Final answer:
In temperate mid-latitude regions, a decrease in primary production during the summer months is often attributed to c) a decrease of nutrients.
Step-by-step explanation:
In temperate mid-latitude regions, primary production decreases during the summer months mainly due to a decrease of nutrients, which is a result of the stratification of ocean waters that inhibits the upward mixing of nutrient-rich deep waters to the surface.Warmer ocean water can lead to stratification, which prevents the mixing of water layers, and as a result, nutrients from deeper water layers do not replenish the surface waters consumed by phytoplankton and other primary producers. This nutrient depletion inhibits the growth of these organisms despite the abundance of sunlight.
Conversely, during the winter months, cooler temperatures and turbulent conditions help mix the water column, which brings nutrients to the surface and supports primary production. Therefore, it is not the warming of ocean water, an overabundance of sunlight, cooling ocean waters, or a lack of sunlight that primarily drives the summer decrease in production, but rather the scarcity of essential nutrients needed for the growth of primary producers. Important biomes like the tropical wet forest display high primary productivity due to their warm temperatures, abundant water, and year-round growing season, unlike biomes with extreme conditions such as deserts and tundra.