Leovinus - I will research it. Meanwhile, off the top of my head: <br /><br />The standard model has the sun losing mass. Exactly how much is the variable. The solar wind stops most accretion, if not all. <br /><br />My doubt would be when the sun passes through a dense (relatively) gas and dust cloud in Milky Way.<br /><br />Or merges with a sub-brown dwarf, etc. <br /><br />Especially in the future during the Andromeda-Milky Way merger.<br /><br />Also, there are widely variant models as to how far earth will move away from the sun by red giant phase - again according to the standard model.<br /><br />Some have earth swallowed up by the sun, while others have earth well beyond the sun's surface in a more distant orbit.<br /><br />Geological evidence has early earth hotter, then milder but more uniform. Astronomy indicates it should have been colder. Perhaps early earth was slightly closer to the sun. Certainly, the greenhouse effect was much stronger than today. Here is just one line of evidence for this:<br /><br />The vast carbonate deposits on earth indicate a very extensive geologic carbon cycle, whereby atmospheric carbon dioxide (CO2) combines with water (H2O) in the oceans: H2O + CO2 yields H2CO3. The CO3 separates as a dissolved negative ion (Co3-), and combines with 'metal' ions dissolved in ocean water, such as sodium (Na+) in salt (NaCl) or Potassium (K) in Potassium salt (KCl) [also Calcium ions, Ca+) to form carbonates, or limestone, which precipitates out to form these vast carbonate deposits.<br /><br />Calculating mathematically, the vast carbonate deposits in earth’s crust indicates a vast CO2 atmosphere in early earth - comparable to Venus at present. <br /><br />And that, in turn, caused a powerful greenhouse effect. <br /><br />Earth has been fine tuned for life in many ways. One way was the change from venus-like to the present life sustaining environment. <br /><br />BTW - one should not ignore tidal interactions. Earth's moon is receding slightl