Schreibersite is generally a rare iron nickel phosphide mineral, (Fe,Ni)3P, though common in iron-nickel meteorites. It has been found on Disko Island in Greenland[5] and Illinois.[6][7]

CategoryPhosphide mineral
Meteorite mineral
(repeating unit)
IMA symbolScb[1]
Strunz classification1.BD.05
Dana classification01.01.21.02
Crystal systemTetragonal
Crystal classDisphenoidal (4)
H-M symbol: (4)
Space groupI4
ColorSilver-white to tin-white, tarnishes brass-yellow or brown
Crystal habitRarely in crystals, hoppered, plates, tablets, rods or needles
Cleavage{001} perfect, {010} indistinct, {110} indistinct
TenacityVery brittle
Mohs scale hardness6.5–7
LusterBrilliant metallic
StreakDark gray
Specific gravity7.0–7.3
Optical propertiesUniaxial

Another name used for the mineral is rhabdite. It forms tetragonal crystals with perfect 001 cleavage. Its color ranges from bronze to brass yellow to silver white. It has a density of 7.5 and a hardness of 6.5 – 7. It is opaque with a metallic luster and a dark gray streak. It was named after the Austrian scientist Carl Franz Anton Ritter von Schreibers (1775–1852), who was one of the first to describe it from iron meteorites.[3]

Schreibersite is reported from the Magura Meteorite, Arva-(present name – Orava), Slovak Republic; the Sikhote-Alin Meteorite in eastern Russia; the São Julião de Moreira Meteorite, Viana do Castelo, Portugal; the Gebel Kamil (meteorite) in Egypt; and numerous other locations including the Moon.[8]

In 2007, researchers reported that schreibersite and other meteoric phosphorus bearing minerals may be the ultimate source for the phosphorus that is so important for life on Earth.[9][10][11] In 2013, researchers reported that they had successfully produced pyrophosphite, a possible precursor to pyrophosphate, the molecule associated with ATP, a co-enzyme central to energy metabolism in all life on Earth. Their experiment consisted of subjecting a sample of schreibersite to a warm, acidic environment typically found in association with volcanic activity, activity that was far more common on the primordial Earth. They hypothesized that their experiment might represent what they termed "chemical life", a stage of evolution which may have led to the emergence of fully biological life as exists today.[12]

In 1986 researchers found lightning can create schreibersite[13] and may have been the source of phosphorus for early life.[14][6][7]

See alsoEdit


  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85: 291–320.
  2. ^ Schreibersite. Mindat.
  3. ^ a b Schreibersite. Webmineral
  4. ^ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C., eds. (2000). "Schreibersite" (PDF). Handbook of Mineralogy. Vol. IV (Arsenates, Phosphates, Vanadates). Chantilly, VA, US: Mineralogical Society of America. ISBN 978-0962209727.
  5. ^ "Power behind primordial soup discovered", Eurekalert, April 4, 2013
  6. ^ a b Hess, Benjamin L.; Piazolo, Sandra; Harvey, Jason (2021-03-16). "Lightning strikes as a major facilitator of prebiotic phosphorus reduction on early Earth". Nature Communications. 12 (1): 1535. Bibcode:2021NatCo..12.1535H. doi:10.1038/s41467-021-21849-2. PMC 7966383. PMID 33727565.
  7. ^ a b Temming, Maria (2021-04-10). "Phosphorus for Earth's earliest life may have been forged by lightning". Science News. Retrieved 2021-04-02.
  8. ^ Hunter R. H.; Taylor L. A. (1982). "Rust and schreibersite in Apollo 16 highland rocks – Manifestations of volatile-element mobility". Lunar and Planetary Science Conference, 12th, Houston, TX, March 16–20, 1981, Proceedings. Section 1. (A82-31677 15–91). New York and Oxford: Pergamon Press. pp. 253–259. Bibcode:1982LPSC...12..253H.
  9. ^ Report of U of A Extra-terrestrial Phosphorus
  10. ^ "5.2.3. The Origin of Phosphorus". The Limits of Organic Life in Planetary Systems. National Academies Press. 2007. p. 56. doi:10.17226/11919. ISBN 978-0309104845.
  11. ^ Sasso, Anne (January 3, 2005) Life's Fifth Element Came From Meteors. Discover Magazine.
  12. ^ Bryant, D. E.; Greenfield, D.; Walshaw, R. D.; Johnson, B. R. G.; Herschy, B.; Smith, C.; Pasek, M. A.; Telford, R.; Scowen, I.; Munshi, T.; Edwards, H. G. M.; Cousins, C. R.; Crawford, I. A.; Kee, T. P. (2013). "Hydrothermal modification of the Sikhote-Alin iron meteorite under low pH geothermal environments. A plausibly prebiotic route to activated phosphorus on the early Earth". Geochimica et Cosmochimica Acta. 109: 90–112. Bibcode:2013GeCoA.109...90B. doi:10.1016/j.gca.2012.12.043.
  13. ^ Essene, E. J.; Fisher, D. C. (1986-10-10). "Lightning Strike Fusion: Extreme Reduction and Metal-Silicate Liquid Immiscibility". Science. 234 (4773): 189–193. Bibcode:1986Sci...234..189E. doi:10.1126/science.234.4773.189. PMID 17746479. S2CID 37215332. Retrieved 2021-04-02.
  14. ^ Pasek, Matthew; Block, Kristin (2009-07-13). "Lightning-induced reduction of phosphorus oxidation state". Nature Geoscience. 2 (8): 553–556. Bibcode:2009NatGe...2..553P. doi:10.1038/ngeo580. Retrieved 2021-04-02.