中国西南地区晚二叠世泥炭地净初级生产力及其控制因素<sup>*</sup>

doi:10.7605/gdlxb.2011.05.001

古地理学报 ›› 2011, Vol. 13 ›› Issue (5): 473-480. doi: 10.7605/gdlxb.2011.05.001

中国西南地区晚二叠世泥炭地净初级生产力及其控制因素^*

邵龙义¹ 汪浩¹ Large D J²

1 中国矿业大学（北京）地球科学与测绘工程学院，北京100083
2 英国诺丁汉大学工程学院，NG72RD

收稿日期:2011-05-15 修回日期:2011-07-01 出版日期:2011-10-01 发布日期:2011-10-01
作者简介:邵龙义，男，1964年生，1989年毕业于中国矿业大学（北京），获工学博士学位，现为中国矿业大学（北京）地球科学与测绘工程学院教授，博士生导师，长期从事沉积学和煤田地质学的教学及研究工作。E-mail:ShaoL@cumb.edu.cn。
基金资助:
*谨以此文祝贺张鹏飞教授九十华诞

国家自然科学基金重点项目（编号：1030213）及国家科技重大专项（编号：2011ZX05009-002）联合资助

Net primary productivity and its control of the Late Permian peatlands in southwestern China

Shao Longyi¹, Wang Hao¹, Large D J²

1 School of Geoscience and Survey Engineering，China University of Mining and Technology(Beijing)，Beijing 100083
2 Faculty of Engineering，University of Nottingham，UK，NG72RD

Received:2011-05-15 Revised:2011-07-01 Online:2011-10-01 Published:2011-10-01
About author:Shao Longyi，born in 1964，graduated and obtained his Ph.D.degree from China University of Mining and Technology(Beijing)in 1989.Now he is a professor at the School of Geoscience and Survey Engineering of China University of Mining and Technology(Beijing)，with main interests in sedimentology and coal geology.

摘要/Abstract

摘要： 米兰科维奇旋回理论是古环境研究中重要的时间“度量”工具。文中以贵州普安糯东17号煤层和云南富源天佑10号煤层为例，对晚二叠世煤层的地球物理测井信号进行频谱分析，以获得其中的米兰科维奇轨道周期参数。研究发现，测井信号所反映出的煤层灰分含量变化受泥炭地发育时期的米兰科维奇轨道周期（123 ka（偏心率）：35.6 ka（斜率）：21.2 ka（岁差））驱动。以煤层剖面中的轨道周期为时间尺度，进一步计算出晚二叠世泥炭地的碳聚集速率为54.3～77.0 gC/（m²·a），对应的净初级生产力(NPP)为543～1540 gC/（m²·a）。基于晚二叠世、晚石炭世和现代热带泥炭地的NPP与各个时期大气成分的对比结果显示，大气中的二氧化碳和氧气含量对陆相生态系统的净初级生产力具有关键性的控制作用。

关键词: 米兰科维奇旋回, 晚二叠世, 泥炭地, 碳聚集速率, 净初级生产力

Abstract: Milankovitch theory is an important tool in constraining time in the palaeoenviorment analysis. In this study，the geophysical logs of the Late Permian No.17 Coal in Nuodong，Puan of Guizhou Province and No.10 Coal in Tianyou，Fuyuan of Yunnan Province are analyzed employing spectral analysis.The result shows that the mineral matter content(ash yield)of the coal was possibly influenced by 123ka(eccentricity)，35.6 ka(obliquity)and 21.2 ka(precession)Milankovitch cycles.Using this timeframe，the Lopingian tropical peatland carbon accumulation rate is calculated to be 54.3～77.0 gC/（m²·a），which is expected to correspond to a NPP of 543～1540 gC/（m²·a）. A comparison of NPP and temporal atmospheric composition among the Late Permian，Late Carboniferous and modern time indicates that the Late Permian NPP calculated is consistent with geochemical and palaeobotanical models，supporting a proposal that terrestrial productivity is mainly controlled by temporal atmospheric O₂ and CO₂ levels.

Key words: Milankovitch cycle, Late Permian, peatland, carbon accumulation rate, net primary productivity(NPP)

中图分类号:

P618.117

邵龙义, 汪浩, Large D J. 中国西南地区晚二叠世泥炭地净初级生产力及其控制因素^*[J]. 古地理学报, 2011, 13(5): 473-480.

Shao Longyi, Wang Hao, Large D J. Net primary productivity and its control of the Late Permian peatlands in southwestern China[J]. JOURNAL OF PALAEOGEOGRAPHY, 2011, 13(5): 473-480.

http://www.gdlxb.cn/CN/Y2011/V13/I5/473

参考文献

郭英廷.1990a.贵州西部晚二叠世古气候［J］.中国煤田地质，2（3）:18-20.
郭英廷.1990b.贵州西部晚二叠世含煤地层的植物古生态［J］.煤炭学报，15:48-49.
李星学，沈光隆，田宝霖，等.1995.中国煤核植物群［M］.见: 李星学（主编）.中国地质时期植物群.广东广州：广州科技出版社，190-221.
罗忠，邵龙义，姚光华，等.2008.滇东黔西上二叠统含煤岩系泥岩粘土矿物组成及环境意义［J］.古地理学报，10（3）：297-304.
邵龙义，刘红梅，田宝霖，等.1998.上扬子地区晚二叠世沉积演化及聚煤［J］.沉积学报，16(2): 55-60.
田宝霖，张连武.1980.贵州水城汪家寨矿区化石图册［M］.北京：煤炭工业出版社，1-110.
Allègre C J.2008.Isotope Geology［M］.Cambridge: Cambridge University Press，1-512.
Aselmann I，Crutzen V.1990.A Global Inventory of Wetland Distribution and Seasonality，Net Primary Productivity，and Estimated Methane Emissions［M］.In: Bouwman A F(ed).Soils and the Greenhouse Effect.Chichester: John Wiley，441-449.
Beerling D J，Woodward F Ⅰ.2001.Vegetation and the Terrestrial Carbon Cycle: Modelling the First 400 Million Years［M］.Cambridge:Cambridge University Press，1-405.
Berger A，Loutre M F，Dehant V.1989.Pre-Quaternary Milankovitch frequencies［J］.Nature，342: 133-133.
Berger A，Loutre M F，Laskar J.1992.Stability of the astronomical frequencies over the earths history for paleoclimate studies［J］.Science，255: 560-566.
Berner R A.2005.The carbon and sulfur cycles and atmospheric oxygen from middle Permian to middle Triassic［J］.Geochimica et Cosmochimica Acta，69: 3211-3217.
Berner R A.2006.Geocarbsulf: A combined model for Phanerozoic atmospheric O₂ and CO₂［J］.Geochimica et Cosmochimica Acta，70: 5653-5664.
Berner R A.2009.Phanerozoic atmospheric oxygen: New results using the geocarbsulf model［J］. American Journal of Science，309: 603-606.
Cleal C J，Thomas B A.2005.Palaeozoic tropical rainforests and their effect on global climates: Is the past the key to the present？［J］.Geobiology，3: 13-31.
Clymo R S，Turunen J，Tolonen K.1998.Carbon accumulation in peatland［J］.Oikos，81: 368-388.
Diessel C，Boyd R，Wadsworth J， et al.2000.On balanced and unbalanced accommodation/peat accumulation ratios in the Cretaceous coals from Gates Formation，Western Canada，and their sequence-stratigraphic significance［J］.International Journal of Coal Geology，43:143-186.
Diessel C F K.1992.Coal-bearing Depositional System［M］. New York: Springer-Verlag，1-721.
Fluteau F，Besse J，Broutin J， et al.2001.Extension of Cathaysian flora during the Permian: Climatic and paleogeographic constraints［J］.Earth and Planetary Science Letters，193: 603-616.
Frakes L，Francis J，Syktus J.1992. Climate Modes of the Phanerozoic［M］.New York: Cambridge University Press，1-274.
Ghil M，Allen M R，Dettinger M D， et al. 2002，Advanced spectral methods for climatic time series［J］.Reviews of Geophysics，40: 1-41.
Greb S F，DiMichele W A，Gastaldo R A.2006.Evolution and Importance of Wetlands in Earth History［M］.In: Greb S F，diMichele W A(eds).Wetlands Through Time.Volume Geological Society of America Special Publication 399， Boulder:1-40.
Hilton J，Cleal C J.2007.The relationship between Euramerican and Cathaysian tropical floras in the Late Palaeozoic: Palaeobiogeographical and palaeogeographical implications［J］.Earth-Science Reviews，85:85-116.
ICS.2009.International Stratigraphic Chart［M］.International Commission on Stratigraphy.
Large D J.2007.A 1.16Ma record of carbon accumulation in western European peatland during the Oligocene from the Ballymoney lignite，Northern Ireland［J］.Journal of the Geological Society，164: 1233-1240.
Large D J，Jones T F，Briggs J， et al.2004.Orbital tuning and correlation of 1.7 my of continuous carbon storage in an early Miocene peatland［J］.Geology，32: 873-876.
Large D J，Jones T F，Somerfield C， et al.2003.High-resolution terrestrial record of orbital climate forcing in coal［J］.Geology，31: 303-306.
Moore P D.1987. Ecological and hydrological aspects of peat formation［J］.Geological Society，London，Special Publications，32: 7-15.
Nadon G C.1998.Magnitude and timing of peat-to-coal compaction［J］.Geology，26: 727-730.
Neue H U，Gaunt J L，Wang Z P， et al.1997.Carbon in tropical wetlands［J］. Geoderma，79: 163-185.
Neuzil S G.1997.Onset and rate of peat and carbon accumulation in four domed ombrogenous peat deposits，Indonesia［C］.In: Rieley J O，Page S E(eds).Biodiversity and Sustainability of Tropical Peatlands.Cardigan: Samara Publishing，55-72.
Page S E，Siegert F，Rieley J O， et al.2002.The amount of carbon released from peat and forest fires in Indonesia during 1997［J］.Nature，420: 61-65.
Schwarzacher W.1993.Cyclostratigraphy and the Milankovitch Theory［M］.Amsterdam: Elsevier，1-225.
Sorensen K W.1993. Indonesian Peat Swamp Forests and their role as a carbon sink［J］.Chemosphere，27: 1065-1082.
Wang H，Shao L，Hao L， et al.2011a.Sedimentology and sequence stratigraphy of the Lopingian(Late Permian)coal measures in southwestern China［J］.International Journal of Coal Geology，83: 168-183.
Wang H，Shao L，Large D J，et al. 2011b.Constraints on carbon accumulation rate and net primary production in Late Permian tropical peatland in SW China［J］. Palaeogeography，Palaeoclimatology， Palaeoecology，300: 152-157.
Wang J，Li H.1998.Paleo-latitude variation of Guizhou terrain from Devonian to Cretaceous［J］.Chinese Journal of Geochemistry，17: 356-361.
Weedon G P.2003.Time-Series Analysis and Cyclostratigraphy: Examining Stratigraphic Records of Environmental Cycles［M］.New York: Cambridge University Press，1-274.
Zaritsky RV.1975.On thickness decrease of parent substance of coal，the 7th International Congress on Carboniferous Stratigraphy and Geology［J］.Comptes Rendus，4: Frefeld，Geologisches Landesamt Nordrhein-Westfalen，393-396.

[1]	邵龙义, 张超, 闫志明, 董大啸, 高彩霞, 李英娇, 徐晓燕, 梁万林, 易同生, 徐锡惠, 黎光明, 陈忠恕, 程爱国. 华南晚二叠世层序—古地理及聚煤规律^*[J]. 古地理学报, 2016, 18(6): 905-919.
[2]	查宇铭, 吴欣松, 余达. 松辽盆地松科1井上白垩统烃源岩有机碳含量与沉积速率的关系^*[J]. 古地理学报, 2016, 18(5): 857-864.
[3]	张运波, 王根厚, 余正伟, 赵宗举, 王明健, 孙衍鹏. 四川盆地中二叠统茅口组米兰科维奇旋回及高频层序[J]. 古地理学报, 2013, 15(6): 777-786.
[4]	曲希玉, 张满利, 刘立, 王德海, 邱隆伟. 中国东北地区晚二叠世岩相古地理特征[J]. 古地理学报, 2013, 15(5): 679-692.
[5]	乔彦国, 时志强, 王艳艳, 张彪. 四川广元上寺剖面晚二叠世—早三叠世旋回地层：基于小波分析的P-T界线地质事件探讨^*[J]. 古地理学报, 2012, 14(3): 403-410.
[6]	刘加强毛志芳王训练周洪瑞高金汉郑楠于蕾. 滇东南地区晚二叠世吴家坪早期岩相古地理^*[J]. 古地理学报, 2012, 14(3): 365-374.
[7]	刘喜停　马志鑫　颜佳新. 扬子地区晚二叠世吴家坪期沉积环境及烃源岩发育的控制因素[J]. 古地理学报, 2010, 12(2): 244-252.

选择文件类型/文献管理软件名称

选择包含的内容

中国西南地区晚二叠世泥炭地净初级生产力及其控制因素^*

Net primary productivity and its control of the Late Permian peatlands in southwestern China

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 7

编辑推荐

Metrics

本文评价

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

中国西南地区晚二叠世泥炭地净初级生产力及其控制因素*

Net primary productivity and its control of the Late Permian peatlands in southwestern China

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 7

编辑推荐

Metrics

本文评价

中国西南地区晚二叠世泥炭地净初级生产力及其控制因素^*