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"Red tides" are spectacular dinoflagellate blooms that occur in the sea and often lead to mass mortality of marine fishes and invertebrates. Human deaths from eating shellfish poisoned with red tide algae is a worldwide problem. Review the evidence available about the origin of red tides, and discuss the implications for general ideas about what controls primary production in the sea. Landsberg (2002) Kubanek et al. (2005), and Wong et al. (2007) discuss this problem.

Short Answer

Expert verified
Red tides, caused by nutrient-rich runoff and environmental factors, alter marine ecosystems and highlight the impact of primary production controls on marine life.

Step by step solution

01

Understand Red Tides

Red tides are harmful algal blooms caused by dinoflagellates, a type of plankton that, under certain conditions, multiply rapidly and form dense concentrations. These blooms are often red or brown in appearance and can release toxins that negatively impact marine ecosystems.
02

Identify Research on the Origin of Red Tides

Research, such as that by Landsberg (2002), explores various causes of red tides, including environmental factors like temperature, salinity, and water circulation patterns. Human activities, such as agricultural runoff and pollution, also contribute to the nutrient loading in coastal waters that often triggers these blooms.
03

Examine Implications on Primary Production Control

Kubanek et al. (2005) and Wong et al. (2007) suggest that factors controlling red tides can influence primary production in the sea. Nutrient availability, particularly nitrogen and phosphorus from runoff, directly affects the growth of photosynthetic plankton, which are primary producers in marine food webs.
04

Discuss Broader Ecological Consequences

Red tides provide insight into the broader ecological impacts of primary production control. The excessive nutrients that promote red tides can lead to unbalanced ecosystems, fish kills, and the accumulation of toxins in marine food chains, affecting both marine life and human populations.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Harmful Algal Blooms
Harmful algal blooms (HABs), often referred to as red tides, occur when certain types of algae, typically dinoflagellates, multiply rapidly in the ocean. These blooms can cause the water to appear red or brown. Particularly alarming is the fact that some of these blooms emit toxins. These toxins are harmful not only to marine animals but also to humans who consume affected seafood, especially shellfish.
The term "harmful" signifies the detrimental impacts these blooms have on marine life, leading to fish kills and endangering shellfish populations. Human activity plays a role in these events, often through nutrient loading from agricultural runoff and pollution. Understanding and managing these blooms are key to protecting marine ecosystems and human health.
Primary Production
Primary production in marine ecosystems is the process in which photosynthetic organisms, like phytoplankton, convert sunlight into chemical energy by producing organic material. This foundational process is vital for health and sustainability, forming the base of the ocean food web.
However, the balance in primary production can be disrupted by nutrient overloads contributing to harmful algal blooms. Excess nutrients like nitrogen and phosphorus, commonly from human activities such as farming, can lead to excessive phytoplankton growth. While these organisms are primary producers, uncontrolled growth can actually harm the broader ecosystem by depleting oxygen concentrations and blocking sunlight from reaching other marine organisms.
Marine Ecosystems
Marine ecosystems are complex networks that include living organisms like plants, animals, and bacteria, as well as the physical environment. From the tiniest plankton to the largest whale, every member plays a role in maintaining this balance. However, events like harmful algal blooms can disrupt these systems.
These disruptions occur when nutrient loading encourages excessive algal growth, which affects the entire food web. Fish and invertebrates suffer, and algae decomposition can consume oxygens necessary for marine life survival. Efforts to understand and mitigate the effects of red tides are crucial to preserving these delicate ecosystems.
Nutrient Loading
Nutrient loading refers to the input of nutrients, primarily nitrogen and phosphorus, into marine ecosystems. These nutrients often come from agricultural runoff, wastewater, and industrial processes.
While nutrients are essential for the growth of marine plants and algae, excessive amounts can lead to harmful phenomena such as algal blooms. These blooms drain the system of oxygen and can produce toxins affecting marine species and humans alike. Strategies to reduce nutrient loading include improved agricultural practices and enhanced wastewater treatment facilities. Addressing nutrient loading is vital to maintain a thriving and balanced marine ecosystem, minimizing the risks of harmful algal blooms.

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Most popular questions from this chapter

Even though the concentration of inorganic phosphate in the water of the North Atlantic Ocean is only about 50% of that found in the other oceans, the North Atlantic is more productive than most of the other oceans. How can one reconcile these observations if nutrients limit primary productivity in the oceans?

In the Great Plains grasslands of the United States, Epstein et al. (1997) showed that primary production of C3 grasses could be predicted from mean annual temperature, with minimal contribution from mean annual precipitation. Discuss why precipitation and soil nutrients do not appear to be relevant variables for C3 grass production in this ecosystem.

North American grasslands are similar in structure to South African grasslands but the grass species differ because of their divergent evolutionary history. Both areas have dominant C4 grasses with less abundant C3 forbs and woody plants. But South Africa has greater climatic variability and poorer soils than North America. Would you expect the two areas to show the same relationships between rainfall and net primary production? Knapp et al. (2006) present an analysis of these questions.

Tilman et al. (1982,p.367) state: We suggest that the spatial and temporal heterogeneity of pelagic environments will prevent us from meaningfully addressing questions on short time scales or small spatial scales. Discuss the general issue of whether there are some questions in community ecology that we cannot answer because of scale.

Photosynthetic organisms produce about 300× 1015g of oxygen per year (Holland 1995 ). If this oxygen accumulated, the oxygen content of the atmosphere would double every 2000 years. Why does this not happen? Is the global system regulated? If so, how is this regulation accomplished?

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