Ecology and the Food Web

The food web

Because autotrophic organisms form the base of the food web, all of the energy available to the ocean ecosystem is derived from phytoplankton, algae, and bacteria. So it is important not to disturb the productivity of the autotrophs. In oceanic food chain, seasonal factors cause fluctuations in the growth rate and size of the phytoplankton crop. Consequently, these factors cause seasonal fluctuations in the growth rates and size of all of the other consumer in the food chain.


Image of the ocean food web

Image of the ocean food web. Plant, animal, and bacterial populations are dependent on the flow of energy and the recycling of nutrients through the food web. The sun fuels the primary production in the surface layers. Herbivores graze the phytoplankton and benthic algae and are in turn consumed by the carnivores. Animals living at lower depths depend on detrital and other organic matter from above. Upwelling recycles nutrients to the surface, where they are used in photosynthesis
Image permitted and copyrighted, "An Introduction to the World's Oceans", Duxbury, 1997, Wm. C. Brown Publishers


Click HERE to view a second food web diagram.

Ecology

Ecosystems function to convert energy from one form to another, such as converting the radiant energy of sunlight to the chemical energy of sugars and other compounds in phytoplankton or algae. In turn, this chemical energy is consumed by other organisms who themselves are consumed. Ecosystems also function as storage places for various chemical elements. Since all organisms are composed of carbon, nitrogen, oxygen, sulfur, phosphorous and other elements. These chemicals are moved from seawater to an organism, such as phytoplankton, algae, or bacteria, and then from one organism to another as each is consumed in succession. At each step, some compounds are lost through respiration, excretion, feces, or death of the organism. In this form, many elements are returned to their nonliving inorganic form as bacteria decompose the compounds in which they were constituted. Once returned to seawater or sediments, these elements become available to organisms, thus starting the cycle of elements all over again. As a result, elements cycle through ecosystems and continue to cycle through until lost permanently, either by conversion to a permanent form, such as petrified wood or limestone.
The amount of living material produced by net and gross primary production can be expressed as the number of organisms produced, their weight, or grams of carbon; this is known as biomass. Biomass is usually reported as the dry weight of organic carbon in grams present under a square meter of sea surface or gC/m2. The rate at which biomass changes, also known as primary productivity, is reported as gC/m2/time.

Phytoplankton Biomass Graph
Phytoplankton biomass, nutrient supply, and surface-water stability responding
to solar energy changes at the middle latitudes in the Northern Hemisphere.

Image permitted and copyrighted, "An Introduction to the World's Oceans", Duxbury, 1997, Wm. C. Brown Publishers


Phytoplankton Biomass Graph

Phytoplankton biomass, nutrient supply, and surface water stability respond to solar energy changes at the middle latitudes in the Northern Hemisphere. Note the interaction between the sunlight, the stability of the surface water, the nutrients in the surface water and the phytoplankton biomass.
Image permitted and copyrighted, "An Introduction to the World's Oceans", Duxbury, 1997, Wm. C. Brown Publishers



Click here to go to the Foundations of Phytoplankton Main Page     Click here to see what are phytoplankton     Click here to go to Ecology and Food Web     Click here to view phytoplankton pictures and satellite images     Click here to go to the Phytoplankton Education Page    Click here to go to page on Special Topics in Oceanography    Click here to go to the El Nino page