Last updated on Aug. 10, 2018
Abstract
NASA’s Mars Rover Curiosity visited Bagnold dune field in Gale Crater, Mars, to study sands there from December 2015 to February 2016 (from Sol 1182 to Sol 1260) (See Figure 1 and http://www.hou.usra.edu/meetings/lpsc2016/pdf/2298.pdf ).
Figure 1: Route map of Mars Rover Curiosity from Sol 1172 to Sol 1260
http://mars.nasa.gov/msl/multimedia/images/?ImageID=7640
http://photojournal.jpl.nasa.gov/catalog/PIA16064
Image Credit: NASA/JPL-Caltech/MSSS
https://www.flickr.com/photos/fossil_lin/30409147796/sizes/o/
https://www.flickr.com/photos/fossil_lin/30445873175/sizes/o/
NASA’s Mars Rover Curiosity acquired the above microscopic image on Jan. 19, 2016 (Sol 1228) at Gobabeb in Namib Dune in Bagnold dune field, Gale Crater, Mars. Twelve red arrows point to well-preserved ooids. These ooids are between 0.1 mm and 0.2 mm in diameter, as they have been sieved with a mesh of 0.15 mm holes. The rover dumped the scooped and sieved particles onto the ground after analyzing similar particles for their chemistry and mineralogy in its laboratory instruments. Image Credit: NASA/JPL-Caltech/MSSS
NASA’s Mars Rover Curiosity acquired the above image (Figure 5) with Mars Hand Lens Imager (MAHLI) on Jan. 23, 2016 (Sol 1231) at Gobabeb in Namib Dune in Bagnold dune field, Gale Crater, Mars. Most of the particles in this image are eroded ooids. Red lines mark some of the ooids. They measure roughly 0.2 mm to 0.4 mm across. Image width: ~2.8 cm. Largest-sized figure:
Image Credit: NASA/JPL-Caltech/MSSS
NASA’s full-sized image with description:
http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=7658
https://www.flickr.com/photos/fossil_lin/24749890260/sizes/o/
http://wretchfossil.blogspot.tw/2016/04/more-martian-microbes-boring-holes-in.html
http://wretchfossil.blogspot.tw/2016/09/microbial-borings-differentiate-ooids.html
Figure 8. Original description: “Mega ooids! Dave’s finger for scale.” The above photo (Figure 8) shows ooids in China Ranch, California, USA. Red lines in the photo mark ooids that have been eroded into hemispheres. Image source: the last fifth photo in http://daveandiztakeonthewest.blogspot.tw/2012/11/china-ranch-and-stretchoween.html
Figure 9 shows spheres that are different from ooids. Original description: “The Utah concretions shown on the left range in diameter from one twenty-fifth of an inch to 2 inches (1 mm to 50 mm), while the Martian versions on the right all measure less than one-fifth of an inch (5 mm) in diameter. (Scale of photos is different.)” (Quoted from http://www.innovations-report.com/html/reports/earth-sciences/report-30313.html )
https://www.flickr.com/photos/fossil_lin/30445874495/sizes/o/
https://www.flickr.com/photos/lunexit/24626790060/in/dateposted/
Image Credit: NASA/JPL-Caltech/MSSS/2di7 & titanio44
NASA’s original raw image: http://mars.nasa.gov/msl/multimedia/raw/?rawid=1242MH0005620020403663C00_DXXX&s=1242 (flipped 180 degrees into the above image)
http://planetary.s3.amazonaws.com/assets/images/4-mars/2016/20160210_MAHLI_1241_Namib_sample_area.jpg,
then transported to Dump Pile D in the same photo.
A2. Putative Martian ooids are seen not only at High Dune (Figure 2) and Namib Dune (Figures 3, 4, 5) but also seen at 18 other places in Gale Crater. (see http://wretchfossil.blogspot.tw/2016/06/numerous-martian-microbes-produced.html). Some of the ooids are still embedded in oolite and many others were drilled out of rocks in 2016.
The environment of Gale Crater over 3.5 billion years ago was a freshwater lake near the Martian equator (see http://authors.library.caltech.edu/60940/). Such concentration, distribution, and environment fit those of ooid sand on Earth. Regarding the geological context of Martian ooids, Martian wind had blown the ooids in the above figures away from the site where they were originally formed (see the third paragraph inhttp://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=7658). Anyway, geologists do not need geological context in order to correctly identify ooids (see Figure 8).
A3. Ooid spheres differ from other kinds of spheres in sizes, colors, and internal structures. Ooids of Earth are mostly 0.25 mm to 1 mm in diameter (note 1). Martian ooids at Bagnold Dune measure ~0.1 mm to 0.5 mm in diameter (Figures 2 to 5).
However, “On Mars, most of the hematite rocks (“blueberries”) are about 0.16 inches (4 millimeters) in diameter, and no larger than 0.24 inches (6.2 millimeters). By contrast, Earth spherules exhibit a large range of sizes, not limited to only a quarter of an inch.” (Quoted from the ninth paragraph in http://news.nationalgeographic.com/news/2014/02/140224-mars-blueberries-water-meteorite-space-science/ )
The colors of Martian ooids include white, yellow translucent, green, grey, and yellow as shown in figures above. Other kinds of spheres do not show all of these colors.
Regarding internal structures, ooids contain nuclei and concentric layers (Figure 10), which are usually lacking in spherical look-alikes, such as chondrules, Martian Blueberries, Utah’s Moqui marbles, etc. Ooids are not ”impact spherules” because no mechanisms allow meteor impacts to form spherules with nuclei and concentric layers. Nothing matches the spherical “ooids” on Mars except ooids of Earth.
In view of the above, yes, they are ooids.
Note 1: See the third paragraph in https://en.wikibooks.org/wiki/Historical_Geology/Ooids_and_oolite and the first paragraph in http://www.sandatlas.org/ooid-sand/.
B. Were the ooids on Mars formed by microbes?
Regarding the formation of ooids, there are non-biological hypotheses, in which ooids get their spherical shape owing to highly agitated water (Ref. 3), such as sea waves pounding on the beaches, that rolls the ooids into the spherical shape. However, there is no highly agitated water in lakes. The spherical ooids at Bagnold Dune are unlikely to have been formed by the non-biological mechanisms because the Martian ooids are in a former lake and there is no evidence that proves ooids are formed by agitated water. On the other hand, there is ample evidence for the biological formation of ooids. Some of the evidence are listed below in B1, B2, and Ref. 3 to Ref. 15. In view of the above and the microbial borings in Martian ooids (Figure 7), the Martian ooids should have been formed by microbes.
B1. Microbes of Earth form ooids in the freshwater lake. Evidence: “Here, we show that photosynthetic microbes not only enhance early carbonate precipitation around the ooid nucleus but also control the formation of the entire cortex in freshwater ooids from Lake Geneva, Switzerland.” (Quoted from the abstract of the article in Ref. 4: “Going nano: A new step toward understanding the processes governing freshwater ooid formation”, displayed at http://geology.gsapubs.org/content/40/6/547.abstract)
The water in Gale Crater of Mars was once fresh water in a lake as mentioned in paragraph A2 above.
B2. Recent research confirms that microbes of Earth form ooids in seawater, as reported in the abstract of Ref. 5:
http://www.hou.usra.edu/meetings/abscicon2015/pdf/7317.pdf
More evidence for microbes forming ooids are listed in Ref. 3 to Ref. 15 below.
C. Ooids Prove Microbial Activities.
Microbes of Earth often bore holes in ooids and Martian microbes did the same thing (see Figure 7). Microbial borings in Figure 7 prove indirectly the existence of Martian microbes. Ooids are not only formed by microbes (see paragraph B) but also contain high organic matter content (Ref. 5).
E. Are chemical experiments essential for identifying ooids?
No. Geologists usually identify ooids with visual observation (Figure 8), because ooids possess unique morphology and unique internal structures. Ooids sometimes may not be identified even when chemical measurement results contain the chemistry of ooids. For example, meteorite ALH84001 contained ooids as evidenced in
http://aem.asm.org/content/68/8/3663/F1.expansion.html
but no scientists identified ooids in the meteorite.
Conclusion
Nothing matches the spherical “ooids” on Mars except ooids of Earth. No evidence proves ooids are formed by agitated water. Ample evidence proves microbes form ooids on Earth. The “ooids” found on Mars should have been formed by microbes, as there is no other proven way for forming such spheres. So, ooids are an apparent and widespread biosignature on Mars.
14. Thompson JB, Huber JA (1997) Microbe and ooid associations; a possible microbial role in the origin of ooids. Abstracts with Programs – Geological Society of America 29: 130.