Productivity in tropical regions can be high due to the abundance of nutrients and sunlight, but it is not necessarily unlimited. Factors such as water availability, temperature extremes, and soil quality can also impact productivity. Over time, nutrient availability may become limited as vegetation gradually depletes the soil.
Tropical rainforests typically have soil with high nutrient levels due to constant decomposition of organic matter. These biomes support a wide array of plant and animal life as a result.
Marine ecosystems, particularly oceans, contribute the most to global net primary productivity. Oceans contain a high diversity of phytoplankton that produce a significant amount of oxygen and sequester carbon dioxide through photosynthesis. This makes marine ecosystems essential in sustaining life and regulating the Earth's climate.
Tropical rainforests have the highest primary production in terrestrial ecosystems due to their high levels of rainfall, sunlight, and warm temperatures that support abundant plant growth. These biomes have a high diversity of plant species that contribute to their high productivity.
The richest biomes in terms of biodiversity and productivity are tropical rainforests and coral reefs. These ecosystems support a wide variety of plant and animal species and play a crucial role in maintaining global biodiversity.
Tropical rainforests are known to support the greatest number of species due to their high biodiversity and stable climate. Coral reefs and estuaries also support a wide variety of species due to their unique ecosystems and high productivity.
Desert < Open ocean < Lake < Tropical rainforest. Desert ecosystems have the lowest primary productivity due to low water availability and extreme conditions. Open ocean ecosystems are next due to limited nutrients. Lake ecosystems have higher productivity as they are more nutrient-rich. Tropical rainforests have the highest productivity due to the abundance of sunlight, water, and nutrients.
Primary productivity in tropical oceans is primarily limited by nutrient availability, particularly nitrogen and phosphorus. Factors such as temperature, light availability, and water movement can also influence primary productivity in tropical oceans. Upwelling events that bring nutrient-rich waters to the surface can enhance primary productivity in these regions.
abundance in tropical and semi-tropical regions
The highest biological productivity is usually found in areas with abundant sunlight, nutrients, and suitable temperatures, such as tropical rainforests, coral reefs, and estuaries. These regions support diverse ecosystems with high levels of primary productivity due to the optimal conditions for plant and algae growth.
Tropical rainforests typically have soil with high nutrient levels due to constant decomposition of organic matter. These biomes support a wide array of plant and animal life as a result.
plants
plants
Thermocline is defined by having increased temperatures in the surface water but cold water temperatures in the deep sea due to sunlight being unable to penetrate ocean waters the deeply. Sunlight and increased temperatures in water is associated with low nutrients therefore anything with a strong thermocline is pertained to low nutrients but high sunlight.
stupid
No, they do not. They are "old soils" and contain very few nutrients.
The rapid rate of decomposition in tropical forests leads to the quick breakdown of organic matter, which results in low nutrient soil. The warm and humid conditions in tropical forests facilitate the activity of decomposers such as bacteria and fungi, accelerating the recycling of nutrients back into the ecosystem. As a result, the soil in tropical forests tends to be nutrient-poor despite the high biological productivity.
Tropical soils are generally nutrient-poor due to high temperatures and heavy rainfall, which lead to rapid decomposition of organic matter and leaching of nutrients. The intense weathering processes in tropical regions also result in the formation of soils with low cation exchange capacity, limiting their ability to retain essential nutrients for plant growth. Additionally, the high levels of precipitation in tropical areas can cause soil erosion, further depleting the soil of nutrients and reducing its fertility over time.