During the Paleocene-Eocene Thermal Maximum (PETM), global temperatures rose rapidly, and marine sediment records show a sharp decrease in the ratio of carbon-13 to carbon-12 (represented as , measured in parts per thousand, ). Two scientists discuss the source of this carbon isotope excursion.
Scientist 1
The PETM warming was triggered by the sudden dissociation of marine methane hydrates (solid lattices of ice trapping methane gas) on the seafloor. Methane hydrates contain biogenic methane, which is highly depleted in (having a value of approximately ). Due to this extremely negative signature, releasing approximately (gigatons) of carbon from hydrates is sufficient to cause the observed global decrease in marine .
Scientist 2
The carbon release was caused by volcanic intrusions (sills) from the North Atlantic Igneous Province heating organic-rich sedimentary basins. This heated organic matter released thermogenic methane and carbon dioxide gas. Thermogenic carbon is moderately depleted in , with an average value of approximately . To produce the observed global decrease in marine using this less-depleted carbon source, a much larger release of carbon—approximately —was required.
Suppose a new geochemical reconstruction determines that the total mass of carbon released during the PETM was approximately . How does this finding align with the viewpoints of the two scientists?
- It supports Scientist 1's viewpoint but contradicts Scientist 2's viewpoint.Answer
- BIt supports Scientist 2's viewpoint but contradicts Scientist 1's viewpoint.
- CIt supports both Scientist 1's and Scientist 2's viewpoints.
- DIt contradicts both Scientist 1's and Scientist 2's viewpoints.