MARS FOREST LIFE
    BIO-DIVERSITY-12
Report #168
August 30, 2009

This report derives from a single MGS 
    MOC E07-02038 image strip of a site in the South 
    Polar Region but well out from the Polar Cap. The view in all the report images 
    here is from one side edge of the strip to the other encompassing as much 
    context information as possible. The general terrain around this site area 
    is characterized by lowlands that tend to shallow water wet conditions at 
    certain times with most of the water sinking into the soil. When dryer colder 
    time comes, what water is left on the surface freezes into low level areas 
    of water ice and the sub-soil is infused with water ice.
    
    An example of this is what you are seeing in the above first image. The most 
    light reflective areas above are low level water ice on the ground surface 
    while the less light reflective areas around it is dryer terrain. This dryer 
    terrain is dryer only in a relative sense to the more light reflective water 
    ice on top of the ground. In warmer periods, the water ice partially melts 
    into these lower profile looking surface ice area shapes soaking into the 
    terrain tending to infuse the relatively dryer terrain with moisture.
    
    As you might logically surmise, the fairly plentiful presence of moisture 
    in this terrain logically creates good conditions for the presence of biological 
    life to take advantage of it. That is what you are looking at with respect 
    to the different dark spots you see both in the terrain and on the more light 
    reflective water ice. Most of this is colony life and particularly that on 
    the water ice. The following report images presented here will represent samples 
    of this living ecology further down the strip below this point. Not included 
    here is very light reflective terrain in the upper half of the strip where 
    reflectivity tends to wash out all evidence detail.

The above second image demonstrates a sample site below that presented in the first image. It is just more of the same but now note with less in larger area water ice on the surface and more dark biological life presence. Note that the dark bio-life here is not really mature enough and therefore large enough to be seen with better visual detail. Also note how the more light reflective but residual water ice tends to collect in the lower level areas tending to form depression like channels in the terrain.

The above third image is a spot a little 
    further down in the strip below the first and second image sites. Now in the 
    left and center areas note that we see the beginning presence of a larger 
    and a bit more mature form of what I call "clump" biological life 
    evidence. From a distant view above like this, the evidence tends to look 
    a little like individual tree tops but it is not a vegetative life forms like 
    trees.
    
    Rather, it and its variations are colony major life forms of some kind unique 
    to this planet. This type of life comes in a number of variations that are 
    also very cold hardy. The variation seen here in this strip is adapted to 
    these South Polar region lowland conditions and look like this but there are 
    others. In my 2001 Report 
    #021 are larger forms looking very much like this but adapted to highland 
    terrain steep slopes. Also here in Report 
    #110 is very similar evidence and again in Report 
    #122 where the evidence is filling shallow trough systems on the South 
    Polar Cap ice itself. This life form is extremely tough and hardy but always 
    consider that it requires plentiful and consistent moisture presence.


The above fourth and fifth images moving 
    progressively down to the bottom of the strip demonstrates more of this major 
    biological life form presence in the terrain. Note that in these images the 
    evidence is in a more mature larger form and in greater densities. However, 
    the evidence here is in a more open configuration similar to a huge bush with 
    many branching's even though it is a colony form and what is seen here is 
    not its most mature form. In its most mature form it develops a more continuous 
    tough surface very similar to Earth Lichen as seen in the previous Reports 
    021, 110 and 122 at the above links.
    
    I would say that that most of this terrain is sort of like a drying and not 
    entirely wet bog here on Earth. Whether you can buy into that moist terrain 
    concept or not, the one prevalent thing that cannot be missed here is that 
    the darker clumpy looking evidence is clearly not natural rock and soil geology 
    and just as clearly represents some form of biological living growth in this 
    terrain. 
    
    It isn't really doing it so much here in these scenes but this type of Mars 
    life in its more mature form can literally jamb into a given area with one 
    colony form pressing tightly against its neighbors completely filling any 
    sunlight space. However, it never mixes with each other and collectively forms 
    a pretty much level field of this evidence. Some gigantic variations of this 
    life form are so broad and of such a low level elevation that they can be 
    and are easily mistaken for cracked geological terrain on Mars.
    
    When partially covered with snow that removes visible surface detail and leaves 
    only the narrow separation cracks between the colonies visible, this cracked 
    terrain impression is even more acute. Then only the huge size of the formations 
    give scientists pause in speculation as to what forces could cause such monstrous 
    geological cracking and especially in such uniform patterns?
    
    What needs to be understood is that water presence is much more prevalent 
    in the South Polar Region than in the North Polar Region. In fact, some lowland 
    areas of the South Polar Region are subject to seasonal flooding spreading 
    out from the Cap with a rising water table in seasonal and general warming 
    trends. This means that there is a greater variety 
    of biological life present in the South Polar Region than in the North Polar 
    Region taking advantage of these more favorable conditions. In many places 
    in the South Polar Region the lowland soil areas tend to have a fairly high 
    residual moisture content year round that is more favorable for smaller size 
    bio-life that carpets the terrain choking out everything else and that smaller 
    life tends to be sunlight reflective rather than dark and light absorbing.
    
    So when resolution is cut in an image to facilitate obfuscation, it is this 
    type of smaller carpeting life that is the most negatively impacted. The visuals 
    are so merged together by the poor resolution and the sunlight reflectivity 
    that the carpeting life looks more like continuous barren terrain. The upper 
    portion of this same reporting strip is like that. I don't show it here because 
    the only thing to see is light reflectivity off of broad surface areas with 
    little or no individual detail.
    
    By contrast, the bio-life evidence pointed out here is both far larger and 
    darker giving some idea of individual shapes and then better visual recognition 
    follows. We here on Earth tend to think of dense forests as consisting of 
    trees and bushes as per our direct experience. However, although there are 
    conventional looking trees and bushes on Mars, there are also dense forests 
    of what appears to be mold and lichen like colony life in mega size forms 
    that tend to hug and carpet broad areas of terrain where the moist conditions 
    are more favorable to them.
    
    They are one of the prevalent life forms on Mars even if they are unfamiliar 
    to the Earth human eye and not easy for us to visually recognize. The wind 
    carried reproductive spores cover vast areas resulting in the dark spots seen 
    everywhere in various stages from small and struggling to survive to flourishing 
    large densely packed forms covering broad areas. They usually do best where 
    moisture is consistently present in the soil and second best when water ice 
    on the surface is low profile and subject to warming conditions melt. In their 
    variety, they even contaminate and survive within surface water on the South 
    Polar Cap itself forming dark lanes in their millions that retain solar heat 
    that in turn erodes the Cap surfaces.
    
    I come back to reporting on this evidence on occasions just because it is 
    strange and less obvious to the Earth human eye and therefore a little too 
    easy to be ignored because it is not understood. To adequately understand 
    Mars, one must also come to terms with understanding its unique biological 
    life differences that play a major role in the planet's development.
    
    DOCUMENTATION
    
    http://www.msss.com/moc_gallery/e07_e12/images/E07/E0702038.html: 
    This link connects you to the official MGS MOC E07-02038 
    science data 3rd listed stright .GIF strip sourced in this report. The evidence 
    starts in the last 40% of the strip and continues to the very bottom.
    
    , Investigator