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Noted Astronomer Found Artificial Pieces of an Interstellar Meteor

By Monica Grady Professor of Planetary and Space Sciences, The Open University

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Avi Loeb, a physicist from Harvard University in the US, has recovered 50 tiny spherical iron fragments from the bottom of the Pacific Ocean that he claims may be material from an interstellar alien spaceship.

Loeb is linking his finding with the passage of a fireball in January 2014. The meteor was observed by sensors of the US Department of Defense that track all objects entering the Earth’s atmosphere. It was recorded as travelling faster than most meteors and eventually broke up over the South Pacific Ocean near Papua New Guinea.
Data on the object is held by Nasa’s Center for Near Earth Object Studies (CNEOS). The meteor’s official name is CNEOS 20140108, and is also referred to as IM1 (for interstellar meteor).
We have already had at least one visitor from interstellar space – the comet ‘Oumuamua. The appearance of 1I/2017U1, the official name for ‘Oumuamua, was certainly an unusual event. The object was observed in 2017 as it was leaving the Solar System. Its trajectory is different from the near-circular orbits of the planets and elliptical orbits of comets.
The comet’s path was traced back, with scientists discovering that it had come from well beyond the outermost fringes of the Solar System. Scientists were excited but also intrigued – although its shape was not captured on camera, the way that light reflected from it as it rotated suggested that it had an odd shape like a cigar when viewed side-on or a plate when viewed from the top.
In a thoughtful article written in 2018, Loeb speculated that ‘Oumuamua might be artificial, rather than natural in origin – the product of an alien civilization. He suggested that we should keep searching for interstellar debris in the Solar System.
In pursuit of such debris, Loeb’s team interrogated the CNEOS database, looking for objects with unusual orbital characteristics. That’s when they found CNEOS 20140108 and, based on its high velocity, suggested it was an interstellar meteor – giving it the more manageable name of IM1.
Modeling the path of the fireball, Loeb identified a specific area of the South Pacific where he believed debris from IM1 would be deposited. Following a dredging operation in the area with a powerful magnet, he now claims to have found material from IM1.
But what are the chances that he has found genuine interstellar debris at all, never mind a spaceship?
The metallic spherules that have been recovered are each about half a millimeter in diameter. It isn’t impossible for them to be of extraterrestrial origin: several previous expeditions have recovered spherules from space from the seabed.
The first expedition to find such samples was HMS Challenger in 1872-76. Material dredged from the ocean floor contained many metallic droplets, described at the time, quite accurately, as “cosmic spherules”. Droplets from space are spherical because they solidify from molten material torn from the surface of meteorites as they traverse the atmosphere.
Subsequent expeditions throughout the 20th century have also found cosmic spherules at the bottom of the ocean, but it has become harder to identify them. This is because, in the 150 years since the Challenger expedition, the amount of pollution has increased on Earth.
In 1872, the industrial revolution was in its infancy in Europe and practically non-existent in the southern hemisphere. Hence pollution such as “fly ash” (waste from burning coal) and particles from vehicles was minimal. Many of these pollutants are also spherical in appearance and metallic in composition.
Today, products from industrial processes and vehicles are everywhere. So, without an actual analysis of the composition of the spherules and a comparison with analyses of meteorites (and common terrestrial pollutants), it is not possible to identify any as extraterrestrial.
But Loeb doesn’t just think the material is from space, he thinks it is from interstellar space – arguing “this could be the first time humans put their hands on interstellar material”.
This is simply not true. We have an abundance of interstellar material on Earth. Some of it is almost certainly on the ocean floor, but not in the form collected by Loeb.
The interstellar material to which I am referring comes in several different varieties. It is well known by astronomers that the interstellar medium – the space between stars – is not empty, but contains several different molecules, many of which are organic (made up of chains or rings of carbon). A portion of these molecules got mixed into the region of space where the Solar System was starting to form.
Stars themselves have also contributed material to the interstellar medium, as they evolved or exploded as supernovas. Some of this material comes as tiny diamonds or sapphires – rare mementoes of stars that lived and died before the Sun was born. These grains became part of the dust cloud that collapsed to form the Solar System, and were eventually carried to Earth in meteorites.
Loeb’s evidence for an extraterrestrial source for the material – never mind an interstellar origin – is rather shaky. He has found metallic spherules. For me (and many others) to accept that these spherules are extraterrestrial, I’d need firm analytical evidence. What is their composition? What is their age? Can we rule out terrestrial pollutants? Can we rule out debris from extraterrestrial material from within the Solar System?
The first question, about composition, has been answered: analysis of the spherules shows them to be mainly iron with a few trace metals.
We know meteors from our Solar System contain iron and nickel, echoing the relative abundances of these metals in the Sun. But the spherules apparently contain “negligible” amounts of nickel – thus indicating that they are almost certainly not from meteors within the Solar System. This does not, however, prove they are interstellar – it merely makes it more likely that they’re terrestrial pollutants.
The most convincing evidence would be to measure an age for the spherules greater than that of the Sun – which would identify them as interstellar.
And that would be amazing, but it would not necessarily identify them as having an artificial, rather than natural origin. I am not sure what evidence would be sufficiently convincing for this – maybe the autograph of the alien engineer who built the spacecraft?

s synchrotron X-ray scanning tunneling microscopy or SX-STM. X-ray spectroscopy in SX-STM is triggered by photoabsorption of core level electrons, which constitutes elemental fingerprints and is effective in identifying the elemental type of the materials directly.

AR #122

MEGA Engineering In The Stars

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First X-ray Taken of a Single Atom

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Since its discovery by Roentgen in 1895, X-rays have been used everywhere, from medical examinations to security screenings in airports. Even Curiosity, NASA’s Mars rover, is equipped with an X-ray device to examine the materials composition of the rocks in Mars. An important usage of X-rays in science is to identify the type of materials in a sample. Over the years, the quantity of materials in a sample required for X-ray detection has been greatly reduced thanks to the development of synchrotron X-rays sources and new instruments. To date, the smallest amount one can X-ray a sample is in attogram, that is about 10,000 atoms or more. This is due to the X-ray signal produced by an atom being extremely weak so that the conventional X-ray detectors cannot be used to detect it. According to Hla, it is a long-standing dream of scientists to X-ray just one atom, which is now being realized by the research team led by him.

“Atoms can be routinely imaged with scanning probe microscopes, but without X-rays one cannot tell what they are made of. We can now detect exactly the type of a particular atom, one atom-at-a-time,  and can simultaneously measure its chemical state,” explained Hla, who is also the director of the Nanoscale and Quantum Phenomena Institute at Ohio University. “Once we are able to do that, we can trace the materials down to ultimate limit of just one atom. This will have a great impact on environmental and medical sciences and maybe even find a cure that can have a huge impact for humankind. This discovery will transform the world.”
Their paper, published in the scientific journal Nature (https://www.nature.com/articles/s41586-023-06011-w) on May 31, 2023, and gracing the cover of the print version of the scientific journal on June 1, 2023, details how Hla and several other physicists and chemists, including Ph.D. students at OHIO, used a purpose-built synchrotron X-ray instrument at the XTIP beamline of Advanced Photon Source and the Center for Nanoscale Materials at Argonne National Laboratory.
For demonstration, the team chose an iron atom and a terbium atom, both inserted in respective molecular hosts. To detect X-ray signal of one atom, the research team supplemented conventional detectors in X-rays with a specialized detector made of a sharp metal tip positioned at extreme proximity to the sample to collect X-ray excited electrons – a technique known as synchrotron X-ray scanning tunneling microscopy or SX-STM. X-ray spectroscopy in SX-STM is triggered by photoabsorption of core level electrons, which constitutes elemental fingerprints and is effective in identifying the elemental type of the materials directly.

AR #64

Power from the Night Side

by Susan Martinez

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X Ray Show Turin Shroud 2000 Years Old

The Shroud of Turin is arguably the most important relic of Christianity. According to tradition, it is the sepulchral sheet that would have wrapped the body of Jesus after the crucifixion. In 1988 the carbon 14 dating of some samples taken from the Shroud, carried out by three distinct laboratories, indicated that it should have only about 7 centuries of history, all in Europe. Therefore, the sheet would be inauthentic since, apparently, it dates back only to the Middle Ages. Now, in a new peer-reviewed study “X-ray Dating of a Turin Shroud’s Linen Sample” published in March 2022, by MDPI Heritage (https://www.mdpi.com/2571-9408/5/2/47), Italian scientist Liberato De Caro has reported that fabric tests show the Shroud is indeed 2,000 years old. De Caro and his colleagues made the discovery by utilizing a technique called “Wide-Angle X-ray Scattering” (WAXS). With such an analysis, it is possible, they say, to evaluate the structural degradation due to natural aging of the cellulose that makes up the fibers of the linen threads.


Textile samples, says the study, are especially vulnerable to contamination of all kinds, which are not always possible to control and to completely remove from the artifact to be dated. Molds and bacteria, colonizing textile fibers, and dirt or carbon-containing minerals, such as limestone, in the empty spaces between fibers represent about 50% of the volume, that at a microscopic level, can be difficult to completely eliminate in the sample cleaning phase. All of that can distort the dating. In fact, the fabric can include new carbon 14, assimilated through epochs subsequent to the one in which the textile originated. Textile samples indeed are the most at risk of contamination for radio dating, and are difficult to eliminate, since the surface per unit of weight exposed to the interaction with the outside is very high, due to the small diameter of the microfibers (10-20 micrometers) and the high number of microfibers per thread (about 200). About half the volume of a natural fiber yarn is actually empty, interstitial space, filled with air or anything else, between the fibers that compose it. Everything that enters the fibers must be carefully removed. If this does not happen, carbon 14 dating is not reliable.


It cannot be ruled out that such a thing could have happened in the 1988 study, a fact confirmed by the fact that moving from the periphery towards the center of the sheet, along the longer side, there is a significant increase in carbon 14. In this way, it is possible to date with X-ray analysis the ancient tissues from which the samples were taken. Starting from the results obtained in the 1988 study, on comparative samples taken from linen fabrics of varying age between 3000 BC and 2000 AD, it was possible to date a sample of the Shroud thread. According to the De Caro study, the Shroud sample analyzed consists of a wire taken near the 1988 / radiocarbon area (angle corresponding to the foot area of the frontal image, near the so-called Raes sample). The size of the linen sample analyzed is approximately 0.5 mm × 1 mm. The integrated WAXS data profiles, obtained on the Shroud sample (orange curve in the figure), are compatible with the similar measurements obtained on a linen sample whose dating, according to historical documents, is 55-74 AD, siege of Masada, Israel (green curve in the figure). The degree of natural aging of the cellulose that constitutes the linen of the investigated sample, obtained by X-ray analysis, showed that the Shroud fabric is much older than the 7 centuries proposed by the radiocarbon dating of 1988.

 

AR #126

“Shroud of Turin”
by William B. Stoecker