科研之友
微信
新浪微博
Facebook
分享链接
摘要
Multiple sulfur isotope signatures and secondary ion mass spectroscopy (SIMS) sulfur isotope compositions of pyrite from two seafloor sites (DH-CL11 and HD109) in seepage areas of the South China Sea were measured in order to study isotope effects of sulfate-driven anaerobic oxidation of methane (SO4-AOM). The multiple sulfur isotopes of pyrite reveal variable ranges for both sites (delta S-34: between -44.1% and -2.9% for DH-CL11 and between -43.8% and -1.6% for HD109; D 33 S: between 0.02% and 0.17% for DH-CL11 and between -0.03% and 0.14% for HD109). SIMS analysis reveals an extreme variability of delta S-34 values (between -50.3% and -2.7% in DH-CL11; between -50.1 and 52.4% in HD109) for three types of pyrite: (1) framboids, (2) zoned aggregates with radial overgrowth surrounding a framboidal core, and (3) euhedral pyrite crystals. The synchronous changes of geochemical proxies (sulfate and methane concentrations, delta S-34(sulfate) and delta O-34(sulfate), delta S-34(pyrite), and pyrite content) at the sulfate-methane transition zone (SMTZ) at site DH-CL11 are interpreted to be induced by SO4- AOM under steady state conditions. In contrast, pyrite content and delta S-34 value fluctuations throughout core HD109 suggest that the sediment at this site was affected by multiple pyritization events during diagenesis. Multiple sulfur isotope signatures of early diagenetic pyrite (i. e., with low and high delta S-34 values, the latter above 315 cmbsf in DH-CL11; above 70 cmbsf in HD109) in the upper sediment column suggest that organoclastic sulfate reduction (OSR) and sulfur disproportionation generated the observed isotopic signatures. In contrast to the early diagenetic S-34 depleted framboids, the higher SIMS delta S-34 values of overgrowth and euhedral crystals suggest a late diagenetic S-34 enriched pool of dissolved sulfide derived from SO4-AOM at the current and paleo-SMTZs. Interestingly, pyrite resulting from SO4-AOM in the SMTZ at site DH-CL11 reveals a distinct pattern with higher D 33 S values, different from pyrite resulting from OSR and sulfur disproportionation. Therefore, paired delta S-34 and D 33 S values may allow to differentiate OSR and SO4-AOM, although a full understand-ing of the isotope effects associated with SO4-AOM is hampered by uncertainties on the actual electron transfer mechanism in the syntrophic SO4-AOM consortium.
