
Here, we compare/contrast two different stromatolites as a cautionary tale for exobiologic studies. The stromatolites are basically identical at the hand sample scale (e.g., the scale most easily imaged by a rover). Both are small (~15 cm tall) branching columnar structures that display finely laminated �light-dark� lamination on the order of ~100 microns thick. The laminae tend to thicken over the tops of the columns and thin towards the sides.
Microscopic examination reveals the laminae in one stromatolite, collected from a subsidiary pool to Obsidian Hot Spring in Yellowstone National Park, are composed entirely of silicified microbial filaments�a classic biogenic structure, with an active cyanobacterial mat on the surface. The laminae in the other stromatolite, collected from a hydrothermal vein in the Tempaiute Range, Nevada, are composed of interlocking bladed calcite�a classic abiotic precipitated fabric. Furthermore, the Tempaiute stromatolites grew surface normal to a high-angle hydrothermal vein deep in the subsurface, in the absence of light.
While the geologic context provides some hint to their potential biogenicity (hot spring/active mat versus subsurface vein), the context may not always be apparent (e.g., a Mars boulder field). At the hand sample scale, many stromatolites may fail the �extraordinary evidence� test�if possible, such structures should be examined in-situ microscopically to help guide our decision.
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