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![]() The outcrop at the Opportunity site is covered by a decomposing or partially fossilized sponge and its gemmules, possibly of the species spongilla. The images make this clear imo. But I'm a mathematician not a biologist and I need some professional feedback. Please take a look, thanks in advance. Sphere close up of Opportunity outcrop 1) http://marsrovers.jpl.nasa.gov/galle...P2953M2M1.HTML Gemmule photo 2) http://waynesword.palomar.edu/plfeb96.htm#gemmules "During the spring gemmule "hatch", the peripheral thesocytes differentiate into a pinacoderm that balloons out, like a bubblegum bubble, through the micropyle. This micropyle bubble makes contact and attaches to the substratum" http://64.78.63.75/samples/04BIORupp...oology7ch5.pdf Sphere with bubble http://marsrovers.jpl.nasa.gov/galle...P2933M2M1.HTML Raw thread image 3) http://www.earthfiles.com/news/news....tegory=Science 4) http://marsrovers.jpl.nasa.gov/galle...P2953M2M1.HTML Imprints of skeletal spicules, very small thread sticking out and casting a shadow upper left corner beneath the two large brown patches. http://marsrovers.jpl.nasa.gov/galle...P2933M2M1.HTML Sponge wall rover image, left of center 5) http://marsrovers.jpl.nasa.gov/galle...P2932M1M1.HTML Diagram of sponge wall, bottom of page 6) http://paleo.cortland.edu/tutorial/P...a/porifera.htm All raw Rover images can be found here http://marsrovers.jpl.nasa.gov/galle...portunity.html The correlation between the Rover images and a sponge gemmule are many. 1) Both show a surface that is grainy, or covered with spicules 2) Both show the aperture and slice 3) Image 3 shows a skeletal spicule as in the left of image 2 just above the word gemmule 4) A gemmule would explain the shiny spheres 5) A gemmule would explain why only some of the Rover spheres show an aperture. 6) A gemmule would explain the occassional sphere 'twins' or bubble. 7) The Opportunity site was chosen for a possible previous marine environment, which sponges occupy. 8) A sponge release of gemmules would explain the uniform and random distribution of the spheres, since no impact boulders or nearby volcanoes are seen near the site. 9) Sponges were perhaps the very first animal life on earth, we should expect a similar first life on Mars. 10 Sponges, spongilla, are known to have a symbiotic relationship with sulfur reducing bacteria, and use it for a primary food source. Such bacteria is associated with hematite, thrives off elemental sulfur, low oxygen and salty environments. Overhead views of Meridiani http://www.msss.com/mars_images/moc/2004/01/24/ The second image shows how the density of spheres settled in the channels. This image shows a recent reef system I believe. Sponge covered rock? http://marsrovers.jpl.nasa.gov/galle...P2555R1M1.HTML Dark dunes http://marsprogram.jpl.nasa.gov/gall.../PIA01695.html http://www.msss.com/mars_images/moc/...se/7707rel.gif http://marsprogram.jpl.nasa.gov/gall.../PIA02398.html It appears that ancient furrows, following precisely where water would stand, are covered in a blanket of dark material similar to the Opportunity site. The clearly defined, if not startling, outline of the dark material shows that fallout from impacts or eruptions are not a possibility. This dark canyons may be additional blooms of recent marine life. "Each gemmule is covered with a protective outer layer and a foraminal aperture. In some species the gemmules are also covered with spicules. Gemmules are commonly produced during the fall, and like the overwintering turions of duckweeds, are able to survive severe winter conditions. The gemmules can withstand repeated freezings and thawings and may be viable for three years are more. Upon germination, a creamy mass of amoebocytes slowly flows out of the foraminal aperture." http://waynesword.palomar.edu/plfeb96.htm#gemmules "One exciting place (that is accessible for some coastal biology classes) to observe living sponges is in intertidal sea caves found along rocky ocean shores. Biology students who investigate these geological features are likely to find 'living paintings' on the cave walls, formed by sponges or groups of sponges. In high wave-shock areas, these sponges are usually only a centimeter or two in thickness. The formation of gemmules is another form of asexual reproduction. This strategy is common for freshwater sponges, but rare in marine species. The gemmule is a densely-matted, hardened ball containing archeocytes protected by collagen and special spicules. In freshwater sponges, these balls survive through the winter and then form a new clone in the spring. http://ebiomedia.com/prod/BOsponges.html "Frozen water makes up as much as 10 percent of the top meter (three feet) of surface material in some regions close to the equator." http://marsprogram.jpl.nasa.gov/odys...20031208a.html Jonathan Maatsch j0nathan @comcast.net s |
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