Abstract
Soil chronosequences derived from landslides with certain time series are the great avenue to elevate our understanding on the processes of pedogenesis, nutrient dynamics, and ecosystem evolution. However, the construction of reliable soil chronosequence from historical landslides remains intricate. Here, we presented a 22,000-year soil chronosequence from multiple landslides on the upper reach of Minjiang River, western China. The variation in a variety of pedogenesis indices and soil nutrients verified the reliability of the chronosequence. The silica-alumina ratio and silica sesquioxide ratio decreased significantly with soil age. This reflected the enrichment of Al/Fe/Ti oxides but the depletion of Si oxides with the soil development. Meanwhile, the values of the Chemical Index of Weathering and the Chemical Index of Alteration increased significantly with soil age, especially from 5 to 89 years. These variations were attributed to the soil weathering, which led to the destruction of soil minerals with the rapid loss of most of cations (e.g., K, Na, Ca, and Mg) during the soil development. The concentrations of carbon and nitrogen in topsoil increased with soil age, and the carbon accumulation rate slowed significantly from 5,500 to 22,000 years. The total phosphorus concentrations decreased with soil age, suggesting the gradual loss of soil phosphorus with soil development. The results indicate that the landslide chronosequence established on the upper reach of Minjiang River is reliable and delineates a long-term soil development process, which will provide a great platform for further improvement of biogeochemical theories and understanding sustainable vegetation restoration.
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References
Alexandre A, Meunier JD, Colin F, et al. (1997) Plant impact on the biogeochemical cycle of silicon and related weathering processes. Geochim Cosmochim Acta 61(3): 677–682. https://doi.org/10.1016/S0016-7037(97)00001-X
An WP, Zhao JQ, Yan XB, et al. (2008) Tectonic deformation of lacustrine sediments in Qiangyang on the Minjiang fault zone and ancient earthquake. Seismology and Geology 30(4): 980–988. (In Chinese).
Ardizzone F, Cardinali M, Galli M, et al. (2007) Identification and mapping of recent rainfall-induced landslides using elevation data collected by airborne lidar. Nat Hazards Earth Syst Sci 7(6), 637–650. https://doi.org/10.5194/nhess-7-637-2007
Beilke AJ and Bockheim JG (2013) Carbon and nitrogen trends in soil chronosequences of the Transantarctic Mountains. Geoderma 197: 117–125. https://doi.org/10.1016/j.geoderma.2013.01.004
Birkeland PW (1974) Pedology, weathering, and geomorphological research. New York: Oxford University. pp 81–181.
Birkeland PW (1990) Soil-geomorphic research-a selective overview. Geomorphology 3(3–4): 207–224. https://doi.org/10.1016/0169-555X(90)90004-A
Błonska E, Lasota J, Piaszczyk W, et al. (2018) The effect of landslide on soil organic carbon stock and biochemical properties of soil. J Soils Sediments 18 (8): 2727–2737. https://doi.org/10.1007/s11368-017-1775-4
Bronk RC (2009) Bayesian analysis of radiocarbon dates. Radiocarbon 51(1): 337–360. https://doi.org/10.2458/azu_js_rc.51.3494
Chai HJ, Liu HC (2002) Study on landslide damming of river in upper of Minjiang river. J Mt Sci 20(5): 616–620(In Chinese).
Chai HJ, Liu HC, Zhang ZY (1995) The catalog of Chinese landslide dam events. J Hazard Mater 4: 1–9 (In Chinese).
Crews TE, Kitayama K, Fownes JH, et al. (1995) Changes in soil phosphorus fractions and ecosystem dynamics across a long chronosequence in Hawaii. Ecology 76(5): 1407–1424. https://doi.org/10.2307/1938144
Dahlgren RA (1994) Soil acidification and nitrogen saturation from weathering of ammonium-bearing rock. Nature 368(6478): 838–841. https://doi.org/10.1038/369340c0
Daniel RM (2001) Evolution of Soils on Quaternary Reef Terraces of Barbados, West Indies. Quat Res 56(1): 66–78. https://doi.org/10.1006/qres.2001.2237
Derry LA, Kurtz AC, Ziegler K, et al. (2005) Biological control of terrestrial silica cycling and export fluxes to watersheds. Nature 433(7027):728–731. https://doi.org/10.1038/nature03299
Dickson BA, Crocker RL (1953) A chronosequence of soils and vegetation near mt shasta, california 2. the development of the forest floors and the carbon and nitrogen profiles of the soils. J Soil Sci 4(2): 143-&. https://doi.org/10.1111/j.1365-2389.1953.tb00650.x
Fang XM (1994) The origin and provenance of Malan loess from the eastern edge of Tibetan plateau and its adjacent areas. Sci China Series B-Chem 24 (5): 539–546. (In Chinese).
Fang XM, Lu LQ, Mason JA, et al. (2003) Pedogenic response to millennial summer monsoon enhancements on the Tibetan Plateau. Quat Int 106: 79–88. https://doi.org/10.1016/S1040-6182(02)00163-5
Gan JJ, Han W, Chun T, et al. (2015) Mechanism and characteristics of multiple catastrophic mudslides of tasi ditch in Li county of Sichuan Province. J Cata 30(4): 59–63. (In Chinese).
Guggenberger G, Baumler R, Zech W, (1998) Weathering of soils developed in eolian material overlaying glacial deposits in Eastern Nepal. Soil Sci 163(4): 325–337. https://doi.org/10.1097/00010694-199804000-00007
Guzzetti F, Mondini AC, Cardinali M, et al (2012) Landslide inventory maps: new tools for an old problem. Earth Sci Rev 112 (1–2): 42–66. https://doi.org/10.1016/j.earscirev.2012.02.001
Han Y, Huh Y, Derry L (2015) Ge/Si ratios indicating hydrothermal and sulfide weathering input to rivers of the Eastern Tibetan Plateau and Mt. Baekdu. Chem Geol 410: 40–52. https://doi.org/10.1016/j.chemgeo.2015.06.001
Harden JW (1982) A quantitative index of soil development from field descriptions: examples from a chronosequence in central california. Geoderma 28(1): 1–28. https://doi.org/10.1016/0016-7061(82)90037-4
Harnois L (1988) The CIW Index: a new chemical index of weathering. Sediment Geol 55(3–4):319–322. https://doi.org/10.1016/0037-0738(88)90137-6
Hassink J (1997) The capacity of soils to preserve organic C and N by their association with clay and silt particles. Plant Soil 191: 77–87. https://doi.org/10.1023/A:1004213929699
Hemingway JD, Hilton, RG, Hovius N, et al. (2018) Microbial oxidation of lithospheric organic carbon in rapidly eroding tropical mountain soils. Science 360 (6385): 209–212. https://doi.org/10.1126/science.aao6463
Hilton RG, Meunier P, Hovius N, et al. (2011) Landslide impact on organic carbon cycling in a temperate montane forest. Earth Surf Process Landf 36(12): 1670–1679. https://doi.org/10.1002/esp.2191
Holloway JM, Dahlgren RA (2002) Nitrogen in rock: occurrences and biogeochemical implications. Global Biogeochem Cycles 16(4): 65–71. https://doi.org/10.1029/2002GB001862
Huang CM and Gong ZT (2001) Quantitative studies on development of tropical soils: A case study in northern Hainan Island. Earth science: Journal of China University of Geosciences 26(3):315–321. (In Chinese).
Huang CM, Gong ZT, Yang DY (2002). Genesis of soils derived from basalt in northern Hainan Island II Iron oxides Acta Pedologica Sinica 39(4):449–457. (In Chinese).
Huang ZG, Zhang WQ, Chen JH, et al. (1996) China Southern red weathering crust. Beijing Ocean Press. pp 38–304.
Huggett RJ (1998) Soil chronosequences, soil development, and soil evolution: acritical review. Catena 32(3–4): 155–172. https://doi.org/10.1016/S0341-8162(98)00053-8
Izquierdo JE, Houlton BZ, Van HTL (2013) Evidence for progressive phosphorus limitation over long-term ecosystem development: examination of a biogeochemical paradigm. Plant Soil 367(1–2): 135–147. https://doi.org/10.1007/s11104-013-1683-3
James LA (1988) Rates of organic carbon accumulation in young mineral soils Near Burroughs Glacier, Glacier Bay, Alaska. Phys Geogr. 9(1): 50–70. https://doi.org/10.1080/02723646.1988.10642339
Janzen HH, Fixen PE, Franzluebbers AJ, et al. (2011) Global prospects rooted in soil science. Soil Sci Soc Am J 75 (1): 1–8. https://doi.org/10.2136/sssaj2009.0216
Jenny H (1969) The Pygmy forest-Podsol ecosystem and its dune associates of the Mendocino Coast. Madrono 20(2): 60–74. http://creativecommons.org/licenses/by-nc/3.0/
Kouno K, Tuchiya Y, Ando T (1995) Measurement of soil microbial biomass phosphorus by an anion-exchange membrane method. Soil Biol Biochem 27(10): 1353–1357. https://doi.org/10.1016/0038-0717(95)00057-L
Lichter J (1998) Primary succession and forest development on coastal Lake Michigan sand dunes. Ecol Monogr 68(4): 487–510. https://doi.org/10.2307/2657151
Lu HH, Yi GH, Zhang TB, et al. (2021) Variations in vegetation cue with climate change and human activity during growing seasons in the Western Sichuan Plateau, China. Remote Sens Lett 12(5): 419–428. https://doi.org/10.1080/2150704X.2021.1895447
Lugo AE and Brown S (1993) Management of tropical soils as sinks or sources of atmospheric carbon. Plant Soil 149(1): 27–41. https://doi.org/10.1007/BF00010760
Martha CE, Ryan B, David V, et al. (2008) A soil chronosequence study of the Reno valley, Italy: Insights into the relative role of climate versus anthropogenic forcing on hillslope processes during the mid-Holocene. Geoderma 147(3): 97–107. https://doi.org/10.1016/j.geoderma.2008.07.011
Murphy J and Riley JP (1962) A modified single solution method for the determination of phosphate in natural waters. Anal Chim Acta 27: 31–36. https://doi.org/10.1016/S0003-2670(00)88444-5
Nesbitt H, Young GM (1984) Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations. Geochim Cosmochim Acta 48(7): 1523–1534. https://doi.org/10.1016/0016-7037(84)90408-3
Nesbitt HW, Young GM (1982) Early proterozoic climate sand plate motions inferred from major element chemistry of lutites. Nature 299(5885):715–717. https://doi.org/10.1038/299715a0
Newman GS, Hart SC (2015) Shifting soil resource limitations and ecosystem retrogression across a three million year semiarid substrate age gradient. Biogeochemistry 124(1–3): 177–186. https://doi.org/10.1007/s10533-015-0090-7
Newman GS, Coble AA, Haskins, KE et al. (2020) The expanding role of deep roots during long-term terrestrial ecosystem development. Biogeochemistry 108(6): 2256–2269. https://doi.org/10.1111/1365-2745.13444
Nie GZ, Gao JG, Deng Y (2004) Preliminary study on earthquake-induced dammed lake. Q Sci 24(3): 293–301. (In Chinese)
Olivia R, Dirk W (2022) Landslides: An emerging model for ecosystem and soil chronosequence research. Earth Sci Rev 231: 104064. https://doi.org/10.1016/j.earscirev.2022.104064
Parker A (1970) An index of weathering for silicate rocks. Geol Mag 107(5): 501–50. https://doi.org/10.1017/S0016756800058581
Peltzer DA, Wardle DA, Allison VJ, et al. (2010) Understanding ecosystem retrogression. Ecol Monogr 80(4): 509–529. https://doi.org/10.1890/09-1552.1
Poeplau C, Don A, Vesterdal L, et al. (2011) Temporal dynamics of soil organic carbon after land-use change in the temperate zone e carbon response functions as a model approach. Glob Change Biol 17(7): 2415–2427. https://doi.org/10.1111/j.1365-2486.2011.02408.x
Post WM, Kwon KC (2000) Soil carbon sequestration and land-use change: processes and potential. Glob Change Biol 6(8): 317–327. https://doi.org/10.1046/j.1365-2486.2000.00308.x
R Core Team (2016) R: A Language and Environment for Statistical Computing. R Foundation for Statistical Computing, Vienna.
Ramos CE, Castellanos EJ, Restrepo C (2012) The transfer of modern organic carbon by landslide activity in tropical montane ecosystems. J Geophys Res Atmos 117 (G3): 2553–2554. https://doi.org/10.1029/2011JG001838
Razak KA, Santangelo M, Van CJ, et al. (2013) Generating an optimal dtm from airborne laser scanning data for landslide mapping in a tropical forest environment. Geomorphology 190(15): 112–125. https://doi.org/10.1016/j.geomorph.2013.02.021
Reimer PJ, Edouard BB, Alex BB, et al. (2013) IntCal13 and marine 13 radiocarbon age calibration curves 0-50,000 years cal BP. Radiocarbon 55(4): 1869–1887. https://doi.org/10.2458/azu_js_rc.55.16947
Rode AA (1961) The soil forming process and soil evolution. Israel Program for Scientific Translations, Jerusalem, Israel.
Schlögel R, Malet JP, Reichenbach P, et al. (2015) Analysis of a landslide multi-date inventory in a complex mountain landscape: the ubaye valley case study. Nat Hazards Earth Syst Sci 3 (3): 2051–2098. https://doi.org/10.5194/nhessd-3-2051-2015
Schulz S, Brankatschk R, DÜMig A, et al. (2013) The role of microorganisms at different stages of ecosystem development for soil formation. Biogeosciences 10 (6): 3983–3996. https://doi.org/10.5194/bg-10-3983-2013
Selmants PC, Hart SC (2010) Phosphorus and soil development: does the walker and syers model apply to semiarid ecosystems? Ecology 91(2): 474–484. https://doi.org/10.1890/09-0243.1
Six J, Conant RT, Paul EA, et al. (2002) Stabilization mechanisms of soil organic matter: implications for c-saturation of soils. Plant Soil 241(2): 155–176. https://doi.org/10.1023/A:1016125726789
Stevens PR and Walker TW (1970) The chronosequence concept and soil formation. Q Rev Biol 45(4): 333–350. https://doi.org/10.1086/406646
Stewart CE, Paustian K, Conant RT, et al. (2007) Soil Carbon saturation: concept, evidence and evaluation. Biogeochemistry 86(1): 19–31. https://doi.org/10.1007/s10533-007-9140-0
Turner BL and Laliberté E (2015) Soil development and nutrient availability along a 2 million-year coastal dune chronosequence under species-rich mediterranean shrubland in Southwestern Australia. Ecosystems 18(2): 287–309. https://doi.org/10.1007/s10021-014-9830-0
Turner BL, Condron LM, Richardson SJ, et al. (2007) Soil organic phosphorus transformations during pedogenesis. Ecosystems 10(7): 1166–1181. https://doi.org/10.1007/s10021-007-9086-z
Turner BL, Condron LM, Wells A, et al. (2012) Soil Nutrient dynamics during podzol development under lowland temperature rain forest in New Zealand. Catena 97: 50–62. https://doi.org/10.1016/j.catena.2012.05.007
Vindušková O, Pánek T, Frouz J (2019) Soil C, N and P Dynamics along a 13 ka chronosequence of landslides under semi-natural temperate forest. Q Sci Rev 213(1): 18–29. https://doi.org/10.1016/j.quascirev.2019.04.001
Vitousek PM, Farrington H (1997) Nutrient limitation and soil development: Experimental test of a biogeochemical theory. Biogeochemistry 37(1): 63–75. https://doi.org/10.1023/A:1005757218475
Vitousek PM, Porder S, Houlton BZ, et al. (2004) Terrestrial phosphorus limitation: mechanisms, implications, and nitrogene phosphorus interactions. Ecol Appl 20(1): 5–15. https://doi.org/10.1890/08-0127.1
Vreeken WJ (1975) Principal kinds of chronosequences and their significance in soil history. Soil Sci 26(4): 378–394. https://doi.org/10.1111/j.1365-2389.1975.tb01962.x
Walker TK, Syers JK (1976) The fate of phosphorus during pedogenesis. Geoderma 15(1): 1–19. https://doi.org/10.1016/0016-7061(76)90066-5
Walker LR, Wardle DA, Bardgett RD, et al. (2010) The use of chronosequences in studies of ecological succession and soil development. J Ecol 98 (4), 725–736. https://doi.org/10.1111/j.1365-2745.2010.01664.x
Wang LS, Wang XQ, Xu XN, et al. (2007) What happened on the upstream of Minjiang River in Sichuan Province 20000 years ago? Earth Sci Front 14(4): 189–196 (In Chinese).
Wang SG, Wang CH, Zhang JS, et al. (2003) Debris flow hazards in Chayuan stream of Wenchuan county, Sichuan Province on August 9, 2003. Mountain Science 21(5): 635–637. (In Chinese)
Wardle DA, Lawrence RW, Bardgett RD (2004) Ecosystem properties and forest decline in contrasting long-term chronosequences. Science 308(5772): 633c–633c. https://doi.org/10.1126/science.1109723
Wu YH, Zhou J, Bing HJ, et al. (2015) Rapid loss of phosphorus during early pedogenesis along a glacier retreat choronosequence, Gongga Mountain (Sw China). Peerj 3(1–2): 26557441. https://doi.org/10.1126/10.7717/peerj.1377
Xie H, Zhong DL, Li Y, et al. (2004) Features of debris flows in the upper reaches of the Changjiang River. Resources and Environment in the Yangtze Basin 13(1): 94–99. (In Chinese)
Xu Q, Li WL, Dong XJ, et al. (2017) The Xinmocun landslide on June 24, 2017 in Maoxian, Sichuan: characteristics and failure mechanism. Chinese Journal of Rock Mechanics and Engineering 36(11): 2612–2628. (In Chinese)
Yaalon DH (1983) Climate, time and soil development. In: Wilding LP, Smeck NE, Hall GF (eds.), Pedogenesis and Soil Taxonomy: I. Concepts and Interactions. Elsevier, Amsterdam. pp 223–251.
Yang L, Luo P, Wen L, et al. (2016) Soil organic carbon accumulation during post-agricultural succession in a karst area, Southwest China. Sci Rep 6(1): 37118. https://doi.org/10.1038/srep37118
Yang X, Post WM (2011) Phosphorus transformations as a function of pedogenesis: a synthesis of soil phosphorus data using Hedley fractionation method. Biogeosci Discuss 8(10): 5907–5934. https://doi.org/10.5194/bg-8-2907-2011
Yang Y, Li D, Zhang G, et al. (2010) Evolution of consequential soils derived from volcanic basalt on tropical leizhou peninsula, South China. Acta Pedologica Sinica 47(5): 123–136. (In Chinese)
Zhao QG, Wang ZQ, Liu ZL (1983) Preliminary studies on genetic properties of the allitic soils in China. Acta Pedologica Sinica 20(4):334–345. (In Chinese)
Zhong J, Li S, Li Z, et al. (2022) Metamorphic fluxes of water and carbon in rivers of the Eastern Qinghai-Tibetan Plateau. Sci China Earth Sci 65(4): 652–661. https://doi.org/10.1007/s11430-021-9873-7
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The research reported in this manuscript is funded by the Key Program of the Chinese Academy of Sciences for International Cooperation (131551KYSB20190028) and the Key Research and Development Projects Foundation of Sichuan, China (Grants No. 2018JZ0075).
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He, Jb., Wu, Yh., Bing, Hj. et al. Soil chronosequence derived from landslides on the upper reach of Minjiang River, western China. J. Mt. Sci. 20, 1282–1292 (2023). https://doi.org/10.1007/s11629-022-7824-5
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DOI: https://doi.org/10.1007/s11629-022-7824-5