A team of marine biologists is investigating the source of organic carbon that supports the food web in the Mariana Trench, located at a depth of over 10,000 meters. The scientists propose three different hypotheses to explain where the organic carbon originates.
* Hypothesis 1: The organic carbon in the trench is derived from dead photosynthetic plankton sinking from the sunlit surface waters.
* Hypothesis 2: The organic carbon is produced locally in the trench by chemosynthetic bacteria that utilize geothermal chemical energy from deep-sea hydrothermal vents.
* Hypothesis 3: The organic carbon consists of terrestrial plant debris transported from land down the slopes of submarine canyons during storm events.
Match each hypothesis with the experimental observation that would most directly invalidate (disprove) it.
- Hypothesis 1Sediment samples show that the organic matter contains no chlorophyll degradation products (such as pheophytin).
- Hypothesis 2The rate of local organic carbon production remains constant after a tectonic event seals all deep-sea hydrothermal vents in the trench.
- Hypothesis 3Chemical analysis shows a complete absence of vascular plant polymers (such as lignin) in the trench sediment.