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Quantifying the carbon source of pedogenic calcite veins in weathered limestone: implications for the terrestrial carbon cycle

  • Lin Zou
  • Lin Dong
  • Meng Ning
  • Kangjun Huang
  • Yongbo Peng
  • Shujian Qin
  • Honglin Yuan
  • Bing ShenEmail author
Original Article
  • 35 Downloads

Abstract

The continent is the second largest carbon sink on Earth’s surface. With the diversification of vascular land plants in the late Paleozoic, terrestrial organic carbon burial is represented by massive coal formation, while the development of soil profiles would account for both organic and inorganic carbon burial. As compared with soil organic carbon, inorganic carbon burial, collectively known as the soil carbonate, would have a greater impact on the long-term carbon cycle. Soil carbonate would have multiple carbon sources, including dissolution of host calcareous rocks, dissolved inorganic carbon from freshwater, and oxidation of organic matter, but the host calcareous rock dissolution would not cause atmospheric CO2 drawdown. Thus, to evaluate the potential effect of soil carbonate formation on the atmospheric pCO2 level, different carbon sources of soil carbonate should be quantitatively differentiated. In this study, we analyzed the carbon and magnesium isotopes of pedogenic calcite veins developed in a heavily weathered outcrop, consisting of limestone of the early Paleogene Guanzhuang Group in North China. Based on the C and Mg isotope data, we developed a numerical model to quantify the carbon source of calcite veins. The modeling results indicate that 4–37 wt% of carbon in these calcite veins was derived from atmospheric CO2. The low contribution from atmospheric CO2 might be attributed to the host limestone that might have diluted the atmospheric CO2 sink. Nevertheless, taking this value into consideration, it is estimated that soil carbonate formation would lower 1 ppm atmospheric CO2 within 2000 years, i.e., soil carbonate alone would sequester all atmospheric CO2 within 1 million years. Finally, our study suggests the C–Mg isotope system might be a better tool in quantifying the carbon source of soil carbonate.

Keywords

Mg isotope Calcite veins Pedogenic carbonate Silicate weathering Carbonate weathering 

Notes

Acknowledgements

We thank Yiwu Wang and Yuhan Wang of Peking University, for their assistance in the field and sample collection. This study is funded by the National Key Technology Program during the 13th Five-Year Plan Period (Grant No. 2016ZX05034001-007) and National Natural Science Foundation of China (Grant No. 41772359).

References

  1. Affek HP, Yakir D (2014) 5.7—the stable isotopic composition of atmospheric CO2. In: Holland HD, Turekian KK (eds) Treatise on geochemistry, 2nd edn. Elsevier, Oxford, pp 179–212.  https://doi.org/10.1016/B978-0-08-095975-7.00407-1 CrossRefGoogle Scholar
  2. Ague JJ, Brimhall GH (1987) Granites of the batholiths of California: products of local assimilation and regional-scale crustal contamination. Geology 15:63–66.  https://doi.org/10.1130/0091-7613(1987)15%3c63:gotboc%3e2.0.co;2 CrossRefGoogle Scholar
  3. Beerling DJ, Chaloner WG, Woodward FI, Algeo Thomas J, Scheckler Stephen E (1998) Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events. Philos Trans R Soc Lond Ser B Biol Sci 353:113–130.  https://doi.org/10.1098/rstb.1998.0195 CrossRefGoogle Scholar
  4. Chi P, Luan HY, Liu M, Lijun X (1994) On the division and correlation of the Cenozoic lithostratigraphic units in Shandong Province. Geol Shandong 10:71–85Google Scholar
  5. Courtillot VE, Renne PR (2003) On the ages of flood basalt events. Comptes Rendus Geosci 335:113–140.  https://doi.org/10.1016/S1631-0713(03)00006-3 CrossRefGoogle Scholar
  6. Curtis MH (2007) Symposium no. 20 Paper no. 897 presentation: oral Pedogenic carbonate: links between biotic and abioticGoogle Scholar
  7. Dietrich F, Diaz N, Deschamps P, Ngounou Ngatcha B, Sebag D, Verrecchia EP (2017) Origin of calcium in pedogenic carbonate nodules from silicate watersheds in the Far North Region of Cameroon: respective contribution of in situ weathering source and dust input. Chem Geol 460:54–69.  https://doi.org/10.1016/j.chemgeo.2017.04.015 CrossRefGoogle Scholar
  8. Doner HE, Lynn WC (1989) Carbonate, halide, sulfate, and sulfide minerals. In: Dixon JB, Weed SB (eds) Minerals in soil environments. SSSA book series, vol 1. Soil Science Society of America, Madison, p 279.  https://doi.org/10.2136/sssabookser1.2ed.c6 Google Scholar
  9. Ducea M (2001) The California Arc: thick granitic batholiths, eclogitic residues, lithospheric-scale thrusting, and magmatic flare-ups. GSA Today 11:4–10CrossRefGoogle Scholar
  10. Galy A, Bar-Matthews M, Halicz L, O’Nions RK (2002) Mg isotopic composition of carbonate: insight from speleothem formation. Earth Planet Sci Lett 201:105–115CrossRefGoogle Scholar
  11. Galy A, Yoffe O, Janney PE, Williams RW, Carignan J (2003) Magnesium isotope heterogeneity of the isotopic standard SRM980 and new reference materials for magnesium-isotope-ratio measurements. J Anal At Spectrom 18:1352–1356CrossRefGoogle Scholar
  12. Gile LH (1966) Morphological and genetic sequences of carbonate accumulation in desert soils. Soil Sci 101:347–360CrossRefGoogle Scholar
  13. Given RK, Wilkinson BH (1987) Perspectives: dolomite abundance and stratigraphic age: constrains on rates and mechanisms of Phanerozoic dolostone formation. J Sediment Petrol 57:1068–1078CrossRefGoogle Scholar
  14. Goudie AS, Viles HA (2012) Weathering and the global carbon cycle: geomorphological perspectives. Earth Sci Rev 113:59–71.  https://doi.org/10.1016/j.earscirev.2012.03.005 CrossRefGoogle Scholar
  15. Hancock GR, Kunkel V, Wells T, Martinez C (2019) Soil organic carbon and soil erosion—understanding change at the large catchment scale. Geoderma 343:60–71.  https://doi.org/10.1016/j.geoderma.2019.02.012 CrossRefGoogle Scholar
  16. Hardie LA (1996) Secular variation in seawater chemistry: an explanation for the coupled secular variation in the mineralogies of marine limestones and potash evaporites over the past 600 my. Geology 24:279–283CrossRefGoogle Scholar
  17. Hayes JM, Waldbauer JR (2006) The carbon cycle and associated redox processes through time. Philos Trans R Soc B Biol Sci 361:931–950.  https://doi.org/10.1098/rstb.2006.1840 CrossRefGoogle Scholar
  18. Henkes GA, Passey BH, Grossman EL, Shenton BJ, Yancey TE, Pérez-Huerta A (2018) Temperature evolution and the oxygen isotope composition of Phanerozoic oceans from carbonate clumped isotope thermometry. Earth Planet Sci Lett 490:40–50.  https://doi.org/10.1016/j.epsl.2018.02.001 CrossRefGoogle Scholar
  19. Higgins JA, Schrag DP (2010) Constraining magnesium cycling in marine sediments using magnesium isotopes. Geochim Cosmochim Acta 74:5039–5053CrossRefGoogle Scholar
  20. Higgins JA, Schrag DP (2015) The Mg isotopic composition of Cenozoic seawater—evidence for a link between Mg-clays, seawater Mg/Ca, and climate. Earth Planet Sci Lett 416:73–81CrossRefGoogle Scholar
  21. Holland HD (1978) The chemistry of the atmosphere and oceans. John Wiley & SonsGoogle Scholar
  22. Hsieh Y-P (1993) Radiocarbon signatures of turnover rates in active soil organic carbon pools. Soil Sci Soc Am J 57:1020–1022.  https://doi.org/10.2136/sssaj1993.03615995005700040023x CrossRefGoogle Scholar
  23. Huang K-J et al (2015) Magnesium isotopic compositions of the Mesoproterozoic dolostones: implications for Mg isotopic systematics of marine carbonates. Geochim Cosmochim Acta 164:333–351.  https://doi.org/10.1016/j.gca.2015.05.002 CrossRefGoogle Scholar
  24. Immenhauser A, Buhl D, Richter D, Niedermayr A, Riechelmann D, Dietzel M, Schulte U (2010) Magnesium-isotope fractionation during low-Mg calcite precipitation in a limestone cave—field study and experiments. Geochim Cosmochim Acta 74:4346–4364.  https://doi.org/10.1016/j.gca.2010.05.006 CrossRefGoogle Scholar
  25. Jenny H (1980) The soil resource: origin and behavior, vol 37. Springer, Berlin.  https://doi.org/10.1007/978-1-4612-6112-4 Google Scholar
  26. Kerr AC (1998) Oceanic plateau formation: a cause of mass extinction and black shale deposition around the Cenomanian–Turonian boundary? J Geol Soc 155:619–626.  https://doi.org/10.1144/gsjgs.155.4.0619 CrossRefGoogle Scholar
  27. Knoll MA, James WC (1987) Effect of the advent and diversification of vascular land plants on mineral weathering through geologic time. Geology 15:1099–1102.  https://doi.org/10.1130/0091-7613(1987)15%3c1099:eotaad%3e2.0.co;2 CrossRefGoogle Scholar
  28. Kump LR, Arthur MA (1999) Interpreting carbon-isotope excursions: carbonates and organic matter. Chem Geol 161:181–198CrossRefGoogle Scholar
  29. Lee YI, Hisada K-I (1999) Stable isotopic composition of pedogenic carbonates of the Early Cretaceous Shimonoseki Subgroup, western Honshu, Japan. Palaeogeogr Palaeoclimatol Palaeoecol 153:127–138.  https://doi.org/10.1016/S0031-0182(99)00069-3 CrossRefGoogle Scholar
  30. Lee C-TA, Cheng X, Horodyskyj U (2006) The development and refinement of continental arcs by primary basaltic magmatism, garnet pyroxenite accumulation, basaltic recharge and delamination: insights from the Sierra Nevada, California. Contrib Mineral Petrol.  https://doi.org/10.1007/s00410-00005-00056-00411 Google Scholar
  31. Lee C-TA et al (2013) Continental arc-island arc fluctuations, growth of crustal carbonates, and long-term climate change. Geosphere 9:21–36.  https://doi.org/10.1130/ges00822.1 CrossRefGoogle Scholar
  32. Li T, Li G (2014) Incorporation of trace metals into microcodium as novel proxies for paleo-precipitation. Earth Planet Sci Lett 386:34–40.  https://doi.org/10.1016/j.epsl.2013.10.011 CrossRefGoogle Scholar
  33. Li J, Liu CQ, Li LB (2010a) The impacts of chemical weathering of carbonate rock by sulfuric acid on the cycling of dissolved inorganic carbon in Changjiang River water. Geochimica 39(4):305–313Google Scholar
  34. Li W-Y, Teng F-Z, Ke S, Rudnick RL, Gao S, Wu F-Y, Chappell BW (2010b) Heterogeneous magnesium isotopic composition of the upper continental crust. Geochim Cosmochim Acta 74:6867–6884.  https://doi.org/10.1016/j.gca.2010.08.030 CrossRefGoogle Scholar
  35. Li W, Chakraborty S, Beard BL, Romanek CS, Johnson CM (2012) Magnesium isotope fractionation during precipitation of inorganic calcite under laboratory conditions. Earth Planet Sci Lett 333–334:304–316.  https://doi.org/10.1016/j.epsl.2012.04.010 CrossRefGoogle Scholar
  36. Li S, Wang Q, Zhang H, Lu H, Martín-Closas C (2016) Charophytes from the Cretaceous—Paleogene transition in the Pingyi Basin (Eastern China) and their Eurasian correlation. Cretac Res 59:179–200.  https://doi.org/10.1016/j.cretres.2015.10.022 CrossRefGoogle Scholar
  37. Liu C, Wang Z, Raub TD, Macdonald FA, Evans DAD (2014) Neoproterozoic cap-dolostone deposition in stratified glacial meltwater plume. Earth Planet Sci Lett 404:22–32.  https://doi.org/10.1016/j.epsl.2014.06.039 CrossRefGoogle Scholar
  38. Livingstone DA (1963) Chemical composition of rivers and lakes: professional paper 440-GGoogle Scholar
  39. Machel H (2004) Concepts and models of dolomitization: a critical reappraisal. Geol Soc Lond Special Publ 235:7–63.  https://doi.org/10.1144/gsl.sp.2004.235.01.02 CrossRefGoogle Scholar
  40. Mavromatis V, Gautier Q, Bosc O, Schott J (2013) Kinetics of Mg partition and Mg stable isotope fractionation during its incorporation in calcite. Geochim Cosmochim Acta 114:188–203.  https://doi.org/10.1016/j.gca.2013.03.024 CrossRefGoogle Scholar
  41. Mermut AR, Amundson R, Cerling TE (2000) The use of isotopes in studying carbonate dynamics in soils. In: Lal R, Kimble JM, Eswaran H, Stewart BA (eds) Global climate change and pedogenic carbonates, Advance in soil science, CRC Lewis Publ, pp 65–85Google Scholar
  42. Nearing MA, Xie Y, Liu B, Ye Y (2017) Natural and anthropogenic rates of soil erosion international soil and water conservation research 5:77–84.  https://doi.org/10.1016/j.iswcr.2017.04.001 CrossRefGoogle Scholar
  43. Nieder R, Benbi D (2008) Carbon and nitrogen in the terrestrial environment. Springer, Berlin.  https://doi.org/10.1007/978-1-4020-8433-1 CrossRefGoogle Scholar
  44. Opfergelt S, Georg RB, Delvaux B, Cabidoche YM, Burton KW, Halliday AN (2012) Mechanisms of magnesium isotope fractionation in volcanic soil weathering sequences, Guadeloupe. Earth Planet Sci Lett 341–344:176–185.  https://doi.org/10.1016/j.epsl.2012.06.010 CrossRefGoogle Scholar
  45. Peng Y et al (2016) Constraining dolomitization by Mg isotopes: a case study from partially dolomitized limestones of the middle Cambrian Xuzhuang Formation. North China Geochem Geophys Geosyst 17:1109–1129CrossRefGoogle Scholar
  46. Qualls RG, Bridgham SD (2005) Mineralization rate of 14C-labelled dissolved organic matter from leaf litter in soils of a weathering chronosequence. Soil Biol Biochem 37:905–916.  https://doi.org/10.1016/j.soilbio.2004.08.029 CrossRefGoogle Scholar
  47. Royer DL (1999) Depth to pedogenic carbonate horizon as a paleoprecipitation indicator? Geology 27:41–52CrossRefGoogle Scholar
  48. Rudnick RL, Gao S (2014) 4.1—composition of the continental crust. In: Holland HD, Turekian KK (eds) Treatise on geochemistry, 2nd edn. Elsevier, Oxford, pp 1–51.  https://doi.org/10.1016/B978-0-08-095975-7.00301-6 Google Scholar
  49. Saulnier S, Rollion-Bard C, Vigier N, Chaussidon M (2012) Mg isotope fractionation during calcite precipitation: an experimental study. Geochim Cosmochim Acta 91:75–91CrossRefGoogle Scholar
  50. Schlesinger W (1985) The formation of caliche in soils of the Mojave Desert, California, vol 49.  https://doi.org/10.1016/0016-7037(85)90191-7
  51. Shen B, Jacobsen B, Lee C-TA, Yin Q-Z, Morton DM (2009) The Mg isotopic systematics of granitoids in continental arcs and implications for the role of chemical weathering in crust formation. Proc Natl Acad Sci 106:20652.  https://doi.org/10.1073/pnas.0910663106 CrossRefGoogle Scholar
  52. Shen B, Wimpenny J, Lee C-TA, Tollstrup D, Yin Q-Z (2013) Magnesium isotope systematics of endoskarns: implications for wallrock reaction in magma chambers. Chem Geol 356:209–214.  https://doi.org/10.1016/j.chemgeo.2013.08.018 CrossRefGoogle Scholar
  53. Sinton CW, Duncan RA, Storey M, Lewis J, Estrada JJ (1998) An oceanic flood basalt province within the Caribbean plate. Earth Planet Sci Lett 155:221–235CrossRefGoogle Scholar
  54. Stanley SM, Hardie LA (1999) Hypercalcification: paleontology links plate tectonics and geochemistry to sedimentology. GSA Today 9:1–7Google Scholar
  55. Su X-S, Wu X-F, Lin XY, Liao ZS, Wang JS (2006) Main chemical constituent of the yellow river water and characteristics of δ ~ (13)C streamwise variation. Yellow Riv 28(5):29–31Google Scholar
  56. Sundquist ET, Ackerman KV (2014) 10.9 - The geologic history of the carbon cycle. In: Holland HD, Turekian KK (eds) Treatise on geochemistry, 2nd edn. Elsevier, Oxford, pp 361–398.  https://doi.org/10.1016/B978-0-08-095975-7.00809-3 CrossRefGoogle Scholar
  57. Teng F-Z (2017) Magnesium isotope geochemistry. Rev Miner Geochem.  https://doi.org/10.1515/9783110545630-008 Google Scholar
  58. Teng F et al (2015) Magnesium isotopic compositions of international geological reference materials. Geostand Geoanal Res 39:329–339.  https://doi.org/10.1111/j.1751-908X.2014.00326.x CrossRefGoogle Scholar
  59. Tipper ET, Galy A, Bickle MJ (2006a) Riverine evidence for a fractionated reservoir of Ca and Mg on the continents: implications for the oceanic Ca cycle. Earth Planet Sci Lett 247:267–279.  https://doi.org/10.1016/j.epsl.2006.04.033 CrossRefGoogle Scholar
  60. Tipper ET, Galy A, Gaillardet J, Bickle MJ, Elderfield H, Carder EA (2006b) The magnesium isotope budget of the modern ocean: constraints from riverine magnesium isotope ratios. Earth Planet Sci Lett 250:241–253.  https://doi.org/10.1016/j.epsl.2006.07.037 CrossRefGoogle Scholar
  61. von Strandmann PAEP, Elliott T, Marschall HR, Coath C, Lai Y-J, Jeffcoate AB, Ionov DA (2011) Variations of Li and Mg isotope ratios in bulk chondrites and mantle xenoliths. Geochim Cosmochim Acta 75:5247–5268.  https://doi.org/10.1016/j.gca.2011.06.026 CrossRefGoogle Scholar
  62. von Strandmann PAEP, Opfergelt S, Lai Y-J, Sigfússon B, Gislason SR, Burton KW (2012) Lithium, magnesium and silicon isotope behaviour accompanying weathering in a basaltic soil and pore water profile in Iceland. Earth Planet Sci Lett 339–340:11–23.  https://doi.org/10.1016/j.epsl.2012.05.035 CrossRefGoogle Scholar
  63. Wimpenny J, Gíslason SR, James RH, Gannoun A, Von Strandmann PAEP, Burton KW (2010) The behaviour of Li and Mg isotopes during primary phase dissolution and secondary mineral formation in basalt. Geochim Cosmochim Acta 74:5259–5279.  https://doi.org/10.1016/j.gca.2010.06.028 CrossRefGoogle Scholar
  64. Wombacher F, Eisenhauer A, Böhm F, Gussone N, Regenberg M, Dullo WC, Rüggeberg A (2011) Magnesium stable isotope fractionation in marine biogenic calcite and aragonite. Geochim Cosmochim Acta 75:5797–5818.  https://doi.org/10.1016/j.gca.2011.07.017 CrossRefGoogle Scholar
  65. Xue J et al (2015) Stepwise evolution of Paleozoic tracheophytes from South China: contrasting leaf disparity and taxic diversity. Earth Sci Rev 148:77–93.  https://doi.org/10.1016/j.earscirev.2015.05.013 CrossRefGoogle Scholar
  66. Young ED, Galy A (2004) The isotope geochemistry and cosmochemistry of magnesium. Rev Miner Geochem 55:197–230.  https://doi.org/10.2138/gsrmg.55.1.197 CrossRefGoogle Scholar
  67. Zamanian K, Pustovoytov K, Kuzyakov Y (2016) Pedogenic carbonates: forms and formation processes. Earth Sci Rev 157:1–17.  https://doi.org/10.1016/j.earscirev.2016.03.003 CrossRefGoogle Scholar

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© Science Press and Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Key Laboratory of Orogenic Belts and Crustal Evolution, MOE and School of Earth and Space SciencePeking UniversityBeijingPeople’s Republic of China
  2. 2.Shaanxi Key Laboratory of Early Life and Environments, Department of GeologyNorthwest UniversityXi’anPeople’s Republic of China
  3. 3.Department of Geology and GeophysicsLouisiana State UniversityBaton RougeUSA

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