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Echinus aurantium: Locations
Environments: marine, transition zone/lower shoreface, shallow subtidal, deep subtidal shelf, carbonate, coastal, offshore, offshore shelf, reef, buildup or bioherm, foreshore, peritidal, offshore ramp.
originally posted by: jeep3r
This was added to the journal on 28 November 2014 with the title "Clues to Wet History in Texture of a Martian Rock". The long & segmented features as well as the round'ish spherules in the lower half are IMO rather intriguing. They compare incredibly well to terrestial crinoids (plant-like marine animals) and a certain genus of cystoids which I will outline more in detail further below. Moreover, the segmented parts are also highly reminiscent of Richard Hoover's infamous 'fossil' which had been ground to dust in the early days of Opportunity's mission:
originally posted by: smurfy
originally posted by: jeep3r
This was added to the journal on 28 November 2014 with the title "Clues to Wet History in Texture of a Martian Rock". The long & segmented features as well as the round'ish spherules in the lower half are IMO rather intriguing. They compare incredibly well to terrestial crinoids (plant-like marine animals) and a certain genus of cystoids which I will outline more in detail further below. Moreover, the segmented parts are also highly reminiscent of Richard Hoover's infamous 'fossil' which had been ground to dust in the early days of Opportunity's mission:
That picture is the one Hoover was talking about. He seems pretty certain about it, and anyway why'd they pick that particular object to do a Jeremy Clarkson on... to look for carbon, it had obviously caught their attention in the first place.
I find this whole thing pretty fascinating.
...Especially when considering Curiosity's recent findings that martian bodies of water have lasted much longer on the surface than previously thought, the case for past life on Mars IMO becomes more and more plausible! ...
I think the erosion/sandblasting taking place on Mars is very much more destructive than on Earth fossils
www.abovetopsecret.com...
In contrast to these relatively fast, short-term erosion rates, average erosion rates on Mars determined mostly from deflation of landing sites over ~100 Myr and 3 Gyr timescales from the literature are of order 0.01 m/Myr or less, which is 3-4 orders of magnitude slower than the slowest terrestrial rates determined over similar timescales. The similarity of these average erosion rates together with the long spatiotemporal scales of averaging involved in their estimation, argues they are representative of the true long-term process rate.
Yes, less than sterling. You seem to assume that the "fossils" would begin eroding as soon as they were formed, before they had become exposed by erosion.
so that brings the 'recent' creation of fossils on Mars closer to 100-150 million years ago, at least to my less than sterling determination of fossil age
Granted, we have only one model. We only know it happened here and we have a pretty good idea of how long it took. We know that by the time there were plants on Earth, Mars had dried up.
That's why I think it's difficult to guestimate how long life takes (ultimately) to evolve into more complex forms. Perhaps the situation on Mars was different
originally posted by: wildespace
Appearances can be deceptive, and many geological formations can look like fossils. Concretions, bubbles, and stuff like that can look organic. For example, here's a rock on the Moon that was examined by the Apollo moon walkers: www.hq.nasa.gov... It's covered with some bubbly melt material on one side.