Palaeoclimate Reconstruction of Middle Permian in Tuha Basin: Evidence from the Fossil Wood Growth Rings
-
摘要: 收集木化石年轮数据有助于古气候重建工作.首次通过对吐哈盆地北东缘中二叠统塔尔郎组中发现的木化石的年轮统计分析，还原了吐哈盆地中二叠世的古气候演化过程.木化石的年轮分析表明：该区中二叠世整体处于季节性明显的北亚热带，气候整体相对温暖，但出现过间歇性相对炎热的气候.木化石较低的晚材率以及部分年轮早材到晚材为过渡突变，反映树木生长时期季节性非常明显，夏季湿热，冬季干冷，为典型的亚热带季风型气候.木化石具较高的平均敏感度 (MS平均可达0.4)，显示树木生长期间受季风气候的影响，环境非常不稳定，每年大气降水量有很大的变化.连续年轮宽度的宽窄不一以及伪年轮的存在，表明当时气候变化频繁，整体较为湿润，但也具有干旱-半干旱的波动.Abstract: The collection of fossil wood growth rings data is helpful for rebuilding paleoclimate. Based on the statistical analysis of fossil wood growth rings from Middle Permian Taerlang Formation in the northeast edge of Tuha basin, the paleoclimate evolution of Middle Permian is reconstructed for the first time. The analysis of fossil wood growth rings shows that this area was subject to north subtropical climate with obvious seasonal variations during the Middle Permian. The paleoclimate was relatively warm, but intermittent hot climate had occurred. The low percentage of latewood and the abrupt transition between earlywood and latewood of some growth rings reflect that the seasonal variations were very obvious during the period of trees' growth. The paleoclimate was prevailed by a subtropical monsoon climate with hot and humid summer and dry and cold winter. The relatively high mean sensitivity (MS average of 0.4) of fossil woods indicates that trees were influenced by monsoon climate during the growth period, and the environment was very unstable with uneven annual precipitation. The change of consecutive growth ring width and the existence of false rings implies that the climate changed frequently and generally was humid with arid and semi-arid fluctuations.
-
Key words:
- Tuha basin /
- Middle Permian /
- fossil wood /
- growth rings /
- climatology
-
图 1 研究区位置
a.研究区的交通位置；b.研究区二叠纪古地理位置 (据Scotese，2002修改)；c.木化石产出位置；1.高速公路；2.国道或省道；3.国界线；4.木化石产地；5.研究区；P2d.大河沿组；P2t.塔尔朗组；P3q.泉子街组
Fig. 1. The traffic of study area
图 2 塔尔朗组木化石样品及年轮的镜下显微特征
a.木化石野外照片，其中地质锤长约30 cm；b.颜色更深的晚材 (绿色箭头)；c.木化石中的年轮 (红色箭头) 与伪年轮 (白色箭头)；d.极窄的晚材，晚材细胞1~3个 (绿色箭头)
Fig. 2. Fossil wood of Taerlang Formation and the microscopic features of growth rings under microscope
图 4 研究区中二叠世古气候演化
Fig. 4. The paleoclimate evolution of study area during the Middle Permian据吴绍组(1996)修改
表 1 木化石年轮计算结果
Table 1. Calculation results of fossil wood growth rings
样品编号 年轮数量 最大轮宽
(mm)最小轮宽
(mm)平均轮宽
(mm)平均细胞个数 平均晚材率
(%)平均早材细胞大小 (μm) 平均敏感度 1302 7 5.32 3.63 4.33 65 15.9 52 0.19 13031 17 9.10 1.22 5.05 99 21.7 49 0.47 13032 18 2.16 0.50 1.20 24 17.8 42 0.39 1304 15 7.76 0.52 4.89 101 12.8 44 0.71 1305 15 6.89 1.88 3.75 60 8.0 44 0.27 1306 无年轮 无年轮 无年轮 无年轮 无年轮 无年轮 57 ﹨ 1307 12 2.27 0.78 1.28 22 12.2 40 0.36 总数/平均 84 3.42 62 14.7 47 0.40 
下载: 导出CSV
-
Artabe, A.E., Spalletti, L.A., Brea, M., et al., 2007.Structure of a Corystosperm Fossil Forest from the Late Triassic of Argentina.Palaeogeography, Palaeoclimatology, Palaeoecology,243(3-4):451-470. doi: 10.1016/j.palaeo.2006.08.011 Barron, E.J., 1985.Numerical Climate Modeling, a Frontier in Petroleum Source Rock Prediction:Results Base on Cretaceous Simulations.AAPG Bulletin,69(3):448-459.doi: 10.1306/AD46250B-16F7-11D7-8645000102C1865D Deng, B.Z., Yu, L.X., Wang, Y.B., et al., 2015.Evolution of Marine Conditions and Sedimentation during the Permian-Triassic Transition in Chibi of Hubei Province.Earth Science,40(2):317-326(in Chinese with English abstract). https://www.researchgate.net/publication/281765968_Evolution_of_marine_conditions_and_sedimentation_during_the_permian-triassic_transition_in_Chibi_of_Hubei_Province Ding, Q.H., Fu, X.P., Li, Y., et al., 2010.Late Mesozoic Fossil Woods from Southeastern Mongolia.Global Geology,29(4):527-542(in Chinese with English abstract). Ding, Q.H., Zhang, W., Zheng, S.L., 2004.Growth Rings Observation on Fossil Woods and Their Implication from Yixian Formation of Lower Cretaceous in Western Liaoning Province.Geological Science and Technology Information,23(1):38-41(in Chinese with English abstract). https://www.researchgate.net/publication/257047899_Sedimentary_laminations_in_the_lacustrine_Jianshangou_Bed_of_the_Yixian_Formation_at_Sihetun_western_Liaoning_China Falcon-Lang, H.J., 2005.Global Climate Analysis of Growth Rings in Woods, and Its Implications for Deep-Time Paleoclimate Studies.Paleobiology,31(3):434-444.doi:10.1666/0094-8373(2005)031[0434:GCAOGR]2.0.CO; 2 Feng, X.H., Cheng, R.M., Xiao, W.F., et al., 2011.Effects of Air Temperature in Growth Season on Masson Pine (Pinus Massoniana) Radial Growth in North Subtropical Region of China.Chinese Journal of Ecology,30(4):650-655(in Chinese with English abstract). https://www.researchgate.net/publication/288750820_Effects_of_air_temperature_in_growth_season_on_Masson_pine_Pinus_massoniana_radial_growth_in_north_subtropical_region_of_China Fritts, H.C., 1976.Tree Rings and Climate.Academic Press, London, 23-56. Fu, Y.L., 2003.Study on the Wood Anatomy of Chinese Fir in Different Growth Environment (Dissertation).Guangxi University, Nanning (in Chinese with English abstract). Han, Y.L., 2000.Palaeogeography of the Permian in Xinjiang.Xinjiang Geology,18(4):330-334(in Chinese). https://www.researchgate.net/profile/Michael_Benton/publication/283980008_Reply_to_the_comment_on_Chu_et_al_Lilliput_effect_in_freshwater_ostracods_during_the_Permian-Triassic_extinction_Palaeogeography_Palaeoclimatology_Palaeoecology_435_2015_38-52/links/565b2aad08ae1ef92980e5d2.pdf?inViewer=0&pdfJsDownload=0&origin=publication_detail Jin, C.D., Wu, Y.Q., Jin, S.Z., et al., 2001.The Wood Structure of Red Pine under Different Environmental Condition.Journal of Northeast Forestry University,29(3):21-24(in Chinese with English abstract). Li, P., 2004.Middle Permian Fossil Wood from Hulusitai in Inner Mongolia, with Reference to Palaeoclimate (Dissertation).Northwest University, Xi'an (in Chinese with English abstract). Li, Q., Wu, S.Z., Qu, X., et al., 2002.Key Climatic Events during Carboniferous-Triassic in Junggar.Xinjiang Geology,20(3):192-195(in Chinese with English abstract). Li, Y., Liang, E.Y., Shao, X.M., 2008.Variations of Picea Crassifolia Tree-Ring Cell Structure and Their Implications to Past Climate in Eastern Margin of Qaidam Basin, Northwest China.Chinese Journal of Applied Ecology,19(3):524-532(in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_yystxb200803011 Li, Y.A., Cheng, G.L., Li, Q., et al., 1992.Paleo-Magnetic Study of the Eastern Xinjiang.Xinjiang Geology,10(4):329-371(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XJDI199204000.htm Liu, H.F., 1992.Discovery of the Permian-Triassic Strata in the Kulai, Hami, Xinjiang Province and Their Significace.Journal of Northwest University,22(2):209-218(in Chinese with English abstract). https://www.researchgate.net/publication/279696666_Discovery_of_the_Permian_volcanic_rocks_in_the_Bingdaban-Houxia_Tianshan_Mountains_and_its_geological_significance Liu, L.J., Yao, Z.Q., 1996.Early Late Permian Ang-Ara Flora from Turpa-Hami Basin.Acta Palaeontologica Sinica,35(6):644-671(in Chinese with English summary). https://www.researchgate.net/publication/301762587_Mesozoic_reactivated_transpressional_structures_and_multi-stage_tectonic_deformation_along_the_Hong-Che_fault_zone_in_the_northwestern_Junggar_Basin_NW_China Liu, Y.L., Liu, Y.Q., 2004.The Distribution and Significance of Lucaogou Formation of Permain in Santanghu Basin.Northwestern Geology,37(2):36-41(in Chinese with English abstract). https://www.researchgate.net/publication/290456449_Geological_characteristics_and_exploration_potential_of_diamictite_tight_oil_in_the_second_Member_of_the_Permian_Lucaogou_Formation_Santanghu_Basin_NW_China Liu, Y.Q., Feng, Q., Zhou, L.F., et al., 2002.Oil-Bearing Concretion Research and Prospect of Oil Analysis of Permian in Tuha Basin.Acta Petrolei Sinica,23(5):40-43(in Chinese). https://www.researchgate.net/publication/292555250_Study_on_oil_and_gas_accumulation_period_of_Yanchang_Formation_of_Triassic_and_Jurassic_in_North_Shaanxi_slope_zone_Ordos_Basin Liu, Y., Shi, J.F., Shishov, V., et al., 2004.Reconstruction of May-July Precipitation in the North Helan Mountain, Inner Mongolia since AD 1726 from Tree-Ring Late Wood Widths.Chinese Science Bulletin,49(4):405-409.doi: 10.1007/BF02900325 Lu, C.X., Xu, F., Qin, Y.L., et al., 2012.Variation Studies on Late Wood Percentage, Tree-Ring Width and Tissue Prportion of Pinus Massoniana Plantation.Guangxi Forestry Science,41(2):81-85 (in Chinese with English abstract). doi: 10.1007/s13196-012-0062-7 Ouyang, S., Wang, Z., Zhan, J.Z., et al., 2003.Palynology of the Carboniferous and Permian Strata of Northern Xinjiang, Northwestern China.University of Science and Technology of China Press, Hefei (in Chinese). Pires, E.F., Guerra-Sommer, M., 2011.Growth Ring Analysis of Fossil Coniferous Woods from Early Cretaceous of Araripe Basin.An Acad Bras Cienc,83(2):409-23.doi: 10.1590/S0001-37652011005000005 Qian, L.J., Shi, Z.Q., Li, Z.W., et al., 2010.Fossil Wood of the Upper Triassic Xujiahe Formation on the Western Margin of Sichuan Basin:Implication for Palaeoclimate.Acta Sedimentologica Sinica,28(2):324-330(in Chinese with English abstract). https://www.researchgate.net/publication/309319431_Paleoclimate_during_depositional_period_of_the_Upper_Triassic_Xujiahe_Formation_in_Sichuan_Basin Rees, P.M., Gibbs, M.T., Ziegler, A.M., et al., 1999.Permian Climates:Evaluating Model Predictions Using Global Paleobotanical Data.The Geological Society of America,27(10):891-894.doi:10.1130/0091-7613(1999)027＜0891:PCEMPU>2.3.CO; 2 Taylor, E.L., Ryberg, P.E., 2007.Tree Growth at Polar Latitudes Based on Fossil Tree Ring Analysis.Palaeogeography, Palaeoclimatology, Palaeoecology,255(3-4):246-264.doi: 10.1016/j.palaeo.2007.06.013 Wang, C.G., Yang, B., 2004.Prospects of Hydrocarbon Exploration of Permian in Turpan-Hami Basin.Xinjiang Petroleum Geology,25(1):17-18(in Chinese with English abstract). https://www.researchgate.net/publication/241122589_Structural_styles_and_hydrocarbon_accumulation_of_the_northern_piedmont_belt_in_the_Taibei_Sag_Turpan-Hami_Basin Wang, H., Shao, X.M., Fang, X.Q., et al., 2011.Responses of Pinus Koraiensis Tree Ring Cell Scale Parameters to Climate Elements in Changbai Mountains.Chinese Journal of Applied Ecology,22(10):2643-2652(in Chinese with English abstract). https://www.researchgate.net/publication/292295495_Variations_trend_of_annual_mean_temperature_and_precipitation_for_the_last_50_years_in_Jilin_Province Wang, T., Yu, D., Li, J.F., et al., 2003.Advances in Research on the Relationship between Climatic Change and Tree-Ring Width.Acta Phytoecologica Sinica,27(1):23-33(in Chinese with English abstract). https://www.researchgate.net/publication/257548168_Relationship_between_projected_changes_in_future_climatic_suitability_and_demographic_and_functional_traits_of_forest_tree_species_in_Spain Wu, S.Z., 1996.Paleoclimate of Lower Permian in Xinjiang.Xinjiang Geology,14(3):270-277 (in Chinese with English abstract). https://www.researchgate.net/profile/Xianghui_Li2/publication/248597502_Paleosols_of_the_Mid-Cretaceous_A_Report_from_Zhejiang_and_Fujian_SE_China/links/5418e27f0cf2218008bf480c.pdf?inViewer=true&disableCoverPage=true&origin=publication_detail Wu, S.Z., 1998.Paleoclimatic Discussion on Carboniferous-Permian Oil-Generating Strata in the Northern Xinjiang.Xinjiang Geology,16(1):58-68 (in Chinese with English abstract). https://www.researchgate.net/publication/291058708_The_two_kinds_of_tectonic_unit_systems_in_Turpan-Hami_Basin_Xinjiang_China Wu, X.D., 1990.Tree Rings and Climate Change.China Meteorological Press, Beijing (in Chinese). Xu, J.L., Liu, Y.X., Liu, Y.Q., et al., 2013.Sedimentology and Basin Evolution of the Early Permian Yierxitu Formation in Turpan-Hami Area, Xinjiang.Geological Bulletin of China, 32(2-3):424-442(in Chinese with English abstract). https://www.researchgate.net/publication/283027582_Sedimento1-ogy_and_basin_evolution_of_the_Early_Permian_Yierxitu_Formation_in_Turpan-Hami_area_Xinjiang Yang, B., 2010.Restoration of the Paleoenvironment of Late Paleozoic in Eastern Xinjiang (Dissertation).Shandong University of Science and Technology, Qingdao (in Chinese with English abstract). Yuan, M.S., 1998.Oil-Gas Distribution Characteristics and Exploration Strategy in Turpan-Hami Basin.Xinjiang Petroleum Geology,19(2):106-111(in Chinese with English abstract). https://www.researchgate.net/publication/292124796_Characteristics_and_distribution_of_natural_gas_in_Turpan-Hami_Basin Zhang, Q.B., Cheng, G.D., Yao, T.D., et al., 2003.A 2, 326 Year Tree-Ring Record of Climate Variability on the Northeastern Qinghai-Tibetan Plateau.Geophysical Research Letters,30(14):1739-1742.doi: 10.1029/2003GL017425 Zhang, X.H., Li, D.W., Yuan, Y.M., et al., 2003.Discovery and Geological Significance of Jurassic Fossil Wood in Dingri Area, Tibet.Earth Science,28(1):20-21(in Chinese). Zheng, H.R., Hu, Z.Q., 2010.Pre-Mesozoic Tectonic Lithofacies Paleogeographic Atlas of Chinese.Geological Publishing House, Beijing (in Chinese). Ziegler, A.M., 1990.Phytogeographic Patterns and Continental Configurations during the Permian Period.Geological Society, London, Memoirs,5(12):363-379. http://mem.lyellcollection.org/content/12/1/363 邓宝柱, 余黎雪, 王永标, 等, 2015.湖北赤壁二叠纪-三叠纪之交古海洋沉积环境演化.地球科学, 40(2):317-326. http://earth-science.net/WebPage/qk.aspx?id=134# 丁秋红, 傅晓平, 李勇, 等, 2010.蒙古东南部晚中生代木化石.世界地质, 29(4):527-542. http://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ201004001.htm 丁秋红, 张武, 郑少林, 2004.辽西下白垩统义县组化石木年轮的观察及其意义.地质科技情报, 23(1):38-41. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200401008.htm 封晓辉, 程瑞梅, 肖文发, 等, 2011.北亚热带生长期温度对马尾松径向生长的影响.生态学杂志, 30(4):650-655. http://www.cnki.com.cn/Article/CJFDTOTAL-STXZ201104005.htm 符韵林, 2003.不同生长环境的杉木木材解剖研究 (硕士学位论文).南宁:广西大学. 韩玉玲, 2000.新疆二叠纪古地理.新疆地质, 18(4):330-334. http://www.cnki.com.cn/Article/CJFDTOTAL-XJDI200004011.htm 金春德, 吴义强, 金顺泽, 等, 2001.不同生长环境赤松木材构造的变异.东北林业大学学报, 29(3):21-24. http://www.cnki.com.cn/Article/CJFDTOTAL-DBLY200103004.htm 李萍, 2004.内蒙古呼鲁斯台中二叠世木化石及古生态研究 (硕士学位论文).西安:西北大学. 李强, 吴绍祖, 屈迅, 等, 2002.试论准噶尔石炭纪-三叠纪重要气候事件.新疆地质, 20(3):192-195. http://www.cnki.com.cn/Article/CJFDTOTAL-XJDI200203003.htm 李雁, 梁尔源, 邵雪梅, 2008.柴达木盆地东缘青海云杉树轮细胞结构变化特征及其对气候的指示.应用生态学报, 19(3):524-532. http://www.cnki.com.cn/Article/CJFDTOTAL-YYSB200803013.htm 李永安, 程国良, 李强, 等, 1992.新疆东部古地磁研究.新疆地质, 10(4):329-371. http://www.cnki.com.cn/Article/CJFDTOTAL-XJDI199204001.htm 刘洪福, 1992.新疆哈密库莱二叠-三叠纪地层的发现及其意义.西北大学学报自然科学版, 22(2):209-218. http://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ199202019.htm 刘陆军, 姚兆奇, 1996.吐鲁番-哈密盆地晚二叠世早期植物群.古生物学报, 35(6):644-671. http://www.cnki.com.cn/Article/CJFDTOTAL-GSWX199606001.htm 刘延莉, 柳益群, 2004.三塘湖盆地二叠纪芦草沟组分布及其意义.西北地质, 37(2):36-41. http://www.cnki.com.cn/Article/CJFDTOTAL-XBDI200402007.htm 柳益群, 冯乔, 周立发, 等, 2002.吐哈盆地二叠系含油结核研究及生油前景分析.石油学报, 23(5):40-43. doi: 10.7623/syxb200205008 卢翠香, 徐峰, 覃引鸾, 等, 2012.人工林马尾松晚材率、年轮宽度和组织比量变异研究.广西林业科学, 41(2):81-85. http://www.cnki.com.cn/Article/CJFDTOTAL-GXLK201202002.htm 欧阳舒, 王智, 詹家祯, 等, 2003.新疆北部石炭纪-二叠纪孢子花粉研究.合肥:中国科学技术大学出版社. 钱利军, 时志强, 李智武, 等, 2010.四川盆地西缘地区上三叠统须家河组化石木年轮的古气候意义.沉积学报, 28(2):324-330. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201002015.htm 王昌桂, 杨飚, 2004.吐哈盆地二叠系油气勘探潜力.新疆石油地质, 25(1):17-18. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200401005.htm 王辉, 邵雪梅, 方修琦, 等, 2011.长白山红松年轮细胞尺度参数对气候要素的响应.应用生态学报, 22(10):2643-2652. http://www.cnki.com.cn/Article/CJFDTOTAL-YYSB201110024.htm 王婷, 于丹, 李江风, 等, 2003.树木年轮宽度与气候变化关系研究进展.植物生态学报, 27(1):23-33. doi: 10.17521/cjpe.2003.0004 吴绍祖, 1996.新疆早二叠世古气候.新疆地质, 14(3):270-277. http://www.cnki.com.cn/Article/CJFDTOTAL-XJDI603.009.htm 吴绍祖, 1998.从古气候探讨新疆北部石炭-二叠纪生油层位.新疆地质, 16(1):58-68. http://www.cnki.com.cn/Article/CJFDTOTAL-XJDI199801006.htm 吴祥定, 1990.树木年轮与气候变化.北京:气象出版社. 徐加林, 刘燕学, 柳永清, 等, 2013.新疆吐鲁番-哈密盆地北部下二叠统伊尔稀土组的沉积特征与盆地演化.地质通报, 32(2-3):424-442. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2013Z1019.htm 杨犇, 2010.东疆地区晚古生代古环境恢复 (硕士学位论文).青岛:山东科技大学. 袁明生, 1998.吐哈盆地油气分布特征及勘探方向.新疆石油地质, 19(2):106-111. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD802.002.htm 张雄华, 李德威, 袁晏明, 等, 2003.西藏定日一带侏罗系硅化木的发现及其地质意义.地球科学, 28(1):20-21. http://earth-science.net/WebPage/Article.aspx?id=2466 郑和荣, 胡宗全, 2010.中国前中生代构造-岩相古地理图集.北京:地质出版社. -
点击查看大图
图(4) / 表(1)
计量
- 文章访问数: 4804
- HTML全文浏览量: 1484
- PDF下载量: 35
- 被引次数: 0
