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Stratigraphy and otolith microchemistry of the naked carp Gymnocypris przewalskii (Kessler) and their indication for water level of Lake Qinghai during the Ming Dynasty of China

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Abstract

Otoliths are biogenic carbonate minerals in the inner ear of teleost fish, whose compositions can record the physical and chemical conditions of the ambient water environment inhabited by individual fish. In this research, the fishbones and otoliths of naked carp sampled near the Bird Island, offshore Lake Qinghai, were dated and analyzed for mineralogy and microchemical compositions. Comparing the microchemical compositions of ancient otoliths with those of modern otoliths, we conclude that the ancient naked carps inhabited a relict lake formed when the lake shrank from a high lake level, by combining with the AMS-14C ages of fishbones and otoliths, the stratigraphy and surrounding topography of the sample site. AMS-14C dating results of ancient fishbones and otoliths show that these naked carps lived from 680 to 300 years ago, i.e. during the Ming Dynasty of China. The X-ray diffraction (XRD) patterns demonstrate that the ancient lapillus is composed of pure aragonite, identical to modern one, indicating that the mineral of lapillus didn’t change after a long time burial and that the ancient lapillus is suitable for comparative analysis thereafter. Microchemical results show that both ratios of Mg/Ca ((70.12±18.50)×10−5) and δ 18O ((1.76±1.03)‰) of ancient lapilli are significantly higher than those of modern lapilli (average Mg/Ca=(3.11±0.41)× 10−5 and δ 18O=(−4.82±0.96)‰). This reflects that the relict water body in which the ancient naked carp lived during the Ming Dynasty was characterized by higher Mg/Ca and δ 18O ratios than modern Lake Qinghai, resulting from strong evaporation after being isolated from the main lake, similar to today’s Lake Gahai. Based upon the stratigraphy and altitude of naked carp remains, it can be inferred that the altitude of lake level of Lake Qinghai reached at least 3202 m with a lake area of 4480 km2 during the Ming Dynasty, approximately ∼5% larger than it is today.

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References

  • An Z S, Colman S M, Zhou W J, et al. 2012. Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka. Sci Rep, 2: 619, doi: 10.1038/srep 00619

    Google Scholar 

  • Andrus C F, Crowe D E, Sandweiss D H, et al. 2002. Otolith δ 18O record of mid-Holocene sea surface temperatures in Peru. Science, 295: 1508–1511

    Article  Google Scholar 

  • Breard S Q, Stringer G L. 1999. Integrated paleoecology and marine vertebrate fauna of the Stone City Formation (Middle Eocene), Brazos River section, Texas. Trans Gulf Coast Assoc Geol Soc, 49: 132–143

    Google Scholar 

  • Campana S E. 1999. Chemistry and composition of fish otoliths pathways, mechanisms and applications. Mar Ecol Prog Ser, 188: 263–297

    Article  Google Scholar 

  • Chen F H, Chen J H, Holmes J A, et al. 2010. Moisture changes over the last millennium in the Arid Central Asia: A review, synthesis and comparison with monsoon region. Quat Sci Rev, 29: 1055–1068

    Article  Google Scholar 

  • Elsdon T S, Gillanders B M. 2004. Fish otolith chemistry influenced by exposure to multiple environmental variables. J Exp Mar Biol Ecol, 313: 269–284

    Article  Google Scholar 

  • Elsdon T S, Gillanders B M. 2003. Reconstructing migratory patterns of fish based on environmental influences on otolith chemistry. Rev Fish Biol Fisher, 13: 219–235

    Article  Google Scholar 

  • Feng S, Tang M C, Zhou L S. 2000. Level fluctuation in Qinghai Lake during the last 600 years (in Chinese with English abstract). J Lake Sci, 12: 205–210

    Google Scholar 

  • Gago-Duport L, Briones M J I, Rodríguez J B, et al. 2008. Amorphous calcium carbonate biomineralization in the earthworm’s calciferous gland: Pathways to the formation of crystalline phases. J Struct Biol, 162: 422–435

    Article  Google Scholar 

  • Gillanders B M, Munro A R. 2012. Hypersaline waters pose new challenges for reconstructing environmental histories of fish based on otolith chemistry. Limnol Oceanogr, 57: 1136–1148

    Article  Google Scholar 

  • Griffiths H I, Holmes J A. 2000. Non-marine ostracods and Quaternary palaeoenvironments. London: Quaternary Research Association. 1–187

    Google Scholar 

  • He D K, Chen Y F, Chen Y Y, et al. 2004. Molecular phylogeny of the specialized schizothoracine fishes (Teleostei: Cyprinidae), with their implications for the uplift of the Qinghai-Tibetan Plateau. Chin Sci Bull, 49: 39–48

    Article  Google Scholar 

  • Henderson A C G, Holmes J A, Zhang J, et al. 2003. A carbon- and oxygen-isotope record of recent environmental change from Qinghai Lake, NE Tibetan Plateau. Chin Sci Bull, 48: 1463–1468

    Article  Google Scholar 

  • Hu G, Jin Z D, Zhang F. 2008. Constraints of authigenic carbonates on trace elements (Sr, Mg) of lacustrine ostracod shells in paleoenvironment reconstruction and its mechanism. Sci China Ser D-Earth Sci, 51: 654–664

    Article  Google Scholar 

  • Høie H, Otterlei E, Folkvord A. 2004. Temperature-dependent fractionation of stable oxygen isotopes in otoliths of juvenile cod (Gadus morhua L.). ICES J Mar Sci, 61: 243–251

    Article  Google Scholar 

  • Jamieson J C. 1953. Phase equilibrium in the system calcite-aragonite. J Chem Phys, 21: 1385–1390

    Article  Google Scholar 

  • Jin Z D, You C F, Wang Y, et al. 2010. Hydrological and solute budgets of Lake Qinghai, the largest lake on the Tibetan Plateau. Quat Int, 218: 151–156

    Article  Google Scholar 

  • Kerr L A, Andrews A H, Frantz B R, et al. 2004. Radiocarbon in otoliths of yelloweye rockfish (Sebastes ruberrimus): A reference time series for the coastal waters of southeast Alaska. Can J Fish Aquat Sci, 61: 443–451

    Article  Google Scholar 

  • Kim S T, O’Neil J R, Hillaire-Marcel C, et al. 2007. Oxygen isotope fractionation between synthetic aragonite and water: Influence of temperature and Mg2+ concentration. Geochim Cosmochim Acta, 71: 4704–4715

    Article  Google Scholar 

  • Li X Y, Xu H Y, Sun Y L, et al. 2007. Lake-level change and water balance analysis at Lake Qinghai, west China during recent decades. Water Resour Manage, 21: 1505–1516

    Article  Google Scholar 

  • Lister G S, Kelts K, Chen K Z, et al. 1991. Lake Qinghai, China: Closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene. Paleogeogr Paleoclimatol Paleoecol, 84: 141–162

    Article  Google Scholar 

  • Liu W G, Li X Z, Zhang L, et al. 2009. Evaluation of oxygen isotopes in carbonate as an indicator of lake evolution in arid areas: The modern Qinghai Lake, Qinghai-Tibet Plateau. Chem Geol, 268: 126–136

    Article  Google Scholar 

  • Liu X J, Lai Z P. 2010. Lake level fluctuations in Qinghai Lake in the Qinghai-Tibetan Plateau since the last interglaciation: A brief review and new data (in Chinese with English abstract). J Earth Environ, 1: 79–89

    Article  Google Scholar 

  • Madsen D B, Ma H Z, Rhode D, et al. 2008. Age constraints on the late Quaternary evolution of Qinghai Lake, Tibetan Plateau. Quat Res, 69: 316–325

    Article  Google Scholar 

  • Nolf D. 1985. Otolithi piscium. In: Schultze H P, ed. Handbook of Paleoichthyology. New York: Gustav Fischer Verlag. 10: 1–145

    Google Scholar 

  • Patterson W P, Smith G R, Lohmann K C. 1993. Continental paleothermometry and seasonality using the isotopic composition of aragonitic otoliths of freshwater fishes. In: Swart P K, et al. eds. Climate Change in Continental Isotopic Records. Washington D C: Geophysical Monograph Series. 191–202

    Chapter  Google Scholar 

  • Reimer P J, Baillie M G L, Bard E, et al. 2009. IntCal09 and Marine09 radiocarbon age calibration curves, 0–50000 years cal BP. Radiocarbon, 51: 1111–1150

    Google Scholar 

  • Rhode D, Ma H Z, Madsen D B, et al. 2010. Paleoenvironmental and archaeological investigation at Qinghai Lake, western China: Geomorphic and chronometric evidence of lake level history. Quat Int, 218: 29–44

    Article  Google Scholar 

  • Wang S M, Li J R. 1991. Lacustrine sediments-An indicator of historical climatic variation-The case of Qinghai Lake and Daihai Lake. Chin Sci Bull, 36: 1364–1368

    Google Scholar 

  • Wang S M, Shi Y F. 1992. Review and discussion on the late Quaternary evolution of Qinghai Lake (in Chinese with English abstract). J Lake Sci, 4: 1–9

    Google Scholar 

  • Watanabe T, Nakamura T, Nara F W, et al. 2009. High-time resolution AMS 14C data sets for Lake Baikal and Lake Hovsgol sediment cores: Changes in radiocarbon age and sedimentation rates during the transition from the last glacial to the Holocene. Quat Int, 205: 12–20

    Article  Google Scholar 

  • Yan J P, Hinderer M, Einsele G. 2002. Geochemical evolution of closed-basin lakes, general model and application to Lakes Qinghai and Turkana. Sediment Geol, 148: 105–122

    Article  Google Scholar 

  • Yi W J, Li X Y, Cui B L, et al. 2010. Climate change and impact on water level of the Qinghai Lake watershed (in Chinese with English abstract). J Arid Meteor, 28: 375–383

    Google Scholar 

  • Yuan S X, Wu X H, Gao S J, et al. 2000. Comparison of different bone pretreatment methods for AMS 14C dating. Nucl Instrum Methods Phys Res Sect B-Beam Interact Mater Atoms, 172: 424–427

    Article  Google Scholar 

  • Zhang H C, Peng J L, Ma Y Z, et al. 2004. Late Quaternary palaeolake levels in Tengger Desert, NW China. Paleogeogr Paleoclimatol Paleoecol, 211: 45–58

    Article  Google Scholar 

  • Zhou L, Jin Z D, Li F C. 2012. Mineralogy of the otoliths of naked carp Gymnocypris przewalskii (Kessler) from Lake Qinghai and its Sr/Ca potential implications for migratory pattern. Sci China Earth Sci, 55: 983–990

    Article  Google Scholar 

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Correspondence to ZhangDong Jin or FuChun Li.

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Wang, Y., Jin, Z., Zhou, L. et al. Stratigraphy and otolith microchemistry of the naked carp Gymnocypris przewalskii (Kessler) and their indication for water level of Lake Qinghai during the Ming Dynasty of China. Sci. China Earth Sci. 57, 2512–2521 (2014). https://doi.org/10.1007/s11430-014-4836-1

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