Welcome to Francis Academic Press

Academic Journal of Environment & Earth Science, 2022, 4(8); doi: 10.25236/AJEE.2022.040802.

Research progress of iron isotopes in plants

Author(s)

Bo Zhao1,2,3,4,5,6

Corresponding Author:
Bo Zhao
Affiliation(s)

1Shaanxi Provincial Land Engineering Construction Group Co., Ltd., Xi’an, Shaanxi, 710075, China

2Institute of Land Engineering and Technology, Shaanxi Provincial Land Engineering Construction Group Co, Ltd., Xi’an, Shaanxi, 710075, China

3Key Laboratory of Degraded and Unused Land Consolidation Engineering, Ministry of Natural Resources, Xi’an, Shaanxi, 710075, China

4Shaanxi Provincial Land Consolidation Engineering Technology Research Center, Xi’an, Shaanxi, 710075, China

5Land Engineering Technology Innovation Center, Ministry of Natural Resources, Xi’an, Shaanxi, 710075, China

6Land Engineering Quality Testing of Shaanxi Land Engineering Construction Group Co, Ltd., Xi’an, Shaanxi, 710075, China

Abstract

Iron is an essential element for plant life activities, and is deeply involved in the material cycle of plant-water-soil. Therefore, it is necessary to understand the iron isotope behavior and fractionation law of iron in the cycle of plant-water-soil, to trace the migration and circulation of iron in the surface biosphere, and to trace the relationship between the biosphere where plants are located and the various plastids in nature. Issues such as interaction play an important role. This paper summarizes the representation methods and basic storage information of iron isotopes, and summarizes two different strategies for absorbing iron from soils and their characteristics of iron isotope fractionation. The results showed that when strategy I plants absorb iron, they will reduce ferric iron first, and absorb light iron isotopes preferentially; while strategy II plants absorb iron after chelating iron without obvious fractionation; some plants can have two iron isotopes at the same time. an absorption mechanism. Iron isotopes have great application potential in the research on the absorption mechanism of iron by plants, and may also have great prospects in future research scenarios such as iron transport in plants and iron distribution in tissues and organs.

Keywords

Iron isotopes, Plants, Strategy I, Strategy II

Cite This Paper

Bo Zhao. Research progress of iron isotopes in plants. Academic Journal of Environment & Earth Science (2022) Vol. 4 Issue 8: 7-12. https://doi.org/10.25236/AJEE.2022.040802.

References

[1] Beard, B.L., Johnson, C.M. High precision iron isotope measurements of terrestrial and lunar materials. Geochimica et Cosmochimica Acta, (1999) 63, 1653-1660.

[2] Wei, H.Z. Solar System Abundances of the Elements. Progress In Astronomy, (1991) 9, 13.

[3] Horvath, D.J. Availability of Manganese and Iron to Plants and Animals. Geological Society of America Bulletin, (1972).

[4] Beard, B.L., Johnson, C.M., Skulan, J.L., Nealson, K.H., Cox, L., Sun, H. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe. Chemical Geology, (2003) 195, 87-117.

[5] Dauphas, N., Craddock, P.R., Asimow, P.D., Bennett, V.C., Nutman, A.P., Ohnenstetter, D. Iron isotopes may reveal the redox conditions of mantle melting from Archean to Present. Earth & Planetary Science Letters, (2009) 288, 255-267.

[6] He, Y., Hu, D., Zhu, C. Progress of iron isotope geochemistry in geoscience. Earth Science Frontiers, (2015) 5, 54-71.

[7] Poitrasson, F. On the iron isotope homogeneity level of the continental crust. Chemical Geology, (2006) 235, 195-200.

[8] Tim, M., Conway, Seth, G., John. Quantification of dissolved iron sources to the North Atlantic Ocean. Nature, (2014).

[9] Jian, S., Xiangkun, Z., Shizhen, L. fe isotope biogeochemical and its application. ACTA GEOLOGICA SINICA, (2015) 89, 3.

[10] Morrissey, J., Guerinot, M.L. Iron Uptake and Transport in Plants: The Good, the Bad, and the Ionome. Chemical Reviews, (2009) 109, 4553-4567.

[11] Schwertmann, U. Solubility and dissolution of iron oxides. Springer Netherlands, (1991).

[12] Sun, A.K., Guerinot, M.L. Mining iron: iron uptake and transport in plants. FEBS Letters, (2007) 581, 2273-2280.

[13] Murad, E., Fischer, W.R. The Geobiochemical Cycle of Iron. Springer Netherlands, (1988).

[14] Robinson, Procter, Connolly. A ferric-chelate reductase for iron uptake from soils. Nature, (1999).

[15] Morth, J.P., Pedersen, B.P., Buch-Pedersen, M.J., Andersen, J.P., Vilsen, B., Palmgren, M.G., Nissen, P. A structural overview of the plasma membrane Na+,K+-ATPase and H+-ATPase ion pumps. Nat Rev Mol Cell Biol, (2011) 12, 60-70.

[16] Schagerlöf, U., Wilson, G., Hebert, H., Al-Karadaghi, S., Hägerhäll, C. Transmembrane topology of FRO2, a ferric chelate reductase from Arabidopsis thaliana. Plant molecular biology, (2006) 62, 215-221.

[17] Bashir, Inoue, Nagasaka, Takahashi, Nakanishi, Mori, Nishizawa. Cloning and characterization of deoxymugineic acid synthase genes in graminaceous plants. PLANT CELL PHYSIOL, (2006) 2006,47, S156-S156.

[18] Nozoye, T., Nagasaka, S., Kobayashi, T., Takahashi, M., Nishizawa, N.K. Phytosiderophore Efflux Transporters Are Crucial for Iron Acquisition in Graminaceous Plants. Journal of Biological Chemistry, (2011) 286, 5446.

[19] Curie, Catherine, Panaviene, Zivile, Loulergue, Clarisse, Dellaporta, Stephen, L., Briat. Maize yellow stripe1 encodes a membrane protein directly involved in Fe(III) uptake. Nature, (2001).

[20] Charlson, D.V., Shoemaker, R.C. Evolution of iron acquisition in higher plants. Journal of plant nutrition, (2006) 29.

[21] Ishimaru, Y., Kim, S., Tsukamoto, T., Oki, H., Kobayashi, T., Watanabe, S., Matsuhashi, S., Takahashi, M., Nakanishi, H., Mori, S. Mutational reconstructed ferric chelate reductase confers enhanced tolerance in rice to iron deficiency in calcareous soil. Proceedings of the National Academy of Sciences of the United States of America, (2007) 104, p.7373-7378.

[22] Guelke, M., Von Blanckenburg, F. Fractionation of stable iron isotopes in higher plants. Environmental science & technology, (2007) 41, 1896-1901.

[23] Guelke-Stelling, M., Von Blanckenburg, F. Fe isotope fractionation caused by translocation of iron during growth of bean and oat as models of strategy I and II plants. Plant and soil, (2012) 352, 217-231.

[24] Von Blanckenburg, F., Von Wirén, N., Guelke, M., Weiss, D.J., Bullen, T.D. Fractionation of metal stable isotopes by higher plants. Elements, (2009) 5, 375-380.

[25] Kiczka, Wiederhold, Jg, Kraemer, Sm, Bourdon, Kretzschmar. Iron Isotope Fractionation during Fe Uptake and Translocation in Alpine Plants RID A-3303-2008. Environ Sci Technol, (2010).

[26] Johnson, C.M., Beard, B.L., Roden, E.E. The iron isotope fingerprints of redox and biogeochemical cycling in modern and ancient Earth. Annu. Rev. Earth Planet. Sci., (2008) 36, 457-493.

[27] Inoue, H., Kobayashi, T., Nozoye, T., Takahashi, M., Kakei, Y., Suzuki, K., Nakazono, M., Nakanishi, H., Mori, S., Nishizawa, N.K. Rice OsYSL15 is an iron-regulated iron(III)-deoxymugineic acid transporter expressed in the roots and is essential for iron uptake in early growth of the seedlings. Journal of Biological Chemistry, (2009) 284, 3470-3479.

[28] Garnier, J., Garnier, J., Vieira, C., Akerman, A., Chmeleff, J., Ruiz, R., Poitrasson, F. Iron isotope fingerprints of redox and biogeochemical cycling in the soil-water-rice plant system of a paddy field. Science of The Total Environment, (2017) 574, 1622-1632.

[29] Michael J, E. Iron stable isotopes track pelagic iron cycling during a subtropical phytoplankton bloom. Proceedings of the National Academy of Sciences of the United States of America, (2015) 112, E15-20.

[30] Sun, R., Wang, B. Iron isotope fractionation during uptake of ferrous ion by phytoplankton. Chemical Geology, (2018).