly reflect the brine temperature at halite crystallization and can be used to reconstruct paleotemperature of brine. This study selected primary halite samples from the 1.22-0.88 Ma section of drill hole SG-1 in the western Qaidam Basin and collected data on 390 fluid inclusions. The maximum and minimum homogenization temperatures were 50 ℃ and 6.8 ℃, respectively, with temperature fluctuations mostly (>90%) within 10 ℃; there is no obvious linear correlation between the size of fluid inclusions in halite and the homogenization temperature. This result indicates that fluid inclusions in halite from hole SG-1 have not been modified by the later hydrothermal solution and the T_h data can directly relate to paleotemperature at halite deposition. The reconstructed paleotemperature in this study may be the brine temperature in warm season as halite generally deposits in warm season, while the maximum value of T_h may be affected by hydrothermal solution and climate. During the MPT period, the homogenization temperature of palaeo-water (mean value, T_h,med) is similar to the average temperature in present-day July in the Qaidam Basin or the surface water temperature in the Mediterranean Sea during the same period, but it is much higher than the annual temperature in the Qaidam Basin or the global average temperature during MPT. The average homogenization temperature (T_h,avg) is higher than all the above temperatures. The coldest climate in the Qaidam Basin during MPT occurred at ~1.165-1.0 Ma.

Key words: halite, fluid inclusion, homogenization temperature, climate change

中图分类号:

P571
P578.32

倪艳华, 李明慧, 方小敏, 孟凡巍, 颜茂都, 刘迎新. 柴达木盆地西部中更新世气候转型期的古水温:来自SG-1钻孔石盐流体包裹体的证据[J]. 地学前缘, 2021, 28(6): 115-124.

NI Yanhua, LI Minghui, FANG Xiaomin, MENG Fanwei, YAN Maodu, LIU Yingxin. Paleotemperature during the Mid-Pleistocene Transition in western Qaidam Basin: Evidence from fluid inclusions in halite from drill hole SG-1[J]. Earth Science Frontiers, 2021, 28(6): 115-124.

参考文献

[1] LOWENSTEIN T K, TIMOFEEFF M N, BRENNAN S T, et al.Oscillations in Phanerozoic seawater chemistry: evidence from fluid inclusions[J]. Science, 2001, 294(5544): 1086-1088.
[2] TIMOFEEFF M N, LOWENSTEIN T K, BRENNAN S T, et al.Evaluating seawater chemistry from fluid inclusions in halite: examples from modern marine and nonmarine environments[J]. Geochimica et Cosmochimica Acta, 2001, 65(14): 2293-2300.
[3] SATTERFIELD C L, LOWENSTEIN T K, VREELAND R H.Paleobrine temperatures, chemistries, and paleoenvironments of Silurian Salina Formation F-1 salt, Michigan Basin, USA, from petrography and fluid inclusions in Halite[J]. Journal of Sedimentary Research, 2005, 75(4): 534-546.
[4] ZAMBITO I V, BENISON K C.Extremely high temperatures and paleoclimate trends recorded in Permian ephemeral lake halite[J]. Geology, 2013, 41(5): 587-590.
[5] 刘兴起, 倪培. 表生环境条件形成的石盐流体包裹体研究进展[J]. 地球科学进展, 2005, 20(8): 856-862.
[6] ROBERTS S M, SPENCER R J.Paleotemperatures preserved in fluid inclusions in halite[J]. Geochimica et Cosmochimica Acta, 1995, 59(19): 3929-3942.
[7] LOWENSTEIN T K, LI J, BROWN C B.Paleotemperatures from fluid inclusions in halite: method verification and a 100000 year paleotemperature record, Death Valley, CA[J]. Chemical Geology, 1998, 150(3/4): 223-245.
[8] BENISON K C, GOLDSTEIN R H.Permian paleoclimate data from fluid inclusions in halite[J]. Chemical Geology, 1999, 154(1/2/3/4): 113-132.
[9] 孟凡巍, 倪培, 葛晨东, 等. 实验室合成石盐包裹体的均一温度以及古气候意义[J]. 岩石学报, 2011, 27(5): 1543-1547.
[10] 卢焕章, 范宏瑞, 倪培, 等. 流体包裹体[M]. 北京: 科学出版社, 2004: 23-45.
[11] MENG F W, NI P, JAMES D S, et al.Ediacaran seawater temperature: evidence from inclusions of Sinian halite[J]. Precambrian Research, 2011, 184(1/2/3/4): 63-69.
[12] ZAMBITO I V, JAMES J.Possibly ubiquitous preservation of microbes in permian halite[C]∥Proceedings of GSA Annual Meeting. Denver: GSA, 2013, 45(7): 316.
[13] 孟凡巍, 张智礼, 卓勤功, 等. 蒸发岩盆地古环境的直接记录: 来自石盐流体包裹体的证据[J]. 矿物岩石地球化学通报, 2018, 37(3): 451-461.
[14] MCCULLOCH D S.Vacuole disappearance temperatures of laboratory-grown hopper halite crystals[J]. Journal of Geophysical Research, 1958, 64(7): 849-854.
[15] 袁见齐, 蔡克勤, 肖荣阁, 等. 云南勐野井钾盐矿床石盐中包裹体特征及其成因的讨论[J]. 地球科学: 中国地质大学学报, 1991(2): 137-948.
[16] 刘成林, 陈永志, 焦鹏程, 等. 罗布泊卤水室内蒸发及天然石盐包裹体均一温度分析探讨[J]. 东华理工学院学报, 2005, 28(4): 306-312.
[17] 王春连, 刘成林, 徐海明, 等. 江陵凹陷沙市组上段石盐包裹体测温学研究[J]. 岩石矿物学杂志, 2013, 32(3): 383-392.
[18] MENG F W, NI P, YUAN X L, et al. Choosing the best ancient analogue for projected future temperatures: a case using data from fluid inclusions of middle-late Eocene halites[J]. Journal of Asian Earth Sciences, 2013, 67/68: 46-50.
[19] ZHANG X Y, MENG F W, LI W X, et al.Reconstruction of Late Cretaceous coastal paleotemperature from halite deposits of the Late Cretaceous Nongbok Formation (Khorat Plateau, Laos)[J]. Palaeoworld, 2016, 25: 425-430.
[20] CLARK P U, ARCHER D.The middle Pleistocene transition: characteristics, mechanisms, and implications for long-term changes in atmospheric p(CO₂)[J]. Quaternary Science Reviews, 2006, 25(23): 3150-3184.
[21] MARLOW J R, LANGE C B, WEFER G, et al.Upwelling intensification as part of the Pliocene-Pleistocene climate transition[J]. Science, 2000, 290: 2288-2291.
[22] MCCLYMONT E L, SOSDIAN S M, ROSELL-MELÉ A, et al.Pleistocene sea-surface temperature evolution: early cooling, delayed glacial intensification, and implications for the mid-Pleistocene climate transition[J]. Earth-Science Reviews, 2013, 123: 173-193.
[23] LISIECKI L E, RAYMO M E. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ¹⁸O records[J]. Paleoceanography, 2005, 20(1): PA1003.
[24] 王婷, 孙有斌, 刘星星. 中更新世气候转型: 特征、机制和展望[J]. 科学通报, 2017, 62(33): 3861-3872.
[25] ZHANG W L, APPEL E, FANG X M, et al.Magnetostratigraphy of deep drilling core SG-1 in the western Qaidam Basin (NE Tibetan Plateau) and its tectonic implications[J]. Quaternary Research, 2012, 78(1): 139-148.
[26] FANG X, ZHANG W, MENG Q, et al.High-resolution magneto-stratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau[J]. Earth and Planetary Science Letters, 2007, 258: 293-306.
[27] PAN G T, WANG L Q, LI R S, et al.Tectonic evolution of the Qinghai-Tibet Plateau[J]. Journal of Asian Earth Sciences, 2012, 53: 3-14.
[28] 张彭熹. 柴达木盆地盐湖[M]. 北京: 科学出版社, 1987: 48-59.
[29] SUN J M, ZHU R X, AN Z S.Tectonic uplift in the northern Tibetan Plateau since 13. 7 Ma ago inferred from molasse deposits along the Altyn Tagh Fault[J]. Earth and Planetary Science Letters, 2005, 235: 641-653.
[30] 沈振枢, 乐昌硕, 雷世太. 柴达木盆地第四纪含盐地层划分及沉积环境[M]. 北京: 地质出版社, 1993: 21-27.
[31] LI M H, FANG X M, WANG J Y, et al.Evaporite minerals of the lower 538.5 m sediments in a long core from the Western Qaidam Basin, Tibet[J]. Quaternary International, 2013, 298: 123-133.
[32] HAN W, FANG X, YE C, et al.Tibet forcing Quaternary stepwise enhancement of westerly jet and central Asian aridification: carbonate isotope records from deep drilling in the Qaidam salt playa, NE Tibet[J]. Global and Planetary Change, 2014, 116: 68-75.
[33] 王九一. 柴达木西部察汗斯拉图凹陷2.8 Ma以来的湖泊沉积演化与亚洲内陆干旱化[D]. 北京: 中国科学院大学, 2012: 36-47.
[34] YANG Y, FANG X, Paleoclimatic significance of rare earth element record of the calcareous lacustrine sediments from a long core (SG-1) in the western Qaidam Basin, NE Tibetan Plateau[J]. Journal of Geochemical Exploration, 2014, 145: 223-232.
[35] 王春虹, 李明慧, 方小敏, 等. 柴达木盆地西部SG-1钻孔中伊蒙混层结构特征及环境意义[J]. 第四纪研究, 2016(4): 917-925.
[36] LI M H, SUN S R, FANG X M, et al.Clay minerals and isotopes of Pleistocene lacustrine sediments from the Western Qaidam Basin, NE Tibetan Plateau[J]. Applied Clay Science, 2018, 162: 382-390.
[37] 李皎. 柴达木盆地西部千米深钻石膏矿物学和稳定同位素特征及其环境意义[D]. 北京: 中国科学院大学, 2017.
[38] LI J, LI M H, FANG X M, et al.Isotopic composition of gypsum hydration water in deep Core SG-1, western Qaidam Basin (NE Tibetan Plateau): implications for paleoclimatic evolution[J]. Global and Planetary Change, 2017, 155: 70-77.
[39] 王慧玲, 李明慧, 方小敏, 等. 柴达木盆地白钠镁矾的矿物学和稳定同位素特征[J]. 矿物岩石, 2018, 38(4): 12-20.
[40] 柳大纲, 陈敬清, 张长美. 柴达木盆地盐湖类型和水化学特征[J]. 盐湖研究, 1996, 4(3): 9-19.
[41] RODRíGUEZ-SANZ M, MORTYN P G, ALFREDO M G, et al. Glacial southern ocean freshening at the onset of the Middle Pleistocene climate transition[J]. Earth and Planetary Science Letters, 2012, 345/346/347/348: 194-202.
[42] PERAL M, BLAMART D, BASSINOT F, et al.Changes in temperature and oxygen isotopic composition of Mediterranean water during the Mid-Pleistocene Transition in the Montalbano Jonico Section (southern Italy) using the clumped-isotope[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2020, 544(15): 109-603.
[43] SNYDER C W.Evolution of global temperature over the past two million years[J]. Nature, 2016, 538(7624): 226-228.
[44] KOUTSODENDRIS A, DIRK S, ERWIN A, et al.Prolonged monsoonal moisture availability preconditioned glaciation of the Tibetan Plateau during the Mid-Pleistocene transition[J]. Geophysical Research Letters, 2018, 45(23): 13020-13030.
[45] ACKERT R P, BRAD S S, HERVÉ G, et al.Long-term cosmogenic ³He production rates from ⁴⁰Ar/³⁹Ar and K-Ar dated Patagonian lava flows at 47°S[J]. Earth and Planetary Science Letters, 2003, 210(1/2): 119-136.
[46] SEJRUP H P, LARSEN E, LANDVIK J, et al.Quaternary glaciations in southern Fennoscandia: evidence from southwestern Norway and the northern North Sea region[J]. Quaternary Science Reviews, 2000, 19(7): 667-685.

柴达木盆地西部中更新世气候转型期的古水温:来自SG-1钻孔石盐流体包裹体的证据

Paleotemperature during the Mid-Pleistocene Transition in western Qaidam Basin: Evidence from fluid inclusions in halite from drill hole SG-1

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	孙辉, 刘晓东. 青藏高原隆升气候效应的数值模拟研究进展概述[J]. 地学前缘, 2022, 29(5): 300-309.
[2]	刘志飞, 陈建芳, 石学法. 深海沉积与全球变化研究的前缘与挑战[J]. 地学前缘, 2022, 29(4): 1-9.
[3]	胡钊彬, 尉建功, 谢志远, 张伙带, 钟广法. 国际大洋钻探全球海平面变化研究进展[J]. 地学前缘, 2022, 29(4): 10-24.
[4]	胡栟铫, 龙飞江, 韩喜彬, 张泳聪, 胡良明, 向波, 葛倩, 边叶萍. 中全新世以来南极宇航员海的古生产力演变[J]. 地学前缘, 2022, 29(4): 113-122.
[5]	张宗言, 刘祥, 李响, 柯学, 张楗钰, 徐亚东. 广东雷州半岛晚渐新世—早更新世孢粉共存因子分析及古气候变化重建[J]. 地学前缘, 2022, 29(2): 303-316.
[6]	S.K.KRIVONOGOV, T.I.KENSHINBAY, R.Kh.KURMANBAEV, B.S.KARIMOVA. 咸海演化的关键问题及其对经济、社会和生态价值的重要启示[J]. 地学前缘, 2021, 28(6): 196-204.
[7]	邵春景, 胡欢, 尹宏伟, 苗忠英, 张雪飞, 李伟强, 夏芝广. 思茅盆地石盐矿物的原位元素含量特征对成矿模式的启示[J]. 地学前缘, 2021, 28(6): 66-78.
[8]	樊馥, 侯献华, 郑绵平, 孟凡巍, 杨振京, 苗青. 柴达木盆地大浪滩梁ZK02孔早—中更新世石盐纯液相流体包裹体均一温度及其对钾盐成矿的约束[J]. 地学前缘, 2021, 28(6): 105-114.
[9]	王军, 张骁, 高岩. 青藏高原植被动态与环境因子相互关系的研究现状与展望[J]. 地学前缘, 2021, 28(4): 70-82.
[10]	欧阳鑫, 章永梅, 顾雪祥, 刘丽, 王路智, 高丽晔. 内蒙古撰山子金矿床流体包裹体特征与矿床成因[J]. 地学前缘, 2021, 28(2): 320-332.
[11]	余晓艳, 郑育宇, 张婷雅, 郭鸿舒, 龙政宇, 万佳鑫, 张存. 云南大丫口祖母绿颜色环带成因对多阶段成矿的指示意义[J]. 地学前缘, 2020, 27(5): 116-125.
[12]	刘洪, 张林奎, 黄瀚霄, 李光明, 欧阳渊, 余槐, 梁维, 张洪铭, 陈小平. 冈底斯西段罗布真浅成低温热液型金银矿的成矿流体演化:来自流体包裹体、H-O同位素的证据[J]. 地学前缘, 2020, 27(4): 49-65.
[13]	王银宏, 刘家军, 张梅, 张方方, 王康, 咸雪辰, 郭灵俊. 内蒙古阿扎哈达铜铋矿床流体包裹体和碳-氧-硫-铅同位素地球化学研究[J]. 地学前缘, 2020, 27(2): 391-404.
[14]	陈宇，曹淑云，邓友国，程雪梅，吕美霞，董彦龙. 哀牢山—红河剪切带中流体记录及地质意义[J]. 地学前缘, 2019, 26(2): 42-57.
[15]	于杰，李诺，张博，疏孙平，陈衍景. 西天山小于赞金矿成矿流体、成矿年代学特征及其地质意义[J]. 地学前缘, 2018, 25(5): 83-95.