Measuring primary productivity using 14c electricity and magnetism study guide

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The theory behind using 14C to measure productivity involves using a labeled tracer to quantify assimilated carbon. The 14C method estimates the uptake and assimilation of dissolved inorganic carbon (DIC) by planktonic algae in the water column. The method is based on the assumption that biological uptake of 14C-labelled DIC is proportional to the biological uptake of the more commonly found 12C DIC. In order to determine uptake, one must know the concentration of DIC naturally occurring in the sample water, the amount of 14C-DIC added, and the amount of 14C retained in particulate matter ( 14C-POC) at the end of the incubation experiment. A 5% metabolic discrimination factor may be applied to the data as well, since organisms preferentially take up lighter isotopes. Carbon uptake can be measured by the following equation:

Aquatic primary productivity generally governs the biological activity of a lake. Since primary productivity makes up the bottom-most trophic level, it provides essential nutrients and energy to higher trophic levels and higher organisms. For instance, primary productivity in a lake may supply oxygen to aerobic organisms such as insects and fish, and so times of stressed productivity may result in a decline in the fish population. Low primary productivity may thus hinder other lake biota by limiting available nutrients. Conversely, extremely high primary productivity may result in algal blooms, which may eventually lead to mass kills at other trophic levels due to nutrient depletion or by high turbidity from massive concentrations of plankton. So, relatively high rates of primary productivity may support the most diverse and largest amount of biomass, but productivity can also become too high for a system to handle. How To- Sample Collection, Protocol, Analysis, and Considerations

There are several protocols for measuring rates of primary productivity via 14C. The basic idea remains the same: before dawn, water samples are collected in a series of bottles- generally two clear and one amber/dark colored bottle through which light is not able to penetrate. The water samples are inoculated with 14C, capped, and placed in the environment they were collected from for a day (this time may vary). Following the incubation, the samples are collected under low light conditions and filtered through a 0.2um filter. The filter is placed into a liquid scintillation vial, acidified to purge excess 14C, and kept cold until it can be analyzed in a scintillation counter.

Rates of primary productivity can range from 0-9000 kcal/m 2/yr, with desert regions having lower rates and estuaries having higher rates (see The Flow of Energy: Primary Production to Higher Trophic Levels for more details). More constrained rates of primary productivity for specific environments may be researched by looking at primary literature for a specific site. Literature

The theory behind using 14C to measure productivity involves using a labeled tracer to quantify assimilated carbon. The 14C method estimates the uptake and assimilation of dissolved inorganic carbon (DIC) by planktonic algae in the water column. The method is based on the assumption that biological uptake of 14C-labelled DIC is proportional to the biological uptake of the more commonly found 12C DIC. In order to determine uptake, one must know the concentration of DIC naturally occurring in the sample water, the amount of 14C-DIC added, and the amount of 14C retained in particulate matter ( 14C-POC) at the end of the incubation experiment. A 5% metabolic discrimination factor may be applied to the data as well, since organisms preferentially take up lighter isotopes. Carbon uptake can be measured by the following equation:

Aquatic primary productivity generally governs the biological activity of a lake. Since primary productivity makes up the bottom-most trophic level, it provides essential nutrients and energy to higher trophic levels and higher organisms. For instance, primary productivity in a lake may supply oxygen to aerobic organisms such as insects and fish, and so times of stressed productivity may result in a decline in the fish population. Low primary productivity may thus hinder other lake biota by limiting available nutrients. Conversely, extremely high primary productivity may result in algal blooms, which may eventually lead to mass kills at other trophic levels due to nutrient depletion or by high turbidity from massive concentrations of plankton. So, relatively high rates of primary productivity may support the most diverse and largest amount of biomass, but productivity can also become too high for a system to handle. How To- Sample Collection, Protocol, Analysis, and Considerations

There are several protocols for measuring rates of primary productivity via 14C. The basic idea remains the same: before dawn, water samples are collected in a series of bottles- generally two clear and one amber/dark colored bottle through which light is not able to penetrate. The water samples are inoculated with 14C, capped, and placed in the environment they were collected from for a day (this time may vary). Following the incubation, the samples are collected under low light conditions and filtered through a 0.2um filter. The filter is placed into a liquid scintillation vial, acidified to purge excess 14C, and kept cold until it can be analyzed in a scintillation counter.

Rates of primary productivity can range from 0-9000 kcal/m 2/yr, with desert regions having lower rates and estuaries having higher rates (see The Flow of Energy: Primary Production to Higher Trophic Levels for more details). More constrained rates of primary productivity for specific environments may be researched by looking at primary literature for a specific site. Literature