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Rock varnish is typically rich in iron and manganese, with the presence of manganese due to bacteria on the surface of the rock. Because the bacteria would not survive on the surface of rocks in the colder, continuously frozen, reaches of Antarctica, scientists were not surprised to discover that rock varnish in the Thiel mountains area of Antarctica consists only of limonite, a form of oxidized iron. This had penetrated from the surface of the rocks into the cracks. However, although moisture is essential to the movement of limonite, snow has not melted in the Thiel Mountains in recent times.

Indicate which statement in the table the given information most strongly suggests is true, and the statement that the given information most strongly suggests is false. Make only two selections, one in each column.
Ture False  
Moisture is required for the presence of significant amounts of manganese in the environment
Moisture is not required for the presence of significant amounts of manganese in the environment
When temperatures in a continuously frozen location increase to above freezing, cracks in rocks there begin to take in rock varnish containing significant amounts of manganese
Rock varnish that is especially rich in iron is mostly extreme cold
Manganese is unable to penetrate into cracks in significant amounts
Temperatures on rocks in the Thiel mountains were above freezing at some point in the past

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