Showing posts with label Comets. Show all posts
Showing posts with label Comets. Show all posts

Sunday, February 2, 2020

                 The vehicles of life


In addition to the stars and planets, the Universe is populated by countless of small planetary bodies and tiny asteroids that act as vehicles of life in space and time.
They are often found far from suns and stars, drifting in the enormous cold and dark distances. 
The smallest, which are the vast majority, remain frozen by hundreds of millions of years without anything disturbing its long sidereal winter.
Others, the largest, have enough mass to generate some heat from their minerals and radioactive compounds.
In these celestial bodies the inner ice can melt forming luke warm  underground seas or lakes. 
These are probably the most common scenarios of the life in the cosmos.
Small bacteria and other hard-to-imagine organisms, survive, they 
reproduce and evolve in these environments, using the limited but lasting
available energy 
The Solar System contains millions, perhaps billions of these bodies. A large amount is far from the Sun, beyond the orbits of Uranus and Neptune. Some are closer to the center, in warmer regions, and occasionally  they get so close to the main star that their ice can vaporize and be ejected in the form of gas and dust.
These small bodies, which are often shown spectacularly in the night skies are called "comets." Some astronomers, increasingly, think that comets and their relatives the dark and cold distances are carriers of life forms whose characteristics
They are hard to imagine. Maybe some of them behave  themselves like true organisms with their "metabolism" and unique life history.
According to Chandra Wickramansinghe, Fred Hoyle and other researchers, life has been a common phenomenon in the Universe for a long time, almost since the beginning (if there were beginnings), spreading through the space embarked on the tiny comets.
Thus the first organisms in the remote origins probably arrived on Earth, several billion years ago. They continued to arrive since the, bringing new genetic contributions throughout the entire geological history of the planet.
Large and small icy blocks bombarded the atmosphere by enriching it with water and other light compounds and elements (nitrogen, methane, carbon dioxide, etc.).
That way, gradually, the original seas formed, the cracks in the crust were filled with water and the mixture of gases became ¡what we call "air" became.
To this atmosphere the gases emanating from the planetary interioralso contributed in a process of degasification that still continues. These gaseous emissions were mainly nitrogen and methane. Nitrogen is still present mostly in the atmosphere, and methane underwent oxidation processes enriching the surface of carbon dioxide and water.
From the book "Peoples, drugs and serpents", D. Antón, Piriguazú Ediciones

Saturday, December 1, 2018



Comets, messengers of life


Comets are icy, Solar System bodies, generally with diameters of a few kilometers (1 to 30 kms) which, when passing close to the Sun, warm and release gases, a process called outgassing.
This produces a visible atmosphere or coma, and sometimes also a tail. These phenomena are due to the effects of solar radiation and the solar wind acting upon the nucleus of the comet. Comet nuclei range from a few hundred metres to tens of kilometres across and are composed of loose collections of ice, dust, and small rocky particles. The coma may be up to 15 times the Earth's diameter, while the tail may stretch one astronomical unit. If sufficiently bright, a comet may be seen from the Earth without the aid of a telescope and may subtend an arc of 30° (60 Moons) across the sky. Comets have been observed and recorded since ancient times by many cultures.
As of July 2018 there are 6,339 known comets, a number that is steadily increasing as they are discovered. However, this represents only a tiny fraction of the total potential comet population, as the reservoir of comet-like bodies in the outer Solar System (in the Oort cloud) is estimated to be one trillion (1,000,000,000,000).
The outer surfaces of cometary nuclei have a very low albedo, making them among the least reflective objects found in the Solar System. 

Comet nuclei with radii of up to 30 kilometres (19 mi) have been observed, but ascertaining their exact size is difficult.
The nucleus of the comet 322P/SOHO is probably only 100–200 metres (330–660 ft) in diameter. A lack of smaller comets being detected despite the increased sensitivity of instruments has led some to suggest that there is a real lack of comets smaller than 100 metres (330 ft) across.[27] Known comets have been estimated to have an average density of 0.6 g/cm3 (0.35 oz/cu in).[28] Because of their low mass, comet nuclei do not  become spherical under their own gravity and therefore have irregular shapes.

The objection that life can't survive in space needs examination. A serious problem for Svante Arrhenius's theory in 1908 was that spores in empty space would be subject to radiation damage, especially in the vicinity of a star. In 1978, Hoyle and Wickramasinghe observe in Lifecloud that if a cloud of bacterial matter were dense enough, the inner contents would be protected from radiation by the outer layers. Other scientists have recently observed that a coating of dust only half a micrometer thick would adequately protect a bacterium from ultraviolet radiation in space.
Hoyle and Wickramasinghe also discuss another means of space travel which solves the radiation problem: comets. And even before that danger was known, the idea that comets could contribute to life on Earth was afoot. Among others, Isaac Newton endorsed it. "Newton considered the continual arrival of cometary material to be essential for life on Earth".
Comets, as astronomer Fred Whipple figured out, are made largely of ice. Much of the ice in comets is frozen water, but ices of other compounds such as carbon monoxide and carbon dioxide are also present. And comets contain, we have recently learned, a large amount of more complex organic compounds. These organic compounds may be limited to a mixture of molecules such as the original Miller - Urey experiment was able to produce, or they may be even more closely related to life; we can't be sure from here, yet. In the interior of a comet, under layers of opaque organic material, viable cells would be shielded from radiation. Of course, freezing slows or stops metabolism, so cells could exist there in suspended animation.
A few larger comets such as Halley's comet have orbits that bring them as close to the sun as Earth is. Even fewer comets, called "sungrazers," actually strike the sun, or pass so close that they are destroyed by it. Most comets reside at distances far beyond that of Pluto, in orbits not confined to the plane in which the planets' orbits lie. They are so numerous that the total mass of comets in solar orbit may be as great as the total mass of the planets. Slight gravitational disturbances caused by the outer planets or neighboring stars can change a comet's orbit completely, steering some closer to the sun, others completely away.
When a comet nears the sun, some of its surface material ablates away, making the comet's "tail." This process usually begins somewhere between the orbits of Jupiter and Mars. Some of the discharged material is gas, some of it is dust. Each makes a different kind of cometary tail. Dust and larger debris left by comets remain for a while in solar orbit. Earth often passes through the orbits of cometary debris, causing meteor showers such as the Perseid meteor shower around August 10 every year, when we cross the orbit of comet Swift-Tuttle.
References.
panspermia.org and wikipedia

Wednesday, August 8, 2018


The best well known comet: 67P/Churyumov-Gerasimenko


If you regard comets as big old dirty snowballs, boringly uniform and featureless, this photo will set you straight. 
A newly released image, which was captured in February 2016 by the European Space Agency's (ESA) Rosetta spacecraft and was processed by amateur astronomer Stuart Atkinson, reveals Comet 67P/Churyumov-Gerasimenko as a little world unto itself, with an eye-catching diversity of exotic terrain.
"It shows the uneven, shadowed surface of the comet in detail; particularly prominent just to the right of center is an upright feature surrounded by scattered depressions, rocky outcrops and debris," ESA officials wrote in an image description Monday (Aug. 6).
The image of Comet 67P/Churyumov-Gerasimenko was captured by the European Space Agency's (ESA) Rosetta spacecraft on Feb. 10, 2016, and was processed by amateur astronomer Stuart Atkinson. ESA released the photo on Aug. 6, 2018.
As it happens with many comets, 67P/Churyumov-Gerasimenko is a dark body with a large proportion of carbon compounds, in addition to ice.  Vapour and dust jets appeared from different zones of the body surface
The image show precisely, that a relatively dark landscape with many cavities that are probably formed as a result of losses of mass and chunks of rocks slowly falling after been ejected.
67P/Churyumov–Gerasimenko (abbreviated as 67P or 67P/C-G) is a Jupiter-family comet. originally from the Kuiper belt with a current orbital of 6.45 years,  a rotation period of approximately 12.4 hours and a maximum velocity of 135,000 km/h (38 km/s; 84,000 mph).
Churyumov–Gerasimenko is approximately 4.3 by 4.1 km (2.7 by 2.5 mi) at its lonst and widest dimensions. It was first observed on photographic plates in 1969 by Soviet agestronomers Kim Ivanocych Churyumov and Svetlana Ivanovna Gerasimenko after whom it was named. It came to perihelion (closest approach to the Sun) on 13 August 2015.


 The best well known comet: 67P/Churyumov-Gerasimenko


If you regard comets as big old dirty snowballs, boringly uniform and featureless, this photo will set you straight. 
A newly released image, which was captured in February 2016 by the European Space Agency's (ESA) Rosetta spacecraft and was processed by amateur astronomer Stuart Atkinson, reveals Comet 67P/Churyumov-Gerasimenko as a little world unto itself, with an eye-catching diversity of exotic terrain.
"It shows the uneven, shadowed surface of the comet in detail; particularly prominent just to the right of center is an upright feature surrounded by scattered depressions, rocky outcrops and debris," ESA officials wrote in an image description Monday (Aug. 6).
The image of Comet 67P/Churyumov-Gerasimenko was captured by the European Space Agency's (ESA) Rosetta spacecraft on Feb. 10, 2016, and was processed by amateur astronomer Stuart Atkinson. ESA released the photo on Aug. 6, 2018.
As it happens with many comets, 67P/Churyumov-Gerasimenko is a dark body with a large proportion of carbon compounds, in addition to ice.  Vapour and dust jets appeared from different zones of the body surface
The image show precisely, that a relatively dark landscape with many cavities that are probably formed as a result of losses of mass and chunks of rocks slowly falling after been ejected.
67P/Churyumov–Gerasimenko (abbreviated as 67P or 67P/C-G) is a Jupiter-family comet. originally from the Kuiper belt with a current orbital of 6.45 years,  a rotation period of approximately 12.4 hours and a maximum velocity of 135,000 km/h (38 km/s; 84,000 mph).
Churyumov–Gerasimenko is approximately 4.3 by 4.1 km (2.7 by 2.5 mi) at its longest and widest dimensions. It was first observed on photographic plates in 1969 by Soviet astronomers Kim Ivanocych Churyumov and Svetlana Ivanovna Gerasimenko after whom it was named. It came to perihelion (closest approach to the Sun) on 13 August 2015.
From:
https://www.space.com/41415-rosetta-comet-67p-landscape-photo.html

Tuesday, August 7, 2018


Comets, life delivery cosmic systems
Comets are like cats. They have tails, and they do precisely what they want — David Levyç+

Comets, as astronomer Fred Whipple figured out, are made largely of ice. Much of the ice in comets is frozen water, but ices of other compounds such as carbon monoxide and carbon dioxide are also present. And comets contain, we have recently learned, a large amount of more complex organic compounds. These organic compounds may be limited to a mixture of molecules such as the original Miller - Urey experiment was able to produce, or they may be even more closely related to life; we can't be sure from here, yet. In the interior of a comet, under layers of opaque organic material, viable cells would be shielded from radiation. Of course, freezing slows or stops metabolism, so cells could exist there in suspended animation.
A few larger comets such as Halley's comet have orbits that bring them as close to the sun as Earth is. Even fewer comets, called "sungrazers," actually strike the sun, or pass so close that they are destroyed by it. Most comets reside at distances far beyond that of Pluto, in orbits not confined to the plane in which the planets' orbits lie. They are so numerous that the total mass of comets in solar orbit may be as great as the total mass of the planets. Slight gravitational disturbances caused by the outer planets or neighboring stars can change a comet's orbit completely, steering some closer to the sun, others completely away.
When a comet nears the sun, some of its surface material ablates away, making the comet's "tail." This process usually begins somewhere between the orbits of Jupiter and Mars. Some of the discharged material is gas, some of it is dust. Each makes a different kind of cometary tail. Dust and larger debris left by comets remain for a while in solar orbit. Earth often passes through the orbits of cometary debris, causing meteor showers such as the Perseid meteor shower around August 10 every year, when we cross the orbit of comet Swift-Tuttle.
Thousands of tons of cometary dust, debris and larger fragments fall to Earth every year. Starting in the late 1960's, U.S. military intelligence observers doing surveillance against enemy missile attacks began to observe and photograph comets and other objects as big as thirty to fifty meters in diameter exploding in the upper atmosphere. From 1975 to 1992, 136 such objects were observed — about eight per year. That information was kept classified until 1993-1994 (5.5). It's worth remembering that four billion years ago, when life on Earth first appeared, the number of comets nearing the sun was hundreds or thousands of times greater than it is now (6).
The study of comets today is rich with surprises. For example, comet Hyakutake, which was easily visible to the naked eye in March, 1996, was first discovered by a Japanese amateur astronomer using binoculars. Astronomers were surprised to learn "Hyakutake contains abundant ethane and methane, compounds never before confirmed in comets" (7-9). On March 27, 1997, NASA announced that a year-long study using Hubble and several Earth-based telescopes shows that the trace ices in the nucleus of comet Hale-Bopp are somehow segregated from water-ice. And on April 21, 1997, astronomers on the Canary Islands reported that Hale-Bopp has a third tail of a kind not seen before; it is composed of sodium gas (11). Following so many new findings, comet theorists are completely rethinking how comets are formed and what they contain. Perhaps in the process they should consider biological causes for some of the unexpected phenomena. For example, on Earth, ethane comes from methane, and methane is made from carbon dioxide by bacteria. This process could happen on comets as well.
Comets Reaching Earth
Many objects that fall into Earth's atmosphere from space are destroyed by heat before they reach Earth's surface. Only the very largest objects have enough momentum to penetrate the atmosphere without slowing down much. The largest comets are in this category. Imagine the fate of living cells deeply embedded in the ice of a large comet. The high heat requirement to melt ice, and water's extremely high heat of vaporization could offer some protection to the cells during a fast trip through the atmosphere. And landing in the ocean would soften the impact. Still, the heat generated by such explosions can be enormous.
Christopher Chyba, Paul Thomas, Leigh Brookshaw and Carl Sagan wrote a study of this problem, published in Science in 1990, entitled "Cometary Delivery of Organic Molecules to the Early Earth"  They carefully calculate the heat generated by high speed impacts with Earth, and then conclude that life's building blocks (not whole cells) could arrive intact. It is reasonable to extend their conclusion to cells, by expanding the scope of their study. Chyba and his coauthors in 1990 admittedly do not examine the case of a comet exploding before impact. However most comets, indeed most large meteoroids of any type except iron ones, would explode before impact. In 1992 Chyba and Sagan did address the explosion of comets in the atmosphere and found that for the delivery of intact organic compounds at least, this method of transfer was far more effective than comets that collide with the surface.
The best known atmospheric explosion of a meteoroid happened eight kilometers above Tunguska in central Siberia on June 30, 1908. The explosion flattened the forest for roughly 15 kilometers in every direction. The object was most likely an asteroid, perhaps 60 meters in diameter, because a comet would have exploded higher in the atmosphere. Our knowledge of this event is indirect because no one investigated the site until twenty years after the explosion. A similar atmospheric explosion, again over Siberia, occurred in 1947. We know that atmospheric explosions before impact by comets and asteroids are common. An explosion in the air would be much gentler than a collision with either Earth's hard surface or the ocean. Matter on the trailing side of a comet exploding in the atmosphere would be significantly slowed by the jolt. And matter located there would also be the best protected from the heat generated during atmospheric entry prior to the explosion.
In March 1965, an object estimated at 7 - 8 meters in diameter exploded 30 kilometers over Revelstoke, Canada. This time investigators arrived promptly and recovered many fragments a few millimeters in size. Most of these were not altered by heat, proving that a plausible delivery mechanism for cells exists .
In a new development, on May 28, 1997, NASA announced observations that comets as large as houses — "thousands per day" — actually break up and are destroyed at 600 to 15,000 miles above Earth. Dr. Lewis A. Frank, the principal investigator for NASA's Polar spacecraft instruments, described their descent as a "relatively gentle 'cosmic rain'." 
Reproduced from
http://www.panspermia.org/comets.htm

Sunday, July 1, 2018


Life in all star systems and outside them

In several articles that I uploaded in fbook and my blog daniloanton-en.blogspot.com I argued, based on the theoretical approaches of Thomas Gold and Fred Hoyle, that life is possible in all celestial bodies with temperatures below 100-200 degrees Celsius . When the surface temperatures of planets, satellites, asteroids and comets, are very cold (for example, below 50-100 degrees centigrade), the internal heat can melt the ice, generating accumulations of groundwater that would allow the existence of live organisms.
Liquid wáter es necessary In order for life to be possible.
This applies to the solar system and all other analogous star systems and to the independent planetary celestial bodies (rogué planets) which are not part of any star system.
That is, there would be trillions of planets (may be in all evolved galaxies) that could potentially harbor living organisms inside them.
In Mars, for example, there could be living underground organisms at depths of the order of a few hundred meter or less  (where the conditions for liquid water are given). In the Moon, on Ganymede, Europe (satellites of Jupiter), Titan. Triton (satellite of Neptune), Pluto and other celestial bodies similar conditions for liquid water also occur at depths of a few hundred meters or a few kilometers.
That is, life would exist everywhere where the temperature and pressure are adequate for liquid water to exist.
It is not logically admissible, as it is maintained in the official geology, that life has originated on Earth or that our planet has exclusivity in that aspect. These hypotheses (I would say beliefs) that the Earth is unique in relation to life is the last vestige of ancient geocentrism.
The non-geocentric theory that sustains the extraterrestrial origin of life is called panspermia.
It is Interesting to reflect on the possible existence of life in comets. They are small bodies (generally less than 10-20 km in diameter) that do not have much internal heat but that seem to contain a large percentage of organic molecules (VERY rich in carbon). Surely comets carry the basic elements of life and perhaps organisms in dormant or active life, probably in the form of spores, and in some cases even active or viable microorganisms. We do not know. But the coherence of nature and the universe makes us think that life is (almost) everywhere. As Fred Hoyle maintained: "life is a property of matter" -

Tuesday, February 28, 2017

Panspermia and the Comet 67P

It's a radical explanation for Comet 67P's features.

There could be extraterrestrial life on Comet 67P/Churyumov-Gerasimenko, the target of the European Space Agency's Rosetta orbiter. That's according to a couple of UK-based scientists who claim that features on the comet's surface could be explained by microorganisms beneath the crust.
It's a radical view, and a controversial one, but astrobiologists Max Wallis from the University of Cardiff and Chandra Wickramasinghe, director of the Buckingham Center for Astrobiology, claim data from the Rosetta mission backs up their theory that the comet could harbour some form of life. "That's the conclusion that we've come to," said Wickramasinghe in a phone call.
He argues that comets could transport life through the galaxy, a theory that would have great implications for our origins and the nature of biology. "The implications would be that life is a truly cosmic phenomenon, not restricted to the Earth," Wickramasinghe said.
The European Space Agency's Rosetta spacecraft has been chasing Comet 67P for years, and made headlines last year when it began to orbit the comet and successfully sent a lander, Philae, onto the surface.

A picture of the comet on 23 June. Image: ESA/Rosetta/NAVCAM
Data from the orbiter and lander's instruments is starting to be published and we're getting to know more about the rubber ducky-shaped comet. We've found organic compounds, and know that the dark surface of 67P is peppered with craters and fissures.
Wickramasinghe and Wallis' model proposes that biology under the icy surface of the comet could produce gases that push through cracks in the surface and replenish organic materials. In a phone call, Wickramasinghe compared the process to "rotting food in a can that pops out when the microbiology gets going and produces a lot of methane or other gases."
"The whole of the geometry of the comet, we have argued, is due to the processes of this kind," he said. The researchers published a paper relating to their theory in the Journal of Astrobiology and Outreach, and Wallis presented it today at the Royal Astonomical Society's National Astronomy Meeting in Wales.
They posit that the life in question would be a kind of extremophile—a tough organism that can survive extreme conditions. In the paper they write that, "While microorganisms probably require liquid water bodies for their early colonising of a comet, they can inhabit cracks in ice and sub-crustal snow, especially if they contain anti-freeze salts and biopolymers."
But it's not a widely accepted theory.
"I am unaware of it having much, if any support in the Rosetta community."
Matt Taylor, project scientist of ESA's Rosetta mission, said in an email that, "Given the radiation conditions and the very very low temperatures, well below -70 on sunlit surface, I don't see this as a possibility and it's not clear to me how much evidence there is backing up this claim."
He added that, "I am unaware of it having much, if any support in the Rosetta community," and that he "[takes] more credence from the plethora of papers coming from the mission from the hundreds of cometary scientists who have gone through the process of peer review of their results."
There are no instruments on Rosetta or Philae to expressly search for life, only organic materials.Wickramasinghe has worked on the idea that comets could harbour life for a long time. He collaborated with the late British astronomer Sir Fred Hoyle on a hypothesis of "panspermia," whereby life on Earth would have originated in space.
Wickramasinghe's previous attempts to provide evidence for panspermia of this kind haven't yet swayed scientific opinion.
A less controversial theory—one that's acknowledged as by ESA as something Rosetta could help uncover—is that comets like 67P could have brought molecules to Earth that acted as the "building blocks of life," rather than life itself: complex organic molecules that could have been precursors to amino acids and "seeded" life as we know it.
Wickramasinghe conceded that the proposal of life on 67P would be disputed by critics, but blamed what he called "a relic of pre-Copernican times" that favours the idea that life is centred on Earth.

Wednesday, October 5, 2016

Comets are alive?

Danilo Anton

Behavior of comets is unpredictable.  They appear from nowhere, they dive into the inner solar system, they are made of ice and rocks and approaching the sun they sublimate their ices.They eject  strong plumes from their surfaces, together with the gases they expel dust particles which are blown by the solar wind forming a coma or a tail.  
They are very dark, their albedo is less than 5%. They are darker than coal. Almost black. Their ices are water,  carbon dioxide and several hydrocarbon and organic compounds and molecules. 
Suddenly they change their brightness without any apparent reason. 
Fred Hoyle, Wikramasinghe and others believe that inside the comets there are bacterial spores and that life came to Earth within these celestial bodies (this theory called "panspermia"). 
Once in a while a new comet hit our planet. Probably this is what happened in Tunguska, Siberia in 1908.  
It is possible that comets not only transport life, as bacteria or spores, they may even be alive themselves. In some way the coincide with the definition of an "organism" because in some way they are "born" and may finally die..  
They are born when they leave the deep freeze far away in the intestellar environment and start their activity during their solar approach. They die when they approach too much to the Sun or after a few thousand orbits next to the Earth and other interior planets. Some of them have elliptic orbits, and even, some have parabollic or hyperbolic orbits. Probably a few are extrasolar visitors . 
When they approach the Sun and they lose their ices they may become asteroids (which in some cases are "dead" comets. or they may disappear in the solar heat or disarticulate in smaller pieces..
The few interplanetary probes that visited comets have confirmed their unusual characteristics, particularly the impressive Rosetta mission which went to accompany comet 67¨/Churyurmov-Geramisenko in its orbit. Several organic molecules were identified during this mission and many doubts still arise about the internal dynamics of these small and mysterious spatial bodies.