Tracing energy inputs into the seafloor using carbonate sediments.

ABSTRACT: Carbonate rocks provide unique and valuable sedimentary archives for secular changes in Earth's physical, chemical, and biological processes. However, reading the stratigraphic record produces overlapping, nonunique interpretations that stem from the difficulty in directly comparing competing biological, physical, or chemical mechanisms within a common quantitative framework. We built a mathematical model that decomposes these processes and casts the marine carbonate record in terms of energy fluxes across the sediment-water interface. Results showed that physical, chemical, and biological energy terms across the seafloor are subequal and that the energetic dominance of different processes varies both as a function of environment (e.g., onshore vs. offshore) as well as with time-varying ch

SUBMITTER: Smith BP 

PROVIDER: S-EPMC9992785 | biostudies-literature | 2023 Feb

REPOSITORIES: biostudies-literature