1. 2. 3. Marine fish cells are hypotonic compared to their seawater environment; their cells lose water by osmosis and gain solutes. If you add heterotrophic respiration and autotrophic respiration together and then subtract that value from gross primary productivity, then you have a more refined estimate of ecosystem carbon storage than NEE. Differential heating due to the earth's tilt generates the global wind AND oceanic circulation patterns
1. 2. 3. Marine fish cells are hypotonic compared to their seawater environment; their cells lose water by osmosis and gain solutes. If you add heterotrophic respiration and autotrophic respiration together and then subtract that value from gross primary productivity, then you have a more refined estimate of ecosystem carbon storage than NEE. Differential heating due to the earth's tilt generates the global wind AND oceanic circulation patterns
Biology: The Unity and Diversity of Life (MindTap Course List)
14th Edition
ISBN:9781305073951
Author:Cecie Starr, Ralph Taggart, Christine Evers, Lisa Starr
Publisher:Cecie Starr, Ralph Taggart, Christine Evers, Lisa Starr
Chapter46: Ecosystems
Section: Chapter Questions
Problem 5SQ: Efficiency of energy transfers in aquatic ecosystem is typically higher than in land ecosystems...
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
Transcribed Image Text:1.
2.
3.
Marine fish cells are hypotonic compared to their seawater environment; their cells
lose water by osmosis and gain solutes.
If you add heterotrophic respiration and autotrophic respiration together and then
subtract that value from gross primary productivity, then you have a more refined estimate
of ecosystem carbon storage than NEE.
Differential heating due to the earth's tilt generates the global wind AND oceanic
circulation patterns
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