Biao Chang / State Key Laboratory of Geological Processes and Mineral Resources; China; Wuhan 430074; China University of Geosciences; School of Earth Science
树成 谢 / 中国地质大学(武汉)
Methane-derived carbonates (MDCs)are commonalong modern and ancient continental margins, and the majority of such formationsare associated with seafloor cold seeps.Here, we document petrographic,rare earth element + yttrium (REE+Y), carbonate clumped isotope temperature (TΔ47) and carbon-isotopic evidence from a shale succession in southern Tibet spanning a ~28-Myrinterval (~113-85 Ma) that coincided with the mid-Cretaceous greenhouse. At least nine limestone nodule-bearing horizonsexhibitseep-associated sedimentary structures,including carbonate fabrics (e.g., micritic crusts, crystal fans, and botryoidal textures) and 13C-depleted isotopic compositions (d13Ccarb <‒32.3‰)indicative of methane-derived carbon sources. Along with sedimentary evidence, the patterns of TΔ47-d13Ccarb-d18Ocarb support precipitation of these MDCsover a large temperature range. The REE+Y compositionsand europium (Eu) anomalies indicate that the release of methane was associated with hydrothermal fluids. Methane may have beenderived from both thermogenic and biogenic sources based on the inorganic carbon isotopic signatures of the carbonate. These nodular carbonate horizonsdocument multipleepisodes of seafloor methane releaseduring the mid-Cretaceous, representing exceptionally long-lived active methane seepage. Massive methane release events may have played a role in generating the greenhouse climate of the mid-Cretaceous.
National Natural Science Foundation of China Geobiology Society National Committee of Stratigraphy of China Ministry of Science and Technology Geological Society of China Paleontological Society of China Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS) Institute of Vertebrate Paleontology and Paleoanthropology, CAS International Commission on Stratigraphy International Paleontological Association
承办单位
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG, Wuhan)