When i "scanned" the HiRISE data from yesterdays releases, I stumbled across an interesting structure in a gully of a crater slope. With an article, I read recently, in mind about the possibilities of detecting fossil signatures on Mars i added the following crop image to my collection:
http://i684.photobucket.com/albums/vv202/marsphotojournal/ESP_011995_1410_RGBNOMAP_knochen_2x.jpg
This crop from the HiRISE data of a Mars southern highlands crater shows something appearing like macro fossil fragments - scattered about 50 m across. Maybe this features got washed free by liquids when the gully been carved. The area visible is about 120 m across. The fragments show some similarity in appearance and are aligned as expected for larger fossils on earth (if well preserved). I also seen a single fragment perfectly just like this fragments in the Ritchey Crater HiRISE data
quotation of the related article
"Along with caves, Boston said some top-notch nooks and crannies on Earth to look for fossils are in things with vertical relief that slices down through layers, like canyon walls, fault escarpments, and river/stream outflow channels. For Mars and other crater-rich environments, obviously crater walls where things are excavated down to some deeper strata are first-rate sites.
"The best thing about these places is that large -- as in macroscopic -- buried fossilized material is usually weathering out of the outcrops. One can see them laying about and follow the fragments to the source," Boston said. "
If considering large macro fossils(thus former large life forms)on Mars slightly possible, may the above image be an example of Bostons assumptions or just a normal geological feature in Mars gullies and ridges?
What else should macro fossils look like from the viewpoint of HIRISE, if there actualy are some visible in exposed spots? :)
HiRISE coverage this article refers to:
Gullies on Pole-Facing Slope and Arcuate Ridges on Crater Floor