Paleobiologists studying hydrothermal vent communities have long debated when tubeworms established their obligate endosymbiosis with sulfur-oxidizing bacteria. Traditionally, scholars posited that this relationship formed during the late Cretaceous period, relying on fossilized seafloor mineral tubes that exhibit microscopic structural striations characteristic of modern tubeworm tissue. However, recent genomic sequencing reveals that the bacterial metabolic pathways for sulfur oxidation diverged much earlier, during the early Jurassic. To reconcile this, researchers argue that the Cretaceous mineral tubes represent a later evolutionary adaptation to mineralized fluid chimneys, and conclude that deep-sea vent ecosystems were colonized by symbiotic tubeworms during the early Jurassic.
Which of the following, if true, would most seriously weaken the researchers' argument regarding the timing of deep-sea vent colonization?
- AModern hydrothermal vents host fluid flows with significantly higher sulfide concentrations than those estimated to have existed during the early Jurassic.
- BRecent oceanic surveys have discovered several previously uncharacterized species of non-symbiotic tubeworms inhabiting shallow volcanic reefs.
- The genomic divergence of sulfur-oxidizing metabolic pathways occurred in free-living ancestral bacteria inhabiting shallow coastal waters long before those bacteria entered into symbiotic relationships with deep-sea tubeworms.Answer
- DFossilized Cretaceous seafloor deposits display a higher ratio of heavy sulfur isotopes than early Jurassic marine sediment layers.
- EMicroscopic structural striations in fossilized mineral tubes are occasionally obscured by post-depositional mineral crystallization.