地质学
碳酸盐
甲烷
地球化学
甲烷厌氧氧化
沉积岩
冷泉
碳同位素
海底扩张
白垩纪
碳酸盐矿物
古生物学
总有机碳
方解石
环境化学
化学
有机化学
作者
Biao Chang,Junhua Huang,Thomas J. Algeo,Richard D. Pancost,Xiaoqiao Wan,Yunsong Xue,Jianzhong Jia,Zhou Wang,Jun Hu,Jiasheng Wang,Sheng Wang,Jiaqi Wu,Shucheng Xie
出处
期刊:Geological Society of America Bulletin
[Geological Society of America]
日期:2022-03-14
卷期号:134 (11-12): 2958-2970
被引量:1
摘要
Abstract Methane-derived carbonates (MDCs) are common along modern and ancient continental margins, and the majority of such formations are 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 m.y. interval (ca. 113–85 Ma) that coincided with the mid-Cretaceous greenhouse event. At least nine limestone nodule-bearing horizons exhibit seep-associated sedimentary structures, including carbonate fabrics (e.g., micritic crusts, crystal fans, and botryoidal textures) and 13C-depleted isotopic compositions (δ13Ccarb < –32.3‰), which are indicative of methane-derived carbon sources. Along with sedimentary evidence, the patterns of TΔ47–δ13Ccarb–δ18Ocarb support precipitation of these MDCs over a large temperature range. The REE + Y compositions and europium (Eu) anomalies indicate that the release of methane was associated with hydrothermal fluids. Methane may have been derived from both thermogenic and biogenic sources based on the inorganic carbon isotopic signatures of the carbonate. These nodular carbonate horizons document multiple episodes of seafloor methane release during the mid-Cretaceous and represent exceptionally long-lived, active methane seepage. Massive methane release events may have played a role in generating the greenhouse climate of the mid-Cretaceous.
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