Passage:
During the Paleocene-Eocene Thermal Maximum (PETM), approximately 56 million years ago, a massive injection of carbon into the atmosphere caused rapid global warming and widespread ocean acidification. Marine geochemists studying fossilized deep-sea scleractinian corals from this period have observed a pronounced decline in skeleton calcification density. Because scleractinian corals build their calcium carbonate skeletons primarily from aragonite—a soluble mineral form of calcium carbonate—researchers long posited that the reduction in calcification density was a direct physiological response to decreased seawater aragonite saturation states during PETM ocean acidification.
However, recent micro-structural analyses of PETM coral fossils present a nuance that challenges this purely chemical explanation. Biomineralization in scleractinian corals is not a passive chemical precipitation process; rather, corals actively regulate the pH within their internal calcifying fluid, elevating it above ambient seawater levels to promote aragonite deposition. Reexaminations of trace element ratios in PETM coral specimens reveal that these organisms maintained their internal pH elevation mechanisms even at the peak of ocean acidification. Consequently, some paleontologists now argue that the observed decrease in coral skeleton calcification during the PETM was not caused by ambient seawater chemistry rendering skeleton building chemically impossible. Instead, they contend that the decline was primarily driven by thermal stress: elevated water temperatures during the PETM forced corals to divert significant metabolic energy toward cellular repair and heat-shock protein synthesis, leaving insufficient energy to fuel the total skeletal mass deposition, even while internal pH elevation was preserved.
Which of the following is an unstated assumption on which the paleontologists' argument regarding the primary cause of the decline in coral calcification depends?
- Corals during the Paleocene-Eocene Thermal Maximum were unable to increase their total metabolic energy intake or production sufficiently to meet both thermal stress repair demands and normal skeletal mass deposition requirements.Answer
- BAmbient seawater temperatures during the Paleocene-Eocene Thermal Maximum exceeded the lethal physiological tolerance threshold for the majority of deep-sea marine invertebrate species.
- CThe energy required to maintain internal calcifying fluid pH elevation increases sharply when ambient seawater aragonite saturation levels decline.
- DFossilized trace element ratios provide an inaccurate measurement of internal calcifying fluid pH in modern scleractinian coral species.
- EScleractinian corals produced higher amounts of heat-shock proteins during the Paleocene-Eocene Thermal Maximum than during any other warming event in Earth's history.