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Influence of Aquatic Plant Photosynthesis on the Reservoir Effect of Genggahai Lake, Northeastern Qinghai-Tibetan Plateau

Published online by Cambridge University Press:  16 November 2017

Yuan Li ,
Mingrui Qiang ,
Yanxiang Jin ,
Li Liu ,
Aifeng Zhou  and
Jiawu Zhang
Yuan Li
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
Mingrui Qiang*
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
Yanxiang Jin
Affiliation:
College of Geographical Science, Qinghai Normal University, Xining 810008, China
Li Liu
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
Aifeng Zhou
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
Jiawu Zhang
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
*
*Corresponding author. Email: [email protected].
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Abstract

Terrestrial plant remains in the sediments of lakes from semi-arid and arid regions are rare and therefore the establishment of a sediment chronology depends on accurate assessment of the reservoir effect of the lake water. In a study of Genggahai Lake in the Gonghe Basin, northeastern Qinghai-Tibetan Plateau, we used accelerator mass spectrometry radiocarbon (AMS 14C) dating to determine the age of (1) dissolved inorganic carbon in the water (DICLW), (2) macrophyte remains in the uppermost samples of core sediments, (3) living P. pectinatus in the lake, and (4) dissolved inorganic carbon of spring water in the catchment. The results show that the ages of the DICLW (910 14C yr BP on average) were much younger than the ages of the groundwater (6330 14C yr BP on average), which may result mainly from CO2 exchange between the lake water and the atmosphere. In addition, the 14C ages of DICLW and macrophyte remains in the uppermost core sediments varied from site to site within the lake, which we ascribe to the different photosynthesis rates of Chara spp. and vascular plants. The higher photosynthesis rate of Chara spp. decreases lake-water pCO2, which leads to more atmospheric CO2 being absorbed by the lake water, and thereby greatly reducing the age of carbon species in areas dominated by Chara spp. Although Genggahai Lake is well mixed, the differences between the apparent ages of the lake water are significantly modulated by the photosynthesis intensity of submerged plants.

Keywords

charophyteChinadissolved inorganic carbonradiocarbon datingreservoir effect
Type
Research Article
Information
Radiocarbon , Volume 60 , Issue 2 , April 2018 , pp. 561 - 569
Copyright
© 2017 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

REFERENCES

Abbott, MB, Stafford, TW. 1996. Radiocarbon geochemistry of modern and ancient Arcticlake systems, Baffin Island, Canada. Quaternary Research 45(3):300–311.Google Scholar
An, ZS, Colman, SM, Zhou, WJ, Li, XQ, Brown, ET, Jull, AJT, Cai, YJ, Huang, YS, Lu, XF, Chang, H, Song, YG, Sun, YB, Xu, H, Liu, WG, Jin, ZD, Liu, XD, Cheng, P, Liu, Y, Ai, L, Li, XZ, Liu, XJ, Yan, LB, Shi, ZG, Wang, XL, Wu, F, Qiang, XK, Dong, JB, Lu, FY, Xu, XW. 2012. Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka. Scientific Reports 2(8):1036.CrossRefGoogle ScholarPubMed
Anderson, L, Abbott, MB, Finney, BP, Burns, SJ. 2005. Regional atmospheric circulation change in the North Pacific during the Holocene inferred from lacustrine carbonate oxygen isotopes, Yukon Territory, Canada. Quaternary Research 64(1):21–35.Google Scholar
Apolinarska, K, Pełechaty, M., Pukacz, A. 2011. CaCO3 sedimentation by modern charophytes (Characeae): can calcified remains and carbonate δ13C and δ18O record the ecological state of lakes? -a review. Studia Limnologica et Telmatologica 5(2):55–66.Google Scholar
Arslan, M, Kadir, S, Abdiglu, E, Kolayli, H. 2006. Origin and formation of kaolin minerals in saprolite of Tertiary alkaline volcanic rocks, Eastern Pontides, NE Turkey. Clay Miner 41(2):597–617.CrossRefGoogle Scholar
Ascough, PL, Cook, GT, Church, MJ, Dunbar, E, Einarsson, A, McGovern, TH, Dugmore, AJ, Perdikaris, S, Hastie, H, Friðricksson, A, Gestsdóttir, H. 2010. Temporal and spatial variations in freshwater 14C reservoir effects: Lake Mývatn, northern Iceland. Radiocarbon 52(2–3):1098–1112.Google Scholar
Bertrand, S, Araneda, A, Vargas, P, Jana, P, Fagel, N, Urrutia, R. 2012. Using the N/C ratio to correct bulk radiocarbon ages from lake sediments: insights from Chilean Patagonia. Quaternary Geochronology 12(2):23–29.Google Scholar
Billett, MF, Garnett, MH, Harvey, F. 2007. UK peatland streams release old carbon dioxide to the atmosphere and young dissolved organic carbon to rivers. Geophysical Research Letters 34(23):135–147.Google Scholar
Blindow, I. 1992. Long and short term dynamics of submerged macrophytes in two shallow eutrophic lakes. Freshwater Biology 28(1):15–27.Google Scholar
Coletta, P, Pentecost, A, Spiro, B. 2001. Stable isotopes in charophyte incrustations: relationships with climate and water chemistry. Palaeogeography, Palaeoclimatology, Palaeoecology 173(1–2):9–19.Google Scholar
Donahue, DJ, Linick, TW, Jull, AJT. 1990. Isotoperatio and background corrections for accelerator mass spectrometry radiocarbon measurements. Radiocarbon 32(2):135–142.Google Scholar
Fontes, JC, Gasse, F, Gibert, E. 1996. Holocene environmental changes in Lake Bangong basin (Western Tibet). Part 1: Chronology and stable isotopes of carbonates of a Holocene lacustrine core. Palaeogeography, Palaeoclimatology, Palaeoecology 120(1–2):25–47.Google Scholar
Gao, YX, Xu, SY, Guo, QY, Zhang, ML. 1962. Monsoon regions in China and regional climate. In: Gao YX, editors. Some Problems on East-Asia Monsoon. Beijing: Science Press. p 49–63. In Chinese.Google Scholar
Geyh, MA, Schotterer, U, Grosjean, M. 1998. Temporal changes of the 14C reservoir effect in lakes. Radiocarbon 40(2):921–931.Google Scholar
Hammarlund, D, Aravena, R, Barnekow, L, Possnert, G. 1997. Multi-component carbon isotope evidence ofearly Holocene environmental change and carbon-flow pathways from a hard-water lake in northern Sweden. Journal of Paleolimnology 18(3):219–233.Google Scholar
Hatté, C, Jull, AJT. 2007. Radiocarbon dating: plant macrofossils. In: Elias SA, editors. Encyclopedia of Quaternary Science. Amsterdam: Elsevier Science. p 2958–2965.CrossRefGoogle Scholar
Hou, JZ, D’Andrea, WJ, Liu, ZH. 2012. The influence of 14C reservoir age on interpretation of paleolimnological records from the Tibetan Plateau. Quaternary Science Reviews 48:67–79.CrossRefGoogle Scholar
Li, Y, Wang, NA, Morrill, C, Anderson, DM, Li, ZL, Zhang, CQ, Zhou, XH. 2012. Millennial-scale erosion rates in three inland drainage basins and their controlling factors since the Last Deglaciation, arid China. Palaeogeography Palaeoclimatology Palaeoecology 365–366(9):263–275.Google Scholar
Liu, XQ, Shen, J, Wang, SM, Wang, YB, Liu, WG. 2007. Southwest monsoon changes indicated by oxygen isotope of ostracode shells from sediments in Lake Qinghai since the Late Glacial. Chinese Science Bulletin 52(4):539–544.CrossRefGoogle Scholar
Longhurst, AR, Harrison, WG. 1989. The biological pump: profiles of plankton production and consumption in the upper ocean. Progress in Oceanography 22(1):47–123.Google Scholar
Martin, CW. 1999. Radiocarbon dating: recent applications and future potential. Geoarchaeology 14(4):371–373.3.0.CO;2-#>CrossRefGoogle Scholar
Mischke, S, Weynell, M, Zhang, C, Wiechert, U. 2013. Spatial variability of 14C reservoir effects in Tibetan Plateau lakes. Quaternary International 313–314:147–155.Google Scholar
Olaaon, IU. 2009. Radiocarbon dating history: early days, questions, and problems met. Radiocarbon 51(1):1–43.Google Scholar
Perrineau, A, Van Der Woerd, J, Jing, LZ, Gaudemer, Y, Pik, R, Tapponnier, P, Thuizat, R, Zheng, RZ. 2011. Incision rate of the Yellow River in northeastern Tibet constrained by cosmogenic isotope dating (10Be, 26Al) of fluvial terraces: implications to catchment evolution and plateau building. London: Geological Society. Special Publication 353(3):459–461.Google Scholar
Qiang, MR, Liu, YY, Jin, YX, Song, L, Huang, XT, Chen, FH. 2014. Holocene record of eolian activity from Genggahai Lake, northeastern Qinghai-Tibetan Plateau, China. Geophysical Research Letters 41(2):589–595.Google Scholar
Qiang, MR, Song, L, Chen, F, Li, MZ, Liu, XX, Wang, Q. 2013. A 16-ka lake-level record inferred from macrofossils in a sediment core from Genggahai Lake, northeastern Qinghai-Tibetan Plateau (China). Journal of Paleolimnology 49(4):575–590.Google Scholar
Qiang, MR, Song, L, Jin, YX, Li, Y, Liu, L, Zhang, JW, Zhao, Y. 2017. A 16-ka oxygen-isotope record from Genggahai Lake on the northeastern Qinghai-Tibetan Plateau: hydroclimatic evolution and changes in atmospheric circulation. Quaternary Science Reviews 162:72–87.Google Scholar
Ray, S, Klenell, M, Choo, KS, Pedersén, M, Snoeijs, P. 2003. Carbon acquisition mechanisms in Chara tomentosa . Aquatic Botany 76(2):141–154.Google Scholar
Sand-Jensen, K. 1983. Photosynthetic carbon sources of stream macrophytes. Journal of Experimental Botany 34(2):198–210.Google Scholar
Shen, J, Liu, XQ, Matsumoto, R, Wang, SM, Yang, XD. 2005a. A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake. Science in China, Series D, Earth Sciences 48(6):742–751.Google Scholar
Shen, J, Liu, XQ, Wang, SM, Matsumoto, R. 2005b. Palaeoclimatic changes in the Qinghai Lake area during the last 18000 years. Quaternary International 136(1):131–140.Google Scholar
Stein, M, Migowski, C, Bookman, R, Lazar, B. 2004. Temporal changes in radiocarbon reservoir age in the Dead Sea-Lake Lisan system. Radiocarbon 46(2):649–655.Google Scholar
Van den Berg, M S, Coops, H, Simons, J, Pilon, J. 2002. A comparative study of the use of inorganic carbon resources by Chara aspera and Potamogeton pectinatus . Aquatic Botany 72(3):219–233.Google Scholar
Xu, SY, Xu, DF, Shi, SR. 1984. A discussion on the development of landforms and evolution of environments in the Gonghe Basin. Journal of Lanzhou University 20:146–157. In Chinese.Google Scholar
Yu, SY, Shen, J, Coleman, SM. 2007. Modeling the radiocarbon reservoir effect in lacustrine systems. Radiocarbon 49(3):1241–1254.Google Scholar
Zhang, HC, Ming, QZ, Lei, GL, Zhang, WX, Fan, HF, Chang, FQ, Wunnemann, B, Hartmann, K. 2006. Dilemma of dating on lacustrine deposits in an hyperarid inland basin of NW China. Radiocarbon 48(2):219–226.Google Scholar
Zhang, JW, Ma, XY, Qiang, MR, Huang, XZ, Li, S, Guo, XY, Henderson, ACG, Holmes, JA, Chen, FH. 2016a. Developing inorganic carbon-based radiocarbon chronologies for Holocene lake sediments in arid NW China. Quaternary Science Reviews 144:66–82.Google Scholar
Zhang, Y, Meyers, PA, Liu, XT, Wang, GP, Ma, XH, Li, XY, Yuan, YX, Wen, BL. 2016b. Holocene climate changes in the central Asia mountain region inferred from a peat sequence from the Altai Mountains, Xinjiang, northwestern China. Quaternary Science Reviews 152:19–30.Google Scholar
Zhou, AF, Chen, FH, Wang, ZL, Yang, ML, Qiang, MR, Zhang, JW. 2009. Temporal change of radiocarbon reservoir effect in Sugan Lake, northwest China during the late Holocene. Radiocarbon 51(2):529–535.Google Scholar
Zhao, C, Yu, ZC, Zhao, Y, Ito, E, Kodama, KP, Chen, FH. 2010. Holocene millennial-scale climate variations documented by multiple lake-level proxies in sediment cores from Hurleg Lake, Northwest China. Journal of Paleolimnology 44(4):995–1008.Google Scholar
Zhou, WJ, Cheng, P, Jull, AJT, Lu, XF, An, ZS, Wang, H, Zhu, YZ, Wu, ZK. 2014. 14C chronostratigraphy for Qinghai Lake in China. Radiocarbon 56(1):143–155.Google Scholar