A 1700-year n-alkanes hydrogen isotope record of moisture changes in sediments from Lake Sugan in the Qaidam Basin, northeastern Tibetan Plateau

Holocene

Volumn 23, Issue 9, 2013, Pages 1350-1354

  Wang, Zheng ^a   Liu, Weiguo ^a,b   Liu, Zhonghui ^c   Wang, Huanye ^a   He, Yuxin ^c   Zhang, Fan ^b  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b XI'AN JIAOTONG UNIVERSITY   (China)

^c UNIVERSITY OF HONG KONG   (Hong Kong)

Author keywords

hydrogen isotope; Lake Sugan; moisture change; Qaidam Basin

Indexed keywords

ARID REGION; GRASS; HUMID ENVIRONMENT; HYDROGEN ISOTOPE; ISOTOPIC COMPOSITION; LACUSTRINE DEPOSIT; LITTLE ICE AGE; MEDIEVAL WARM PERIOD; MOISTURE TRANSFER; SHRUB;

CHINA; QAIDAM BASIN; QINGHAI; QINGHAI-XIZANG PLATEAU; SUGAN LAKE;

POACEAE;

EID: 84881579878     PISSN: 09596836     EISSN: 14770911     Source Type: Journal    
DOI: 10.1177/0959683613486941     Document Type: Article

References (45)

1. Aichner B,Herzschuh U,Wilkes H.Influence of aquatic macrophytes on the stable carbon isotopic signatures of sedimentary organic matter in lakes on the Tibetan Plateau.Organic Geochemistry. 2010;41:706-718.
2. Castaneda IS,Schouten S.A review of molecular organic proxies for examining modern and ancient lacustrine environments.Quaternary Science Reviews. 2011;30:2851-2891.
3. Chen FH,Chen JH,Holmes JA, et al.Moisture changes over the last millennium in the Arid Central Asia: A review, synthesis and comparison with monsoon region.Quaternary Science Review. 2010;29:1055-1068.
4. Chen JH,Chen FH,Zhang EL, et al.A 1000-year chironomid-based salinity reconstruction from varved sediments of Sugan Lake, Qaidam Basin, arid Northwest China, and its palaeoclimatic signifi{ligature}cance.Chinese Science Bulletin. 2009;54:3749-3759.
5. Chikaraishi Y,Naraoka H.Compound-specific δD-δ13C analyses of n-alkanes extracted from terrestrial and aquatic plants.Phytochemistry. 2003;63:361-371.
6. Chikaraishi Y,Naraoka H.δ13C and δD relationships among three n-alkyl compound classes (n-alkanoic acid, n-alkane and n-alkanol) of terrestrial higher plants.Organic Geochemistry. 2007;38:198-215.
7. Feakins SJ,Sessions AL.Controls on the D/H ratios of plant leaf waxes in an arid ecosystem.Geochimica et Cosmochimica Acta. 2010;74:2128-2141.
8. Gao S,Su PX,Yan QD, et al.Canopy and leaf gas exchange of Haloxylon ammodendron under different soil moisture regimes.Science China Life Sciences. 2010;53:718-728.
9. He Y,Liu W,Zhao C, et al.Solar influenced late holocene temperature changes on the northern Tibetan Plateau.Chinese Science Bulletin. 2013;:1-7.
10. Herzschuh U,Kramer A,Mischkec S, et al.Quantitative climate and vegetation trends since the late glacial on the northeastern Tibetan Plateau deduced from Koucha Lake pollen spectra.Quaternary Research. 2009;71:162-171.
11. Holmes JA,Zhang J,Chen F, et al.Paleoclimatic implications of an 850-year oxygen-isotope record from the northern Tibetan Plateau.Geophysical Research Letters. 2007;34:L23403.
12. Hou J,D'Andrea WJ,Huang Y.Can sedimentary leaf waxes record D/H ratios of continental precipitation? Field, model, and experimental assessments.Geochimica et Cosmochimica Acta. 2008;72:3503-3517.
13. Hou J,Huang Y,Oswald WW, et al.Centennial-scale compound-specific hydrogen isotope record of Pleistocene-Holocene climate transition from Southern New England.Geophysical Research Letters. 2007;34:L19706.
14. Hou JZ,D'Andrea WJ,Liu Z.The influence of 14C reservoir age on interpretation of paleolimnological records from the Tibetan Plateau.Quaternary Science Reviews. 2012;48:67-79.
15. Hou XVegetation Atlas of China. Beijing: Science Press China; 2001:.
16. Huang Y,Shuman B,Wang Y, et al.Hydrogen isotope ratios of palmitic acid in lacustrine sediments record late Quaternary climate variations.Geology. 2002;30:1103-1106.
17. Jia G,Wei K,Chen F, et al.Soil n-alkane δD vs. altitude gradients along Mount Gongga, China.Geochimica et Cosmochimica Acta. 2008;72:5165-5174.
18. Li C,Sessions AL,Valentine DL, et al.D/H variation in terrestrial lipids from Santa Barbara Basin over the past 1400 years: A preliminary assessment of paleoclimatic relevance.Organic Geochemistry. 2011;42:15-24.
19. Liu HY,Cui HT,Pott R, et al.The surface pollen of the woodland-steppe ecotone in southeastern Inner Mongolia, China.Review of Palaeobotany and Palynology. 1999;105:237-250.
20. Liu W,Huang Y.Compound specific D/H ratios and molecular distributions of higher plant leaf waxes as novel paleoenvironmental indicators in the Chinese Loess Plateau.Organic Geochemistry. 2005;36:851-860.
21. Liu W,Yang H.Multiple controls for the variability of hydrogen isotopic compositions in higher plant n-alkanes from modern ecosystems.Global Change Biology. 2008;14:2166-2177.
22. Liu W,Yang H,Li LW.Hydrogen isotopic compositions of n-alkanes from terrestrial plants correlate with their ecological life forms.Oecologia. 2006;150:330-338.
23. Liu Y,Cai QF,Song HM,An ZS,Linderholm HW.Amplitudes, rates, periodicities and causes of temperature variations in the past 2485 years and future trends over the central-eastern Tibetan Plateau.Chinese Science Bulletin. 2011;56:2986-2994.
24. Luo P,Peng PA,Gleixner G, et al.Empirical relationship between leaf wax n-alkane δD and altitude in the Wuyi, Shennongjia and Tianshan Mountains, China: Implications for paleoaltimetry.Earth and Planetary Science Letters. 2011;301:285-296.
25. McInerney FA,Helliker BR,Freeman KH.Hydrogen isotope ratios of leaf wax n-alkanes in grasses are insensitive to transpiration.Geochimica et Cosmochimica Acta. 2011;75:541-554.
26. Mann ME.On smoothing potentially non-stationary climate time series.Geophysical Research Letters. 2004;31:L07214.
27. Polissar PJ,Freeman KH.Effects of aridity and vegetation on plant-wax δD in modern lake sediments.Geochimica et Cosmochimica Acta. 2010;74:5785-5797.
28. Qiang MR,Chen FH,Zhang JW, et al.Climatic changes documented by stable isotopes of sedimentary carbonate in Lake Sugan, northeastern Tibetan Plateau of China, since 2 ka BP.Chinese Science Bulletin. 2005;50:1930-1939.
29. Sachse D,Radke J,Gleixner G.Hydrogen isotope ratios of recent lacustrine sedimentary n-alkanes record modern climate variability.Geochimica et Cosmochimica Acta. 2004;68:4877-4889.
30. Schefusz E,Schouten S,Schneider RR.Climatic controls on central African hydrology during the past 20,000 years.Nature. 2005;437:1003-1006.
31. Sessions AL,Burgoyne TW,Schimmelmann A, et al.Fractionation of hydrogen isotopes in lipid biosynthesis.Organic Geochemistry. 1999;30:1193-1200.
32. Sessions AL,Jahnke LL,Schimmelmann A, et al.Hydrogen isotope fractionation in lipids of the methane-oxidizing bacterium.Methylococcus capsulatus. Geochimica et Cosmochimica Acta. 2002;66:3955-3969.
33. Smith FA,Freeman KH.Influence of physiology and climate on δD of leaf wax n-alkanes from C3 and C4 grasses.Geochimica et Cosmochimica Acta. 2006;70:1172-1187.
34. Soon W,Baliunas S,Idso C, et al.Reconstructing climatic and environmental changes of the past 1000 years: A reappraisal.Energy & Environment. 2003;14:233-296.
35. Tarasov PE,Jolly D,Kaplan JO.A continuous late glacial and Holocene record of vegetation changes in Kazakhstan.Palaeogeography, Palaeoclimatology, Palaeoecology. 1997;136:281-292.
36. Tierney JE,Russell JM,Huang Y, et al.Northern Hemisphere controls on tropical southeast African slimate during the past 60,000 years.Science. 2008;322:252-255.
37. Weijers JWH,Schefuß E,Schouten S, et al.Coupled thermal and hydrological evolution of tropical Africa over the last deglaciation.Science. 2007;315:1701-1704.
38. Wu FS,Ge L,Cai ZP, et al.Phytoplankton diversity of algae in Suganhu Lake in Gansu Province.Acta Botanica Boreali-Occidentalia Sinica. 2008;28:2521-2526.
39. Wu JG.Potential effects of climate change in future on the distributions of 7 desert plants in China.Arid Land Geography. 2011;34:595.
40. Yang B,Brauning A,Shi YF.Late Holocene temperature fluctuations on the Tibetan Plateau.Quaternary Science Reviews. 2003;22:2335-2344.
41. Zhang J,Holmes JA,Chen F, et al.An 850-year ostracod-shell trace-element record from Sugan Lake, northern Tibetan Plateau, China: Implications for interpreting the shell chemistry in high-Mg/Ca waters.Quaternary International. 2009;194:119-133.
42. Zhang K,Zhao Y,Yu ZC, et al.A 2700-year high resolution pollen record of climate change from varved Sugan Lake in the Qaidam Basin, northeastern Tibetan Plateau.Palaeogeography, Palaeoclimatology, Palaeoecology. 2010;297:290-298.
43. Zhang Z,Sachs JP.Hydrogen isotope fractionation in freshwater and marine algae: II. Temperature and nitrogen limited growth rate effects.Organic Geochemistry. 2009;40:428-439.
44. Zhao Y,Yu Z,Liu X, et al.Late Holocene vegetation and climate oscillations in the Qaidam Basin of the northeastern Tibetan Plateau.Quaternary Research. 2010;73:59-69.
45. Zhou AF,Chen FH,Qiang MR, et al.The discovery of annually laminated sediments (varves) from shallow Sugan Lake in inland arid China and their paleoclimatic significance.Science in China (D Series). 2007;50:1218-1224.