东南极拉斯曼丘陵湖泊沉积生物标志物记录及其环境气候意义

doi:10.3724/SP.J.1084.2012.00205

极地研究 ›› 2012, Vol. 24 ›› Issue (3): 205-214.DOI: 10.3724/SP.J.1084.2012.00205

• 研究论文 • 下一篇

东南极拉斯曼丘陵湖泊沉积生物标志物记录及其环境气候意义

刘毅¹ 罗宇涵¹ 孙松² 何毓新³ 柳中晖³ 孙立广¹

¹中国科学技术大学地球和空间科学学院极地环境研究室，安徽合肥 230026；
²中国科学院海洋研究所海洋生态与环境重点实验室，山东青岛，266071；
³香港大学地球科学系，香港5. 香港大学地球科学系

收稿日期:2012-02-23 修回日期:2012-03-16 出版日期:2012-09-30 发布日期:2012-09-30
通讯作者: 孙立广
基金资助:
极地专项：极地生态地质学与环境综合考察——中山站DOME-A断面生态指示计;国家重点基础研究发展计划：中国西沙群岛和北极黄河站持久有机污染物（POPS）调查持久性有机污染物POPS的环境安全、演变趋势与控制原理;国家自然科学基金：全新世南极南海典型岛屿对全球变化的生态响应与对比

BIOMARKERS RECORDS FROM LACUSTRINE SEDIMENT, LASEMANN HILLS, EAST ANTARCTICA

Liu Yi¹, Luo Yuhan¹, Sun Song², He Yuxin³, Liu Zhonghui³, Sun Liguang¹

¹Institute of Polar Environment, Department of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China;
²Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
³Department of Earth Sciences, The University of Hong Kong, Hong Kong, China

Received:2012-02-23 Revised:2012-03-16 Online:2012-09-30 Published:2012-09-30

摘要/Abstract

摘要： 东南极拉斯曼丘陵地区莫愁湖（69°22.3’ S，76°22.0’ E）沉积柱中的有机生物标志物记录了全新世中晚期该地区气候演变过程。不饱和长链烯酮在沉积柱111-76 cm （6450-5100 cal. yr. BP）和36-30 cm（3700-3500 cal. yr. BP）深度有检出，76 cm深度以上基本消失，表明该地区在5100 cal. yr. BP前后气候开始由冷转暖，冰川消融，陆壳抬升，相对海平面下降，同时大量的冰融水使湖泊逐渐淡化。沉积柱底部长链烯酮的检出阶段与东南极相对海平面较高时期相一致，而沉积柱36-30 cm（3700-3500 cal. yr. BP）深度不饱和长链烯酮的痕量检出则揭示了一个短暂的气候干冷，湖泊盐度升高的时期。沉积物中正构烷烃反映的当地气候变化所控制的湖生植物群落演变过程与上述过程基本一致。

关键词: 东南极, 拉斯曼丘陵, 长链烯酮, 正构烷烃, 相对海平面

Abstract: Biomarker records from Mochou lake sediments, Larsemann Hills (69°22.3′S, 76°22.0′E), East Antarctica, reveals mid-late Holocene climate history in the region. . As biomarkers for a limited number of certain haptophytes, the long chain alkenones (LCAs) were found from bottom to 76 cm of the sediment core (6500-5100 cal. yr. BP), a period with high relative sea level. Trace amounts of LCAs were also found at 36-30 cm (3700-3500 cal. yr. BP), which reflected change of lake salinity caused by cold climate with fewer ice melt water and higher evaporation. The absence of LCAs above 76cm (about 5100 cal. yr. BP) was consistent with the climate switching from cold to warm and gradually dropping of relative sea level, resulting in more glacial melting water and less intrusion of sea water. The evolution of n-alkanes (C19-C33) reflected the same history of hygrophyte population.

Key words: East Antarctica, Larsemann Hills, long chain alkenones, n-alkanes, relative sea-level

刘毅罗宇涵孙松何毓新柳中晖孙立广. 东南极拉斯曼丘陵湖泊沉积生物标志物记录及其环境气候意义[J]. 极地研究, 2012, 24(3): 205-214.

Liu Yi，Luo Yuhan，Sun Song，He Yuxin，Liu Zhonghui，Sun Liguang. BIOMARKERS RECORDS FROM LACUSTRINE SEDIMENT, LASEMANN HILLS, EAST ANTARCTICA[J]. ADVANCES IN POLAR SCIENCE, 2012, 24(3): 205-214.

参考文献

[1]Franzmann P D,Dobson S J.The Phylogeny of Bacteria from a Modern Antarctic Refuge[J].Antarctic Science,1993,5(3):267-270

[2]Taton A,Grubisic S,Balthasart P,et al.Biogeographical distribution and ecological ranges of benthic cyanobacteria in East Antarctic lakes[J].Fems Microbiology Ecology,2006,57(2):272-289

[3]Kerr R A.Antarctic Ozone Hole Is Still Deepening[J].Science,1986,232(4758):1602-1602

[4]Rowland F S.Chlorofluorocarbons and the Antarctic Ozone Hole[J].Environmental Conservation,1986,13(3):193-194

[5]Crutzen P J,Arnold F.Nitric-Acid Cloud Formation in the Cold Antarctic Stratosphere - a Major Cause for the Springtime Ozone Hole[J].Nature,1986,324(6098):651-655

[6]Feldstein S B.Subtropical Rainfall and the Antarctic Ozone Hole[J].Science,2011,332(6032):925-926

[7]Laybourn-Parry J,Pearce D A.The biodiversity and ecology of Antarctic lakes: models for evolution[J].Philosophical Transactions of the Royal Society B-Biological. Sciences,2007,362(1488):2273-2289

[8]Oswald G K A,Robin G d Q.LAke beneath the ANtarctic ice sheet[J].Nature,1973,(245):251-254

[9]Siegert M J.Lakes beneath the ice sheet: The occurrence,analysis,and future exploration of Lake Vostok and other Antarctic subglacial lakes[J].Annual Review of Earth and Planetary Sciences,2005,33:215-245

[10]Kapitsa A P,Ridley J K,Robin G D,et al.A large deep freshwater lake beneath the ice of central East Antarctica[J].Nature,1996,381(6584):684-686

[11]Zwartz D,Bird M,Stone J,et al.Holocene sea-level change and ice-sheet history in the Vestfold Hills,East Antarctica[J].Earth and Planetary Science Letters,1998,155(1-2):131-145

[12]Hodson D A,Doran P T,Roberts D,et al.Palaeolimnological studies from the Antarctic and sub-Antarctic islands[J].In Long-term environmental change in Arctic and Antarctic lakes,2004,:419-474

[13]Sun L G,Xie Z Q,Zhao J L.Palaeoecology - A 3,000-2000 record of penguin populations[J].Nature,2000,407(6806):858-858

[14]Hodgson D A,Noon P E,Vyverman W,et al.Were the Larsemann Hills ice-free through the Last Glacial Maximum? [J].Antarctic Science,2001,13(4):440-454

[15]Roberts D,McMinn A,Zwartz D.An initial palaeosalinity history of Jaw Lake,Bunger Hills based on a diatom-salinity transfer function applied to sediment cores[J].Antarctic Science,2000,12(2):172-176

[16]Cromer L,Gibson J A E,Swadling K M,et al,.Faunal microfossils: Indicators of Holocene ecological change in a saline Antarctic lake[J].Palaeogeography Palaeoclimatology Palaeoecology,2005,221(1-2):83-97

[17]Eglinton G,Hamilton R J.Leaf epicuticular waxes [J].Science,,156(1322):1335-

[18]Cranwell P A,Eglinton G,Robinson N.1987Lipids of Aquatic Organisms as Potential Contributors to Lacustrine Sediments[J].. Organic Geochemistry,1967,11(6):513-527

[19]Rieley G,Collier R J,Jones D M.et alSources of Sedimentary Lipids Deduced from Stable Carbon Isotope Analyses of Individual Compounds[J].. Nature,6334,1991:352-

[20]Volkman J K.A Review of Sterol Markers for Marine and Terrigenous Organic-Matter[J].Organic Geochemistry,1986,9(2):83-99

[21]Brassell S C,Eglinton G,Marlowe I T.et alMolecular Stratigraphy - a New Tool for Climatic Assessment[J].. Nature,6058,1986:320-

[22]Prahl F G,Delange G J,Lyle M.et alPost-Depositional Stability of Long-Chain Alkenones under Contrasting Redox Conditions[J].. Nature,6241,1989:341-

[23]Sikes E L,Farrington J W,Keigwin L D.Use of the Alkenone Unsaturation Ratio U-37-K to Determine Past Sea-Surface Temperatures - Core-Top Sst Calibrations and Methodology Considerations[J].Earth and Planetary Science Letters,1991,104(1):36-47

[24]Rontani J F,Cuny P,Grossi V,Beker B.Stability of long-chain alkenones in senescing cells of Emiliania huxleyi: effect of photochemical and aerobic microbial degradation on the alkenone unsaturation ratio (U-37(k'))[J].Organic Geochemistry,1997,26(7-8):503-509

[25]Volkman J K,Eglinton G,Corner E D S,et al,.Long-Chain Alkenes and Alkenones in the Marine Coccolithophorid Emiliania-Huxleyi[J].Phytochemistry,1980,19(12):2619-2622

[26]Marlowe I T,Brassell S C,Eglinton G,et al,.Long chain unsaturated ketones and esters in living algae and marine sediments[J][J].Organic Geochemistry,1984,6:135-

[27]Conte M H,Eglinton G.Alkenone and Alkenoate Distributions within the Euphotic Zone of the Eastern North-Atlantic - Correlation with Production Temperature[J].Deep-Sea Research Part I-Oceanographic Research Papers,1993,40(10):1935-1961

[28]Cranwell P A.Long-Chain Unsaturated-Ketones in Recent Lacustrine Sediments[J].Geochimica Et Cosmochimica Acta,1985,49(7):1545-1551

[29]Li J G,Philp R P,Pu F,et al,.Long-chain alkenones in Qinghai Lake sediments[J][J].Geochimica Et Cosmochimica Acta,1996,60(2):235-241

[30]Chu G Q,Sun Q,Li S Q,et al,.Long-chain alkenone distributions and temperature dependence in lacustrine surface sediments from China[J][J].Geochimica Et Cosmochimica Acta,2005,69(21):4985-5003

[31]Zink K G,Leythaeuser D,Melkonian M,et al,.Temperature dependency of long-chain alkenone distributions in Recent to fossil limnic sediments and in lake waters[J][J].Geochimica Et Cosmochimica Acta,2001,65(2):253-265.,2001,65(2):253-265

[32]Pearson E J,Juggins S,Farrimond P.Distribution and significance of long-chain alkenones as salinity and temperature indicators in Spanish saline lake sediments[J].Geochimica Et Cosmochimica Acta,2008,72(16):4035-4046

[33]Coolen M J L,Muyzer G,Rijpstra W I C,et al,.Combined DNA and lipid analyses of sediments reveal changes in Holocene haptophyte and diatom populations in an Antarctic lake[J][J].Earth and Planetary Science Letters,2004,223(1-2):225-239

[34]Zhang G,Sheng G Y,Peng P A,et al.,Molecular organic geochemical peculiarities of lacustrine core sediments in Fildes Peninsula,King George Island,Antarctica[J][J].Chinese Science Bulletin,2000,45:67-

[35]D'Andrea W J,Huang Y.Long chain alkenones in Greenland lake sediments: Low delta C-13 values and exceptional abundance[J].Organic Geochemistry,2005,36:1234-1241

[36]D'Andrea W J,Lage M,Martiny J B H,et al,.Alkenone producers inferred from well-preserved 18S rDNA in Greenland lake sediments[J][J].Journal of Geophysical Research-Biogeosciences,2006,111:-

[37]Theroux S,D'Andrea W J,Toney J,et al,.Phylogenetic diversity and evolutionary relatedness of alkenone-producing haptophyte algae in lakes: Implications for continental paleotemperature reconstructions[J][J].Earth and Planetary Science Letters,2010,300(3-4):311-320

[38]Roberts D,McMinn A.A diatom-based palaeosalinity history of Ace Lake,Vestfold Hills,Antarctica[J].Holocene,1999,9(4):401-408

[39]Roberts D,Roberts J L,Gibson J A E,et al,.Palaeohydrological modelling of Ace Lake,Vestfold Hills,Antarctica[J].Holocene,1999,9(5):515-520

[40]Meinschein W G,Barghoorn E S,Schopf J W.Biological remnants in a precambrian sediment[J].Science,1964,145(3629):262-263

[41]Nott C J,Xie S C,Avsejs L A,et al,.n-Alkane distributions in ombrotrophic mires as indicators of vegetation change related to climatic variation[J][J].Organic Geochemistry,2000,31(2-3):231-235

[42]卞林根,薛正夫.逯昌贵[J].拉斯曼丘陵的短期气候特征。极地研究,1998,10(1):37-46

[43]Liang Y L,Wang J,Li Z H.Preliminary study of freshwater ecology systems around Zhongshan Station of China,[J].Antarctica. In Chen L. Q. (ed.): Collection of Papers of Chinese Research Program on the Antarctic,1999,:28-36

[44]Verleyen E,Hodgson D A,Sabbe K,et al,.Late Quaternary deglaciation and climate history of the Larsemann Hills (East Antarctica) [J][J].Journal of Quaternary Science,2004,19(4):361-375

[45]Liu X D,Sun L G,Xie Z Q,et al,.A preliminary record of the historical seabird population in the Larsemann Hills,East Antarctica,from geochemical analyses of Mochou Lake sediments[J][J].Boreas,2007,36(2):182-197

[46]Verleyen E,Hodgson D A,Milne G A,et al,.Relative sea-level history from the Lambert Glacier region,East Antarctica,and its relation to deglaciation and Holocene glacier readvance[J][J].Quaternary Research,2005,63(1):45-52

[47]Ingolfsson O,Hjort C,Berkman P A,et al,.Antarctic glacial history since the Last Glacial Maximum: an overview of the record on land[J][J].Antarctic Science,1998,10(3):326-344

[48]黄婧,王新明,孙立广.东南极戴维斯站企鹅粪土沉积物有机地球化学特征[J].极地研究,2009,21(2):141-150

[49]Emslie S D,Woehler E J.A 9000-2005 record of Adelie penguin occupation and diet in the Windmill Islands,East Antarctica[J].Antarctic Science,2005,17(1):57-66

[50]Cremer H,Gore D,Melles M,et al,.Palaeoclimatic significance of late Quaternary diatom assemblages from southern Windmill Islands,East Antarctica[J][J].Palaeogeography Palaeoclimatology Palaeoecology,2003,195(3-4):261-280

[51]Hodgson D A,McMinn A,Kirkup H,et al,.Colonization,succession,and extinction of marine floras during a glacial cycle: A case study from the Windmill Islands (east Antarctica) using biomarkers[J][J].Paleoceanography,2003,18(3):1067-1079

[52]Bjorck S,Olsson S,EllisEvans C,et al,.Late Holocene palaeoclimatic records from lake sediments on James Ross Island,Antarctica[J][J].Palaeogeography Palaeoclimatology Palaeoecology,1996,121(3-4):195-220

[53]Kulbe T,Melles M,Verkulich S R,et al,.East Antarctic climate and environmental variability over the last 9400 2001s inferred from marine sediments of the Bunger Oasis[J].Arctic Antarctic and Alpine Research,2001,33(2):223-230

[54]Hodgson D A,Verleyen E,Squier A H,et al,.Interglacial environments of coastal east Antarctica: comparison of MIS 1 (Holocene) and MIS 5e (Last Interglacial) lake-sediment records[J][J].Quaternary Science Reviews,2006,25(1-2):179-197

[55]McMinn A.Late Holocene increase in sea ice extent in fjord of the Vestfold Hills,eastern Antarctica[J].Antarctic Science,2000,11(80-88):80-

[56]Hodgson D A,Verleyen E,Sabbe K,et al,.Late Quaternary climate-driven environmental change in the Larsemann Hills,East Antarctica,multi-proxy evidence from a lake sediment core[J].Quaternary Research,2005,64(1):83-99

[57]Ingolfsson O,Hjort C,Humlum O.Glacial and climate history of the Antarctic Peninsula since the Last Glacial Maximum[J].Arctic Antarctic and Alpine Research,2003,35(2):175-186

东南极拉斯曼丘陵湖泊沉积生物标志物记录及其环境气候意义

BIOMARKERS RECORDS FROM LACUSTRINE SEDIMENT, LASEMANN HILLS, EAST ANTARCTICA

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