黄土高原微生物膜类脂物和碳酸盐二元同位素重建古温度的研究进展

季顺川; 彭廷江; 聂军胜; 彭文彬

doi:10.3724/SP.J.1140.2013.03151

黄土高原微生物膜类脂物和碳酸盐二元同位素重建古温度的研究进展

兰州大学西部环境与气候变化研究院, 兰州 730000

基金项目:
兰州大学中央高校基本科研业务费专项资金项目(860552)；国家自然科学基金项目(41172329)；教育部新世纪人才基金项目(NCET-09-0443)

详细信息

作者简介: 季顺川(1987-),男,硕士生,主要从事古气候变化研究,E-mail:jisc11@lzu.edu.cn

中图分类号: P579

收稿日期: 2012-06-20

修回日期: 2012-09-20

QUANTITATIVE PALEOTEMPERERATURE RECONSTRUCTION OF THE CHINESE LOESS PLATEAU: A REVIEW

Key Laboratory of Western China's Environmental Systems, Ministry of Education, Lanzhou University, Lanzhou 730000

Received Date: 20 June 2012

Revised Date: 20 September 2012

摘要

摘要: 黄土高原地区连续的黄土沉积是研究古气候演变的天然档案,如何选取气候环境意义较为明确的代用指标重建古环境是当前研究的热点议题。尽管磁化率、粒度、碳酸钙和孢粉等被广泛地用于东亚地区冬夏季风历史的半定量重建,但是,对于该地区更为细致的古温度定量重建工作却少有涉及,目前尚处于起步阶段。鉴于黄土-古土壤巨大的研究潜力以及古温度定量重建对深入理解古气候演变及其驱动机制的特殊意义,黄土高原地区古温度研究应给予高度关注。在已发表的黄土高原古温度重建的两种方法(MBT/CBT、二元同位素)基础上,详细介绍MBT/CBT和二元同位素的原理和应用;进而总结该地区晚中新世以来的温度变化历史并讨论生物标志化合物和二元同位素在黄土高原地区的应用前景和存在问题。
- 古温度 /
- MBT/CBT指标 /
- 二元同位素 /
- 定量重建 /
- 黄土高原
Abstract: The continuous late Miocene-Pliocene red-clay sequence and the Quaternary loess sequence on the Chinese Loess Plateau (CLP) have provided valuable information for the study of Asian paleoclimate history. Although numerous climatic proxies have been applied to Chinese loess, few are able to reflect paleotemperature history of the CLP. Here we reviewed the theory of two novel paleotemperature proxies (MBT/CBT, and "clumped isotope") and their application to the CLP to further understand the temperature history of the CLP. Applying these two proxies to the same materials will be able to further test their validity in reflecting temperature history on the CLP and is the natural step in future paleoclimate studies.
- paleotemperature /
- MBT/CBT /
- clumped isotope /
- quantitative restruction /
- Chinese loess plateau

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参考文献(56)

[1]	Liu T S. Loess and the Environment[M]. Beijing:China Ocean Press, 1985.
[2]	An Z S, Kutzbach J E, Prell W L, et al, Evolution of Asian monsoons and phased uplift of the Himalaya -Tibetan plateau since Late Miocene times[J]. Nature, 2001, 411:62-66.
[3]	Guo Z T, Peng S Z, Hao Q Z, et al, Late Miocene -Pliocene development of Asian aridification asrecorded in the red-earth formation in northern China[J].Global and Planetary Change, 2004, 41:135-145
[4]	Porter S C, An Z S. Correlation between climate events in the North Atlantic and China during the last glaciation[J]. Nature, 1995, 375:305-308.
[5]	Guo Z T, Liu T S, Fedoroff N, et al. Climate extremes in Loess of China coupled with the strength of deep-water formation in the North Atlantic[J]. Global and Planetary Change,1998,18:113-128.
[6]	Fang X M, Li J J, van der Voo R. Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800000 years BP related to Tibetan uplift[J]. Earth and Planetary Science Letters, 1999, 165:129-144.
[7]	Ding Z L, Yang S L, Sun J M, et al. Iron geochemistry of loess and red clay deposits in the Chinese Loess Plateau and implications for long term Asian monsoon evolution in the last 7.0 Ma[J]. Earth and Planetary Science Letters,2001,85:99-109.
[8]	Nie J S, King J W, Fang X M. Correlation between the magnetic susceptibility record of the Chinese aeolian sequences and the marine benthic oxygen isotope record[J]. Geochemistry Geophysics Geosystems, 2008, 9:1-7.
[9]	Kukla G, An Z S, Melice J, et al. Magnetic susceptibility of Chinese Loess:Transactions of the Royal Society of Edinburgh[J]. Earth Sciences,1990, 81:263-288.
[10]	Guo Z, Liu T, Guiot J, et al. High frequency pulses of East Asian monsoon climate in the last two glaciations:Link with the North Atlantic[J]. Climate Dynamics, 1996,12:701-709.
[11]	Sun D H, Shaw J, An Z S, et al. Magnetostratig-raphy and paleoclimatic interpretation of a continuous 7.2 Ma Late Cenozoic Eolian sediments from the Chinese loess plateau[J]. Geophysical Research Letters, 1998, 25:85-88.
[12]	Lu H Y, Liu X D, Zhang F Q, et al. Astronomical calibration of loess-paleosol deposits at Luochuan,central Chinese Loess Plateau[J]. Palaeogeography,Palaeoclimatology, Palaeoecology, 1999, 154:237-246.
[13]	Sun J M. Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau[J]. Earth and Planetary Science Letters, 2002, 203:845-859.
[14]	Bloemendal J,and Liu X M. Rock magnetism and geochemistry of two plio-pleistocene Chinese loess-palaeosol sequences-implications for Quantitative paleoprecipitation reconstruction[J]. Palaeogeography,Palaeoclimatology,Palaeoecology, 2005, 226:149-166.
[15]	Song Y G, Fang X M, Torii M, et al. Late Neogene rock magnetic record of climatic variation from Chinese eolian sediments related to uplift of the Tibetan Plateau[J]. Journal of Asian Earth Sciences, 2006,30:324-332.
[16]	Lu H Y, Wu N Q, Liu K B, et al. Phytoliths as quantitative indicators for the reconstruction of past environmental conditions in China Ⅱ:palaeoenvironmental reconstruction in the Loess Plateau[J]. Quaternary Science Reviews, 2007,26:759-772.
[17]	Heller F, Liu T S. Magnetostratigraphical dating of loess deposits in China[J]. Nature, 1982,300:431-433.
[18]	An Z S, Kukla G, Porter S C, et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130000 years[J]. Quaternary Research, 1991,36:29-36.
[19]	Lu H Y, Han J M, Wu N Q, et al. Magnetic susceptibility of the modern soils in China and paleoclimatic significance[J]. Science in China (Series B), 1994, 24:1290-1297.
[20]	Liu X M, Rolph T, Bloemendal J,et al. Quantitative estimates of palaeoprecipitation at Xifeng area, in the loess plateau of China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,1995, 113:243-248.
[21]	Maher B A, Thompson R, Zhou L P. Spatial and temporal reconstructions of changes in the Asia paleomonsoon:a new mineral magnetic approach[J].Earth and Planetary Science Letters,1994,125:461-471.
[22]	Nie J S, Song Y, King J W, et al. Consistent grainsize distribution of pedogenic maghemite of surface soils and Miocene loessic soils on the Chinese Loess Plateau[J]. Journal of Quaternary Science, 2010,25:261-266.
[23]	Lu H Y, Han J M, Wu N Q, et al. Magnetic susceptibility of the modern soils in China and paleoclimatic significance[J]. Science in China (Series B), 1994,24:1290-1297.
[24]	Han J M, Wu N Q, et al. The magnetic susceptibility of modern soils in China and its use for paleoclimate reconstruction[J]. Earth and Environmental Science, 1996, 40:262-275.
[25]	Wang Z R, Schauble E A, Eiler J M. Equilibrium thermodynamics of multiply substituted isotopologues of molecular gases[J]. Geochimica et Cosmochimica Acta, 2004, 68:4779-4797.
[26]	Eiler J M. "Clumped-isotope" geochemistry:The study of naturally-occurring, multiply-substituted isotopologues[J]. Earth and Planetary Science Letters, 2007,262:309-327.
[27]	Eiler J M. A practical guide to clumped isotope geochemistry[J]. geochimica et Cosmochimica Acta, 2006, 70:A157.
[28]	Ghosh P, Adkins J, Affek H, et al. ¹³C-¹⁸O bonds in carbonate minerals:A new kind of Paleoth-Ermometer[J]. Geochimica et Cosmochimica Acta,2006, 70:1439-1456.
[29]	Schauble E A, Ghosh P, Eiler J M. Preferential formation of ¹³C-¹⁸O bonds in carbonate minerals, estimated using first-principles lattice dynamics[J]. Geochimica et Cosmochimica Acta,2006, 70:2510-2529.
[30]	Affek H P, Bar-Matthews M, Ayalon, et al. Glacial/interglacial temperature variations in Soreq cave Speleothemsas recorded by "clumped isotope" thermometry[J]. Geochimica et Gosmochimica Acta, 2008, 72:5351-5360.
[31]	Sun Q, Chu G Q, Liu M M. Distributions and temperature dependence of branched glycerol dialkyl glycerol tetraethers in recent lacustrine sediments from China and Nepal[J]. Journal of Geophysical Reseach, 2011,116:G01008.
[32]	Eiler J M. Paleoclimate reconstruction using carbonate clumped isotope thermometry[J]. Quaternary Sciengce Reciews,2011,30(25-26):3575-3588.
[33]	Dennis K J, Affek H P, Passey B H, et al. Defining an absolute reference frame for "clumped isotope" studies of O₂[J]. Geochimicaet Cosmochimica Acta,2011,75(22):7117-7131.
[34]	Keating-Bitonti C R, Ivany L C,Affek H P,et al. Warm, not super-hot, temperatures in the early Eocene subtropics[J]. Geology,2011,39(8):771-774.
[35]	Daeron M, Guo W, Eiler J, et al. (CO)-C-13-O-18 clumping in speleothems:Observations from natural caves and precipitation experimes[J]. Geochimica et Cosmochimica Acta, 2011,75(12):3303-3317.
[36]	Peterse F, Prins M A, Beets C J, et al. Decoupled warming and monsoon precipitation in East Asia over the last deglaciation[J]. Earth and Planntary Science Letters,2011,301(1-2):256-264.
[37]	Li G, Nie J S, Steven C,et al. The importance of solar insolation on the temperature variations for the past 110 kyr on the Chinese loess plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2012,317-318:128-133.
[38]	Zachos J C, Schouten S, Bohaty S, et al. Extreme warming of mid-latitude coastal ocean during the Paleocene-Eocene thermal maximum:Inferences from TEX₈₆ and isotope data[J]. Geology, 2006, 34(9):737-740.
[39]	Kim J H, Schouten S, Hopmans E C, et al. Global sediment core-top calibration of the TEX86 paleothermometer in the ocean[J]. Geochimica et Cosmochimica Acta, 2008,72(4):1154-1173.
[40]	Hopmans E C, Weijers J W H, Schefu E, et al. A novel proxy for terrestrial organic matter in sediments based on branched and isoprenoid tetraether lipids[J]. Earth and Planetary Science Letters, 2004, 224:107-116.
[41]	Peterse F, Kim J H, Schouten S, et al. Constraintson the application of the MBT/CBT palaeothermometer in high latitude environments (Svalbard,Norway)[J]. Organic Geochemistry, 2009,40:692-699.
[42]	Weijers J W H, Schouten S, van den Donker J C,et al. Environmental controls on bacterial tetraether membrane lipid distribution in soils[J]. Geochimica et Cosmochimica Acta, 2007,71:703-713.
[43]	Weijers J W H, Schefu E, Schouten S, et al. Coupled thermal and hydrological evolution of tropical Africa over the last deglaciation[J]. Science, 2007, 315:1701-1704.
[44]	Weijers J W H, Schouten S, Schefu E, et al. Disentangling marine, soil and plant organic carbon contributions to continental margin sediments:A multi-proxy approach in a 20000 year sediment record from the Congo deep sea fan[J]. Geochimicaet Cosmochimica Acta, 2009, 73:119-132.
[45]	Damst S J S, Ossebaar J, Abbas B, et al. Fluxes and distribution of tetraether lipids in an equatorial African lake:constraints on the application of the TEX₈₆ palaeothermometer and BIT index in lacustrine settings[J]. Geochimica et Cosmochimica Acta, 2009, 73:4232-4249.
[46]	Tierney J E, Russella J M, Eggermontc H,et al. Environmental controls on branched tetraether lipid distributions in tropical East African lake sediments[J]. Geochimica et Cosmochimica Acta, 2010,74:4902-4918.
[47]	Hopmans E C, Schouten S, Pancost R D, et al. Analysis of intact tetraether lipids in archaeal cell material and sediments by high performance liquid chromatography/atmospheric pressure chemical ionization mass spectrometry[J]. Rapid Communications in Mass Spectrometry,2000, 14:585-589.
[48]	Hao Q Z, Guo Z T, Qiao Y S, et al. Geochemical evidence for the provenance of middle Pleistocene loess deposits in southern China[J]. Quaternary Science Reviews, 2010, 29:3317-3326.
[49]	Oldfield F, Bloemendal J. Rock-magnetic properties confirm the eolian origin of Miocene sequences from the west of the Chinese loess plateau sediment[J]. Geol., 2010,doi:10.1016/j. sedgeo.2010.11.009
[50]	党心悦, 杨欢,谢树成, 末次冰期以来渭南黄土类脂物的分布特征及其古气候意义[C]//中国古生物学会第26届学术年会论文集.2011.[DANG Xinyue, YANG Huan, XIE Shucheng. Characteristics of the distribution of lipids in the Weinan loess and its paleoclimate significance since the Last Glacial[C]//The 26th session of the Palaeontological Society of China. 2011.]
[51]	Urey H C. The thermodynamic properties of isotopic substances[J]. Journal of the Chemical Society,1947:562-581.
[52]	Suarez M B, Passey B H, Kaakinen A. Paleosol carbonate multiple isotopologue signature of active East Asian summer monsoons during the late Miocene and Pliocene[J]. Geology, 2011,39(12):1151-1154.
[53]	Came R E, Eiler J M, Veizer J, et al. Coupling of surface temperatures and atsmospheric CO₂ concentrations during the Palaeozoic era[J]. Nature,2007,449:198-201.
[54]	Passey B H, Levina N E, Cerling T E, et al. High-temperature environments of human evolution in East Africa based on bond ordering in paleosol Carbonates[J]. Earth and Planetary Sciences,2010, 107(25):11245-11249.
[55]	Huntington K W, Eiler J M, Affek H P, et al. Methods and limitations of "clumped" CO₂ isotope(Δ47) analysis by gas-source isotope ratio mass spectrometry[J]. Research Article,2009,44(9):1318-1329.
[56]	Eilera J M, Schaublea E.¹⁸O¹³C¹⁶O in earth's atmosphere[J]. Geochimica et Cosmochimica Acta, 2004, 23(68):4767-4777.

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黄土高原微生物膜类脂物和碳酸盐二元同位素重建古温度的研究进展

兰州大学西部环境与气候变化研究院, 兰州 730000

作者简介: 季顺川(1987-),男,硕士生,主要从事古气候变化研究,E-mail:jisc11@lzu.edu.cn

QUANTITATIVE PALEOTEMPERERATURE RECONSTRUCTION OF THE CHINESE LOESS PLATEAU: A REVIEW

Key Laboratory of Western China's Environmental Systems, Ministry of Education, Lanzhou University, Lanzhou 730000

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