Abstract
Saline lakes are useful repositories for paleo-climatic records. In recent years, magnetic properties of saline lake sediments have been widely applied to establish paleo-climatic change. However, the influence factors of magnetic properties in saline lakes have not been fully understood, which complicates the paleoenvironmental interpretation. Here, we present a rock magnetic analyses result of LOP1 profile (40°26′09″′N, 90°21′23″E) from Lop Nur, a well-known saline lake, located in the eastern Tarim Basin in northwestern China. We combined the particle size, total organic content, and mineral characteristics analysis to assess the influence factors of magnetic properties in Lop Nur and its environmental significance. The results indicate that early diagenesis is the major influence factor on magnetic properties of Lop Nur saline sediments. Authigenic greigite and pyrite are identified within organic-rich sediments, which produce zones with high and low magnetic susceptibilities, respectively. The different authigenic iron sulfide contents in different layers are related to sedimentary environment changes. Sufficient supplies of organic matter and sulphate and low sedimentation rates favour the pyritization process. Moreover, if pyritization was constrained, intermediate greigite formed and was preserved. In oxidizing environments, sediment magnetic properties are consistent with those of source materials from Tarim Basin and are mainly controlled by particle size and hydrodynamic sorting of mainly detrital magnetite is largely unaffected by early diagenesis. Our study demonstrates that magnetic properties can provide a robust approach for studying depositional environment change in saline lake. In addition, the information obtained in this study would also provide insights into the geochemical processes of iron element in saline lakes.
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References
Berner RA (1984) Sedimentary pyrite formation: An update. Geochimica et Cosmochimica Acta 48(4): 605–615. https://doi.org/10.1016/0016-7037(84)90089-9
Blanchet CL, Thouveny N, Vidal L (2009) Formation and preservation of greigite(Fe3S4) in sediments from the Santa Barbara Basin: Implications for paleoenvironmental changes during the past 35 ka. Paleoceanography 24: PA2224. https://doi.org/10.1029/2008PA001719
Bloemendal J, Liu X (2005) Rock magnetism and geochemistry of two Plio-Pleistocene Chinese loess-palaeosol sequences—implications for quantitative palaeoprecipitation reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecolog. 226(1): 149-166. https://doi.org/10.1016/j.palaeo.2005.05.008
Canfield DE, Berner RA (1987) Dissolution and pyritization of magnetite in anoxic marine sediments. Geochimica et Cosmochimica Acta 51(3): 645–659. https://doi.org/10.1016/0016-7037(87)90076-7
Chaparro MAE, Córdoba FE, Lecomte KL, et al. (2017) Sedimentary analysis and magnetic properties of Lake Anónima, Vega Island. Antarctic Science 29: 429–444. https://doi.org/10.1017/S0954102017000116
Cutter GA, Kluckhohn RS (1999) The cycling of particulate carbon, nitrogen, sulfur, and sulfur species(iron monosulfide, greigite, pyrite, and organic sulfur) in the water columns of Framvaren Fjord and the Black Sea. Marine Chemistry 67(3): 149–160. https://doi.org/10.1016/S0304-4203(99)00056-0
Day R, Fuller M, Schmidt VA (1977) Hysteresis properties of titanomagnetites: Grain-size and compositional dependence. Physics of The Earth and Planetary Interiors 13(4): 260–267. https://doi.org/10.1016/0031-9201(77)90108-X
Dekkers MJ, Passier HF, Schoonen, MAA (2000) Magnetic properties of hydrothermally synthesized greigite (Fe3S4)--II. High-and low-temperature characteristics. Geophysical Journal International 141(3): 809–819. https://doi.org/10.1016/S0304-4203(99)00056-0
Dekkers MJ, Schoonen MAA (1996) Magnetic properties of hydrothermally synthesized greigite(Fe3S4)-I. Rock magnetic parameters at room temperature. Geophysical Journal International 126(2): 360–368. https://doi.org/10.1029/2008GC002276
Dong Z, Lv P, Qian G, et al. (2012) Research progress in China’s Lop Nur. Earth-Science Reviews 111(1): 142–153. https://doi.org/10.1016/j.earscirev.2011.11.003
Ebert Y, Shaar R, Emmanuel S, et al. (2018) Overwriting of sedimentary magnetism by bacterially mediated mineral alteration. Geology 46(4): 291–294. https://doi.org/10.1130/G39706.1
Evans ME, Heller F (2003) Environmental Magnetism: Principles and Applications of Enviromagnetics. Academic Press, San Diego.
Evans ME, Heller F, Bloemendal J, et al. (1997) Natural magnetic archives of past global change. Surveys in Geophysics 18(2–3): 183–196. https://doi.org/10.1023/A:1006583809200
Fu CF, Bloemendal J, Qiang XK, et al. (2015) Occurrence of greigite in the Pliocene sediments of Lake Qinghai, China, and its paleoenvironmental and paleomagnetic implications. Geochemistry Geophysics Geosystems.16(5): 1293–1306. https://doi.org/10.1002/2014GC005677
Fu Y, von Dobeneck T, Franke C, et al. (2008) Rock magnetic identification and geochemical process models of greigite formation in Quaternary marine sediments from the Gulf of Mexico(IODP Hole U1319A). Earth and Planetary Science Letters 275(3–4): 233–245. https://doi.org/10.1016/j.epsl.2008.07.034
Ge C, Zhang WG, Dong CY, et al. (2015) Magnetic mineral diagenesis in the river-dominated inner shelf of the East China Sea, China. Journal of Geophysical Research-Solid Earth 120(7): 4720–4733. https://doi.org/10.1002/2015JB011952
Heiri O, Lotter AF, Lemcke G (2001) Loss on ignition as a method for estimating organic and carbonate content in sediments: Reproducibility and comparability of results. Journal of Paleolimnology 25(1): 101–110. https://doi.org/10.1023/A:1008119611481
Jelinowska A, Tucholka P, Gasse F, et al. (1995) Mineral magnetic record of environment in Late Pleistocene and Holocene sediments, Lake Manas, Xinjiang, China. Geophysical Research Letters 22(8): 953–956. https://doi.org/10.1029/95GL00708
Jiang WT, Horng CS, Roberts AP, et al. (2001) Contradictory magnetic polarities in sediments and variable timing of neoformation of authigenic greigite. Earth and Planetary Science Letters 193(1–2): 1–12. https://doi.org/10.1016/S0012-821X(01)00497-6
Kao SJ, Horng CS, Roberts AP, et al. (2004) Carbon-sulfur-iron relationships in sedimentary rocks from southwestern Taiwan: Influence of geochemical environment on greigite and pyrrhotite formation. Chemical Geology 203(1): 153–168. https://doi.org/10.1016/j.chemgeo.2003.09.007
Karlin R, Levi S (1983) Diagenesis of magnetic minerals in recent hemipelagic sediments. Nature 303(5915): 327–330. https://doi.org/10.1038/303327a0
King J, Banerjee SK, Marvin J (1982) A comparison of different magnetic methods for determining the relative grain size of magnetite in natural materials: Some results from lake sediments. Earth and Planetary Science Letters 59 (2):404–419. https://doi.org/10.1016/0012-821X(82)90142-X
Lascu L, Plank C (2013) A new dimension to sediment magnetism: Charting the spatial variability of magnetic properties across lake basins. Global and Planetary Change 110: 340–349. https://doi.org/10.1016/j.gloplacha.2013.03.013
Li C, Yang S, Zhan W (2012) Magnetic properties of sediments from major rivers, aeolian dust, loess soil and desert in China. Journal of Asian Earth Sciences 45: 190–200. https://doi.org/10.1016/j.jseaes.2011.10.010
Li W, Hu Z, Zhang W, et al. (2017) Influence of provenance and hydrodynamic sorting on the magnetic properties and geochemistry of sediments of the Oujiang River, China. Marine Geology 387: 1–11. https://doi.org/10.1016/j.margeo.2017.03.002
Lin Y, Xu L, Mu G (2018) Differential erosion and the formation of layered yardangs in the Loulan region (Lop Nur): Eastern Tarim Basin. Aeolian Research 30: 41–47. https://doi.org/10.1016/j.aeolia.2017.12.002
Liu C, Zhang JF, Jiao P, et al. (2016) The Holocene history of Lop Nur and its palaeoclimate implications. Quaternary Science Reviews 148: 163–175. https://doi.org/10.1016/j.quascirev.2016.07.016
Liu QS, Roberts AP, Larrasoaña JC, et al. (2012) Environmental magnetism: Principles and applications. Reviews of Geophysics 50: RG4002. https://doi.org/10.1029/2012RG000393
Liu S, Zhang W, He Q, et al. (2010) Magnetic properties of East China Sea shelf sediments off the Yangtze Estuary: Influence of provenance and particle size. Geomorphology 119(3): 212–220. https://doi.org/10.1016/j.geomorph.2010.03.027
Ma CM, Wang FB, Cao QY, et al. (2008) Climate and environment reconstruction during the Medieval Warm Period in Lop Nur of Xinjiang, China. Chinese Science Bulletin 53(19): 3016–3027. https://doi.org/10.1007/s11434-008-0366-6
Maher BA (1988) Magnetic properties of some synthetic submicron magnetites. Geophysical Journal International 94(1): 83–96. https://doi.org/10.1111/j.1365-246X.1988.tb03429.x
Maher BA (2007) Environmental magnetism and climate change. Contemporary Physics 48(5): 247–274. https://doi.org/10.1080/00107510801889726
Maher BA (2011) The magnetic properties of Quaternary aeolian dusts and sediments, and their palaeoclimatic significance. Aeolian Research 3(2): 87–144. https://doi.org/10.1016/j.aeolia.2011.01.005
Oldfield F (2013) Mud and magnetism: Records of late Pleistocene and Holocene environmental change recorded by magnetic measurements. Journal of Paleolimnology 49(3): 465–480. https://doi.org/10.1007/s10933-012-9648-8
Qiang MR, Chen FH, Zhang JW, et al. (2007) Grain size in sediments from Lake Sugan: A possible linkage to dust storm events at the northern margin of the Qinghai-Tibetan Plateau. Environmental Geology. 51(7): 1229–1238. https://doi.org/10.1007/s00254-006-0416-9
Reinholdsson M, Snowball I, Zillén L, et al. (2013) Magnetic enhancement of Baltic Sea sapropels by greigite magnetofossils. Earth and Planetary Science Letters 366: 137–150. https://doi.org/10.1016/j.epsl.2013.01.029
Roberts AP (1995) Magnetic properties of sedimentary greigite (Fe3S4). Earth and Planetary Science Letters 134(3): 227–236. https://doi.org/10.1016/0012-821X(95)00131-U
Roberts AP. (2015) Magnetic mineral diagenesis. Earth-Science Reviews 15: 1–47. https://doi.org/10.1016/j.earscirev.2015.09.010
Roberts A P, Chang L, Rowan CJ, et al. (2011) Magnetic properties of sedimentary greigite(Fe3S4): An update. Reviews of Geophysics 49: RG1002. https://doi.org/10.1029/2010RG000336.
Roberts AP, Turner GM (1993) Diagenetic formation of ferrimagnetic iron sulphide minerals in rapidly deposited marine sediments, South Island, New Zealand. Earth and Planetary Science Letters 115(1–4): 257–273. https://doi.org/10.1016/0012-821X(93)90226-Y
Roberts AP, Weaver R (2005) Multiple mechanisms of remagnetization involving sedimentary greigite(Fe3S4). Earth and Planetary Science Letters 231(3): 263–277. https://doi.org/10.1016/j.epsl.2004.11.024
Robinson SG, Sahota JTS, Oldfield F (2000) Early diagenesis in North Atlantic abyssal plain sediments characterized by rockmagnetic and geochemical indices. Marine Geology 163(1): 77–107. https://doi.org/10.1016/S0025-3227(99)00108-5
Ron H, Nowaczyk NR, Frank U, et al. (2007) Greigite detected as dominating remanence carrier in Late Pleistocene sediments, Lisan formation, from Lake Kinneret(Sea of Galilee), Israel. Geophysical Journal International 170(1):117-131. https://doi.org/10.1111/j.1365-246X.2007.03425.x
Rowan CJ, Roberts AP, Broadbent T (2009) Reductive diagenesis, magnetite dissolution, greigite growth and paleomagnetic smoothing in marine sediments: A new view. Earth and Planetary Science Letters 277(1): 223–235. https://doi.org/10.1016/j.epsl.2008.10.016
Sagnotti L, Cascella A, Ciaranfi N, et al. (2010) Rock magnetism and palaeomagnetism of the Montalbano Jonico section (Italy): Evidence for late diagenetic growth of greigite and implications for magnetostratigraphy. Geophysical Journal International 180(3): 1049–1066. https://doi.org/10.1111/j.1365-246X.2009.04480.x
Snowball I, Thompson R (1988) The occurrence of greigite in sediments from Loch Lomond. Journal of Quaternary Science 3(2): 121–125. https://doi.org/10.1002/jqs.3390030203
Snowball I, Thompson R (1990) A stable chemical remanence in Holocene sediments. Journal of Geophysical Research: Solid Earth. 95(B4): 4471–4479. https://doi.org/10.1029/JB095iB04p04471
Sternbeck J, Sohlenius G (1997) Authigenic sulfide and carbonate mineral formation in Holocene sediments of the Baltic Sea. Chemical Geology 135(1): 55–73. https://doi.org/10.1016/S0009-2541(96)00104-0
Thompson R, Oldfield F (1986) Environmental Magnetism. Allen and Unwin, London.
Tudryn A, Giannesini PJ, Guichard F, et al. (2014) The role of iron minerals in laminae formation in Late Pleistocene sediments of the Caspian Sea. Quaternary International 345: 68–76. https://doi.org/10.1016/j.quaint.2013.04.024
Tudryn A, Tucholka P, Gibert E, et al. (2010) A late Pleistocene and Holocene mineral magnetic record from sediments of Lake Aibi, Dzungarian Basin, NW China. Journal of Paleolimnology 44(1): 109–121. https://doi.org/10.1007/s10933-009-9391-y
Wang L, Pan YX, Li JH, et al. (2008) Magnetic properties related to thermal treatment of pyrite. Science in China Series D-Earth Sciences 51(8): 1144–1153. https://doi.org/10.1007/s11430-008-0083-7
Wang ML, Liu CL, Jiao PC, et al. (2001) Saline Lake Potash Resources in the Lop Nur, Xinjiang. Geology Press, Beijing(In Chinese).
Wang YH, Zhang WG, Liu XJ, et al. (2015) Formation of greigite under different climate conditions in the Yellow River delta. Science China-Earth Sciences 58(2): 300–308. https://doi.org/10.1007/s11430-014-4981-6
Weaver R, Roberts AP, Barker AJ (2002) A late diagenetic(synfolding) magnetization carried by pyrrhotite: Implications for paleomagnetic studies from magnetic iron sulphide-bearing sediments. Earth and Planetary Science Letters 200(3–4): 371–386. https://doi.org/10.1016/S0012-821X(02)00652-0
Xia XC, Wang FB, Zhao YJ (2007) Lop Nur of China. Science Press, Beijing(In Chinese).
Xiao JL, Chang ZG, Fan JW, et al. (2012) The link between grain-size components and depositional processes in a modern clastic lake. Sedimentology 59(3): 1050–1062. https://doi.org/10.1111/j.1365-3091.2011.01294.x
Yamazaki T (2009) Environmental magnetism of Pleistocene sediments in the North Pacific and Ontong-Java Plateau: Temporal variations of detrital and biogenic components. Geochemistry Geophysics Geosystems 10, Q07Z04. https://doi.org/10.1029/2009GC002413.
Yang Y, Wang RJ, Liu J, et al. (2015) Regional dust activity history during the past 45 ka reflected by sensitive grain-size components in Lop Nur, Xinjiang. Earth Science Frontiers 22(5): 247–258.(In Chinese).
Yuan GY, Yuan L (1998) An approach to the environmental changes in Lop Nur history. Acta Geographica Sinica 53(Supplement): 83–89(In Chinese).
Zhang WG, Yu LZ (2003) Magnetic properties of tidal flat sediments of the Yangtze Estuary and its relationship with particle size. Science in China Series D-Earth Sciences 46(9): 954–966. https://doi.org/10.1007/BF02991341
Acknowledgements
This study was supported by the National Natural Science Foundation of China (Grant No. 41701012) and the project “Comprehensive Scientific Investigation of Natural and Cultural Heritage in the Lop Nur Region” (Grant No. 2014FY210500). We thank CHEN Dan for her help with drawing. We thank the anonymous reviewer for their constructive comments, and thank Andrew P. Roberts for the language improvement.
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Li, W., Mu, Gj., Lin, Yc. et al. Magnetic mineral diagenesis in sediments of saline lake Lop Nur. J. Mt. Sci. 16, 548–560 (2019). https://doi.org/10.1007/s11629-018-5073-4
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DOI: https://doi.org/10.1007/s11629-018-5073-4