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Actual site specific weathering rates also depend on the degree of rock surface fracturing and probably also on microbial rock surface colonization (Davis et al. 2007).
Similar(59)
and microbial processes in spring and stream microbialites (e.g., travertines, tufas, sinters) and exposed sedimentary and rock surface habitats (endolithic habitats and cryptogamic covers), is of particular importance for the more comprehensive understanding of past life because these represent terrestrial habitats expected on ancient continental surfaces.
Clearing rock surface.
Clearing rock surface; nothing found.
Clearing rock surface inside boundary wall.
Clearing rock surface east of this area.
Clearing to rock surface west of mastaba area.
Continued the clearance of the rock surface here.
Right: Kaitlin Maguire scanning a rock surface for microfossils.
The presence of striations on most sampled rock surfaces validates our assumption of negligible rock surface erosion.
The photoautotrophic Cyanidium apparently survives below the rock surface where sufficient light is available for photosynthesis.
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