Dr manuel states:
We have little quantitative information about what the early Earth looked like.
However, measurements show that:
1. Earth accreted in layers, beginning with the formation of an iron core upon which the silicate mantle was later deposited.
2. The lower mantle surrounding that iron core never melted and retains highly volatile elements like He-3 today.
3. Earth's upper mantle melted to produce the atmosphere and crust within the first 200 My. The upper mantle stopped releasing volatile elements to the atmosphere while extinct I-129 and Pu-244 were still alive.
These measurements are summarized in ""The xenon record of extinct radioactivities in the Earth," Science 174, 1334-1336 (1971) and "The noble gas record of the terrestrial planets," Geochemical Journal 15, 245-267 (1981).
Io is much further from the Sun, where iron is a rare element. It is doubtful that its early history parallels those of the Earth and other terrestrial planets
I would add in Dr Manuel, that measurements do not support your contention that the earth accreted on an iron core, rather measurements almost universally support the premise that the earth accreted and then melted, resulting in the formation of an iron core.
Further, you have given no mechanism by which silicates formed farther out from the earth's early orbit could have migrated in to accrete on the newly formed iron core, nor have you given any explanation for the how a lack of differentation would have occurred in the aftermath of the proto-earth having been struck by a mars-sized body.
Recent measurements by Romanowicz et al at the University of California, Berkley have identified hot "superplumes" of material rising from the lower mantle (~ 2800 KM below the lithosphere) and earlier measurements also identified cooler "downplumes" in other areas of the planet.
William White at Cornell also found evidence of mantle recycling in measurements he and his team performed at the Society Islands, and this finding was reconfirmed later by Jon D. Woodhead of the Australian National University through measurements he made of the abundant oxygen isotope ratios at Pitcairn Island.
This could not be the case if the lower mantal remained undifferenciated and/or unmelted as you maintain.
There are a myriad of other studies which also support the premise that the lower mantle is melted. This must also lead to the conclusion that the lower mantle is differentiated, because it could not remain undifferentiated while melted.
Now no doubt you will again refer to your paper regarding the anomalties in the isotopes of He and Xe. Might I suggest that you instead refer to some independant findings from anyone other than you and your collaborators so that we might gain an unbiased view of your findings?
Might I also suggest that you outline a mechanism whereby the isotope readings you obtained might have arisen in the accretion method of planet formation? Or is it your position that such readings are impossible in that method?
All civilizations become either spacefaring or extinct.~ Carl Sagan ~
Humanity must rise above the Earth, to the top of the atmosphere and beyond, for only then will we fully understand the world in which we live.~Socrates, 500 B.C. ~
Let every man judge according to his own standards, by what he has himself read, not by what others tell him. ~Albert Einstein~