In August researchers at the University of Arizona found an answer: Schreibersite, an iron - nickel phosphide that occurs
in iron meteorites, could have provided all the phosphorus needed.
Not exact matches
The amount of nickel - 60 found
in meteorite samples — particularly
in comparison to the amount of stable, «ordinary»
iron - 56 — can indicate how much
iron - 60 was present when the larger parent body from which the
meteorite broke off was formed.
Tiny pockets of sulfur and
iron (yellow) inside a diamond (blue) inside a
meteorite suggest the
meteorite was once part of a long - lost planet
in the early solar system.
Iron - nickel alloys are ubiquitous: they are found at the earth's core and
in meteorites.
SCRAPS of
iron found scattered around what became known as Meteor Crater
in Arizona convinced geologist Daniel Barringer that a huge
iron meteorite lay buried there.
It turned out that the rock had an elevated manganese - to -
iron ratio — higher than that
in Earth rocks and consistent with other martian
meteorites.
«
Iron meteorites would bring that
in very nicely,» he theorizes.
Many
meteorites contain high levels of metallic
iron, so if one falls
in a humid jungle climate, the combination of moisture and oxygen will corrode it.
Further studies at the site uncovered 74 fragments of the original
iron meteorite, the researchers report
in this month's issue of Geology.
The majority of this 6 inch
meteorite consists of
iron - nickel metal, and the darker - colored structure
in the center is schreibersite.
Geologist Matthew Pasek of the University of Arizona
in Tucson, who previously studied the possibility that early life used phosphorus from
iron meteorites, knew that cloud - to - ground lightning was one of the few natural phenomena that could produce enough energy to create phosphite.
«Having looked at some of the published trace element data for this artefact, it looks pretty convincing to me that this is very likely originated from Chinga
iron meteorite,» says Meenakshi Wadhwa, director of the Center for Meteorite Studies at Arizona State University
meteorite,» says Meenakshi Wadhwa, director of the Center for
Meteorite Studies at Arizona State University
Meteorite Studies at Arizona State University
in Tempe.
A weapon as legendary as the dagger of King Tutankhamun needs an epic backstory, and last year X-ray analysis showed that the
iron in the blade came from
meteorites.
A form of magnetite (
iron oxide) was detected
in the
meteorite that, on Earth, is produced only within the bodies of certain bacteria.
The signatures of pyroxene, an
iron - and magnesium - rich mineral,
in these
meteorites have been found to match those of rocks observed on Vesta's surface.
Dorothy Cross, Table Telescope, 2016, cast
iron table, antique brass telescope, gilded human skull,
meteorite, table 49 x 28 cm / 19.3 x 11
in, telescope 5 cm x 26/91 cm / 2
in x 1059.4
in
The main result of this research, is that the variations of the flux, as predicted from the galactic model and as observed from the
Iron meteorites is
in sync with the occurrence of ice - age epochs on Earth.
The so - called «Galactic Cosmic Rays» probably come directly from the Sun's pulsar core, and were recorded as a gradient
in cosmic ray exposures of
meteorites at the birth of the solar system:
iron meteorites > stone
meteorites > carbonaceous chondrites
Researchers have found that an
iron - containing mineral called dusty olivine, present
in meteorites, retains a record of the magnetic field from the early solar system around 4.6 billion years ago.