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| Average Nitrate and Phosphate Concentrations in Seawater after Volcanic Eruption | ||||
|---|---|---|---|---|
| Nutrient | Seawater in lava-affected area, 5-45 meters below surface | Seawater in lava-affected area, 75-125 meters below surface | Seawater outside of lava-affected area, 5-45 meters below surface | Seawater outside of lava-affected area, 75-125 meters below surface |
| Nitrate (micromoles per liter) | 3.1 | 0.4 | ≤0.03 | ≤0.01 |
| Phosphate (micromoles per liter) | 0.17 | 0.09 | 0.14 | 0.06 |
at 5-45 meters below the surface, the average concentration of phosphate was about the same in the seawater in the lava-affected area as in the seawater outside of the lava-affected area.
for both depth ranges measured, the average concentrations of nitrate were substantially higher in the seawater in the lava-affected area than in the seawater outside of the lava-affected area.
for both depth ranges measured in the seawater in the lava-affected area, the average concentrations of nitrate were substantially higher than the average concentrations of phosphate.
in the seawater outside of the lava-affected area, there was little change in the average concentration of nitrate from 75-125 meters below the surface to 5-45 meters below the surface.
North American gray wolves experience more outbreaks of distemper virus than other wolf species do.
the gene variant that results in black fur may be linked to immunity to the distemper virus.
the average life span of gray wolves is likely to increase over time because of a particular gene variant.
gray-furred wolves will soon replace black-furred wolves across North America.
artifacts from the fourteenth century CE are more commonly recovered than are artifacts from the thirteenth century CE.
the artifacts originated elsewhere and eventually reached Kuulo Kataa through trade or migration.
Kuulo Kataa was founded by people from a different region than had previously been assumed.
excavations at Kuulo Kataa may have inadvertently damaged some artifacts dating to the fourteenth century CE.
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