Most productivity in open oceans is limited to surface waters primarily due to the availability of sunlight, which is essential for photosynthesis. Phytoplankton, the primary producers in marine ecosystems, thrive in the well-lit epipelagic zone (the upper layer of the ocean) where light penetrates. Below this layer, light diminishes rapidly, restricting photosynthetic activity and, consequently, the overall productivity of marine life. Additionally, nutrient availability tends to decrease with depth, further limiting productivity in the deeper ocean waters.
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.
Coastal Surface waters in all major oceans.
surface
ocean fronts
Surface waters in the hydrosphere are made up of oceans, seas, lakes, rivers, and streams. These bodies of water are interconnected through the water cycle, with water evaporating from oceans and lakes, forming clouds, and eventually falling back to the surface as precipitation.
Upwelling increases productivity by lifting nutrients to the surface.
Surface waters of the Earth are typically referred to as "water bodies" or "water sources," which include oceans, seas, rivers, lakes, and streams. These surface waters play a crucial role in supporting various ecosystems and human activities.
Yes, the interconnected waters of the oceans cover over 70% of the Earth's surface. Oceans play a crucial role in regulating the planet's climate, supporting marine life, and providing a source of food and livelihood for many people around the world.
Plant planktons, or phytoplankton, require sunlight to perform photosynthesis and produce energy. In deep oceans, sunlight does not penetrate to the same extent as in shallower waters, making it challenging for phytoplankton to survive and thrive due to limited light availability. Consequently, phytoplankton are typically found in surface waters where sunlight can reach them for photosynthesis.
The transition between the warm surface layer and the deep cold water in the oceans is marked by a distinct boundary called the thermocline. The thermocline is a region where temperature decreases rapidly with depth, signaling the shift from warmer surface waters to cooler deep waters in the ocean.
Primary productivity can be limited by water availability in terrestrial ecosystems, as water is needed for photosynthesis to occur. In aquatic ecosystems, primary productivity can also be limited by water availability, as light penetration can be reduced in murky waters, limiting the amount of photosynthesis that can take place. Additionally, drought conditions can directly reduce primary productivity in both terrestrial and aquatic ecosystems.
No, they live in warmer waters along coasts in temperate climates and in the oceans of the tropics. They live in shallow waters so they can stay warmer, until winter when they move to deeper waters to avoid the colder surface water.